[SECTION 11. SOILS 11-1](#soils)

[11.A Soil Survey Map and Report 11-1](#soil-survey-map-and-report)

[11.B Limitations Report 11-3](#limitations-report)

[11.B.1 Soil Hazards 11-3](#soil-hazards)

[11.B.2 Soil Erosion 11-4](#soil-erosion)

[11.B.3 Shallow Depth to Bedrock 11-7](#shallow-depth-to-bedrock)

[11.C Hydric Soils 11-9](#hydric-soils)

[11.D Wetland Investigation Report 11-14](#wetland-investigation-report)

[11.D.1 Introduction 11-14](#introduction)

[11.D.2 Methods 11-15](#methods)

[11.D.3 Results of Field Investigations
11-16](#results-of-field-investigations)

[11.D.4 Forested Wetlands 11-17](#forested-wetlands)

[11.D.5 Scrub-Shrub Wetlands 11-18](#scrub-shrub-wetlands)

[11.D.6 Emergent Wetlands 11-20](#emergent-wetlands)

[11.D.7 Unconsolidated Bottom Wetlands
11-21](#unconsolidated-bottom-wetlands)

[11.D.8 Functions and Values 11-21](#functions-and-values)

[11.D.9 Freshwater Wetlands of Special Significance
11-25](#freshwater-wetlands-of-special-significance)

[11.D.10 Wetland Impacts and Impact Avoidance and Minimization
11-27](#wetland-impacts-and-impact-avoidance-and-minimization)

[11.D.11 Compensation 11-29](#compensation)

[11.D.12 References for Wetlands Investigation Report
11-29](#references-for-wetlands-investigation-report)

TABLES

[Table 11-1. Summary of Soils with Elevated Erosion Hazard Potential
along Route^1^ 11-5](#__RefHeading___Toc102263176)

[Table 11-2. Summary of Shallow Soils along Route
11-7](#__RefHeading___Toc102263177)

[Table 11-3. Summary of Hydric Soils along Route
11-9](#__RefHeading___Toc102263178)

[Table 11-4. Summary of Wetlands Designated as FWSS Along Route
11-26](#__RefHeading___Toc102263179)

**APPENDICES**

APPENDIX 11-1: SOIL AND GEOTECHNICAL SURVEYS

APPENDIX 11-2: SOIL SURVEY MAPS

APPENDIX 11-3: SUMMARY OF SOIL CHARACTERISTICS

APPENDIX 11-4: CUMULATIVE SUMMARY OF SOILS ALONG ROUTE

APPENDIX 11-5: REPRESENTATIVE WETLAND FIELD DATA FORMS AND PHOTOGRAPHIC
DOCUMENTATION

APPENDIX 11-6: WETLAND SUMMARY TABLE

#  SOILS

## Soil Survey Map and Report

This section summarizes the soils which are traversed by the proposed
Northeast Reliability Interconnect (NRI) right-of-way (ROW). This
summary is based on existing United States Department of Agriculture
(USDA) and Natural Resources Conservation Service (NRCS) soil survey
data. The characteristics of soils expected to be encountered and the
associated soil limitations along the proposed route are described
herein based on available USDA and NRCS soil survey data for those
counties crossed by the proposed route. No field surveys were performed
along the ROW for the purpose of this discussion. In addition to
anticipated conditions (which are extrapolated from the soil survey
data), real conditions will be continually assessed during construction
activities, and any areas of concern (erosion hazards, unstable soils,
etc.) will be appropriately addressed as encountered in the field. The
applicable USDA soil survey maps and soils series descriptions are
included in the Class D Medium Intensity Soil Survey provided in
Appendix 11-1. The proposed route for the NRI has been superimposed on
the maps.

It should be noted that BHE also completed a Class C Medium High
Intensity soil survey and a preliminary geotechnical study for the
Orrington Substation expansion area. Based on the Class C soil survey,
soils underlying the existing structure consist solely of Udorthents
(fill), and soils in the area of the proposed expansion have been
identified as Elmwood-Swanton complex. The Class C soil survey was used
primarily for developing the storm water management plan for the
substation expansion area. The geotechnical study was completed for
project engineering purposes. The Class C soil survey and geotechnical
study are provided as separate reports in Appendix 11-1.

The proposed NRI ROW passes through portions of Penobscot, Hancock, and
Washington counties in Maine, totaling 84.25-miles in length. The route
begins at the existing substation in Orrington and runs roughly
northeasterly to the Canadian border in Baileyville.

The first approximately 22 miles lies within Penobscot County, where
USDA/NRCS soil survey data are available. The route then leaves
Penobscot County near milepost 22 and traverses through portions of
Hancock County and Washington County that have no available soil survey
data. Near milepost 74, the route enters into a portion of Washington
County where soil survey data is again available and runs roughly
northeasterly for another approximately 10 miles into Baileyville to the
Canadian border. Soil survey maps depicting the proposed route through
these areas are provided in Appendix 11-2. Soil survey data is not
available for approximately 52 of the 84-mile route. A more detailed
description of the proposed route for the transmission line ROW is
provided in Section 1, Development Description.

The available USDA and NRCS soil survey data indicate that the route
traverses 36 different soil series, associations or complexes
(representing a total of 31 different soil series, with some found in
various complexes and associations). These are further subdivided into
54 different map units based on features such as stone content and
slope.

Appendix 11-3 of this report lists, in tabular format, each soil map
unit as it is encountered along the proposed route, as well as a
summarized description of each soil. The first column of the table lists
the *Map Unit Symbol* (i.e., TvD, or 340B) representing the soil series
crossed as depicted on the soil survey maps. The second, third, and
fourth columns indicate mileage interval and distance along the route
over which each soil unit is traversed. The *Map Unit Name* column lists
the soil series. All of the data in Appendix 11-3 are taken from the
USDA and NRCS survey information.

The *Range of Slope* column lists a range of slopes (i.e., 0-15 percent)
relative to each soil map unit. The slope ranges listed herein are based
solely on map unit designations and descriptions, and may vary in the
field. Steep slopes may pose limitations relative to equipment access.
Some areas with steep slopes may be subject to increased erosion hazard
when disturbed. Some areas may require extra attention to erosion and
sedimentation control during construction and restoration.

The *Drainage* column describes the drainage classification for the soil
map unit. Soil drainage classes vary from very poorly drained to
excessively drained. Drainage classes are associated with inherent
parent material characteristics, soil texture, and topographical
setting.

The *Soil Type* column provides a general description of the parent
material in which each soil map unit is formed. The *Depth to Bedrock*
column indicates whether the bedrock surface is generally greater than
or less than 60 inches below the ground surface. The column *Water Table
Depth* indicates the typical depth to groundwater during the wet season.
The typical depth to seasonal high water table is directly related to
the assigned drainage classification.

The next two columns list the range of *K* *factor*, which is an
indication of the soil's surface susceptibility to sheet or rill
erosion, and the *Erosion Hazard Potential (EHP)*. The K factor may
range from 0.0 (non-erodible) to 1.0 (extremely erodible). A soil with a
high K factor will be more susceptible to erosion and sediment control
problems during the transmission line construction than a soil with a
low K factor. The EHP indicates the woodland management erosion hazard
potential based on the soil interpretation records.

The final column, *Hydric Soil*, identifies whether the soil type is
considered to be a hydric soil. This information was derived from the
NRCS Hydric Soils of Maine list. The list was created by using criteria
that were developed by the [National Technical Committee for Hydric
Soils](http://soils.usda.gov/use/hydric/ntchs/index.html) and are
discussed further in Section 11.C Hydric Soils.

## Limitations Report

### Soil Hazards

The main soil hazards that must be considered relative to the proposed
installation are hydric soils (Section 11.C), erosion hazard potential,
and shallow depth to bedrock. Soils with elevated erosion hazard
potential may require control techniques beyond those typically employed
during construction operations. Soils with shallow depth to bedrock may
require hammering, drilling and/or blasting to accomplish pole
installation. It should be noted that the size of the required
excavations for pole installation are usually only a few feet in width
and depth. In most cases, erosion and shallow bedrock hazards can be
overcome using special, yet common and feasible techniques.

In addition to hazards that have been identified based on published USDA
and NRCS soil survey data, some unexpected impediments may be
encountered in the field: for example, surface stoniness, boulders,
ledge outcroppings, and dense gravel may impact the placement of utility
structures. Such impediments will be appropriately addressed if and when
they are encountered.

### Soil Erosion

Erosion potential is listed as slight for the majority of the route that
has available soil survey data; however, erosion and sedimentation
control measures will be utilized wherever necessary to reduce the
impact of any erosion during construction activities. BHE has developed
an NRI Project Erosion and Sedimentation Control Plan (NRI E&S Plan or
Plan) based on the best management practices (BMPs) contained in the
Maine Department of Environmental Protection's (DEP) *Maine Erosion and
Sediment Control BMPs*, dated March 2003. The NRI E&S Plan is provided
in Appendix 14-1 of this application.

A total of 14.3 percent of the total linear distance of mapped soils
identified along the proposed route are comprised of map units with
"slight to moderate" and higher erosion hazard ratings. Table 11-1 lists
the map units that are associated with elevated erosion hazard, their
locations along the route, and their erosion hazard ratings.

  -------------------------------------------------------------------------------------------------------------------------------------------
  []{#__RefHeading___Toc102263176                                                                                              
  .anchor}Table 11-1. Summary of                                                                                               
  Soils with Elevated Erosion                                                                                                  
  Hazard Potential along Route^1^                                                                                              
  --------------------------------- -------------------------------- ----------- -------------- -------------- --------------- --------------
  **Map Unit Symbol**               **Map Unit Name**                **Erosion   **From         **To           **Map Unit      ***Percent of
                                                                     Hazard**    (milepost)**   (milepost)**   Traverse        Total Measured
                                                                                                               Distance        Distance***
                                                                                                               (feet)**        

  ** **                             ** **                            ** **       ** **          ** **          ***Total        
                                                                                                               Distance        
                                                                                                               (feet)***       

  **Lk**                            Limerick (Charles)               Moderate to 12.03          12.06          200             *** ***
                                                                     severe                                                    

  ** **                                                                                                        ***200***       ***0.12%***

  **PgC**                           Plaisted                         Slight to   5.25           5.31           304             *** ***
                                                                     moderate                                                  

  ** **                                                                                                        ***304***       ***0.18%***

  **PrE**                           Plaisted                         Moderate to 5.99           6.05           280             *** ***
                                                                     severe                                                    

  ** **                                                                          7.27           7.39           606             *** ***

  ** **                                                                                                        ***885***       ***0.52%***

  **RmC**                           Rockland & Thorndike             Slight to   11.86          11.95          513             *** ***
                                                                     moderate                                                  

  ** **                                                                          12.06          12.10          214             *** ***

  ** **                                                                          19.31          19.36          270             *** ***

  ** **                                                                                                        ***998***       ***0.59%***

  **RmD**                           Rockland & Thorndike             Slight to   11.79          11.86          354             *** ***
                                                                     moderate                                                  

  ** **                                                                          11.95          12.01          321             *** ***

  ** **                                                                          12.10          12.17          352             *** ***

  ** **                                                                                                        ***1027***      ***0.61%***

  **Sa**                            Saco (Medomak)                   Moderate to 9.72           9.77           283             *** ***
                                                                     severe                                                    

  ** **                                                                          9.79           9.80           85              *** ***

  ** **                                                                          15.41          15.47          346             *** ***

  ** **                                                                          20.14          20.18          212             *** ***

  ** **                                                                                                        ***925***       ***0.55%***

  **SfC**                           Stetson & Suffield               Moderate    18.56          18.83          1400            *** ***

  ** **                                                                          19.00          19.14          757             *** ***

  ** **                                                                                                        ***2157***      ***1.28%***

  **SuC2**                          Suffield eroded                  Moderate to 9.80           9.86           312             *** ***
                                                                     severe                                                    

  ** **                                                                                                        ***312***       ***0.18%***

  **SvC**                           Suffield                         Moderate to 5.42           5.50           424             *** ***
                                                                     severe                                                    

  ** **                                                                                                        ***424***       ***0.25%***

  **TkB**                           Thorndike                        Slight to   7.05           7.21           857             *** ***
                                                                     moderate                                                  

  ** **                                                                                                        ***857***       ***0.51%***

  **TvB**                           Thorndike                        Slight to   12.26          12.32          305             *** ***
                                                                     moderate                                                  

  ** **                                                                          15.29          15.38          441             *** ***

  ** **                                                                          21.04          21.12          424             *** ***

  ** **                                                                          21.38          21.45          388             *** ***

  ** **                                                                          21.94          22.01          380             *** ***

  ** **                                                                                                        ***1939***      ***1.15%***

  **TvC**                           Thorndike                        Slight to   19.83          19.86          197             *** ***
                                                                     moderate                                                  

                                                                                                               ***197***       ***0.12%***

  **340B**                          Telos-Elliottsville-Monarda      Slight to   74.39          74.50          562             *** ***
                                    complex                          moderate                                                  

  ** **                                                                          74.57          74.60          159             *** ***

  ** **                                                                          76.46          76.78          1683            *** ***

  ** **                                                                          77.20          77.34          763             *** ***

  ** **                                                                          77.46          77.59          644             *** ***

  ** **                                                                          79.27          79.39          614             *** ***

  ** **                                                                                                        ***4425***      ***2.62%***

  **340C**                          Chesuncook-Elliottsville-Telos   Slight to   74.78          74.99          1093            *** ***
                                    complex                          moderate                                                  

  ** **                                                                          75.04          75.53          2577            *** ***

  ** **                                                                          75.62          75.71          477             *** ***

  ** **                                                                          75.79          76.29          2674            *** ***

  ** **                                                                          77.43          77.46          208             *** ***

  ** **                                                                          77.67          77.76          464             *** ***

  ** **                                                                          77.83          77.91          402             *** ***

  ** **                                                                                                        ***7896***      ***4.68%***

  **344C**                          Danforth-Elliottsville complex   Slight to   81.18          81.47          1539            *** ***
                                                                     moderate                                                  

  ** **                                                                                                        ***1539***      ***0.91%***

  ***Total Measured Distance of                                                                                ***24,084***    ***14.28%***
  Shallow Soils***                                                                                                             

  ***Total Measured Distance***                                                                                ***168,687***   ***14.28%***

  ^1^ Includes only those soils                                                                                                
  with \"slight to moderate\" and                                                                                              
  greater erosion hazard ratings.                                                                                              
  -------------------------------------------------------------------------------------------------------------------------------------------

### Shallow Depth to Bedrock

The majority of the mapped portion of the proposed route crosses soils
that are listed as "very deep;" i.e., they have greater than 60 inches
of soil over bedrock. Of the total linear distance of mapped soils along
the route, 11.7 percent are comprised of map units listed as having
shallow depths to bedrock. Table 11-2 lists these map units, their
locations along the proposed route, and their depth to bedrock
estimates.

  ----------------------------------------------------------------------------------------------------------------------------------
  []{#__RefHeading___Toc102263177                                                                                     
  .anchor}Table 11-2. Summary of                                                                                      
  Shallow Soils along Route                                                                                           
  --------------------------------- -------------------------------- ------------ --------- --------- --------------- --------------
  **Map Unit Symbol**               **Map Unit Name**                **Depth to   **From    **To      **Map Unit      ***Percent of
                                                                     Bedrock      (mile     (mile     Traverse        Total Measured
                                                                     (inches)**   post)**   post)**   Distance        Distance***
                                                                                                      (feet)**        

  ** **                             ** **                            ** **        ** **     ** **     ***Total        
                                                                                                      Distance        
                                                                                                      (feet)***       

  **RmC**                           Rockland & Thorndike             0-12         11.86     11.95     513             *** ***

  ** **                                                                           12.06     12.10     214             *** ***

  ** **                                                                           19.31     19.36     270             *** ***

  ** **                                                                                               ***998***       ***0.59%***

  **RmD**                           Rockland & Thorndike             0-12         11.79     11.86     354             *** ***

  ** **                                                                           11.95     12.01     321             *** ***

  ** **                                                                           12.10     12.17     352             *** ***

  ** **                                                                                               ***1027***      ***0.61%***

  **TkB**                           Thorndike                        0-20         7.05      7.21      857             *** ***

  ** **                                                                                               ***857***       ***0.51%***

  **TvB**                           Thorndike                        10-20        12.26     12.32     305             *** ***

  ** **                                                                           15.29     15.38     441             *** ***

  ** **                                                                           21.04     21.12     424             *** ***

  ** **                                                                           21.38     21.45     388             *** ***

  ** **                                                                           21.94     22.01     380             *** ***

  ** **                                                                                               ***1939***      ***1.15%***

  **TvC**                           Thorndike                        10-20        19.83     19.86     197             *** ***

                                                                                                      ***197***       ***0.12%***

  **340B**                          Telos-Elliottsville-Monarda      20-40        74.39     74.50     562             *** ***
                                    complex                                                                           

  ** **                                                                           74.57     74.60     159             *** ***

  ** **                                                                           76.46     76.78     1683            *** ***

  ** **                                                                           77.20     77.34     763             *** ***

  ** **                                                                           77.46     77.59     644             *** ***

  ** **                                                                           79.27     79.39     614             *** ***

  ** **                                                                                               ***4425***      ***2.62%***

  **340C**                          Chesuncook-Elliottsville-Telos   20-40        74.78     74.99     1093            *** ***
                                    complex                                                                           

  ** **                                                                           75.04     75.53     2577            *** ***

  ** **                                                                           75.62     75.71     477             *** ***

  ** **                                                                           75.79     76.29     2674            *** ***

  ** **                                                                           77.43     77.46     208             *** ***

  ** **                                                                           77.67     77.76     464             *** ***

  ** **                                                                           77.83     77.91     402             *** ***

  ** **                                                                                               ***7896***      ***4.68%***

  **341C**                          Elliotsville-Monson              10-40        75.53     75.62     476             *** ***

  ** **                                                                           75.71     75.79     400             *** ***

  ** **                                                                                               ***876***       ***0.52%***

  **344C**                          Danforth-Elliottsville complex   20-40        81.18     81.47     1539            *** ***

  ** **                                                                                               ***1539***      ***0.91%***

  ***Total Measured Distance of                                                                       ***19,753***    ***11.71%***
  Shallow Soils***                                                                                                    

  ***Total Measured Distance***                                                                       ***168,687***   ***11.71%***
  ----------------------------------------------------------------------------------------------------------------------------------

## Hydric Soils

Hydric soil is defined as a soil that has formed under conditions of
saturation, flooding or ponding long enough during the growing season to
develop anaerobic conditions in the upper part. These soils can pose
limitations due to seasonal or year-round wetness. Some hydric soils can
be compacted if exposed to heavy equipment when wet. Those soils that
are associated with wetlands are under state and/or federal
jurisdiction. Often, the limitations associated with hydric soils can be
circumvented by conducting operations during dry or frozen seasons, or
by using BMPs. Applicable BMPs are incorporated in the NRI E&S Plan
(Appendix 14-1). These practices will be adhered to whenever necessary
during construction of the proposed line.

Of the total linear distance of mapped soils along the proposed route,
55.4 percent is comprised of map units that are listed as hydric. Table
11-3, below, lists these map units and the locations where they occur
along the route.

+----------+---------+-----+--------+--------+--------+-------------+
| []{#__R  |         |     |        |        |        |             |
| efHeadin |         |     |        |        |        |             |
| g___Toc1 |         |     |        |        |        |             |
| 02263178 |         |     |        |        |        |             |
| .anch    |         |     |        |        |        |             |
| or}Table |         |     |        |        |        |             |
| 11-3.    |         |     |        |        |        |             |
| Summary  |         |     |        |        |        |             |
| of       |         |     |        |        |        |             |
| Hydric   |         |     |        |        |        |             |
| Soils    |         |     |        |        |        |             |
| along    |         |     |        |        |        |             |
| Route    |         |     |        |        |        |             |
+==========+=========+=====+========+========+========+=============+
| **Map    | **Map   | **  | **From | **To   | **Map  | ***Percent  |
| Unit     | Unit    | Hyd | (mile  | (mile  | Unit   | of Total    |
| Symbol** | Name**  | ric | p      | p      | Tr     | Measured    |
|          |         | Soi | ost)** | ost)** | averse | Distance*** |
|          |         | l** |        |        | Di     |             |
|          |         |     |        |        | stance |             |
|          |         | *   |        |        | (f     |             |
|          |         | *(Y |        |        | eet)** |             |
|          |         | or  |        |        |        |             |
|          |         | N   |        |        |        |             |
|          |         | )** |        |        |        |             |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    | ** **   | **  | ** **  | ** **  | **     |             |
|          |         |  ** |        |        | *Total |             |
|          |         |     |        |        | Di     |             |
|          |         |     |        |        | stance |             |
|          |         |     |        |        | (fe    |             |
|          |         |     |        |        | et)*** |             |
+----------+---------+-----+--------+--------+--------+-------------+
| **BoA**  | Bi      | Y   | 0.95   | 1.59   | 3417   | *** ***     |
|          | ddeford |     |        |        |        |             |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 2.73   | 2.84   | 578    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 2.96   | 3.07   | 584    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 3.39   | 3.50   | 618    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 4.54   | 4.62   | 383    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 5.58   | 5.66   | 422    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 5.73   | 5.79   | 286    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 8.20   | 8.41   | 1127   | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 8.52   | 8.67   | 797    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 9.06   | 9.19   | 701    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 9.30   | 9.44   | 786    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 10.10  | 10.15  | 269    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 10.31  | 10.59  | 1446   | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 10.69  | 10.81  | 616    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
|          |         |     | 11.06  | 11.08  | 101    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| *        |         |     | 11.32  | 11.47  | 788    | *** ***     |
| * **(BoA |         |     |        |        |        |             |
| Contin   |         |     |        |        |        |             |
| ued...)  |         |     |        |        |        |             |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 11.63  | 11.73  | 532    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 13.17  | 13.34  | 906    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 17.44  | 17.53  | 467    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 17.63  | 17.68  | 293    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 21.58  | 21.90  | 1695   | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     |        |        | ***16, | ***9.97%*** |
|          |         |     |        |        | 810*** |             |
+----------+---------+-----+--------+--------+--------+-------------+
| **BxB**  | Buxton, | Y   | 3.72   | 3.78   | 295    | *** ***     |
|          | S       |     |        |        |        |             |
|          | cantic, |     |        |        |        |             |
|          | &       |     |        |        |        |             |
|          | Bi      |     |        |        |        |             |
|          | ddeford |     |        |        |        |             |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 4.12   | 4.15   | 180    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 4.30   | 4.32   | 89     | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 5.10   | 5.14   | 212    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 5.39   | 5.42   | 144    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 5.84   | 5.97   | 678    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 6.05   | 6.25   | 1085   | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 6.40   | 6.50   | 530    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 7.02   | 7.05   | 143    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 7.87   | 8.20   | 1733   | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 8.41   | 8.46   | 259    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 8.67   | 9.06   | 2059   | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 10.59  | 10.69  | 566    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 10.81  | 11.01  | 1060   | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 11.08  | 11.17  | 496    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 11.73  | 11.75  | 65     | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 13.76  | 13.97  | 1110   | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 14.11  | 14.19  | 426    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 14.90  | 15.03  | 637    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 15.47  | 15.87  | 2095   | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 16.91  | 16.98  | 414    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 19.38  | 19.47  | 466    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 19.62  | 19.69  | 332    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 20.09  | 20.14  | 232    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 20.18  | 20.32  | 769    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 20.35  | 20.67  | 1691   | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 21.90  | 21.94  | 223    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 22.01  | 22.04  | 141    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     |        |        | ***18, | *           |
|          |         |     |        |        | 129*** | **10.75%*** |
+----------+---------+-----+--------+--------+--------+-------------+
| **Lk**   | L       | Y   | 12.03  | 12.06  | 200    | *** ***     |
|          | imerick |     |        |        |        |             |
|          | (C      |     |        |        |        |             |
|          | harles) |     |        |        |        |             |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     |        |        | ***    | ***0.12%*** |
|          |         |     |        |        | 200*** |             |
+----------+---------+-----+--------+--------+--------+-------------+
| **MrB**  | Monarda | Y   | 7.39   | 7.42   | 190    | *** ***     |
|          | &       |     |        |        |        |             |
|          | Burnham |     |        |        |        |             |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 7.64   | 7.87   | 1209   | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 12.39  | 12.49  | 480    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 12.65  | 12.84  | 1040   | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 12.96  | 13.06  | 502    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 13.60  | 13.76  | 874    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 14.19  | 14.48  | 1550   | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 15.96  | 16.13  | 882    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 16.23  | 16.34  | 597    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 17.33  | 17.44  | 586    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 19.47  | 19.58  | 546    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 19.78  | 19.83  | 257    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 19.86  | 19.92  | 273    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 20.67  | 20.83  | 847    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 21.12  | 21.27  | 775    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 21.50  | 21.58  | 434    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     |        |        | ***11, | ***6.55%*** |
|          |         |     |        |        | 041*** |             |
+----------+---------+-----+--------+--------+--------+-------------+
| **MsC**  | Monarda | Y   | 6.90   | 7.02   | 644    | *** ***     |
|          | &       |     |        |        |        |             |
|          | Burnham |     |        |        |        |             |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 11.01  | 11.06  | 239    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 11.75  | 11.79  | 222    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 12.17  | 12.26  | 491    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 12.32  | 12.39  | 382    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 19.36  | 19.38  | 132    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     |        |        | ***2   | ***1.25%*** |
|          |         |     |        |        | 110*** |             |
+----------+---------+-----+--------+--------+--------+-------------+
| **Mu**   | muck    | Y   | 11.47  | 11.63  | 871    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     |        |        | ***    | ***0.52%*** |
|          |         |     |        |        | 871*** |             |
+----------+---------+-----+--------+--------+--------+-------------+
| **Pa**   | Peat &  | Y   | 17.53  | 17.63  | 520    | *** ***     |
|          | Muck    |     |        |        |        |             |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     |        |        | ***    | ***0.31%*** |
|          |         |     |        |        | 520*** |             |
+----------+---------+-----+--------+--------+--------+-------------+
| **RaB**  | Red     | Y   | 16.98  | 17.15  | 868    | *** ***     |
|          | Hook &  |     |        |        |        |             |
|          | A       |     |        |        |        |             |
|          | therton |     |        |        |        |             |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 17.68  | 18.01  | 1727   | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     |        |        | ***2   | ***1.54%*** |
|          |         |     |        |        | 595*** |             |
+----------+---------+-----+--------+--------+--------+-------------+
| **Sa**   | Saco    | Y   | 9.72   | 9.77   | 283    | *** ***     |
|          | (M      |     |        |        |        |             |
|          | edomak) |     |        |        |        |             |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 9.79   | 9.80   | 85     | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 15.41  | 15.47  | 346    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 20.14  | 20.18  | 212    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     |        |        | ***    | ***0.55%*** |
|          |         |     |        |        | 925*** |             |
+----------+---------+-----+--------+--------+--------+-------------+
| **ScB**  | Scantic | Y   | 0.22   | 0.55   | 1730   | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 1.76   | 1.93   | 908    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 2.68   | 2.73   | 274    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 4.96   | 5.10   | 752    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 6.50   | 6.82   | 1699   | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 6.85   | 6.90   | 238    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 9.50   | 9.63   | 702    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 10.15  | 10.31  | 881    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 11.17  | 11.32  | 783    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 12.49  | 12.57  | 461    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 14.48  | 14.68  | 1040   | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 15.16  | 15.29  | 696    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     |        |        | ***10, | ***6.03%*** |
|          |         |     |        |        | 165*** |             |
+----------+---------+-----+--------+--------+--------+-------------+
| **332B** | L       | Y   | 83.44  | 83.53  | 498    | *** ***     |
|          | amoine- |     |        |        |        |             |
|          | Buxton- |     |        |        |        |             |
|          | Scantic |     |        |        |        |             |
|          | complex |     |        |        |        |             |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 83.68  | 83.71  | 108    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 83.73  | 83.87  | 735    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     |        |        | ***1   | ***0.80%*** |
|          |         |     |        |        | 341*** |             |
+----------+---------+-----+--------+--------+--------+-------------+
| **333A** | Sca     | Y   | 83.71  | 83.73  | 140    | *** ***     |
|          | ntic-bi |     |        |        |        |             |
|          | ddeford |     |        |        |        |             |
|          | asso    |     |        |        |        |             |
|          | ciation |     |        |        |        |             |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     |        |        | ***    | ***0.08%*** |
|          |         |     |        |        | 140*** |             |
+----------+---------+-----+--------+--------+--------+-------------+
| **340B** | Telos-  | Y   | 74.39  | 74.50  | 562    | *** ***     |
|          | Elliott |     |        |        |        |             |
|          | sville- |     |        |        |        |             |
|          | Monarda |     |        |        |        |             |
|          | complex |     |        |        |        |             |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 74.57  | 74.60  | 159    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 76.46  | 76.78  | 1683   | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 77.20  | 77.34  | 763    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 77.46  | 77.59  | 644    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 79.27  | 79.39  | 614    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     |        |        | ***4   | ***2.62%*** |
|          |         |     |        |        | 425*** |             |
+----------+---------+-----+--------+--------+--------+-------------+
| **340C** | Ch      | Y   | 74.78  | 74.99  | 1093   | *** ***     |
|          | esuncoo |     |        |        |        |             |
|          | k-Ellio |     |        |        |        |             |
|          | ttsvill |     |        |        |        |             |
|          | e-Telos |     |        |        |        |             |
|          | complex |     |        |        |        |             |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 75.04  | 75.53  | 2577   | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 75.62  | 75.71  | 477    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 75.79  | 76.29  | 2674   | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 77.43  | 77.46  | 208    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 77.67  | 77.76  | 464    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 77.83  | 77.91  | 402    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     |        |        | ***7   | ***4.68%*** |
|          |         |     |        |        | 896*** |             |
+----------+---------+-----+--------+--------+--------+-------------+
| **348B** | Monard  | Y   | 74.50  | 74.57  | 379    | *** ***     |
|          | a-Telos |     |        |        |        |             |
|          | asso    |     |        |        |        |             |
|          | ciation |     |        |        |        |             |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 74.99  | 75.04  | 278    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 76.29  | 76.46  | 879    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 76.78  | 76.87  | 505    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 76.96  | 77.06  | 533    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 77.59  | 77.67  | 443    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 77.76  | 77.83  | 392    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 77.91  | 78.21  | 1606   | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 78.53  | 78.83  | 1594   | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 78.97  | 79.00  | 161    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 79.07  | 79.27  | 1098   | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 79.39  | 79.93  | 2857   | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 80.08  | 80.21  | 703    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 80.31  | 80.41  | 565    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 80.50  | 80.61  | 623    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 80.79  | 80.84  | 300    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 82.20  | 82.23  | 180    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 82.30  | 82.36  | 290    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 82.48  | 82.54  | 326    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 82.91  | 82.95  | 249    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     |        |        | ***13, | ***8.28%*** |
|          |         |     |        |        | 960*** |             |
+----------+---------+-----+--------+--------+--------+-------------+
| **39M**  | Wo      | Y   | 81.99  | 82.20  | 1064   | *** ***     |
|          | nsqueak |     |        |        |        |             |
|          | and     |     |        |        |        |             |
|          | Buc     |     |        |        |        |             |
|          | ksport: |     |        |        |        |             |
|          | fre     |     |        |        |        |             |
|          | quently |     |        |        |        |             |
|          | flooded |     |        |        |        |             |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     | 83.38  | 83.44  | 305    | *** ***     |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     |        |        | ***1   | ***0.81%*** |
|          |         |     |        |        | 369*** |             |
+----------+---------+-----+--------+--------+--------+-------------+
| **39P**  | Bu      | Y   | 80.84  | 81.04  | 1015   | *** ***     |
|          | cksport |     |        |        |        |             |
|          | and     |     |        |        |        |             |
|          | Wo      |     |        |        |        |             |
|          | nsqueak |     |        |        |        |             |
+----------+---------+-----+--------+--------+--------+-------------+
| ** **    |         |     |        |        | ***1   | ***0.60%*** |
|          |         |     |        |        | 015*** |             |
+----------+---------+-----+--------+--------+--------+-------------+
| ***Total |         |     |        |        | ***93, | *           |
| Measured |         |     |        |        | 512*** | **55.44%*** |
| Distance |         |     |        |        |        |             |
| of       |         |     |        |        |        |             |
| Shallow  |         |     |        |        |        |             |
| Soils*** |         |     |        |        |        |             |
+----------+---------+-----+--------+--------+--------+-------------+
| ***Total |         |     |        |        | *      | *           |
| Measured |         |     |        |        | **168, | **55.44%*** |
| Dis      |         |     |        |        | 687*** |             |
| tance*** |         |     |        |        |        |             |
+----------+---------+-----+--------+--------+--------+-------------+

## Wetland Investigation Report

### Introduction

This section presents the results of the field investigation of wetlands
located within or immediately adjacent to the proposed ROW in Penobscot,
Hancock, and Washington counties. The purpose of the investigation was
to determine the presence and extent of areas within the proposed
project corridor that meet the criteria for federal and state
jurisdictional wetlands according to the United States Army Corps of
Engineers (Corps) guidelines (Section 404 of the Clean Water Act) and
DEP's Natural Resources Protection Act (NRPA) (38 MRSA §§ 480-A to
480-Z) and Chapter 310 NRPA Wetland Protection Rules. Wetland scientists
conducted the majority of wetland delineations during the Fall of 2004.

A wetland summary table that provides wetland impact acreages, wetland
area converted from forested to scrub-shrub or emergent wetland types,
any criteria that are met for designation as a freshwater wetland of
special significance (FWSS), and the type of structure located in the
wetland, if any, is provided in Appendix 11-6. Representative data forms
and photographic documentation of representative wetland community types
is provided in Appendix 11-5. In addition, a complete set of full-sized
Plan and Profile drawings of the proposed ROW, which includes delineated
wetland boundaries, is provided with this application.

### Methods

Identification of wetland and stream resources within the study area was
done using a two-phase approach. First, the wetland resources along the
route were studied through use of available National Wetland Inventory
(NWI) maps, NRCS soil surveys, and existing wetland mapping associated
with the Maritimes & Northeast Pipeline project. Second, field
delineation of all the wetlands crossed by the route was conducted in
compliance with state and federal requirements. Wetland scientists
conducted the majority of wetland delineations during the Fall of 2004.

Wetland delineations were performed using the *Corps of Engineers
Wetland Delineation Manual* (Environmental Laboratory 1987). The
"routine on-site determination method" was selected as the most
appropriate delineation technique. Wetlands were considered present when
observations of vegetation, hydrology, and soils indicated that the
three parameter criteria for wetland identification were met.
Wetland/upland boundaries were flagged in most locations and the wetland
boundaries were located using a Global Positioning System (GPS). Soils
were classified according to *Field Indicators for Identifying Hydric
Soils in New England* (New England Hydric Soils Technical Committee
1998). All wetlands were classified using the United States Fish and
Wildlife Service's (USFWS) wetland classification system (e.g., PFO1)
(Cowardin et. al. 1979).

During the wetland field effort, any perennial or intermittent waterbody
crossings were also noted. Waterbody crossings were classified according
to the Land Use Regulation Commission's (LURC) Chapter 10 Land Use
Districts and Standards. Waterbodies were either classified as *major*
or *minor* according to these standards. Major waterbodies are defined
as "flowing water downstream from a point where such water drains 50
square miles" (e.g., Narraguagus River). Minor waterbodies are defined
as "flowing water upstream of a point where such water drains less than
50 square miles" (e.g., Meadow Brook).

### Results of Field Investigations

Because the proposed NRI route is located adjacent to existing ROWs and
within predominately forested areas, the majority of wetland cover types
along the route are palustrine forested and scrub-shrub wetlands
(approximately 292.89 acres or 86.5 percent of all wetlands crossed by
the project) (see Section 7, Wildlife and Fisheries, Table 7-1). Wetland
crossing locations and impacts were determined from the project Plan and
Profile drawings on which the GPS data locating wetland boundaries and
proposed clearing limits of the project were plotted.

No wetlands will be permanently or temporarily impacted as a result of
construction or operations at the Orrington Substation and the proposed
ROW has been sited such that there will be no loss of wetland acreage,
except for the insignificant amount that occurs where a structure (pole)
is set. As shown on the project Plan and Profile drawings and on the
Wetland Summary Table (Appendix 11-6), structure locations were sited to
the maximum extent practicable to be outside of wetlands. Therefore
wetland impacts from the project will be either temporary in nature or
the result of conversion of forested wetland to scrub-shrub or emergent
wetland types along the ROW. Furthermore, there will be no permanent
loss of functions of these wetlands. In addition, siting the route to be
co-located with existing ROWs, to the maximum extent practicable,
effectively reduces the total amount of forested wetland affected by the
project. As such and consistent with other utility projects in Maine, no
wetland mitigation plan has been developed for this project. Section
11.D.10 and Appendix 11-6 provide complete tabulation of all wetlands
affected by construction and operation of the project.

### Forested Wetlands

***Palustrine Forested System (PFO)***

Forested wetland affected by this project will be needle-leaved
evergreen or broad-leaved deciduous. Generally, these forested wetlands
consist of seasonally flooded/saturated conditions. Wildlife habitat and
groundwater discharge are the principal functions associated with
forested wetlands.

***Needle-leaved Evergreen (PFO4)***

Evergreen wetlands are dominated by 20- to 50-foot-high needle-leaved or
scale-leaved trees growing in peat or mineral soils. The dominant tree
species of evergreen wetlands are balsam fir (*Abies balsamea*) and red
spruce (*Picea rubens*), and are otherwise known as spruce-fir swamps.
The herbaceous layer tends to be quite sparse with herbs such as
goldthread (*Coptis groenlandica*) being locally common. This community
tended to be located along stream and bog margins.

Another evergreen community sparingly found along the route consists of
the northern white cedar (*Thuja occidentalis*) swamp. These areas can
consist of mixed stands of cedar, balsam fir, and red maple (*Acer
rubrum*). This community is relatively common in poorly drained basins
along streams or small ponds (Maine Natural Areas Program \[NAP\] 2001).
The shrub layer is typically sparse, but with high diversity of
bryophytes and herbs. Because these communities occur in more alkaline
conditions than other evergreen wetlands, several botanical features
such as calciphilic (i.e., calcium loving) orchids may be found in these
habitats. Sawtelle Heath in Baileyville includes a white cedar
component.

Another forested wetland community found along the route consists of the
spruce-larch wooded bog. This community can consist of black spruce
(*Picea mariana*) and/or American larch (*Larix* *laricina*) trees
growing over typical bog vegetation of ericad shrubs, graminoids, and
peat mosses. Typically, canopy closure is usually less than 50 percent.
Dwarf shrubs, herbs, and tree regeneration cover the ground, and peat
mosses form close to 100 percent cover. These areas are nutrient poor,
and may occur as part of fens (NAP 2001).

***Broad-leaved Deciduous (PFO1)***

The broad-leaved deciduous wetlands along this route were primarily red
maple-sensitive fern (*Onoclea sensibilis*) swamps. This forested
wetland type occurred on poorly drained basins or small depressional
areas in close association with drainage channels, or on floodplains of
medium-sized streams to small rivers (NAP 2001). Standing water and
surface saturation is common throughout the growing season. The shrub
layer typically consisted of northern arrow-wood (*Viburnum
recognitum*), winterberry (*Ilex verticillata*), and red maple saplings.
The diverse herbaceous layer consisted of sensitive fern, cinnamon fern
(*Osmunda cinnamomea*), bluejoint (*Calamagrostis canadensis*), manna
grass (*Glyceria obtusa*), and various sedge species (*Carex* species
\[spp.\]). Broad-leaved deciduous wetlands were found throughout the
project area, specifically on floodplains of the Dead Stream and Machias
River.

### Scrub-Shrub Wetlands

***Palustrine Scrub-Shrub System (PSS)***

Scrub-shrub wetlands are dominated by woody vegetation less than 20 feet
tall, including true shrubs, young trees, and trees and shrubs that are
small or stunted because of environmental conditions (Cowardin et al.
1979). Community equilibrium in this wetland type varies from relatively
stable "climax" shrub communities under wetter conditions, to
regenerating forested wetlands recently disturbed by activities such as
logging. The scrub-shrub communities found along this route were
seasonally flooded and often saturated to the surface throughout the
growing season and soils ranged from mineral to organic. The principal
wetland functions associated with these scrub-shrub wetlands consist of
wildlife habitat and sediment stabilization. The three general types of
scrub-shrub wetlands that occur in the region are inland fresh meadows,
scrub-shrub wetlands associated with streams, and peatland bogs.

***Broad-leaved Deciduous (PSS1)***

Broad-leaved deciduous scrub-shrub wetlands encountered along the
proposed ROW were usually associated with waterbodies, in wet
depressions, along the fringes of emergent wetlands, and in the
transition zones between emergent wetlands and upland communities. Soils
were usually mineral or muck and hydrology ranged from seasonally and
semi-permanently saturated, to seasonally flooded. The dominant species
of shrubs in these wetlands along the proposed ROW typically included
speckled alder (*Alnus incana*), steeple-bush (*Spiraea* *tomentosa*),
willow species (*Salix* spp.), highbush blueberry (*Vaccinium
corymbosum*), mountain holly (*Nemopanthus mucronatus*), northern
arrow-wood and winterberry. Depending on the density of shrub cover, the
herbaceous layer ranged from sparse to dense, and common species include
joe-pye-weed (*Eupatorium* *maculatum*), boneset (*E. perfoliatum*),
blue vervain (*Verbena hastata*) and various graminoids.

***Needle-leaved Evergreen (PSS4)***

Another scrub-shrub wetland found along the route consisted of
needle-leaved evergreen species and are dominated by small or stunted
individuals of species such as balsam fir, northern white cedar, and
red, white, or black spruce. Also, often intermixed with these species,
is the needle-leaved deciduous American larch. This wetland type, in
areas crossed by the project, were typically found in semi-permanently
saturated organic soils that occur in cool, poorly drained depressions,
or in seasonally saturated mineral soils. Many of the wetlands in this
class are fed by springs, or enriched by the seepage of cold,
minerotrophic groundwater. Deciduous shrubs, such as leatherleaf
(*Chamaedaphne calyculata*), sheep laurel (*Kalmia* *angustifolia*),
wild raisin (*Viburnum cassinoides*), and red-osier dogwood (*Cornus
stolonifera*), may comprise a significant component of the shrub cover.
Characteristic herbs are cinnamon fern, goldthread, cotton grasses
(*Eriophorum* spp.), and creeping snowberry (*Gaultheria hispidula*).

Percent cover of shrubs within this wetland type is variable, ranging
from around 50 percent in the more stable communities on wetter sites,
to 80 to 90 percent in regenerating coniferous communities on drier
sites.

### Emergent Wetlands

***Palustrine Emergent System (PEM)***

The emergent wetlands along the route typically consisted of tussock
sedge (*Carex stricta*) meadow, mixed graminoid-shrub marsh, and cattail
(*Typha latifolia*) marsh. The principal wetland functions found in
association with the emergent wetlands included wildlife habitat,
sediment retention, and sediment stabilization.

***Emergent Marsh (PEM1)***

Sedge meadow communities are typically seasonally flooded/saturated
areas with standing water through much of the growing season with
organic soils (NAP 2001). Tussock sedge, bluejoint grass, and woolgrass
(*Scirpus cyperinus*) usually dominated this community. All three of
these species were usually associated with monotypic stands (up to four
feet in height) that were common throughout the route. In general, these
wetlands were found along slow moving streams, shrub bog margins, and
swales between small hills.

The mixed graminoid-shrub marsh community found along the route
typically consisted of grasses and sedges on mineral soils (NAP 2001).
Species associated with this wetland type included bluejoint grass, fowl
manna grass, and wool grass. Shallow sedge (*Carex lurida*), fringed
sedge (*Carex crinita*), broom sedge (*Carex scoparia*), sensitive fern,
and bluejoint were also frequently encountered. This community also
consisted of a sparse shrub layer dominated by meadowsweet. These
primarily graminoid communities were usually located along stream
channels and culverted areas where scouring limits the development of
peat. In addition, this community was also associated with beaver
flowage areas within temporarily-ponded forested wetlands.

The cattail marsh communities along the route were located in basins or
depressions along slow moving streams or in large isolated depressions
where past disturbance was evident. Shrub communities consisting of
speckled alder and meadowsweet were frequently associated with the
cattail wetlands. Representative cattail communities were found along
the existing ROW near the Orrington Substation.

### Unconsolidated Bottom Wetlands

***Palustrine Unconsolidated Bottom (PUB and PUBb)***

[]{.mark}

Unconsolidated bottom wetlands are characterized by a lack of large
stable surfaces for plant and animal attachment with less than 25
percent cover of particles smaller than stones and less than 30 percent
cover by vegetation. They basically consist of open water with small
amounts of emergent and submergent plants. Wetlands classified as PUBb
are unconsolidated bottom wetlands that have been created or modified by
the action of beaver. In these types of wetlands, visible hydrologic
changes have occurred as a result of beaver activity. The principal
functions of unconsolidated bottom wetlands along the route included
wildlife habitat, groundwater recharge and, floodflow alteration.

### Functions and Values

Through the pre-application process it was determined that detailed
functional assessments were not required for each wetland impacted by
construction of the proposed project. Due to the nature of the proposed
project, all impacts to wetlands will be temporary or result only in a
change in cover type, and there will be no permanent loss of functions
and values. The following section provides a general presentation of the
principal functions and values of wetlands, by class, for wetland
impacts along the proposed ROW. The functions and values presented
below, are based on a descriptive, best professional judgment approach,
with reference to the methodology recommended by the Corp's New England
District -- *The Highway Methodology Workbook Supplement: Wetland
Functions and Values - A Descriptive Approach* (Corps Highway
Methodology) (Corp's 1999). Thirteen wetland functions and values are
recognized under the Corps methodology:

-   Groundwater Recharge/Discharge

-   Floodflow Alteration (Storage & Desynchronization)

-   Fish and Shellfish Habitat

-   Sediment/Toxicant Pathogen Retention

-   Nutrient Removal/Retention/Transformation

-   Production Export (Nutrient)

-   Sediment/Shoreline Stabilization

-   Wildlife Habitat

-   Recreation (Consumptive & Non-Consumptive)

-   Educational/Scientific Value

-   Uniqueness/Heritage

-   Visual Quality/Aesthetics

-   Threatened or Endangered Species Habitat

The Corps Highway Methodology provides a list of considerations and
qualifiers that are used to assess occurrence of each function or value,
followed by a subjective determination of Principal Functions and
Values, with documentation of supporting rationale on standard forms.
The list of considerations and qualifiers are used in the function and
values assessment of each wetland class, although a narrative approach
is employed in lieu of the standard forms.

***Palustrine Forested Wetlands***

Forested wetlands are the dominant wetland class along the proposed
route and within the region. Most are dominated by needle-leaved
evergreen trees (softwoods), including balsam fir*,* red spruce, black
spruce, and hybrids between these two species, American larch, and
northern white cedar. (Additional discussion of northern white cedar
swamps is provided below.) Broad-leaved deciduous trees (hardwoods),
especially red maple, black ash (*Fraxinus nigra*), and gray birch
(*Betula populifolia*) are also present but are seldom dominant; only a
few deciduous forested swamps were noted in the vicinity of the project.
Depending on the density of the crown cover, a shrubby understory can be
moderately well developed, although in this region it is often nearly
lacking. Ground-layer herbs are frequently sparse (due to shade) but
there is often a well-eveloped moss layer, including *Sphagnum* moss in
patches. The ground surface typically had a "hummock-hollow"
micro-relief. Drainage patterns varied from non-existent to
well-defined.

The basic recognized functions and values of forested wetlands of this
region are for stormwater and meltwater storage, stream and watershed
protection, water quality maintenance and wildlife habitat. They may
also, in areas of fractured bedrock, help in groundwater recharge. These
wetlands would be well-suited for trapping sediments or nutrients;
however, there is typically little input because the area is mostly
naturally and heavily vegetated (in contrast to agricultural or
urbanized areas which generate large sediment and nutrient loads). They
are generally not significant for other recognized functions and values.
Forested wetlands will be converted primarily to scrub-shrub wetlands as
result of this project. However, it is important to note that these
areas will still maintain their primary functions as the hydrology of
these systems will not be altered.

***Forested Wetlands - Northern White Cedar Swamps***

This subclass of forested wetlands is dominated by northern white cedar
and is indicative of slightly enriched, typically calcareous, soils.
Functions and values overall are the same as for other forested swamps:
stormwater storage, stream protection, water quality maintenance and
wildlife habitat. However, they are more likely to have a groundwater
discharge function. Such seepage swamps are less likely to provide a
stormwater storage function, although other cedar swamps have topography
that would provide storage. Northern white cedar swamps will be
converted primarily to scrub-shrub wetlands as result of this project,
dominated by cedar saplings. However, it is important to note that these
areas will still maintain their primary functions as the hydrology of
these systems will not be altered.

***Scrub-Shrub Wetlands (exclusive of peatlands)***

Scrub-shrub wetlands are generally associated with the fringes of
emergent wetlands and medium-sized to large streams or small rivers.
Scrub-shrub wetlands are usually wetter than forested wetlands, often
with seasonal standing water and a longer hydroperiod. Drainage patterns
are normally well established.

Scrub-shrub wetlands in general have functions similar to forested
wetlands. Because they often receive over bank flooding they are
significant in flood alteration, and often protect stream banks from
erosion. They can provide a similar stream course and watershed
protection, but because they are of lesser extent than forested
wetlands, are probably less significant overall for this function. They
may, however, be more productive in terms of food resources. Because
they were usually more structurally diverse, they appeared to support a
different and typically more diverse suite of associated wildlife
species than forested wetlands. This was especially true because they
were often associated with streams that can act as wildlife corridors.

***Scrub-Shrub Wetlands - Peatlands (bogs and fens)***

A particular type of wetland frequent in the region is the
peat-accumulating bog or heath. These often occur in small kettleholes
associated with esker systems; alternatively, they occur in broader
basins where they may be very large. Some peatlands associated with
groundwater discharge or higher nutrient (especially calcium) levels are
known as fens. Bogs are highly acidified environments, usually dominated
by *Sphagnum* mosses and by dwarf shrubs of the heath family such as
sheep laurel (*Kalmia angustifolia*), leatherleaf, and rhodora
(*Rhododendron canadense*). Fens have a more diverse plant community
that is usually dominated by non-*Sphagnum* mosses, sedges, and other
graminoids (*Scirpus* spp., *Eriophorum* spp.).

Functions and values of peatlands are somewhat different than those of
other wetlands when evaluated by criteria outlined in the Corps Highway
Methodology. They are generally more self-contained than other wetlands,
and primary production is often limited due to poor nutrition. However,
they may perform groundwater recharge, organic retention, nutrient
removal, and other functions. Also, they are widely considered "unique"
and, because they are often prominent in the landscape they are
aesthetically pleasing. Fens may support a number of rare plant species.
No fen areas were identified along the proposed corridor.

***Emergent Wetlands***

There are few large emergent areas along the proposed route. The
following discussion therefore pertains to beaver meadow type areas that
occur along small streams that will be crossed, or to open areas under
the existing power lines that would otherwise be forested wetlands.
Because they are generally small in extent and because beaver dams are
not permanent, these wetlands are generally not significant for
meltwater, floodwater or stormwater storage. However, because of the
vegetative structure, with normally dense, erect emergent vegetation,
they are often important for trapping sediments and nutrients within the
system, and for erosion control. They can be quite productive
(especially invertebrates), and may supply a large amount of food into
the system. Therefore they are significant for wildlife and often
support wildlife in greater concentrations than other wetland classes.
They are important fisheries habitats as well. Other wetlands functions
and values are limited.

***Palustrine Unconsolidated Bottom (PUB and PUBb)***

A very small fraction of the wetlands located within the proposed NRI
ROW (total of 5 wetlands) were classified as unconsolidated bottom
wetlands. These wetland communities were typically found along or
adjacent to major waterbodies. A representative PUB wetland was
identified along Stud Mill Road where the connecting waterbody flows
between Lower Sabao Lake and Burnt Land Lake. The principal functions of
unconsolidated bottom wetlands along the route included wildlife
habitat, groundwater recharge and floodflow alteration.

### Freshwater Wetlands of Special Significance

Wetlands occurring along the project route were designated as FWSS if
they met at least one of the eight criteria specified by NRPA's Wetland
Protection Rules (Chapter 310 § 4(A)). The project crosses 112 wetlands
meeting at least one of the eight criteria, 41 of which meet more than
one criterion. These areas are randomly located along the ROW and are
well dispersed throughout. A summary of wetlands meeting the criteria
for FWSS is presented below in Table 11-4.

+------------------------------------+---------------------------------+
| []{#__RefHeading___Toc102263179    |                                 |
| .anchor}Table 11-4. Summary of     |                                 |
| Wetlands Designated as FWSS Along  |                                 |
| Route                              |                                 |
+------------------------------------+---------------------------------+
| **Maine State Criteria^1^**        | **Number of NRI Wetlands**      |
|                                    |                                 |
|                                    | **Meeting Criteria**            |
+------------------------------------+---------------------------------+
| 4(A)(1)                            | 3                               |
+------------------------------------+---------------------------------+
| 4(A)(2)                            | 58                              |
+------------------------------------+---------------------------------+
| 4(A)(3)                            | 0                               |
+------------------------------------+---------------------------------+
| 4(A)(4)                            | 14                              |
+------------------------------------+---------------------------------+
| 4(A)(5)                            | 3                               |
+------------------------------------+---------------------------------+
| 4(A)(6)                            | 22                              |
+------------------------------------+---------------------------------+
| 4(A)(7)                            | 7                               |
+------------------------------------+---------------------------------+
| 4(A)(8)                            | 63                              |
+------------------------------------+---------------------------------+

**Notes:**

^1^ Freshwater Wetlands of Special Significance (FWSS) are defined by
the DEP in Chapter 310 Wetland Protection Rules pursuant to NRPA (NRPA
-- 38 M.R.S.A. § 480-A to 480-Z). Wetlands occurring along the project
route were designated as FWSS if they met one of the eight criteria
specified in Chapter 310 Rules (Chapter 310 § 4(A)), as explained in the
key below:

KEY:

> 4(A)(1) = The digital shapefile data from the NAP was used to
> determine whether the wetlands contained a natural community that is
> critically imperiled (S1) or imperiled (S2) as defined by NAP (Chapter
> 310 § 4(A)(1)).
>
> 4(A)(2) = Digital data from the Maine Department of Inland Fisheries
> and Wildlife (DIFW) was used to determine whether the wetlands met the
> criterion of "significant wildlife habitat". The freshwater wetland
> contains significant wildlife habitat as defined by 38 M.R.S.A. §
> 480-B(10)" (Chapter 310 § 4(A)(2)).
>
> 4(A)(3) = None of the wetlands are located within the coastal zone to
> qualify as within 250 feet of a coastal wetland. Therefore, this
> characteristic of a FWSS does not apply to freshwater wetlands in the
> project area.
>
> 4(A)(4) = Digital data from United States Geological Survey (USGS)
> quad sheets, Maine Office of GIS (MEOGIS) 24k pond shapefiles, and the
> lacustrine attribute found in NWI shapefiles were used to determine
> whether wetlands were, "located within 250 feet of the normal high
> water line, and within the same watershed, of any lake or pond
> classified as GPA under 38 M.R.S.A. § 465-A" (Chapter 310 § 4(A)(4)).
>
> 4(A)(5) = NWI wetlands designated as PAB (Palustrine Aquatic Bottom)
> or Riverine were considered FWSS under the criterion, "Aquatic
> vegetation, emergent marsh vegetation, or open water. The freshwater
> wetland contains under normal circumstances at least 20,000 square
> feet of aquatic vegetation, emergent marsh vegetation or open water,
> unless the 20,000 or more square foot area is the result of an
> artificial ponds or impoundment" (Chapter 310 § 4(A)(5)).
>
> 4(A)(6) = For the criterion, "Wetlands subject to flooding. The
> freshwater wetland area is inundated with floodwater during a 100-year
> flood event based on flood insurance maps produced by the Federal
> Emergency Management Agency (FEMA) or other site-specific information"
> (Chapter 310 § 4(A)(6)). FEMA digital and hardcopy maps were used to
> determine the wetland's location in relation to the 100-year flood
> elevation.
>
> 4(A)(7) = The peatlands criterion is defined as freshwater wetlands
> that are or contain peatlands, except that the DEP may determine that
> a previously mined peatland, or portion thereof, is not a wetland of
> special significance (Chapter 310 § 4(A)(7)). To determine this
> evaluation criteria the "Ba" modifier in NWI shapefiles attribute
> column was used to determine peatlands. The "Ba" modifier signifies
> that the wetland is a peatland.
>
> 4(A)(8) = The MEOGIS 24k rivers and streams shapefiles were used to
> determine the criterion, "river, stream, or brook. The freshwater
> wetland area is located within 25 feet of a river, stream, or brook"
> (Chapter 310 § 4(A)(8)). A 25-foot buffer was created at the edge of
> the river or stream shapefiles and any wetlands within the buffer were
> labeled as FWSS.

Of the total FWSS crossed by the project, three (less than one percent
of all wetlands crossed by the project) were classified as critically
imperiled or imperiled communities, 58 (15 percent) were considered
significant wildlife habitat, 14 (four percent) were located near a lake
or pond classified as GPA under 38 M.R.S.A. § 465-A, three (less than
one percent) contained the specified amount of aquatic vegetation,
emergent marsh vegetation, or open water, 22 (six percent) were subject
to flooding, 7 (two percent) were known peatlands, and 63 (16 percent)
were located within 25 feet of a river, stream, or brook. None of the
wetlands were located within the coastal zone to qualify as within 250
feet of a coastal wetland. Therefore, FWSS characteristic A(3) does not
apply to freshwater wetlands in the project area. In addition, due to
the size of delineated wetlands in comparison to the larger significant
wildlife habitat areas, more than one wetland may be located within a
single significant wildlife habitat. Overall, there were 45 significant
wildlife habitat areas in the vicinity of the proposed project area and
58 wetlands were located within these areas. For specific criteria met
by each wetland and distribution of FWSS along the proposed ROW, refer
to the Wetland Summary Table in Appendix 11-6. Ninety-three (83 percent)
of these FWSS wetlands already occur along existing ROWs corridors.
Furthermore, these resources are not associated with or in close
proximity to the Orrington Substation.

### Wetland Impacts and Impact Avoidance and Minimization

The assessment conducted for the proposed route shows that approximately
175.86 acres of forested wetland will be permanently converted to an
early successional cover type (as indicated in Table 7-1). Permanent
cover type conversion will occur to forested wetland areas but there
will be no permanent fill of forested wetlands. The conversion of
forested wetland cover types will result from initial clearing for
construction and follow-up vegetation maintenance practices during
project operation.

Although 43.56 acres of emergent wetland and 117.03 acres of scrub-shrub
wetland are located within the proposed ROW, only minimal temporary
impacts will occur to these wetlands. All affected emergent or
scrub-shrub wetland areas along the ROW will be maintained in an
emergent or scrub-shrub wetland state from ongoing vegetation
maintenance during operation. There will be essentially no impact to the
very small amount of unconsolidated bottom wetlands present (1.66 acres)
because they are primarily open water and the limited amount of
vegetation present will be unaffected by clearing or ROW maintenance.

Temporary impacts during construction will be minimized by conducting
winter clearing and construction to the maximum extent practicable, use
of construction mats when working in or crossing wetlands that are not
frozen and prompt restoration of disturbed areas following construction.
Removal of stumps will typically not be required in wetlands unless
necessary to install a structure. The stumps that are left in place may
promote natural regeneration within the construction ROW depending on
the species. Restoration of wetland areas (and therefore the temporary
nature of impacts) will be expedited by minimizing the duration of work
required for structure installation within wetland areas. Because the
hydrology of the wetlands along the route will not be altered (i.e., no
inflow/outflow restrictions), no permanent impact to principal functions
such as groundwater discharge or sediment stabilization are expected.
Impacts to the wildlife habitat value of wetlands are anticipated during
the construction period, but will be similarly short-term.

Additional details regarding the minimization of wetland impacts during
construction are provided in Section 14, Erosion and Sedimentation
Control, of this application and most specifically in the NRI E&S Plan,
provided in Appendix 14-1. The NRI E&S Plan provides detailed
descriptions of the erosion control measures that will be incorporated
into the construction and restoration phases of the project to minimize
adverse environmental impacts. Construction practices that will be
utilized by BHE to minimize impacts to wetlands will include the
following protective measures:

-   Erosion and sedimentation control barriers will be installed across
    the ROW on any slopes leading into wetlands and along the edge of
    the construction area, as necessary, to prevent disturbed soils from
    flowing into wetlands that are on or adjacent to the ROW.

-   Construction equipment operating within wetlands will be limited
    primarily to that needed to clear the area, drill the hole necessary
    for pole structures, set the pole structures, and restore the
    impacted area.

-   Construction activities within wetlands with saturated soils or
    standing water will be limited to wintertime, frozen soil
    conditions, as much as practicable, to minimize disturbance and
    compaction. If the ground is not frozen, either wide-tracked or
    balloon-tired equipment will be used. If significant rutting occurs,
    equipment will operate from construction mats.

Herbicide use will be prohibited within 25 feet of all wetlands with
standing water (See Appendix 10-1, the NRI Post-Construction
Right-of-Way Vegetation Maintenance Plan).

### Compensation

No permanent loss of wetland acreage will occur as a result of the
proposed NRI. No wetland compensation is proposed or required.

### References for Wetlands Investigation Report

Cowardin, L.M., V. Carter, F.C. Golet, E.T. LaRoe. 1979. *Classification
of Wetlands and Deepwater Habitats of the United States.* U.S. Dept. of
Interior, Fish and Wildlife Service. FWS/OBS-79/31. 131 pp.

Environmental Laboratory. 1987. *Corps of Engineers Wetlands Delineation
Manual.* Dept. of Army Waterways Experiment Station, Corps of Engineers,
Vicksburg, MS. Technical Report Y-87-1. 100 pp.

Maine Natural Areas Program. 2001. *Natural landscapes of Maine: A
Classification of Ecosystems and Natural Communities.* Department of
Conservation. Augusta, Maine. 79 pp.

New England Hydric Soils Technical Committee. 1998, 2^nd^ ed., *Field
Indicators for Identifying Hydric Soils in New England,* New England
Interstate Water Pollution Control Commission, Wilmington, MA. 76 pp.

U.S. Army Corps of Engineers (Corp). 1999. *The Highway Methodology
Workbook Supplement: Wetland Functions and Values - A Descriptive
Approach*. New England District. NAEEP-360-1-30a. September. 32 pp.

**APPENDIX 11-1**

**SOIL AND GEOTECHNICAL SURVEYS**

**APPENDIX 11-2**

**[SOIL SURVEY MAPS]{.smallcaps}**

**APPENDIX 11-3**

**SUMMARY OF SOIL CHARACTERISTICS**

**APPENDIX 11-3**

**NORTHEAST RELIABILITY INTERCONNECT**

**SUMMARY OF SOIL CHARACTERISTICS**

  ------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------
  **Map Unit **From**   **To**    **Distance**   **Map Unit Name**                **Range of  **Frequency of    **Drainage**   **Soil Type        **Depth to   **High      **K factor  **Erosion Hazard  **Hydric
  Symbol**                                                                        Slope (%)** Stones**                         (parent            Bedrock      Water Table (erosion    Potential**       Soil**
                                                                                                                               material)**        (inches)**   Depth       factor)**                     
                                                                                                                                                               (feet)**                                  
  ---------- ---------- --------- -------------- -------------------------------- ----------- ----------------- -------------- ------------------ ------------ ----------- ----------- ----------------- -----------
             **(mile    **(mile   **(feet)**                                                                                                                                                             **(Y or
             post)**    post)**                                                                                                                                                                          N)**

  BuA        0.00       0.03      182            Buxton                           0-2         N/A               moderately     glaciolacustrine   \>60         1.5-3.0     .32-.49     slight            N
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                               sediments                                                                 

  SeB        0.03       0.14      549            Stetson                          2-8         N/A               well drained   glaciofluvial      \>60         \>6.0       .5-.17      slight            N
                                                                                                                               deposits                                                                  

  BnC        0.14       0.22      446            Bangor                           8-15        very stony        well drained   firm glacial till  \>60         \>6.0       .20-.28     slight            N

  ScB        0.22       0.55      1730           Scantic                          0-8         N/A               poorly drained glaciomarine and   \>60         surface     .32-.49     slight            Y
                                                                                                                               glaciolacustrine                                                          
                                                                                                                               deposits                                                                  

  BnC        0.55       0.73      930            Bangor                           8-15        very stony        well drained   firm glacial till  \>60         \>6.0       .20-.28     slight            N

  HvC        0.73       0.83      569            Howland                          8-15        stony/bouldery    moderately     glacial till       \>60         1.0-2.0     .17-.24     slight            N
                                                                                                                well drained                                                                             

  DyB        0.83       0.95      591            Dixmont                          2-8         very stony        moderately     glacial till       \>60         1.0-2.0     0.28        slight            N
                                                                                                                well drained                                                                             

  BoA        0.95       1.59      3417           Biddeford                        0-3         N/A               very poorly    glaciolacustrine   \>60         +1.0-0.5    .32-.49     slight            Y
                                                                                                                drained        and glaciomarine                                                          
                                                                                                                               sediments                                                                 

  BuB        1.59       1.76      866            Buxton                           2-8         scattered pebbles moderately     glaciolacustrine   \>60         1.5-3.0     .32-.49     slight            N
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                to somewhat    sediments                                                                 
                                                                                                                poorly drained                                                                           

  ScB        1.76       1.93      908            Scantic                          0-8         N/A               poorly drained glaciomarine and   \>60         surface     .32-.49     slight            Y
                                                                                                                               glaciolacustrine                                                          
                                                                                                                               deposits                                                                  

  BuC        1.93       1.97      217            Buxton                           8-15        scattered pebbles moderately     glaciolacustrine   \>60         1.5-3.0     .32-.49     slight-moderate   N
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                to somewhat    sediments                                                                 
                                                                                                                poorly drained                                                                           

  BuB        1.97       2.07      502            Buxton                           2-8         scattered pebbles moderately     glaciolacustrine   \>60         1.5-3.0     .32-.49     slight            N
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                to somewhat    sediments                                                                 
                                                                                                                poorly drained                                                                           

  BuC        2.07       2.10      194            Buxton                           8-15        scattered pebbles moderately     glaciolacustrine   \>60         1.5-3.0     .32-.49     slight-moderate   N
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                to somewhat    sediments                                                                 
                                                                                                                poorly drained                                                                           

  BuB        2.10       2.13      169            Buxton                           2-8         scattered pebbles moderately     glaciolacustrine   \>60         1.5-3.0     .32-.49     slight            N
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                to somewhat    sediments                                                                 
                                                                                                                poorly drained                                                                           

  SuB        2.13       2.68      2884           Suffield                         2-8         sandy surface     well drained   glaciomarine and   \>60         1.5-3.0     .32-.49     slight            N
                                                                                              soil                             glaciolacustrine                                                          
                                                                                                                               deposits                                                                  

  ScB        2.68       2.73      274            Scantic                          0-8         N/A               poorly drained glaciomarine and   \>60         surface     .32-.49     slight            Y
                                                                                                                               glaciolacustrine                                                          
                                                                                                                               deposits                                                                  

  BoA        2.73       2.84      578            Biddeford                        0-3         N/A               very poorly    glaciolacustrine   \>60         +1.0-0.5    .32-.49     slight            Y
                                                                                                                drained        and glaciomarine                                                          
                                                                                                                               sediments                                                                 

  PgB        2.84       2.92      432            Plaisted                         2-8         stony             well drained   glacial till       \>60         1.5-2.5     .24-.28     slight            N

  SuB        2.92       2.96      211            Suffield                         2-8         sandy surface     well drained   glaciomarine and   \>60         1.5-3.0     .32-.49     slight            N
                                                                                              soil                             glaciolacustrine                                                          
                                                                                                                               deposits                                                                  

  BoA        2.96       3.07      584            Biddeford                        0-3         N/A               very poorly    glaciolacustrine   \>60         +1.0-0.5    .32-.49     slight            Y
                                                                                                                drained        and glaciomarine                                                          
                                                                                                                               sediments                                                                 

  BuA        3.07       3.12      248            Buxton                           0-2         N/A               moderately     glaciolacustrine   \>60         1.5-3.0     .32-.49     slight            N
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                               sediments                                                                 

  SuB        3.12       3.31      1001           Suffield                         2-8         sandy surface     well drained   glaciomarine and   \>60         1.5-3.0     .32-.49     slight            N
                                                                                              soil                             glaciolacustrine                                                          
                                                                                                                               deposits                                                                  

  BuB        3.31       3.39      399            Buxton                           2-8         scattered pebbles moderately     glaciolacustrine   \>60         1.5-3.0     .32-.49     slight            N
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                to somewhat    sediments                                                                 
                                                                                                                poorly drained                                                                           

  BoA        3.39       3.50      618            Biddeford                        0-3         N/A               very poorly    glaciolacustrine   \>60         +1.0-0.5    .32-.49     slight            Y
                                                                                                                drained        and glaciomarine                                                          
                                                                                                                               sediments                                                                 

  HvB        3.50       3.72      1172           Howland                          0-8         stony/bouldery    moderately     glacial till       \>60         1.0-2.0     .20-.24     slight            N
                                                                                                                well drained                                                                             

  BxB        3.72       3.78      295            Buxton, Scantic, & Biddeford     0-8         stony/bouldery    moderately     glaciolacustrine   \>60         1.0-3.0     .32-.49     slight            Y
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                to somewhat    sediments                                                                 
                                                                                                                poorly drained                                                                           

  PrC        3.78       4.12      1787           Plaisted                         5-15        stony             well drained   glacial till       \>60         1.5-2.5     .20-.24     slight            N

  BxB        4.12       4.15      180            Buxton, Scantic, & Biddeford     0-8         stony/bouldery    moderately     glaciolacustrine   \>60         1.0-3.0     .32-.49     slight            Y
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                to somewhat    sediments                                                                 
                                                                                                                poorly drained                                                                           

  BuB        4.15       4.28      688            Buxton                           2-8         scattered pebbles moderately     glaciolacustrine   \>60         1.5-3.0     .32-.49     slight            N
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                to somewhat    sediments                                                                 
                                                                                                                poorly drained                                                                           

  BuA        4.28       4.30      106            Buxton                           0-2         N/A               moderately     glaciolacustrine   \>60         1.5-3.0     .32-.49     slight            N
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                               sediments                                                                 

  BxB        4.30       4.32      89             Buxton, Scantic, & Biddeford     0-8         stony/bouldery    moderately     glaciolacustrine   \>60         1.0-3.0     .32-.49     slight            Y
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                to somewhat    sediments                                                                 
                                                                                                                poorly drained                                                                           

  BuA        4.32       4.39      357            Buxton                           0-2         N/A               moderately     glaciolacustrine   \>60         1.5-3.0     .32-.49     slight            N
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                               sediments                                                                 

  BuB        4.39       4.51      640            Buxton                           2-8         scattered pebbles moderately     glaciolacustrine   \>60         1.5-3.0     .32-.49     slight            N
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                to somewhat    sediments                                                                 
                                                                                                                poorly drained                                                                           

  SuB        4.51       4.54      177            Suffield                         2-8         sandy surface     well drained   glaciomarine and   \>60         1.5-3.0     .32-.49     slight            N
                                                                                              soil                             glaciolacustrine                                                          
                                                                                                                               deposits                                                                  

  BoA        4.54       4.62      383            Biddeford                        0-3         N/A               very poorly    glaciolacustrine   \>60         +1.0-0.5    .32-.49     slight            Y
                                                                                                                drained        and glaciomarine                                                          
                                                                                                                               sediments                                                                 

  SuB        4.62       4.64      132            Suffield                         2-8         sandy surface     well drained   glaciomarine and   \>60         1.5-3.0     .32-.49     slight            N
                                                                                              soil                             glaciolacustrine                                                          
                                                                                                                               deposits                                                                  

  BuA        4.64       4.69      281            Buxton                           0-2         N/A               moderately     glaciolacustrine   \>60         1.5-3.0     .32-.49     slight            N
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                               sediments                                                                 

  SuB        4.69       4.73      216            Suffield                         2-8         sandy surface     well drained   glaciomarine and   \>60         1.5-3.0     .32-.49     slight            N
                                                                                              soil                             glaciolacustrine                                                          
                                                                                                                               deposits                                                                  

  BuA        4.73       4.96      1168           Buxton                           0-2         N/A               moderately     glaciolacustrine   \>60         1.5-3.0     .32-.49     slight            N
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                               sediments                                                                 

  ScB        4.96       5.10      752            Scantic                          0-8         N/A               poorly drained glaciomarine and   \>60         surface     .32-.49     slight            Y
                                                                                                                               glaciolacustrine                                                          
                                                                                                                               deposits                                                                  

  BxB        5.10       5.14      212            Buxton, Scantic, & Biddeford     0-8         stony/bouldery    moderately     glaciolacustrine   \>60         1.0-3.0     .32-.49     slight            Y
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                to somewhat    sediments                                                                 
                                                                                                                poorly drained                                                                           

  BnC        5.14       5.22      432            Bangor                           8-15        very stony        well drained   firm glacial till  \>60         \>6.0       .20-.28     slight            N

  BnD        5.22       5.25      164            Bangor                           15-25       very stony        well drained   firm glacial till  \>60         \>6.0       .20-.28     slight            N

  PgC        5.25       5.31      304            Plaisted                         8-15        stony             well drained   glacial till       \>60         1.5-2.5     .24-.28     slight-moderate   N

  BnD        5.31       5.39      421            Bangor                           15-25       very stony        well drained   firm glacial till  \>60         \>6.0       .20-.28     slight            N

  BxB        5.39       5.42      144            Buxton, Scantic, & Biddeford     0-8         stony/bouldery    moderately     glaciolacustrine   \>60         1.0-3.0     .32-.49     slight            Y
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                to somewhat    sediments                                                                 
                                                                                                                poorly drained                                                                           

  SvC        5.42       5.50      424            suffield                         8-15        fine sandy loam   well drained   glaciomarine and   \>60         \>6.0       .32-.49     moderate-severe   N
                                                                                                                               glaciolacustrine                                                          
                                                                                                                               deposits                                                                  

  BuA        5.50       5.52      140            Buxton                           0-2         N/A               moderately     glaciolacustrine   \>60         1.5-3.0     .32-.49     slight            N
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                               sediments                                                                 

  SuB        5.52       5.58      316            Suffield                         2-8         sandy surface     well drained   glaciomarine and   \>60         1.5-3.0     .32-.49     slight            N
                                                                                              soil                             glaciolacustrine                                                          
                                                                                                                               deposits                                                                  

  BoA        5.58       5.66      422            Biddeford                        0-3         N/A               very poorly    glaciolacustrine   \>60         +1.0-0.5    .32-.49     slight            Y
                                                                                                                drained        and glaciomarine                                                          
                                                                                                                               sediments                                                                 

  BnD        5.66       5.73      369            Bangor                           15-25       very stony        well drained   firm glacial till  \>60         \>6.0       .20-.28     slight            N

  BoA        5.73       5.79      286            Biddeford                        0-3         N/A               very poorly    glaciolacustrine   \>60         +1.0-0.5    .32-.49     slight            Y
                                                                                                                drained        and glaciomarine                                                          
                                                                                                                               sediments                                                                 

  BnD        5.79       5.84      307            Bangor                           15-25       very stony        well drained   firm glacial till  \>60         \>6.0       .20-.28     slight            N

  BxB        5.84       5.97      678            Buxton, Scantic, & Biddeford     0-8         stony/bouldery    moderately     glaciolacustrine   \>60         1.0-3.0     .32-.49     slight            Y
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                to somewhat    sediments                                                                 
                                                                                                                poorly drained                                                                           

  DyC        5.97       5.99      103            Dixmont                          8-15        very stony        moderately     glacial till       \>60         1.0-2.0     0.28        slight            N
                                                                                                                well drained                                                                             

  PrE        5.99       6.05      280            Plaisted                         15-45       stony             well drained   glacial till       \>60         1.5-2.5     .17-.24     moderate-severe   N

  BxB        6.05       6.25      1085           Buxton, Scantic, & Biddeford     0-8         stony/bouldery    moderately     glaciolacustrine   \>60         1.0-3.0     .32-.49     slight            Y
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                to somewhat    sediments                                                                 
                                                                                                                poorly drained                                                                           

  BuA        6.25       6.40      802            Buxton                           0-2         N/A               moderately     glaciolacustrine   \>60         1.5-3.0     .32-.49     slight            N
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                               sediments                                                                 

  BxB        6.40       6.50      530            Buxton, Scantic, & Biddeford     0-8         stony/bouldery    moderately     glaciolacustrine   \>60         1.0-3.0     .32-.49     slight            Y
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                to somewhat    sediments                                                                 
                                                                                                                poorly drained                                                                           

  ScB        6.50       6.82      1699           Scantic                          0-8         N/A               poorly drained glaciomarine and   \>60         surface     .32-.49     slight            Y
                                                                                                                               glaciolacustrine                                                          
                                                                                                                               deposits                                                                  

  BuA        6.82       6.85      146            Buxton                           0-2         N/A               moderately     glaciolacustrine   \>60         1.5-3.0     .32-.49     slight            N
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                               sediments                                                                 

  ScB        6.85       6.90      238            Scantic                          0-8         N/A               poorly drained glaciomarine and   \>60         surface     .32-.49     slight            Y
                                                                                                                               glaciolacustrine                                                          
                                                                                                                               deposits                                                                  

  MsC        6.90       7.02      644            Monarda & Burnham                0-15        extremely stony   very poorly    dense glacial till \>60         0-1.5       .17-.28     slight            Y
                                                                                                                drained                                                                                  

  BxB        7.02       7.05      143            Buxton, Scantic, & Biddeford     0-8         stony/bouldery    moderately     glaciolacustrine   \>60         1.0-3.0     .32-.49     slight            Y
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                to somewhat    sediments                                                                 
                                                                                                                poorly drained                                                                           

  TkB        7.05       7.21      857            Thorndike                        2-8         rock outcrops     well drained   thin glacial till  0-20         none above  .17-.28     slight to         N
                                                                                                                               over bedrock                    bedrock                 moderate          

  BnB        7.21       7.27      329            Bangor                           0-8         very stony        well drained   firm glacial till  \>60         \>6.0       .20-.28     slight            N

  PrE        7.27       7.39      606            Plaisted                         15-45       stony             well drained   glacial till       \>60         1.5-2.5     .17-.24     moderate-severe   N

  MrB        7.39       7.42      190            Monarda & Burnham                0-8         stony/bouldery    poor           dense glacial till \>60         0-1.5       .17-.28     slight            Y

  BaC        7.42       7.46      204            Bangor                           8-15        very stony        well drained   firm glacial till  \>60         \>6.0       .20-.28     slight            N

  BaB        7.46       7.51      268            Bangor                           2-8         very stony        well drained   firm glacial till  \>60         \>6.0       .20-.28     slight            N

  BnB        7.51       7.64      668            Bangor                           0-8         very stony        well drained   firm glacial till  \>60         \>6.0       .20-.28     slight            N

  MrB        7.64       7.87      1209           Monarda & Burnham                0-8         stony/bouldery    poorly drained dense glacial till \>60         0-1.5       .17-.28     slight            Y

  BxB        7.87       8.20      1733           Buxton, Scantic, & Biddeford     0-8         stony/bouldery    moderately     glaciolacustrine   \>60         1.0-3.0     .32-.49     slight            Y
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                to somewhat    sediments                                                                 
                                                                                                                poorly drained                                                                           

  BoA        8.20       8.41      1127           Biddeford                        0-3         N/A               very poorly    glaciolacustrine   \>60         +1.0-0.5    .32-.49     slight            Y
                                                                                                                drained        and glaciomarine                                                          
                                                                                                                               sediments                                                                 

  BxB        8.41       8.46      259            Buxton, Scantic, & Biddeford     0-8         stony/bouldery    moderately     glaciolacustrine   \>60         1.0-3.0     .32-.49     slight            Y
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                to somewhat    sediments                                                                 
                                                                                                                poorly drained                                                                           

  PrC        8.46       8.52      315            Plaisted                         5-15        stony             well drained   glacial till       \>60         1.5-2.5     .20-.24     slight            N

  BoA        8.52       8.67      797            Biddeford                        0-3         N/A               very poorly    glaciolacustrine   \>60         +1.0-0.5    .32-.49     slight            Y
                                                                                                                drained        and glaciomarine                                                          
                                                                                                                               sediments                                                                 

  BxB        8.67       9.06      2059           Buxton, Scantic, & Biddeford     0-8         stony/bouldery    moderately     glaciolacustrine   \>60         1.0-3.0     .32-.49     slight            Y
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                to somewhat    sediments                                                                 
                                                                                                                poorly drained                                                                           

  BoA        9.06       9.19      701            Biddeford                        0-3         N/A               very poorly    glaciolacustrine   \>60         +1.0-0.5    .32-.49     slight            Y
                                                                                                                drained        and glaciomarine                                                          
                                                                                                                               sediments                                                                 

  BuA        9.19       9.30      554            Buxton                           0-2         N/A               moderately     glaciolacustrine   \>60         1.5-3.0     .32-.49     slight            N
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                               sediments                                                                 

  BoA        9.30       9.44      786            Biddeford                        0-3         N/A               very poorly    glaciolacustrine   \>60         +1.0-0.5    .32-.49     slight            Y
                                                                                                                drained        and glaciomarine                                                          
                                                                                                                               sediments                                                                 

  BuA        9.44       9.50      291            Buxton                           0-2         N/A               moderately     glaciolacustrine   \>60         1.5-3.0     .32-.49     slight            N
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                               sediments                                                                 

  ScB        9.50       9.63      702            Scantic                          0-8         N/A               poorly drained glaciomarine and   \>60         surface     .32-.49     slight            Y
                                                                                                                               glaciolacustrine                                                          
                                                                                                                               deposits                                                                  

  BuB        9.63       9.72      446            Buxton                           2-8         scattered pebbles moderately     glaciolacustrine   \>60         1.5-3.0     .32-.49     slight            N
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                to somewhat    sediments                                                                 
                                                                                                                poorly drained                                                                           

  Sa         9.72       9.77      283            Saco (Medomak)                   Nearly      N/A               very poorly    silty alluvial     \>60         0.1-0.5     .28-.49     moderate-severe   Y
                                                                                  level                         drained        deposits                                                                  

  stream     9.77       9.79      92             N/A                              N/A         N/A               N/A            N/A                N/A          N/A         N/A         N/A               N/A

  Sa         9.79       9.80      85             Saco (Medomak)                   Nearly      N/A               very poorly    silty alluvial     \>60         0.1-0.5     .28-.49     moderate-severe   Y
                                                                                  level                         drained        deposits                                                                  

  SuC2       9.80       9.86      312            Suffield eroded                  8-15        sandy surface     well drained   glaciomarine and   \>60         1.5-3.0     .32-.49     moderate-severe   N
                                                                                              soil                             glaciolacustrine                                                          
                                                                                                                               deposits                                                                  

  SuB        9.86       9.98      603            Suffield                         2-8         sandy surface     well drained   glaciomarine and   \>60         1.5-3.0     .32-.49     slight            N
                                                                                              soil                             glaciolacustrine                                                          
                                                                                                                               deposits                                                                  

  BuA        9.98       10.04     313            Buxton                           0-2         N/A               moderately     glaciolacustrine   \>60         1.5-3.0     .32-.49     slight            N
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                               sediments                                                                 

  SuB        10.04      10.10     310            Suffield                         2-8         sandy surface     well drained   glaciomarine and   \>60         1.5-3.0     .32-.49     slight            N
                                                                                              soil                             glaciolacustrine                                                          
                                                                                                                               deposits                                                                  

  BoA        10.10      10.15     269            Biddeford                        0-3         N/A               very poorly    glaciolacustrine   \>60         +1.0-0.5    .32-.49     slight            Y
                                                                                                                drained        and glaciomarine                                                          
                                                                                                                               sediments                                                                 

  ScB        10.15      10.31     881            Scantic                          0-8         N/A               poorly drained glaciomarine and   \>60         surface     .32-.49     slight            Y
                                                                                                                               glaciolacustrine                                                          
                                                                                                                               deposits                                                                  

  BoA        10.31      10.59     1446           Biddeford                        0-3         N/A               very poorly    glaciolacustrine   \>60         +1.0-0.5    .32-.49     slight            Y
                                                                                                                drained        and glaciomarine                                                          
                                                                                                                               sediments                                                                 

  BxB        10.59      10.69     566            Buxton, Scantic, & Biddeford     0-8         stony/bouldery    moderately     glaciolacustrine   \>60         1.0-3.0     .32-.49     slight            Y
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                to somewhat    sediments                                                                 
                                                                                                                poorly drained                                                                           

  BoA        10.69      10.81     616            Biddeford                        0-3         N/A               very poorly    glaciolacustrine   \>60         +1.0-0.5    .32-.49     slight            Y
                                                                                                                drained        and glaciomarine                                                          
                                                                                                                               sediments                                                                 

  BxB        10.81      11.01     1060           Buxton, Scantic, & Biddeford     0-8         stony/bouldery    moderately     glaciolacustrine   \>60         1.0-3.0     .32-.49     slight            Y
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                to somewhat    sediments                                                                 
                                                                                                                poorly drained                                                                           

  MsC        11.01      11.06     239            Monarda & Burnham                0-15        extremely stony   very poorly    dense glacial till \>60         0-1.5       .17-.28     slight            Y
                                                                                                                drained                                                                                  

  BoA        11.06      11.08     101            Biddeford                        0-3         N/A               very poorly    glaciolacustrine   \>60         +1.0-0.5    .32-.49     slight            Y
                                                                                                                drained        and glaciomarine                                                          
                                                                                                                               sediments                                                                 

  BxB        11.08      11.17     496            Buxton, Scantic, & Biddeford     0-8         stony/bouldery    moderately     glaciolacustrine   \>60         1.0-3.0     .32-.49     slight            Y
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                to somewhat    sediments                                                                 
                                                                                                                poorly drained                                                                           

  ScB        11.17      11.32     783            Scantic                          0-8         N/A               poorly drained glaciomarine and   \>60         surface     .32-.49     slight            Y
                                                                                                                               glaciolacustrine                                                          
                                                                                                                               deposits                                                                  

  BoA        11.32      11.47     788            Biddeford                        0-3         N/A               very poorly    glaciolacustrine   \>60         +1.0-0.5    .32-.49     slight            Y
                                                                                                                drained        and glaciomarine                                                          
                                                                                                                               sediments                                                                 

  Mu         11.47      11.63     871            muck                             N/A         N/A               very poorly    decomposed organic N/A          N/A         N/A         N/A               Y
                                                                                                                drained        materials                                                                 

  BoA        11.63      11.73     532            Biddeford                        0-3         N/A               very poorly    glaciolacustrine   \>60         +1.0-0.5    .32-.49     slight            Y
                                                                                                                drained        and glaciomarine                                                          
                                                                                                                               sediments                                                                 

  BxB        11.73      11.75     65             Buxton, Scantic, & Biddeford     0-8         stony/bouldery    moderately     glaciolacustrine   \>60         1.0-3.0     .32-.49     slight            Y
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                to somewhat    sediments                                                                 
                                                                                                                poorly drained                                                                           

  MsC        11.75      11.79     222            Monarda & Burnham                0-15        extremely stony   very poorly    dense glacial till \>60         0-1.5       .17-.28     slight            Y
                                                                                                                drained                                                                                  

  RmD        11.79      11.86     354            Rockland & Thorndike             Strongly    stony/cobbly      somewhat       thin glacial till  0-12         N/A         .17-.28     slight to         N
                                                                                  sloping                       excessively    over bedrock                                            moderate          
                                                                                                                drained                                                                                  

  RmC        11.86      11.95     513            Rockland & Thorndike             sloping     extremely rocky   well drained   thin glacial till  0-12         N/A         .17-.28     slight to         N
                                                                                                                               over bedrock                                            moderate          

  RmD        11.95      12.01     321            Rockland & Thorndike             Strongly    stony/cobbly      somewhat       thin glacial till  0-12         N/A         .17-.28     slight to         N
                                                                                  sloping                       excessively    over bedrock                                            moderate          
                                                                                                                drained                                                                                  

  stream     12.01      12.03     70             N/A                              N/A         N/A               N/A            N/A                N/A          N/A         N/A         N/A               N/A

  Lk         12.03      12.06     200            Limerick (Charles)               Nearly      occasional rock   poorly drained silty and sandy    \>60         0-1.5       .20-.49     moderate-severe   Y
                                                                                  level       outcrops                         stream deposits,                                                          
                                                                                                                               loamy alluvium                                                            

  RmC        12.06      12.10     214            Rockland & Thorndike             sloping     extremely rocky   well drained   thin glacial till  0-12         N/A         .17-.28     slight to         N
                                                                                                                               over bedrock                                            moderate          

  RmD        12.10      12.17     352            Rockland & Thorndike             Strongly    stony/cobbly      somewhat       thin glacial till  0-12         N/A         .17-.28     slight to         N
                                                                                  sloping                       excessively    over bedrock                                            moderate          
                                                                                                                drained                                                                                  

  MsC        12.17      12.26     491            Monarda & Burnham                0-15        extremely stony   very poorly    dense glacial till \>60         0-1.5       .17-.28     slight            Y
                                                                                                                drained                                                                                  

  TvB        12.26      12.32     305            Thorndike                        2-8         very stony        well drained   thin glacial till  10-20        none above  .17-.28     slight to         N
                                                                                                                               over bedrock                    bedrock                 moderate          

  MsC        12.32      12.39     382            Monarda & Burnham                0-15        extremely stony   very poorly    dense glacial till \>60         0-1.5       .17-.28     slight            Y
                                                                                                                drained                                                                                  

  MrB        12.39      12.49     480            Monarda & Burnham                0-8         stony/bouldery    poorly drained dense glacial till \>60         0-1.5       .17-.28     slight            Y

  ScB        12.49      12.57     461            Scantic                          0-8         N/A               poorly drained glaciomarine and   \>60         surface     .32-.49     slight            Y
                                                                                                                               glaciolacustrine                                                          
                                                                                                                               deposits                                                                  

  HvB        12.57      12.65     383            Howland                          0-8         stony/bouldery    moderately     glacial till       \>60         1.0-2.0     .20-.24     slight            N
                                                                                                                well drained                                                                             

  MrB        12.65      12.84     1040           Monarda & Burnham                0-8         stony/bouldery    poorly drained dense glacial till \>60         0-1.5       .17-.28     slight            Y

  PrC        12.84      12.90     323            Plaisted                         5-15        stony             well drained   glacial till       \>60         1.5-2.5     .20-.24     slight            N

  HvB        12.90      12.96     315            Howland                          0-8         stony/bouldery    moderately     glacial till       \>60         1.0-2.0     .20-.24     slight            N
                                                                                                                well drained                                                                             

  MrB        12.96      13.06     502            Monarda & Burnham                0-8         stony/bouldery    poorly drained dense glacial till \>60         0-1.5       .17-.28     slight            Y

  PrC        13.06      13.17     598            Plaisted                         5-15        stony             well drained   glacial till       \>60         1.5-2.5     .20-.24     slight            N

  BoA        13.17      13.34     906            Biddeford                        0-3         N/A               very poorly    glaciolacustrine   \>60         +1.0-0.5    .32-.49     slight            Y
                                                                                                                drained        and glaciomarine                                                          
                                                                                                                               sediments                                                                 

  PrC        13.34      13.44     538            Plaisted                         5-15        stony             well drained   glacial till       \>60         1.5-2.5     .20-.24     slight            N

  HvB        13.44      13.60     805            Howland                          0-8         stony/bouldery    moderately     glacial till       \>60         1.0-2.0     .20-.24     slight            N
                                                                                                                well drained                                                                             

  MrB        13.60      13.76     874            Monarda & Burnham                0-8         stony/bouldery    poorly drained dense glacial till \>60         0-1.5       .17-.28     slight            Y

  BxB        13.76      13.97     1110           Buxton, Scantic, & Biddeford     0-8         stony/bouldery    moderately     glaciolacustrine   \>60         1.0-3.0     .32-.49     slight            Y
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                to somewhat    sediments                                                                 
                                                                                                                poorly drained                                                                           

  PrC        13.97      14.11     714            Plaisted                         5-15        stony             well drained   glacial till       \>60         1.5-2.5     .20-.24     slight            N

  BxB        14.11      14.19     426            Buxton, Scantic, & Biddeford     0-8         stony/bouldery    moderately     glaciolacustrine   \>60         1.0-3.0     .32-.49     slight            Y
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                to somewhat    sediments                                                                 
                                                                                                                poorly drained                                                                           

  MrB        14.19      14.48     1550           Monarda & Burnham                0-8         stony/bouldery    poorly drained dense glacial till \>60         0-1.5       .17-.28     slight            Y

  ScB        14.48      14.68     1040           Scantic                          0-8         N/A               poorly drained glaciomarine and   \>60         surface     .32-.49     slight            Y
                                                                                                                               glaciolacustrine                                                          
                                                                                                                               deposits                                                                  

  HvB        14.68      14.90     1187           Howland                          0-8         stony/bouldery    moderately     glacial till       \>60         1.0-2.0     .20-.24     slight            N
                                                                                                                well drained                                                                             

  BxB        14.90      15.03     637            Buxton, Scantic, & Biddeford     0-8         stony/bouldery    moderately     glaciolacustrine   \>60         1.0-3.0     .32-.49     slight            Y
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                to somewhat    sediments                                                                 
                                                                                                                poorly drained                                                                           

  HvB        15.03      15.16     720            Howland                          0-8         stony/bouldery    moderately     glacial till       \>60         1.0-2.0     .20-.24     slight            N
                                                                                                                well drained                                                                             

  ScB        15.16      15.29     696            Scantic                          0-8         N/A               poorly drained glaciomarine and   \>60         surface     .32-.49     slight            Y
                                                                                                                               glaciolacustrine                                                          
                                                                                                                               deposits                                                                  

  TvB        15.29      15.38     441            Thorndike                        2-8         very stony        well drained   thin glacial till  10-20        none above  .17-.28     slight to         N
                                                                                                                               over bedrock                    bedrock                 moderate          

  stream     15.38      15.41     157            N/A                              N/A         N/A               N/A            N/A                N/A          N/A         N/A         N/A               N/A

  Sa         15.41      15.47     346            Saco (Medomak)                   Nearly      N/A               very poorly    silty alluvial     \>60         0.1-0.5     .28-.49     moderate-severe   Y
                                                                                  level                         drained        deposits                                                                  

  BxB        15.47      15.87     2095           Buxton, Scantic, & Biddeford     0-8         stony/bouldery    moderately     glaciolacustrine   \>60         1.0-3.0     .32-.49     slight            Y
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                to somewhat    sediments                                                                 
                                                                                                                poorly drained                                                                           

  HvB        15.87      15.96     485            Howland                          0-8         stony/bouldery    moderately     glacial till       \>60         1.0-2.0     .20-.24     slight            N
                                                                                                                well drained                                                                             

  MrB        15.96      16.13     882            Monarda & Burnham                0-8         stony/bouldery    poorly drained dense glacial till \>60         0-1.5       .17-.28     slight            Y

  PrC        16.13      16.23     517            Plaisted                         5-15        stony             well drained   glacial till       \>60         1.5-2.5     .20-.24     slight            N

  MrB        16.23      16.34     597            Monarda & Burnham                0-8         stony/bouldery    poorly drained dense glacial till \>60         0-1.5       .17-.28     slight            Y

  PrC        16.34      16.74     2144           Plaisted                         5-15        stony             well drained   glacial till       \>60         1.5-2.5     .20-.24     slight            N

  HvB        16.74      16.91     850            Howland                          0-8         stony/bouldery    moderately     glacial till       \>60         1.0-2.0     .20-.24     slight            N
                                                                                                                well drained                                                                             

  BxB        16.91      16.98     414            Buxton, Scantic, & Biddeford     0-8         stony/bouldery    moderately     glaciolacustrine   \>60         1.0-3.0     .32-.49     slight            Y
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                to somewhat    sediments                                                                 
                                                                                                                poorly drained                                                                           

  RaB        16.98      17.15     868            Red Hook & Atherton              0-8         scattered bedrock poorly drained glaciofluvial      \>60         0.5-1.5     .17-.32     slight            Y
                                                                                              outcrops                         deposits                                                                  

  MaB        17.15      17.33     957            Machias                          0-8         gravelly/cobbly   moderately     gravelly sola over \>60         1.5-2.5     .10-.17     slight            N
                                                                                                                well drained   glaciofluvial                                                             
                                                                                                                               deposits                                                                  

  MrB        17.33      17.44     586            Monarda & Burnham                0-8         stony/bouldery    poorly drained dense glacial till \>60         0-1.5       .17-.28     slight            Y

  BoA        17.44      17.53     467            Biddeford                        0-3         N/A               very poorly    glaciolacustrine   \>60         +1.0-0.5    .32-.49     slight            Y
                                                                                                                drained        and glaciomarine                                                          
                                                                                                                               sediments                                                                 

  Pa         17.53      17.63     520            Peat & Muck                      N/A         peat & muck       very poorly    decomposed organic N/A          N/A         N/A         N/A               Y
                                                                                                                drained        materials                                                                 
                                                                                                                organic soil                                                                             

  BoA        17.63      17.68     293            Biddeford                        0-3         N/A               very poorly    glaciolacustrine   \>60         +1.0-0.5    .32-.49     slight            Y
                                                                                                                drained        and glaciomarine                                                          
                                                                                                                               sediments                                                                 

  RaB        17.68      18.01     1727           Red Hook & Atherton              0-8         scattered bedrock poorly drained glaciofluvial      \>60         0.5-1.5     .17-.32     slight            Y
                                                                                              outcrops                         deposits                                                                  

  MaB        18.01      18.25     1279           Machias                          0-8         gravelly/cobbly   moderately     gravelly sola over \>60         1.5-2.5     .10-.17     slight            N
                                                                                                                well drained   glaciofluvial                                                             
                                                                                                                               deposits                                                                  

  CnB        18.25      18.39     729            Colton                           2-8         gravelly/cobbly   excessive      glaciofluvial      \>60         \>6.0       .17-.20     slight            N
                                                                                                                               sdeposits                                                                 

  CnC        18.39      18.44     259            Colton                           8-15        bouldery/         excessive      glaciofluvial      \>60         \>6.0       .17-.20     slight            N
                                                                                              occasional                       sdeposits                                                                 
                                                                                              outcrops                                                                                                   

  HvC        18.44      18.56     650            Howland                          8-15        stony/bouldery    moderately     glacial till       \>60         1.0-2.0     .17-.24     slight            N
                                                                                                                well drained                                                                             

  SfC        18.56      18.83     1400           Stetson & Suffield               0-15        gravelly          well drained   glaciofluvial      \>60         \>6.0       .05-.49     moderate          N
                                                                                                                               deposits                                                                  

  MaB        18.83      19.00     907            Machias                          0-8         gravelly/cobbly   moderately     gravelly sola over \>60         1.5-2.5     .10-.17     slight            N
                                                                                                                well drained   glaciofluvial                                                             
                                                                                                                               deposits                                                                  

  SfC        19.00      19.14     757            Stetson & Suffield               0-15        gravelly          well drained   glaciofluvial      \>60         \>6.0       .05-.49     moderate          N
                                                                                                                               deposits                                                                  

  BnB        19.14      19.31     876            Bangor                           0-8         very stony        well drained   firm glacial till  \>60         \>6.0       .20-.28     slight            N

  RmC        19.31      19.36     270            Rockland & Thorndike             sloping     extremely rocky   well drained   thin glacial till  0-12         N/A         .17-.28     slight to         N
                                                                                                                               over bedrock                                            moderate          

  MsC        19.36      19.38     132            Monarda & Burnham                0-15        extremely stony   very poorly    dense glacial till \>60         0-1.5       .17-.28     slight            Y
                                                                                                                drained                                                                                  

  BxB        19.38      19.47     466            Buxton, Scantic, & Biddeford     0-8         stony/bouldery    moderately     glaciolacustrine   \>60         1.0-3.0     .32-.49     slight            Y
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                to somewhat    sediments                                                                 
                                                                                                                poorly drained                                                                           

  MrB        19.47      19.58     546            Monarda & Burnham                0-8         stony/bouldery    poorly drained dense glacial till \>60         0-1.5       .17-.28     slight            Y

  HvB        19.58      19.62     249            Howland                          0-8         stony/bouldery    moderately     glacial till       \>60         1.0-2.0     .20-.24     slight            N
                                                                                                                well drained                                                                             

  BxB        19.62      19.69     332            Buxton, Scantic, & Biddeford     0-8         stony/bouldery    moderately     glaciolacustrine   \>60         1.0-3.0     .32-.49     slight            Y
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                to somewhat    sediments                                                                 
                                                                                                                poorly drained                                                                           

  HvB        19.69      19.78     487            Howland                          0-8         stony/bouldery    moderately     glacial till       \>60         1.0-2.0     .20-.24     slight            N
                                                                                                                well drained                                                                             

  MrB        19.78      19.83     257            Monarda & Burnham                0-8         stony/bouldery    poorly drained dense glacial till \>60         0-1.5       .17-.28     slight            Y

  TvC        19.83      19.86     197            Thorndike                        8-15        many rock         well drained   thin glacial till  10-20        \>6.0       .17-.20     slight to         N
                                                                                              outcrops                         over bedrock                                            moderate          

  MrB        19.86      19.92     273            Monarda & Burnham                0-8         stony/bouldery    poorly drained dense glacial till \>60         0-1.5       .17-.28     slight            Y

  PrC        19.92      20.09     938            Plaisted                         5-15        stony             well drained   glacial till       \>60         1.5-2.5     .20-.24     slight            N

  BxB        20.09      20.14     232            Buxton, Scantic, & Biddeford     0-8         stony/bouldery    moderately     glaciolacustrine   \>60         1.0-3.0     .32-.49     slight            Y
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                to somewhat    sediments                                                                 
                                                                                                                poorly drained                                                                           

  Sa         20.14      20.18     212            Saco (Medomak)                   Nearly      N/A               very poorly    silty alluvial     \>60         0.1-0.5     .28-.49     moderate-severe   Y
                                                                                  level                         drained        deposits                                                                  

  BxB        20.18      20.32     769            Buxton, Scantic, & Biddeford     0-8         stony/bouldery    moderately     glaciolacustrine   \>60         1.0-3.0     .32-.49     slight            Y
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                to somewhat    sediments                                                                 
                                                                                                                poorly drained                                                                           

  MaB        20.32      20.35     160            Machias                          0-8         gravelly/cobbly   moderately     gravelly sola over \>60         1.5-2.5     .10-.17     slight            N
                                                                                                                well drained   glaciofluvial                                                             
                                                                                                                               deposits                                                                  

  BxB        20.35      20.67     1691           Buxton, Scantic, & Biddeford     0-8         stony/bouldery    moderately     glaciolacustrine   \>60         1.0-3.0     .32-.49     slight            Y
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                to somewhat    sediments                                                                 
                                                                                                                poorly drained                                                                           

  MrB        20.67      20.83     847            Monarda & Burnham                0-8         stony/bouldery    poorly drained dense glacial till \>60         0-1.5       .17-.28     slight            Y

  HvB        20.83      21.04     1093           Howland                          0-8         stony/bouldery    moderately     glacial till       \>60         1.0-2.0     .20-.24     slight            N
                                                                                                                well drained                                                                             

  TvB        21.04      21.12     424            Thorndike                        2-8         very stony        well drained   thin glacial till  10-20        none above  .17-.28     slight to         N
                                                                                                                               over bedrock                    bedrock                 moderate          

  MrB        21.12      21.27     775            Monarda & Burnham                0-8         stony/bouldery    poorly drained dense glacial till \>60         0-1.5       .17-.28     slight            Y

  HvB        21.27      21.38     568            Howland                          0-8         stony/bouldery    moderately     glacial till       \>60         1.0-2.0     .20-.24     slight            N
                                                                                                                well drained                                                                             

  TvB        21.38      21.45     388            Thorndike                        2-8         very stony        well drained   thin glacial till  10-20        none above  .17-.28     slight to         N
                                                                                                                               over bedrock                    bedrock                 moderate          

  HvB        21.45      21.50     240            Howland                          0-8         stony/bouldery    moderately     glacial till       \>60         1.0-2.0     .20-.24     slight            N
                                                                                                                well drained                                                                             

  MrB        21.50      21.58     434            Monarda & Burnham                0-8         stony/bouldery    poorly drained dense glacial till \>60         0-1.5       .17-.28     slight            Y

  BoA        21.58      21.90     1695           Biddeford                        0-3         N/A               very poorly    glaciolacustrine   \>60         +1.0-0.5    .32-.49     slight            Y
                                                                                                                drained        and glaciomarine                                                          
                                                                                                                               sediments                                                                 

  BxB        21.90      21.94     223            Buxton, Scantic, & Biddeford     0-8         stony/bouldery    moderately     glaciolacustrine   \>60         1.0-3.0     .32-.49     slight            Y
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                to somewhat    sediments                                                                 
                                                                                                                poorly drained                                                                           

  TvB        21.94      22.01     380            Thorndike                        2-8         very stony        well drained   thin glacial till  10-20        none above  .17-.28     slight to         N
                                                                                                                               over bedrock                    bedrock                 moderate          

  BxB        22.01      22.04     141            Buxton, Scantic, & Biddeford     0-8         stony/bouldery    moderately     glaciolacustrine   \>60         1.0-3.0     .32-.49     slight            Y
                                                                                                                well drained   and glaciomarine                                                          
                                                                                                                to somewhat    sediments                                                                 
                                                                                                                poorly drained                                                                           

  HvB        22.04      22.09     269            Howland                          0-8         stony/bouldery    moderately     glacial till       \>60         1.0-2.0     .20-.24     slight            N
                                                                                                                well drained                                                                             

  NO DATA    22.09      74.39                                                                                                                                                                             

  340B       74.39      74.50     562            Telos-Elliottsville-Monarda      0-8         very stony        well drained   firm glacial till  20-40        0-1.5       .15-.32     slight to         Y
                                                 complex                                                        to poorly                                                              moderate          
                                                                                                                drained                                                                                  

  348B       74.50      74.57     379            Monarda-Telos association        0-8         very stony        somewhat       dense glacial till \>60         0-1.5       .15-.32     slight            Y
                                                                                                                poorly to                                                                                
                                                                                                                poorly drained                                                                           

  340B       74.57      74.60     159            Telos-Elliottsville-Monarda      0-8         very stony        well drained   firm glacial till  20-40        0-1.5       .15-.32     slight to         Y
                                                 complex                                                        to poorly                                                              moderate          
                                                                                                                drained                                                                                  

  345B       74.60      74.66     317            Telos-Chesuncook association     0-8         very stony        moderately     firm glacial till  \>60         .5-2.5      .24-.32     slight            N
                                                                                                                well to                                                                                  
                                                                                                                somewhat                                                                                 
                                                                                                                poorly drained                                                                           

  391A       74.66      74.74     407            not described                    not         not described     not described  not described      not          not         not         not described     not
                                                                                  described                                                       described    described   described                     described

  345B       74.74      74.78     238            Telos-Chesuncook association     0-8         very stony        moderately     firm glacial till  \>60         .5-2.5      .24-.32     slight            N
                                                                                                                well to                                                                                  
                                                                                                                somewhat                                                                                 
                                                                                                                poorly drained                                                                           

  340C       74.78      74.99     1093           Chesuncook-Elliottsville-Telos   3-15        very stony        moderately     firm glacial till  20-40        0-1.5       .15-.32     slight to         Y
                                                 complex                                                        well to                                                                moderate          
                                                                                                                somewhat                                                                                 
                                                                                                                poorly drained                                                                           

  348B       74.99      75.04     278            Monarda-Telos association        0-8         very stony        somewhat       dense glacial till \>60         0-1.5       .15-.32     slight            Y
                                                                                                                poorly to                                                                                
                                                                                                                poorly drained                                                                           

  340C       75.04      75.53     2577           Chesuncook-Elliottsville-Telos   3-15        very stony        moderately     firm glacial till  20-40        0-1.5       .15-.32     slight to         Y
                                                 complex                                                        well to                                                                moderate          
                                                                                                                somewhat                                                                                 
                                                                                                                poorly drained                                                                           

  341C       75.53      75.62     476            Elliotsville-Monson              3-15        very stony        moderately     glacial till       10-40        \>6\'       .24-.32     slight            N
                                                                                                                well to                                                                                  
                                                                                                                somewhat                                                                                 
                                                                                                                excessively                                                                              
                                                                                                                drained                                                                                  

  340C       75.62      75.71     477            Chesuncook-Elliottsville-Telos   3-15        very stony        moderately     firm glacial till  20-40        0-1.5       .15-.32     slight to         Y
                                                 complex                                                        well to                                                                moderate          
                                                                                                                somewhat                                                                                 
                                                                                                                poorly drained                                                                           

  341C       75.71      75.79     400            Elliotsville-Monson              3-15        very stony        moderately     glacial till       10-40        \>6\'       .24-.32     slight            N
                                                                                                                well to                                                                                  
                                                                                                                somewhat                                                                                 
                                                                                                                excessively                                                                              
                                                                                                                drained                                                                                  

  340C       75.79      76.29     2674           Chesuncook-Elliottsville-Telos   3-15        very stony        moderately     firm glacial till  20-40        0-1.5       .15-.32     slight to         Y
                                                 complex                                                        well to                                                                moderate          
                                                                                                                somewhat                                                                                 
                                                                                                                poorly drained                                                                           

  348B       76.29      76.46     879            Monarda-Telos association        0-8         very stony        somewhat       dense glacial till \>60         0-1.5       .15-.32     slight            Y
                                                                                                                poorly to                                                                                
                                                                                                                poorly drained                                                                           

  340B       76.46      76.78     1683           Telos-Elliottsville-Monarda      0-8         very stony        well drained   firm glacial till  20-40        0-1.5       .15-.32     slight to         Y
                                                 complex                                                        to poorly                                                              moderate          
                                                                                                                drained                                                                                  

  348B       76.78      76.87     505            Monarda-Telos association        0-8         very stony        somewhat       dense glacial till \>60         0-1.5       .15-.32     slight            Y
                                                                                                                poorly to                                                                                
                                                                                                                poorly drained                                                                           

  345C       76.87      76.96     435            Chesuncook-Telos association     3-15        very stony        moderately     firm glacial till  \>60         .5-2.5      .24-.32     slight            N
                                                                                                                well to                                                                                  
                                                                                                                somewhat                                                                                 
                                                                                                                poorly drained                                                                           

  348B       76.96      77.06     533            Monarda-Telos association        0-8         very stony        somewhat       dense glacial till \>60         0-1.5       .15-.32     slight            Y
                                                                                                                poorly to                                                                                
                                                                                                                poorly drained                                                                           

  345B       77.06      77.20     747            Telos-Chesuncook association     0-8         very stony        moderately     firm glacial till  \>60         .5-2.5      .24-.32     slight            N
                                                                                                                well to                                                                                  
                                                                                                                somewhat                                                                                 
                                                                                                                poorly drained                                                                           

  340B       77.20      77.34     763            Telos-Elliottsville-Monarda      0-8         very stony        well drained   firm glacial till  20-40        0-1.5       .15-.32     slight to         Y
                                                 complex                                                        to poorly                                                              moderate          
                                                                                                                drained                                                                                  

  345B       77.34      77.43     431            Telos-Chesuncook association     0-8         very stony        moderately     firm glacial till  \>60         .5-2.5      .24-.32     slight            N
                                                                                                                well to                                                                                  
                                                                                                                somewhat                                                                                 
                                                                                                                poorly drained                                                                           

  340C       77.43      77.46     208            Chesuncook-Elliottsville-Telos   3-15        very stony        moderately     firm glacial till  20-40        0-1.5       .15-.32     slight to         Y
                                                 complex                                                        well to                                                                moderate          
                                                                                                                somewhat                                                                                 
                                                                                                                poorly drained                                                                           

  340B       77.46      77.59     644            Telos-Elliottsville-Monarda      0-8         very stony        well drained   firm glacial till  20-40        0-1.5       .15-.32     slight to         Y
                                                 complex                                                        to poorly                                                              moderate          
                                                                                                                drained                                                                                  

  348B       77.59      77.67     443            Monarda-Telos association        0-8         very stony        somewhat       dense glacial till \>60         0-1.5       .15-.32     slight            Y
                                                                                                                poorly to                                                                                
                                                                                                                poorly drained                                                                           

  340C       77.67      77.76     464            Chesuncook-Elliottsville-Telos   3-15        very stony        moderately     firm glacial till  20-40        0-1.5       .15-.32     slight to         Y
                                                 complex                                                        well to                                                                moderate          
                                                                                                                somewhat                                                                                 
                                                                                                                poorly drained                                                                           

  348B       77.76      77.83     392            Monarda-Telos association        0-8         very stony        somewhat       dense glacial till \>60         0-1.5       .15-.32     slight            Y
                                                                                                                poorly to                                                                                
                                                                                                                poorly drained                                                                           

  340C       77.83      77.91     402            Chesuncook-Elliottsville-Telos   3-15        very stony        moderately     firm glacial till  20-40        0-1.5       .15-.32     slight to         Y
                                                 complex                                                        well to                                                                moderate          
                                                                                                                somewhat                                                                                 
                                                                                                                poorly drained                                                                           

  348B       77.91      78.21     1606           Monarda-Telos association        0-8         very stony        somewhat       dense glacial till \>60         0-1.5       .15-.32     slight            Y
                                                                                                                poorly to                                                                                
                                                                                                                poorly drained                                                                           

  345B       78.21      78.53     1661           Telos-Chesuncook association     0-8         very stony        moderately     firm glacial till  \>60         .5-2.5      .24-.32     slight            N
                                                                                                                well to                                                                                  
                                                                                                                somewhat                                                                                 
                                                                                                                poorly drained                                                                           

  348B       78.53      78.83     1594           Monarda-Telos association        0-8         very stony        somewhat       dense glacial till \>60         0-1.5       .15-.32     slight            Y
                                                                                                                poorly to                                                                                
                                                                                                                poorly drained                                                                           

  345B       78.83      78.97     736            Telos-Chesuncook association     0-8         very stony        moderately     firm glacial till  \>60         .5-2.5      .24-.32     slight            N
                                                                                                                well to                                                                                  
                                                                                                                somewhat                                                                                 
                                                                                                                poorly drained                                                                           

  348B       78.97      79.00     161            Monarda-Telos association        0-8         very stony        somewhat       dense glacial till \>60         0-1.5       .15-.32     slight            Y
                                                                                                                poorly to                                                                                
                                                                                                                poorly drained                                                                           

  345B       79.00      79.07     355            Telos-Chesuncook association     0-8         very stony        moderately     firm glacial till  \>60         .5-2.5      .24-.32     slight            N
                                                                                                                well to                                                                                  
                                                                                                                somewhat                                                                                 
                                                                                                                poorly drained                                                                           

  348B       79.07      79.27     1098           Monarda-Telos association        0-8         very stony        somewhat       dense glacial till \>60         0-1.5       .15-.32     slight            Y
                                                                                                                poorly to                                                                                
                                                                                                                poorly drained                                                                           

  340B       79.27      79.39     614            Telos-Elliottsville-Monarda      0-8         very stony        well drained   firm glacial till  20-40        0-1.5       .15-.32     slight to         Y
                                                 complex                                                        to poorly                                                              moderate          
                                                                                                                drained                                                                                  

  348B       79.39      79.93     2857           Monarda-Telos association        0-8         very stony        somewhat       dense glacial till \>60         0-1.5       .15-.32     slight            Y
                                                                                                                poorly to                                                                                
                                                                                                                poorly drained                                                                           

  345B       79.93      80.08     785            Telos-Chesuncook association     0-8         very stony        moderately     firm glacial till  \>60         .5-2.5      .24-.32     slight            N
                                                                                                                well to                                                                                  
                                                                                                                somewhat                                                                                 
                                                                                                                poorly drained                                                                           

  348B       80.08      80.21     703            Monarda-Telos association        0-8         very stony        somewhat       dense glacial till \>60         0-1.5       .15-.32     slight            Y
                                                                                                                poorly to                                                                                
                                                                                                                poorly drained                                                                           

  345B       80.21      80.31     485            Telos-Chesuncook association     0-8         very stony        moderately     firm glacial till  \>60         .5-2.5      .24-.32     slight            N
                                                                                                                well to                                                                                  
                                                                                                                somewhat                                                                                 
                                                                                                                poorly drained                                                                           

  348B       80.31      80.41     565            Monarda-Telos association        0-8         very stony        somewhat       dense glacial till \>60         0-1.5       .15-.32     slight            Y
                                                                                                                poorly to                                                                                
                                                                                                                poorly drained                                                                           

  345B       80.41      80.50     438            Telos-Chesuncook association     0-8         very stony        moderately     firm glacial till  \>60         .5-2.5      .24-.32     slight            N
                                                                                                                well to                                                                                  
                                                                                                                somewhat                                                                                 
                                                                                                                poorly drained                                                                           

  348B       80.50      80.61     623            Monarda-Telos association        0-8         very stony        somewhat       dense glacial till \>60         0-1.5       .15-.32     slight            Y
                                                                                                                poorly to                                                                                
                                                                                                                poorly drained                                                                           

  345B       80.61      80.79     922            Telos-Chesuncook association     0-8         very stony        moderately     firm glacial till  \>60         .5-2.5      .24-.32     slight            N
                                                                                                                well to                                                                                  
                                                                                                                somewhat                                                                                 
                                                                                                                poorly drained                                                                           

  348B       80.79      80.84     300            Monarda-Telos association        0-8         very stony        somewhat       dense glacial till \>60         0-1.5       .15-.32     slight            Y
                                                                                                                poorly to                                                                                
                                                                                                                poorly drained                                                                           

  39P        80.84      81.04     1015           Bucksport and Wonsqueak          0-2         N/A               very poorly    decomposed organic \>60         +1.0-0.5    0.49        slight            Y
                                                                                                                drained        materials                                                                 

  343B       81.04      81.18     749            not described                    0-8         not described     not described  not described      not          not         not         not described     not
                                                                                                                                                  described    described   described                     described

  344C       81.18      81.47     1539           Danforth-Elliottsville complex   3-15        very stony        well drained   glacial till       20-40        \>6         .15-.28     slight to         N
                                                                                                                                                                                       moderate          

  343B       81.47      81.68     1087           not described                    0-8         not described     not described  not described      not          not         not         not described     not
                                                                                                                                                  described    described   described                     described

  380C       81.68      81.82     777            Masardis-Sheepscot complex       0-15        gravelly fine     moderately     glaciofluvial      \>60         1.5-3.0     .10-.17     slight            N
                                                                                              sandy loam        well to        sands and gravels                                                         
                                                                                                                somewhat                                                                                 
                                                                                                                excessively                                                                              
                                                                                                                drained                                                                                  

  Gravel Pit 81.82      81.89     354            Gravel Pit                       N/A         N/A               N/A            N/A                N/A          N/A         N/A         N/A               N/A

  316C       81.89      81.99     547            not described                    not         not described     not described  not described      not          not         not         not described     not
                                                                                  described                                                       described    described   described                     described

  39M        81.99      82.20     1064           Wonsqueak and Bucksport:         0-2         N/A               very poorly    decomposed organic \>60         +1.0-0.5    0.49        slight            Y
                                                 frequently flooded                                             drained        materials                                                                 

  348B       82.20      82.23     180            Monarda-Telos association        0-8         very stony        somewhat       dense glacial till \>60         0-1.5       .15-.32     slight            Y
                                                                                                                poorly to                                                                                
                                                                                                                poorly drained                                                                           

  345B       82.23      82.30     394            Telos-Chesuncook association     0-8         very stony        moderately     firm glacial till  \>60         .5-2.5      .24-.32     slight            N
                                                                                                                well to                                                                                  
                                                                                                                somewhat                                                                                 
                                                                                                                poorly drained                                                                           

  348B       82.30      82.36     290            Monarda-Telos association        0-8         very stony        somewhat       dense glacial till \>60         0-1.5       .15-.32     slight            Y
                                                                                                                poorly to                                                                                
                                                                                                                poorly drained                                                                           

  345B       82.36      82.48     621            Telos-Chesuncook association     0-8         very stony        moderately     firm glacial till  \>60         .5-2.5      .24-.32     slight            N
                                                                                                                well to                                                                                  
                                                                                                                somewhat                                                                                 
                                                                                                                poorly drained                                                                           

  348B       82.48      82.54     326            Monarda-Telos association        0-8         very stony        somewhat       dense glacial till \>60         0-1.5       .15-.32     slight            Y
                                                                                                                poorly to                                                                                
                                                                                                                poorly drained                                                                           

  345B       82.54      82.84     1580           Telos-Chesuncook association     0-8         very stony        moderately     firm glacial till  \>60         .5-2.5      .24-.32     slight            N
                                                                                                                well to                                                                                  
                                                                                                                somewhat                                                                                 
                                                                                                                poorly drained                                                                           

  345C       82.84      82.91     365            Chesuncook-Telos association     3-15        very stony        moderately     firm glacial till  \>60         .5-2.5      .24-.32     slight            N
                                                                                                                well to                                                                                  
                                                                                                                somewhat                                                                                 
                                                                                                                poorly drained                                                                           

  348B       82.91      82.95     249            Monarda-Telos association        0-8         very stony        somewhat       dense glacial till \>60         0-1.5       .15-.32     slight            Y
                                                                                                                poorly to                                                                                
                                                                                                                poorly drained                                                                           

  345C       82.95      83.01     284            Chesuncook-Telos association     3-15        very stony        moderately     firm glacial till  \>60         .5-2.5      .24-.32     slight            N
                                                                                                                well to                                                                                  
                                                                                                                somewhat                                                                                 
                                                                                                                poorly drained                                                                           

  345B       83.01      83.15     774            Telos-Chesuncook association     0-8         very stony        moderately     firm glacial till  \>60         .5-2.5      .24-.32     slight            N
                                                                                                                well to                                                                                  
                                                                                                                somewhat                                                                                 
                                                                                                                poorly drained                                                                           

  345C       83.15      83.30     777            Chesuncook-Telos association     3-15        very stony        moderately     firm glacial till  \>60         .5-2.5      .24-.32     slight            N
                                                                                                                well to                                                                                  
                                                                                                                somewhat                                                                                 
                                                                                                                poorly drained                                                                           

  345B       83.30      83.38     400            Telos-Chesuncook association     0-8         very stony        moderately     firm glacial till  \>60         .5-2.5      .24-.32     slight            N
                                                                                                                well to                                                                                  
                                                                                                                somewhat                                                                                 
                                                                                                                poorly drained                                                                           

  39M        83.38      83.44     305            Wonsqueak and Bucksport:         0-2         N/A               very poorly    decomposed organic \>60         +1.0-0.5    0.49        slight            Y
                                                 frequently flooded                                             drained        materials                                                                 

  332B       83.44      83.53     498            Lamoine-Buxton-Scantic complex   0-15        N/A               moderately to  glaciomarine       \>60         +1.0-3.0    .32-.49     slight            Y
                                                                                                                poorly drained deposits                                                                  

  345C       83.53      83.68     821            Chesuncook-Telos association     3-15        very stony        moderately     firm glacial till  \>60         .5-2.5      .24-.32     slight            N
                                                                                                                well to                                                                                  
                                                                                                                somewhat                                                                                 
                                                                                                                poorly drained                                                                           

  332B       83.68      83.71     108            Lamoine-Buxton-Scantic complex   0-15        N/A               moderately to  glaciomarine       \>60         +1.0-3.0    .32-.49     slight            Y
                                                                                                                poorly drained deposits                                                                  

  333A       83.71      83.73     140            Scantic-Biddeford association    0-3         N/A               poorly to very glaciolacustrine   \>60         +1.0-1.0    .32-.49     slight            Y
                                                                                                                poorly drained and glaciomarine                                                          
                                                                                                                               sediments                                                                 

  332B       83.73      83.87     735            Lamoine-Buxton-Scantic complex   0-15        N/A               moderately to  glaciomarine       \>60         +1.0-3.0    .32-.49     slight            Y
                                                                                                                poorly drained deposits                                                                  

  345C       83.87      84.06     1000           Chesuncook-Telos association     3-15        very stony        moderately     firm glacial till  \>60         .5-2.5      .24-.32     slight            N
                                                                                                                well to                                                                                  
                                                                                                                somewhat                                                                                 
                                                                                                                poorly drained                                                                           

  345B       84.06      84.16     502            Telos-Chesuncook association     0-8         very stony        moderately     firm glacial till  \>60         .5-2.5      .24-.32     slight            N
                                                                                                                well to                                                                                  
                                                                                                                somewhat                                                                                 
                                                                                                                poorly drained                                                                           

  345C       84.16      84.25     498            Chesuncook-Telos association     3-15        very stony        moderately     firm glacial till  \>60         .5-2.5      .24-.32     slight            N
                                                                                                                well to                                                                                  
                                                                                                                somewhat                                                                                 
                                                                                                                poorly drained                                                                           
  ------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------

**APPENDIX 11-4**

**CUMULATIVE SUMMARY OF SOILS ALONG ROUTE**

**APPENDIX 11-4**

**NORTHEAST RELIABILITY INTERCONNECT**

**CUMMULATIVE SUMMARY OF SOILS ALONG ROUTE**

<table>
<colgroup>
<col style="width: 8%" />
<col style="width: 12%" />
<col style="width: 9%" />
<col style="width: 9%" />
<col style="width: 9%" />
<col style="width: 9%" />
<col style="width: 9%" />
<col style="width: 8%" />
<col style="width: 11%" />
<col style="width: 11%" />
</colgroup>
<thead>
<tr class="header">
<th><strong>Map Unit Symbol</strong></th>
<th><strong>Map Unit Name</strong></th>
<th><strong>Range of Slope (%)</strong></th>
<th><p><strong>Hydric Soil</strong></p>
<p><strong>(Y or N)</strong></p></th>
<th><strong>Erosion Hazard</strong></th>
<th><strong>Depth to Bedrock (inches)</strong></th>
<th><strong>From (mile post)</strong></th>
<th><strong>To (mile post)</strong></th>
<th><strong>Map Unit Traverse Distance (feet)</strong></th>
<th rowspan="2"><em><strong>Percent of Total Measured
Distance</strong></em></th>
</tr>
<tr class="odd">
<th><strong> </strong></th>
<th><strong> </strong></th>
<th><strong> </strong></th>
<th><strong> </strong></th>
<th><strong> </strong></th>
<th><strong> </strong></th>
<th><strong> </strong></th>
<th><strong> </strong></th>
<th><em><strong>Total Distance (feet)</strong></em></th>
</tr>
</thead>
<tbody>
<tr class="odd">
<td><strong>BaB</strong></td>
<td>Bangor</td>
<td>2-8</td>
<td>N</td>
<td>Slight</td>
<td>&gt;60</td>
<td>7.46</td>
<td>7.51</td>
<td>268</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>268</strong></em></td>
<td><em><strong>0.16%</strong></em></td>
</tr>
<tr class="odd">
<td><strong>BaC</strong></td>
<td>Bangor</td>
<td>8-15</td>
<td>N</td>
<td>Slight</td>
<td>&gt;60</td>
<td>7.42</td>
<td>7.46</td>
<td>204</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>204</strong></em></td>
<td><em><strong>0.12%</strong></em></td>
</tr>
<tr class="odd">
<td><strong>BnB</strong></td>
<td>Bangor</td>
<td>0-8</td>
<td>N</td>
<td>Slight</td>
<td>&gt;60</td>
<td>7.21</td>
<td>7.27</td>
<td>329</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>7.51</td>
<td>7.64</td>
<td>668</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>19.14</td>
<td>19.31</td>
<td>876</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>1874</strong></em></td>
<td><em><strong>1.11%</strong></em></td>
</tr>
<tr class="odd">
<td><strong>BnC</strong></td>
<td>Bangor</td>
<td>8-15</td>
<td>N</td>
<td>Slight</td>
<td>&gt;60</td>
<td>0.14</td>
<td>0.22</td>
<td>446</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>0.55</td>
<td>0.73</td>
<td>930</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>5.14</td>
<td>5.22</td>
<td>432</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>1807</strong></em></td>
<td><em><strong>1.07%</strong></em></td>
</tr>
<tr class="odd">
<td><strong>BnD</strong></td>
<td>Bangor</td>
<td>15-25</td>
<td>N</td>
<td>Slight</td>
<td>&gt;60</td>
<td>5.22</td>
<td>5.25</td>
<td>164</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>5.31</td>
<td>5.39</td>
<td>421</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>5.66</td>
<td>5.73</td>
<td>369</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>5.79</td>
<td>5.84</td>
<td>307</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>1261</strong></em></td>
<td><em><strong>0.75%</strong></em></td>
</tr>
<tr class="even">
<td><strong>BoA</strong></td>
<td>Biddeford</td>
<td>0-3</td>
<td>Y</td>
<td>Slight</td>
<td>&gt;60</td>
<td>0.95</td>
<td>1.59</td>
<td>3417</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>2.73</td>
<td>2.84</td>
<td>578</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>2.96</td>
<td>3.07</td>
<td>584</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>3.39</td>
<td>3.50</td>
<td>618</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>4.54</td>
<td>4.62</td>
<td>383</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>5.58</td>
<td>5.66</td>
<td>422</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>5.73</td>
<td>5.79</td>
<td>286</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>8.20</td>
<td>8.41</td>
<td>1127</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>8.52</td>
<td>8.67</td>
<td>797</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>9.06</td>
<td>9.19</td>
<td>701</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>9.30</td>
<td>9.44</td>
<td>786</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>10.10</td>
<td>10.15</td>
<td>269</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>10.31</td>
<td>10.59</td>
<td>1446</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>10.69</td>
<td>10.81</td>
<td>616</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>11.06</td>
<td>11.08</td>
<td>101</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>11.32</td>
<td>11.47</td>
<td>788</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>11.63</td>
<td>11.73</td>
<td>532</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>13.17</td>
<td>13.34</td>
<td>906</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td colspan="6">(BoA continued…)</td>
<td>17.44</td>
<td>17.53</td>
<td>467</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>17.63</td>
<td>17.68</td>
<td>293</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>21.58</td>
<td>21.90</td>
<td>1695</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>16810</strong></em></td>
<td><em><strong>9.97%</strong></em></td>
</tr>
<tr class="even">
<td><strong>BuA</strong></td>
<td>Buxton</td>
<td>0-2</td>
<td>N</td>
<td>Slight</td>
<td>&gt;60</td>
<td>0.00</td>
<td>0.03</td>
<td>182</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>3.07</td>
<td>3.12</td>
<td>248</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>4.28</td>
<td>4.30</td>
<td>106</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>4.32</td>
<td>4.39</td>
<td>357</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>4.64</td>
<td>4.69</td>
<td>281</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>4.73</td>
<td>4.96</td>
<td>1168</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>5.50</td>
<td>5.52</td>
<td>140</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>6.25</td>
<td>6.40</td>
<td>802</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>6.82</td>
<td>6.85</td>
<td>146</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>9.19</td>
<td>9.30</td>
<td>554</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>9.44</td>
<td>9.50</td>
<td>291</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>9.98</td>
<td>10.04</td>
<td>313</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>4588</strong></em></td>
<td><em><strong>2.72%</strong></em></td>
</tr>
<tr class="odd">
<td><strong>BuB</strong></td>
<td>Buxton</td>
<td>2-8</td>
<td>N</td>
<td>Slight</td>
<td>&gt;60</td>
<td>1.59</td>
<td>1.76</td>
<td>866</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>1.97</td>
<td>2.07</td>
<td>502</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>2.10</td>
<td>2.13</td>
<td>169</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>3.31</td>
<td>3.39</td>
<td>399</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>4.15</td>
<td>4.28</td>
<td>688</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>4.39</td>
<td>4.51</td>
<td>640</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>9.63</td>
<td>9.72</td>
<td>446</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>3709</strong></em></td>
<td><em><strong>2.20%</strong></em></td>
</tr>
<tr class="odd">
<td><strong>BuC</strong></td>
<td>Buxton</td>
<td>8-15</td>
<td>N</td>
<td>Slight</td>
<td>&gt;60</td>
<td>1.93</td>
<td>1.97</td>
<td>217</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>2.07</td>
<td>2.10</td>
<td>194</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>410</strong></em></td>
<td><em><strong>0.24%</strong></em></td>
</tr>
<tr class="even">
<td><strong>BxB</strong></td>
<td>Buxton, Scantic, &amp; Biddeford</td>
<td>0-8</td>
<td>Y</td>
<td> </td>
<td>&gt;60</td>
<td>3.72</td>
<td>3.78</td>
<td>295</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td>Slight</td>
<td> </td>
<td>4.12</td>
<td>4.15</td>
<td>180</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>4.30</td>
<td>4.32</td>
<td>89</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>5.10</td>
<td>5.14</td>
<td>212</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>5.39</td>
<td>5.42</td>
<td>144</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>5.84</td>
<td>5.97</td>
<td>678</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>6.05</td>
<td>6.25</td>
<td>1085</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>6.40</td>
<td>6.50</td>
<td>530</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td colspan="6"><strong> </strong>(BxB Continued…)</td>
<td>7.02</td>
<td>7.05</td>
<td>143</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>7.87</td>
<td>8.20</td>
<td>1733</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>8.41</td>
<td>8.46</td>
<td>259</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>8.67</td>
<td>9.06</td>
<td>2059</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>10.59</td>
<td>10.69</td>
<td>566</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>10.81</td>
<td>11.01</td>
<td>1060</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>11.08</td>
<td>11.17</td>
<td>496</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>11.73</td>
<td>11.75</td>
<td>65</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>13.76</td>
<td>13.97</td>
<td>1110</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>14.11</td>
<td>14.19</td>
<td>426</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>14.90</td>
<td>15.03</td>
<td>637</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>15.47</td>
<td>15.87</td>
<td>2095</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>16.91</td>
<td>16.98</td>
<td>414</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>19.38</td>
<td>19.47</td>
<td>466</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>19.62</td>
<td>19.69</td>
<td>332</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>20.09</td>
<td>20.14</td>
<td>232</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>20.18</td>
<td>20.32</td>
<td>769</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>20.35</td>
<td>20.67</td>
<td>1691</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>21.90</td>
<td>21.94</td>
<td>223</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>22.01</td>
<td>22.04</td>
<td>141</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>18,129</strong></em></td>
<td><em><strong>10.75%</strong></em></td>
</tr>
<tr class="odd">
<td><strong>CnB</strong></td>
<td>Colton</td>
<td>2-8</td>
<td>N</td>
<td>Slight</td>
<td>&gt;60</td>
<td>18.25</td>
<td>18.39</td>
<td>729</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>729</strong></em></td>
<td><em><strong>0.43%</strong></em></td>
</tr>
<tr class="odd">
<td><strong>CnC</strong></td>
<td>Colton</td>
<td>8-15</td>
<td>N</td>
<td>Slight</td>
<td>&gt;60</td>
<td>18.39</td>
<td>18.44</td>
<td>259</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>259</strong></em></td>
<td><em><strong>0.15%</strong></em></td>
</tr>
<tr class="odd">
<td><strong>DyB</strong></td>
<td>Dixmont</td>
<td>2-8</td>
<td>N</td>
<td>Slight</td>
<td>&gt;60</td>
<td>0.83</td>
<td>0.95</td>
<td>591</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>591</strong></em></td>
<td><em><strong>0.35%</strong></em></td>
</tr>
<tr class="odd">
<td><strong>DyC</strong></td>
<td>Dixmont</td>
<td>8-15</td>
<td>N</td>
<td>Slight</td>
<td>&gt;60</td>
<td>5.97</td>
<td>5.99</td>
<td>103</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>103</strong></em></td>
<td><em><strong>0.06%</strong></em></td>
</tr>
<tr class="odd">
<td><strong>Gravel Pit</strong></td>
<td>Gravel Pit</td>
<td>N/A</td>
<td>N/A</td>
<td>Slight</td>
<td>&gt;60</td>
<td>81.82</td>
<td>81.89</td>
<td>354</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>354</strong></em></td>
<td><em><strong>0.21%</strong></em></td>
</tr>
<tr class="odd">
<td><strong>HvB</strong></td>
<td>Howland</td>
<td>0-8</td>
<td>N</td>
<td>Slight</td>
<td>&gt;60</td>
<td>3.50</td>
<td>3.72</td>
<td>1172</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>12.57</td>
<td>12.65</td>
<td>383</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>12.90</td>
<td>12.96</td>
<td>315</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>13.44</td>
<td>13.60</td>
<td>805</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>14.68</td>
<td>14.90</td>
<td>1187</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>15.03</td>
<td>15.16</td>
<td>720</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>15.87</td>
<td>15.96</td>
<td>485</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>16.74</td>
<td>16.91</td>
<td>850</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>19.58</td>
<td>19.62</td>
<td>249</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>19.69</td>
<td>19.78</td>
<td>487</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>20.83</td>
<td>21.04</td>
<td>1093</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>21.27</td>
<td>21.38</td>
<td>568</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>21.45</td>
<td>21.50</td>
<td>240</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>22.04</td>
<td>22.09</td>
<td>269</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>8823</strong></em></td>
<td><em><strong>5.23%</strong></em></td>
</tr>
<tr class="even">
<td><strong>HvC</strong></td>
<td>Howland</td>
<td>8-15</td>
<td>N</td>
<td>Slight</td>
<td>&gt;60</td>
<td>0.73</td>
<td>0.83</td>
<td>569</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>18.44</td>
<td>18.56</td>
<td>650</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>1219</strong></em></td>
<td><em><strong>0.72%</strong></em></td>
</tr>
<tr class="odd">
<td><strong>Lk</strong></td>
<td>Limerick (Charles)</td>
<td>Nearly level</td>
<td>Y</td>
<td>Moderate to severe</td>
<td>&gt;60</td>
<td>12.03</td>
<td>12.06</td>
<td>200</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>200</strong></em></td>
<td><em><strong>0.12%</strong></em></td>
</tr>
<tr class="odd">
<td><strong>MaB</strong></td>
<td>Howland</td>
<td>8-15</td>
<td>N</td>
<td>Slight</td>
<td> </td>
<td>17.15</td>
<td>17.33</td>
<td>957</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>18.01</td>
<td>18.25</td>
<td>1279</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>18.83</td>
<td>19.00</td>
<td>907</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>20.32</td>
<td>20.35</td>
<td>160</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>3302</strong></em></td>
<td><em><strong>1.96%</strong></em></td>
</tr>
<tr class="even">
<td><strong>MrB</strong></td>
<td>Monarda &amp; Burnham</td>
<td>0-8</td>
<td>Y</td>
<td>Slight</td>
<td>&gt;60</td>
<td>7.39</td>
<td>7.42</td>
<td>190</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>7.64</td>
<td>7.87</td>
<td>1209</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>12.39</td>
<td>12.49</td>
<td>480</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>12.65</td>
<td>12.84</td>
<td>1040</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>12.96</td>
<td>13.06</td>
<td>502</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>13.60</td>
<td>13.76</td>
<td>874</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>14.19</td>
<td>14.48</td>
<td>1550</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>15.96</td>
<td>16.13</td>
<td>882</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>16.23</td>
<td>16.34</td>
<td>597</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>17.33</td>
<td>17.44</td>
<td>586</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>19.47</td>
<td>19.58</td>
<td>546</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td colspan="6">(MrB Continued…)</td>
<td>19.78</td>
<td>19.83</td>
<td>257</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>19.86</td>
<td>19.92</td>
<td>273</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>20.67</td>
<td>20.83</td>
<td>847</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>21.12</td>
<td>21.27</td>
<td>775</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>21.50</td>
<td>21.58</td>
<td>434</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>11,041</strong></em></td>
<td><em><strong>6.55%</strong></em></td>
</tr>
<tr class="odd">
<td><strong>MsC</strong></td>
<td>Monarda &amp; Burnham</td>
<td>0-15</td>
<td>Y</td>
<td>Slight</td>
<td>&gt;60</td>
<td>6.90</td>
<td>7.02</td>
<td>644</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>11.01</td>
<td>11.06</td>
<td>239</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>11.75</td>
<td>11.79</td>
<td>222</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>12.17</td>
<td>12.26</td>
<td>491</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>12.32</td>
<td>12.39</td>
<td>382</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>19.36</td>
<td>19.38</td>
<td>132</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>2110</strong></em></td>
<td><em><strong>1.25%</strong></em></td>
</tr>
<tr class="even">
<td><strong>Mu</strong></td>
<td>muck</td>
<td>N/A</td>
<td>Y</td>
<td>N/A</td>
<td>N/A</td>
<td>11.47</td>
<td>11.63</td>
<td>871</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>871</strong></em></td>
<td><em><strong>0.52%</strong></em></td>
</tr>
<tr class="even">
<td><strong>Pa</strong></td>
<td>Peat &amp; Muck</td>
<td>N/A</td>
<td>Y</td>
<td>N/A</td>
<td>N/A</td>
<td>17.53</td>
<td>17.63</td>
<td>520</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>520</strong></em></td>
<td><em><strong>0.31%</strong></em></td>
</tr>
<tr class="even">
<td><strong>PgB</strong></td>
<td>Plaisted</td>
<td>2-8</td>
<td>N</td>
<td>Slight</td>
<td>&gt;60</td>
<td>2.84</td>
<td>2.92</td>
<td>432</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>432</strong></em></td>
<td><em><strong>0.26%</strong></em></td>
</tr>
<tr class="even">
<td><strong>PgC</strong></td>
<td>Plaisted</td>
<td>8-15</td>
<td>N</td>
<td>Slight to moderate</td>
<td>&gt;60</td>
<td>5.25</td>
<td>5.31</td>
<td>304</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>304</strong></em></td>
<td><em><strong>0.18%</strong></em></td>
</tr>
<tr class="even">
<td><strong>PrC</strong></td>
<td>Plaisted</td>
<td>5-15</td>
<td>N</td>
<td>Slight</td>
<td>&gt;60</td>
<td>3.78</td>
<td>4.12</td>
<td>1787</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>8.46</td>
<td>8.52</td>
<td>315</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>12.84</td>
<td>12.90</td>
<td>323</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>13.06</td>
<td>13.17</td>
<td>598</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>13.34</td>
<td>13.44</td>
<td>538</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>13.97</td>
<td>14.11</td>
<td>714</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>16.13</td>
<td>16.23</td>
<td>517</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>16.34</td>
<td>16.74</td>
<td>2144</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>19.92</td>
<td>20.09</td>
<td>938</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>7874</strong></em></td>
<td><em><strong>4.67%</strong></em></td>
</tr>
<tr class="even">
<td><strong>PrE</strong></td>
<td>Plaisted</td>
<td>15-45</td>
<td>N</td>
<td>Moderate to severe</td>
<td>&gt;60</td>
<td>5.99</td>
<td>6.05</td>
<td>280</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>7.27</td>
<td>7.39</td>
<td>606</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>885</strong></em></td>
<td><em><strong>0.52%</strong></em></td>
</tr>
<tr class="odd">
<td><strong>RaB</strong></td>
<td>Red Hook &amp; Atherton</td>
<td>0-8</td>
<td>Y</td>
<td>Slight</td>
<td> </td>
<td>16.98</td>
<td>17.15</td>
<td>868</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>17.68</td>
<td>18.01</td>
<td>1727</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>2595</strong></em></td>
<td><em><strong>1.54%</strong></em></td>
</tr>
<tr class="even">
<td><strong>RmC</strong></td>
<td>Rockland &amp; Thorndike</td>
<td>sloping</td>
<td>N</td>
<td>Slight to moderate</td>
<td>0-12</td>
<td>11.86</td>
<td>11.95</td>
<td>513</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>12.06</td>
<td>12.10</td>
<td>214</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>19.31</td>
<td>19.36</td>
<td>270</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>998</strong></em></td>
<td><em><strong>0.59%</strong></em></td>
</tr>
<tr class="even">
<td><strong>RmD</strong></td>
<td>Rockland &amp; Thorndike</td>
<td>Strongly sloping</td>
<td>N</td>
<td>Slight to moderate</td>
<td>0-12</td>
<td>11.79</td>
<td>11.86</td>
<td>354</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>11.95</td>
<td>12.01</td>
<td>321</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>12.10</td>
<td>12.17</td>
<td>352</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>1027</strong></em></td>
<td><em><strong>0.61%</strong></em></td>
</tr>
<tr class="even">
<td><strong>Sa</strong></td>
<td>Saco (Medomak)</td>
<td>Nearly level</td>
<td>Y</td>
<td>Moderate to severe</td>
<td>&gt;60</td>
<td>9.72</td>
<td>9.77</td>
<td>283</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>9.79</td>
<td>9.80</td>
<td>85</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>15.41</td>
<td>15.47</td>
<td>346</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>20.14</td>
<td>20.18</td>
<td>212</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>925</strong></em></td>
<td><em><strong>0.55%</strong></em></td>
</tr>
<tr class="odd">
<td><strong>ScB</strong></td>
<td>Scantic</td>
<td>0-8</td>
<td>Y</td>
<td>Slight</td>
<td>&gt;60</td>
<td>0.22</td>
<td>0.55</td>
<td>1730</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>1.76</td>
<td>1.93</td>
<td>908</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>2.68</td>
<td>2.73</td>
<td>274</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>4.96</td>
<td>5.10</td>
<td>752</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>6.50</td>
<td>6.82</td>
<td>1699</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>6.85</td>
<td>6.90</td>
<td>238</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>9.50</td>
<td>9.63</td>
<td>702</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>10.15</td>
<td>10.31</td>
<td>881</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>11.17</td>
<td>11.32</td>
<td>783</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>12.49</td>
<td>12.57</td>
<td>461</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>14.48</td>
<td>14.68</td>
<td>1040</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>15.16</td>
<td>15.29</td>
<td>696</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>10,165</strong></em></td>
<td><em><strong>6.03%</strong></em></td>
</tr>
<tr class="even">
<td><strong>SeB</strong></td>
<td>Stetson</td>
<td>2-8</td>
<td>N</td>
<td>Slight</td>
<td>&gt;60</td>
<td>0.03</td>
<td>0.14</td>
<td>549</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>549</strong></em></td>
<td><em><strong>0.33%</strong></em></td>
</tr>
<tr class="even">
<td><strong>SfC</strong></td>
<td>Stetson &amp; Suffield</td>
<td>0-15</td>
<td>N</td>
<td>Moderate</td>
<td>&gt;60</td>
<td>18.56</td>
<td>18.83</td>
<td>1400</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>19.00</td>
<td>19.14</td>
<td>757</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>2157</strong></em></td>
<td><em><strong>1.28%</strong></em></td>
</tr>
<tr class="odd">
<td><strong>stream</strong></td>
<td>N/A</td>
<td>N/A</td>
<td>N/A</td>
<td>Slight</td>
<td>&gt;60</td>
<td>9.77</td>
<td>9.79</td>
<td>92</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>12.01</td>
<td>12.03</td>
<td>70</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>15.38</td>
<td>15.41</td>
<td>157</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>319</strong></em></td>
<td><em><strong>0.19%</strong></em></td>
</tr>
<tr class="odd">
<td><strong>SuB</strong></td>
<td>Suffield</td>
<td>2-8</td>
<td>N</td>
<td>Slight</td>
<td>&gt;60</td>
<td>2.13</td>
<td>2.68</td>
<td>2884</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>2.92</td>
<td>2.96</td>
<td>211</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>3.12</td>
<td>3.31</td>
<td>1001</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>4.51</td>
<td>4.54</td>
<td>177</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>4.62</td>
<td>4.64</td>
<td>132</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>4.69</td>
<td>4.73</td>
<td>216</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>5.52</td>
<td>5.58</td>
<td>316</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>9.86</td>
<td>9.98</td>
<td>603</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>10.04</td>
<td>10.10</td>
<td>310</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>5849</strong></em></td>
<td><em><strong>3.47%</strong></em></td>
</tr>
<tr class="odd">
<td><strong>SuC2</strong></td>
<td>Suffield eroded</td>
<td>8-15</td>
<td>N</td>
<td>Moderate to severe</td>
<td>&gt;60</td>
<td>9.80</td>
<td>9.86</td>
<td>312</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>312</strong></em></td>
<td><em><strong>0.18%</strong></em></td>
</tr>
<tr class="odd">
<td><strong>SvC</strong></td>
<td>suffield</td>
<td>8-15</td>
<td>N</td>
<td>Moderate to severe</td>
<td>&gt;60</td>
<td>5.42</td>
<td>5.50</td>
<td>424</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>424</strong></em></td>
<td><em><strong>0.25%</strong></em></td>
</tr>
<tr class="odd">
<td><strong>TkB</strong></td>
<td>Thorndike</td>
<td>2-8</td>
<td>N</td>
<td>Slight to moderate</td>
<td>0-20</td>
<td>7.05</td>
<td>7.21</td>
<td>857</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>857</strong></em></td>
<td><em><strong>0.51%</strong></em></td>
</tr>
<tr class="odd">
<td><strong>TvB</strong></td>
<td>Thorndike</td>
<td>2-8</td>
<td>N</td>
<td>Slight to moderate</td>
<td>10-20</td>
<td>12.26</td>
<td>12.32</td>
<td>305</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>15.29</td>
<td>15.38</td>
<td>441</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>21.04</td>
<td>21.12</td>
<td>424</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>21.38</td>
<td>21.45</td>
<td>388</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>21.94</td>
<td>22.01</td>
<td>380</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>1939</strong></em></td>
<td><em><strong>1.15%</strong></em></td>
</tr>
<tr class="odd">
<td><strong>TvC</strong></td>
<td>Thorndike</td>
<td>8-15</td>
<td>N</td>
<td>Slight to moderate</td>
<td>10-20</td>
<td>19.83</td>
<td>19.86</td>
<td>197</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>197</strong></em></td>
<td><em><strong>0.12%</strong></em></td>
</tr>
<tr class="odd">
<td><strong>316C</strong></td>
<td>not described</td>
<td>not described</td>
<td>not described</td>
<td>Slight</td>
<td>&gt;60</td>
<td>81.89</td>
<td>81.99</td>
<td>547</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>547</strong></em></td>
<td><em><strong>0.32%</strong></em></td>
</tr>
<tr class="odd">
<td><strong>332B</strong></td>
<td>Lamoine-Buxton-Scantic complex</td>
<td>0-15</td>
<td>Y</td>
<td>Slight</td>
<td>&gt;60</td>
<td>83.44</td>
<td>83.53</td>
<td>498</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>83.68</td>
<td>83.71</td>
<td>108</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>83.73</td>
<td>83.87</td>
<td>735</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>1341</strong></em></td>
<td><em><strong>0.80%</strong></em></td>
</tr>
<tr class="odd">
<td><strong>333A</strong></td>
<td>Scantic-biddeford association</td>
<td>0-3</td>
<td>Y</td>
<td>Slight</td>
<td>&gt;60</td>
<td>83.71</td>
<td>83.73</td>
<td>140</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>140</strong></em></td>
<td><em><strong>0.08%</strong></em></td>
</tr>
<tr class="odd">
<td><strong>340B</strong></td>
<td>Telos-Elliottsville-Monarda complex</td>
<td>0-8</td>
<td>Y</td>
<td>Slight to moderate</td>
<td>20-40</td>
<td>74.39</td>
<td>74.50</td>
<td>562</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>74.57</td>
<td>74.60</td>
<td>159</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>76.46</td>
<td>76.78</td>
<td>1683</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>77.20</td>
<td>77.34</td>
<td>763</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>77.46</td>
<td>77.59</td>
<td>644</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>79.27</td>
<td>79.39</td>
<td>614</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>4425</strong></em></td>
<td><em><strong>2.62%</strong></em></td>
</tr>
<tr class="even">
<td><strong>340C</strong></td>
<td>Chesuncook-Elliottsville-Telos complex</td>
<td>3-15</td>
<td>Y</td>
<td>Slight to moderate</td>
<td>20-40</td>
<td>74.78</td>
<td>74.99</td>
<td>1093</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>75.04</td>
<td>75.53</td>
<td>2577</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>75.62</td>
<td>75.71</td>
<td>477</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>75.79</td>
<td>76.29</td>
<td>2674</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>77.43</td>
<td>77.46</td>
<td>208</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>77.67</td>
<td>77.76</td>
<td>464</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>77.83</td>
<td>77.91</td>
<td>402</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>7896</strong></em></td>
<td><em><strong>4.68%</strong></em></td>
</tr>
<tr class="even">
<td><strong>341C</strong></td>
<td>Elliotsville-Monson</td>
<td>3-15</td>
<td>N</td>
<td>Slight</td>
<td>10-40</td>
<td>75.53</td>
<td>75.62</td>
<td>476</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>75.71</td>
<td>75.79</td>
<td>400</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>876</strong></em></td>
<td><em><strong>0.52%</strong></em></td>
</tr>
<tr class="odd">
<td><strong>343B</strong></td>
<td>Not described</td>
<td>0-8</td>
<td>Not described</td>
<td>Not described</td>
<td>Not described</td>
<td>81.04</td>
<td>81.18</td>
<td>749</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>81.47</td>
<td>81.68</td>
<td>1087</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>1836</strong></em></td>
<td><em><strong>1.09%</strong></em></td>
</tr>
<tr class="even">
<td><strong>344C</strong></td>
<td>Danforth-Elliottsville complex</td>
<td>3-15</td>
<td>N</td>
<td>Slight to moderate</td>
<td>20-40</td>
<td>81.18</td>
<td>81.47</td>
<td>1539</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>1539</strong></em></td>
<td><em><strong>0.91%</strong></em></td>
</tr>
<tr class="even">
<td><strong>345B</strong></td>
<td>Telos-Chesuncook association</td>
<td>0-8</td>
<td>N</td>
<td>Slight</td>
<td>&gt;60</td>
<td>74.60</td>
<td>74.66</td>
<td>317</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>74.74</td>
<td>74.78</td>
<td>238</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>77.06</td>
<td>77.20</td>
<td>747</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>77.34</td>
<td>77.43</td>
<td>431</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>78.21</td>
<td>78.53</td>
<td>1661</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>78.83</td>
<td>78.97</td>
<td>736</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>79.00</td>
<td>79.07</td>
<td>355</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>79.93</td>
<td>80.08</td>
<td>785</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>80.21</td>
<td>80.31</td>
<td>485</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>80.41</td>
<td>80.50</td>
<td>438</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>80.61</td>
<td>80.79</td>
<td>922</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>82.23</td>
<td>82.30</td>
<td>394</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>82.36</td>
<td>82.48</td>
<td>621</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>82.54</td>
<td>82.84</td>
<td>1580</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>83.01</td>
<td>83.15</td>
<td>774</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>83.30</td>
<td>83.38</td>
<td>400</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>84.06</td>
<td>84.16</td>
<td>502</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>11,386</strong></em></td>
<td><em><strong>6.75%</strong></em></td>
</tr>
<tr class="even">
<td><strong>345C</strong></td>
<td>Chesuncook-Telos association</td>
<td>3-15</td>
<td>N</td>
<td>Slight</td>
<td>&gt;60</td>
<td>76.87</td>
<td>76.96</td>
<td>435</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>82.84</td>
<td>82.91</td>
<td>365</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>82.95</td>
<td>83.01</td>
<td>284</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>83.15</td>
<td>83.30</td>
<td>777</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>83.53</td>
<td>83.68</td>
<td>821</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>83.87</td>
<td>84.06</td>
<td>1000</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>84.16</td>
<td>84.25</td>
<td>498</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>4181</strong></em></td>
<td><em><strong>2.48%</strong></em></td>
</tr>
<tr class="even">
<td><strong>348B</strong></td>
<td>Monarda-Telos association</td>
<td>0-8</td>
<td>Y</td>
<td>Slight</td>
<td>&gt;60</td>
<td>74.50</td>
<td>74.57</td>
<td>379</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>74.99</td>
<td>75.04</td>
<td>278</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>76.29</td>
<td>76.46</td>
<td>879</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>76.78</td>
<td>76.87</td>
<td>505</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>76.96</td>
<td>77.06</td>
<td>533</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>77.59</td>
<td>77.67</td>
<td>443</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>77.76</td>
<td>77.83</td>
<td>392</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>77.91</td>
<td>78.21</td>
<td>1606</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>78.53</td>
<td>78.83</td>
<td>1594</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>78.97</td>
<td>79.00</td>
<td>161</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>79.07</td>
<td>79.27</td>
<td>1098</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>79.39</td>
<td>79.93</td>
<td>2857</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>80.08</td>
<td>80.21</td>
<td>703</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>80.31</td>
<td>80.41</td>
<td>565</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>80.50</td>
<td>80.61</td>
<td>623</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>80.79</td>
<td>80.84</td>
<td>300</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>82.20</td>
<td>82.23</td>
<td>180</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>82.30</td>
<td>82.36</td>
<td>290</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>82.48</td>
<td>82.54</td>
<td>326</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>82.91</td>
<td>82.95</td>
<td>249</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>13,960</strong></em></td>
<td><em><strong>8.28%</strong></em></td>
</tr>
<tr class="odd">
<td><strong>380C</strong></td>
<td>Masardis-Sheepscot complex</td>
<td>0-15</td>
<td>N</td>
<td>Slight</td>
<td>&gt;60</td>
<td>81.68</td>
<td>81.82</td>
<td>777</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>777</strong></em></td>
<td><em><strong>0.46%</strong></em></td>
</tr>
<tr class="odd">
<td><strong>391A</strong></td>
<td>not described</td>
<td>not described</td>
<td>not described</td>
<td>Slight</td>
<td>&gt;60</td>
<td>74.66</td>
<td>74.74</td>
<td>407</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>407</strong></em></td>
<td><em><strong>0.24%</strong></em></td>
</tr>
<tr class="odd">
<td><strong>39M</strong></td>
<td>Wonsqueak and Bucksport: frequently flooded</td>
<td>0-2</td>
<td>Y</td>
<td>Slight</td>
<td>&gt;60</td>
<td>81.99</td>
<td>82.20</td>
<td>1064</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="even">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td>83.38</td>
<td>83.44</td>
<td>305</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>1369</strong></em></td>
<td><em><strong>0.81%</strong></em></td>
</tr>
<tr class="even">
<td><strong>39P</strong></td>
<td>Bucksport and Wonsqueak</td>
<td>0-2</td>
<td>Y</td>
<td>Slight</td>
<td>&gt;60</td>
<td>80.84</td>
<td>81.04</td>
<td>1015</td>
<td><em><strong> </strong></em></td>
</tr>
<tr class="odd">
<td><strong> </strong></td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td> </td>
<td><em><strong>1015</strong></em></td>
<td><em><strong>0.60%</strong></em></td>
</tr>
<tr class="even">
<td colspan="8"><em><strong>Total Measured Distance</strong></em></td>
<td><em><strong>168,687</strong></em></td>
<td><em><strong>100.00%</strong></em></td>
</tr>
</tbody>
</table>

**APPENDIX 11-5**

**REPRESENTATIVE WETLAND FIELD DATA FORMS AND PHOTOGRAPHIC
DOCUMENTATION**

**APPENDIX 11-6**

**WETLAND SUMMARY TABLE**