alea-institute/kl3m-data-sample-004-shuffled huggingface dataset:
## Breadcrumb

-  Publications 
-  Reports 

#           Overview of landslide problems, research, and mitigation, Cincinnati, Ohio, area      

      July 1, 1996    

View Document

Landslides cause much damage to property throughout the metropolitan area of Cincinnati, Ohio. Most landslides occur in unconsolidated deposits, including colluvium, till, glacial lake clays, and man-made fill derived from colluvium and glacial deposits. Landslides in thin colluvium are widespread on steeper slopes that wall the valleys of the Ohio River and its tributaries. Abundant landslides also form in thick colluvium on flatter slopes, especially where the colluvium has been disturbed by earthwork. Unusual block glides and block-extrusion glides form where till rests on lake clay. Through the years, knowledge of the distribution and causes of landslides has increased as a result of many investigations. This knowledge became part of the basis for landslide mitigation programs adopted by the City of Cincinnati and Hamilton County, Ohio. In 1974 the Cincinnati City Council passed an excavation and fill ordinance to help reduce landslide damage in areas of new construction. In 1989 following much additional study, Cincinnati created a geotechnical office within its Department of Public Works. The office, which is staffed by a geotechnical engineer, an engineering geologist, and two technicians, carries out a mitigation program. Since 1989, members of the geotechnical staff have worked in several ways to reduce landslide damage in the city; their work includes engineering-geologic mapping of selected parts of the city, inspection of retaining walls that impact public right-of-way, review of proposed construction in hillside areas, inspecting and arranging for repair of landslide areas that affect city property, and compiling geologic and geotechnical data on landslide areas within the city. In 1990, Hamilton County also adopted an excavation and fill ordinance to help reduce the damage due to landslides in areas of new construction.

## Citation Information

## Related Content

                  -              Connect           

#### Rex Baum

##### Research Geologist Emeritus

Landslide Hazards Program

baum@usgs.gov

303-273-8610

## Related Content

#### Rex Baum

##### Research Geologist Emeritus

Landslide Hazards Program

baum@usgs.gov

303-273-8610

### Study Area

### Contact

####             Water Resources Mission Area - Headquarters        

USGS Headquarters12201 Sunrise Valley DriveReston, VA20192United States

### Explore Search

                  - Natural Hazards
                  - United States
                  - Ohio

View All **
```

[Federal Register Volume 76, Number 154 (Wednesday, August 10, 2011)]
[Notices]
[Pages 49510-49511]
From the Federal Register Online via the Government Printing Office [www.gpo.gov]
[FR Doc No: 2011-20255]

=======================================================================
-----------------------------------------------------------------------

NATIONAL FOUNDATION ON THE ARTS AND THE HUMANITIES

National Endowment for the Arts

Proposed Collection; Comment Request

ACTION: Notice.

-----------------------------------------------------------------------

SUMMARY: The National Endowment for the Arts (NEA), as part of its 
continuing effort to reduce paperwork and respondent burden, conducts a 
preclearance consultation program to provide the general public and 
federal

[[Page 49511]]

agencies with an opportunity to comment on proposed and/or continuing 
collections of information in accordance with the Paperwork Reduction 
Act of 1995 (PRA95) [44 U.S.C. 3506(c)(A)]. This program helps to 
ensure that requested data can be provided in the desired format, 
reporting burden (time and financial resources) is minimized, 
collection instruments are clearly understood, and the impact of 
collection requirements on respondents can be properly assessed. 
Currently, the NEA is soliciting comments concerning the proposed 
information collection on grant applicant satisfaction with application 
guidance and materials provided on the NEA Web site and by NEA staff. A 
copy of the current information collection request can be obtained by 
contacting the office listed below in the address section of this 
notice.

DATES: Written comments must be submitted to the office listed in the 
address section below on or before October 8, 2011. The NEA is 
particularly interested in comments which:
     Evaluate whether the proposed collection of information is 
necessary for the proper performance of the functions of the agency, 
including whether the information will have practical utility;
     Evaluate the accuracy of the agency's estimate of the 
burden of the proposed collection of information including the validity 
of the methodology and assumptions used;
     Enhance the quality, utility, and clarity of the 
information to be collected; and
     Minimize the burden of the collection of information on 
those who are to respond, including through the use of appropriate 
automated, electronic, mechanical, or other technological collection 
techniques or other forms of information technology, e.g., permitting 
electronic submissions of responses.

ADDRESSES: Sunil Iyengar, National Endowment for the Arts, 1100 
Pennsylvania Avenue, NW., Room 616, Washington, DC 20506-0001, 
telephone (202) 682-5424 (this is not a toll-free number), fax (202) 
682-5677.

Kathleen Edwards,
Director, Administrative Services, National Endowment for the Arts.
[FR Doc. 2011-20255 Filed 8-9-11; 8:45 am]
BILLING CODE 7537-01-P
```
# Fourth Court of Appeals

**San Antonio, Texas**

JUDG MENT

No. 04

- 19

- 00020

- CV

Robert M. STONE , Raymond S. DeLeon, and John Salas,

Appellants

v.

THE CARLSON LAW FIRM

, Appellee

From the 407th Judicial District Court, Bexar County, Texas

Trial Court No. 2015

- CI

- 16271

Honorable Karen H. Pozza, Judge Presiding

BEFORE CHIEF JUSTICE MARION

, JUSTICE MARTINEZ , AND JUSTICE ALVAREZ

In accordance with this court’s opinion of this date, this appeal is DISMISSED FOR

WANT OF PROSECUTION. Costs of appeal are taxed against appellants.

SIGNED March 27, 2019.

_________________________________ Sandee Bryan Marion, Chief Justice
James M. WEST, Appellant/Petitioner(s), v. STATE of Florida, Appellee/Respondent(s).

CASE NO.: 2D17-2919

District Court of Appeal of Florida, Second District.

August 10, 2017

**DECISION WITHOUT PUBLISHED OPINION**

Denied.
1

UNITED STATES BANKRUPTCY COURT

SOUTHERN DISTRICT OF FLORIDA

Miami Division

In re: Case No. 19-17849-RAM

Chapter 13

CECILIA BRAVO

Debtor

____________________________/

ORDER GRANTING DEBTOR’S EXPEDITED MOTION TO CONTINUE THE 

AUTOMATIC STAY

THIS CASE having come before the Court on July 11, 2019 at 9:00 AM on the Debtor’s

Expedited Motion to Continue the Automatic Stay [DE #9] Pursuant to §362(c)(4)(B), this Court having 

reviewed the Motion and being otherwise duly advised in the premises, it is thereupon:

ORDERED AND ADJUDGED that:

1. The Debtor’s Motion to Continue the Automatic Stay [DE #9] is GRANTED, subject to the 

conditions stated below.

ORDERED in the Southern District of Florida on July 14, 2019.

Robert A. Mark, Judge

United States Bankruptcy Court

_____________________________________________________________________________

Case 19-17849-RAM Doc 22 Filed 07/15/19 Page 1 of 2
2

2. The Automatic Stay shall be in full force and effect against all creditors until further order of 

this Court or upon any subsequent order granting relief from the automatic stay. The stay is also subject 

to§362(c)(4)(C). 

###

Submitted by:

Robert A. Stiberman, Esq.

STIBERMAN LAW, P.A.

2601 Hollywood Blvd

Hollywood, FL 33020

954-922-2283

Ras@stibermanlaw.com

Attorney Robert A. Stiberman is directed to serve copies of this order on all interested parties and file a 

certificate of service.

Case 19-17849-RAM Doc 22 Filed 07/15/19 Page 2 of 2
## Breadcrumb

-  Publications 
-  Articles 

#           The mutual interference of artesian wells on Long Island, New York      

      August 26, 1937    

The withdrawal of water from a well necessarily produces a drop in water‐level in the well. The ground‐water level in the vicinity of the well from which the water is withdrawn likewise declines, but the amount of decline decreases with increasing distance from the well, so that a cone of depression of the water‐surface in the vicinity of the well is produced. The cone of depression is an actual water‐surface if the ground‐water is not confined under pressure. If the ground‐water is under artesian pressure, the cone of depression is a depression in the piezometric surface. If the cones of depression of two or more wells ending in the same formation overlap, interference of the wells occurs. In this case (the combined yield of the wells when pumped simultaneously will be less than the sum of the individual yields if the wells are pumped separately. In choosing the proper spacing of wells from the operator's point of view, it is important to know the lateral extent of the cones of depression of supply‐wells ending in a given formation. In many installations two or more wells are so closely spaced that their mutual interference is excessive.

## Citation Information

### Study Area

### Explore Search

                  - United States
                  - Western Long Island
                  - New York

View All **
## Breadcrumb

-  Publications 
-  Articles 

#           Meter-scale morphology of the north polar region of mars      

      January 1, 2007    

Mars' north pole is covered by a dome of layered ice deposits. Detailed (∼30 centimeters per pixel) images of this region were obtained with the High-Resolution Imaging Science Experiment on board the Mars Reconnaissance Orbiter (MRO). Planum Boreum basal unit scarps reveal cross-bedding and show evidence for recent mass wasting, flow, and debris accumulation. The north polar layers themselves are as thin as 10 centimeters but appear to be covered by a dusty veneer in places, which may obscure thinner layers. Repetition of particular layer types implies that quasi-periodic climate changes influenced the stratigraphic sequence in the polar layered deposits, informing models for recent climate variations on Mars.

## Citation Information

## Related Content

                  -              Connect           

####             Kenneth Edward Herkenhoff, Ph.D. (Former Employee)          

##### Research Geologist

Astrogeology Science Center

## Related Content

####             Kenneth Edward Herkenhoff, Ph.D. (Former Employee)          

##### Research Geologist

Astrogeology Science Center

### Contact

####               Astrogeology Science Center          

2255 N. Gemini DriveFlagstaff, AZ86001United States

928-556-7000

928-556-7014

### Explore Search

                  - Mars

View All **
TEXAS COURT OF APPEALS, THIRD DISTRICT, AT AUSTIN

NO. 03-12-00551-CV

In re Honorable Jennifer Tharp, Criminal District Attorney of Comal County, Texas

ORIGINAL PROCEEDING FROM COMAL COUNTY

M E M O R A N D U M O P I N I O N

The petition for writ of mandamus is denied. See Tex. R. App. P. 52.8(a).

__________________________________________

Melissa Goodwin, Justice

Before Chief Justice Jones, Justices Rose and Goodwin

Filed: August 23, 2012
UNPUBLISHED

UNITED STATES COURT OF APPEALS 

FOR THE FOURTH CIRCUIT 

No. 08-7244

DEMETRIUS HILL, 

 Plaintiff - Appellant, 

 v. 

WARDEN HAYNES; A. W. GILL; WARDEN DRIVER; CAPTAIN ODDO; 

LIEUTENANT CLEMENS; LIEUTENANT GIFFORD; LIEUTENANT TRAIT; 

CORRECTIONAL OFFICER SPOTLAN; FOSTER; CORRECTIONAL OFFICER 

MORGAN; COUNSELOR MORRERO; ETRIS, 

 Defendants - Appellees. 

Appeal from the United States District Court for the Northern 

District of West Virginia, at Martinsburg. John Preston Bailey, 

Chief District Judge. (3:06-cv-00136-JPB-JSK) 

Submitted: March 10, 2009 Decided: April 1, 2009 

Before NIEMEYER, TRAXLER, and GREGORY, Circuit Judges. 

Remanded by unpublished per curiam opinion. 

Demetrius Hill, Appellant Pro Se. Helen Campbell Altmeyer, 

Assistant United States Attorney, Wheeling, West Virginia, for 

Appellees.

Unpublished opinions are not binding precedent in this circuit. 
PER CURIAM: 

 Demetrius Hill seeks to appeal the district court’s 

order declining to adopt the magistrate judge’s recommendation 

and dismissing Hill’s civil complaint without prejudice. The 

district court’s judgment was entered on March 5, 2008. Hill’s 

notice of appeal was filed on July 16, 2008, the day on which he 

delivered it to prison officials for mailing. See Fed. R. App. 

P. 4(c)(1); Houston v. Lack, 487 U.S. 266, 276 (1988). In his 

notice of appeal, Hill stated that he did not receive notice of 

the district court’s order until July 9, 2008, when he received 

a copy of the district court’s docket sheet, in response to his 

request to the district court for the status of his case. 

 Parties are accorded thirty days after entry of the 

district court’s final judgment or order to note an appeal, Fed. 

R. App. P. 4(a)(1)(A), unless the district court extends the 

appeal period under Fed. R. App. P. 4(a)(5) or reopens the 

appeal period under Fed. R. App. P. 4(a)(6). This appeal period 

is “mandatory and jurisdictional.” Browder v. Dir., Dep’t of 

Corr., 434 U.S. 257, 264 (1978) (quoting United States v. 

Robinson, 361 U.S. 220, 229 (1960)). 

 Hill’s notice of appeal is clearly untimely filed. 

However, under Rule 4(a)(6), the district court may reopen the 

time to file an appeal if (1) the moving party did not receive 

notice of entry of judgment within twenty-one days after entry, 

2 
3 

(2) the motion is filed within 180 days of entry of judgment or 

within seven days of receiving notice from the court, whichever 

is earlier, and (3) no party would be prejudiced. We remand to 

the district court to determine whether Hill is entitled to the 

benefit of Rule 4(a)(6) to reopen the time to file an appeal. 

The record, as supplemented, will then be returned to this court 

for further consideration. 

REMANDED
## Breadcrumb

-  Publications 
-  Books 

#           Long-period earthquake simulations in the Wasatch Front, UT: misfit characterization and ground motion estimates      

      January 1, 2011    

View Document

In this research we characterize the goodness-of-fit between observed and synthetic seismograms from three small magnitude (M3.6-4.5) earthquakes in the region using the Wasatch Front community velocity model (WCVM) in order to determine the ability of the WCVM to predict earthquake ground motions for scenario earthquake modeling efforts. We employ the goodness-of-fit algorithms and criteria of Olsen and Mayhew (2010). In focusing comparisons on the ground motion parameters that are of greatest importance in engineering seismology, we find that the synthetic seismograms calculated using the WCVM produce a fair fit to the observed ground motion records up to a frequency of 0.5 Hz for two of the modeled earthquakes and up to 0.1 Hz for one of the earthquakes. In addition to the reference seismic material model (WCVM), we carry out earthquake simulations using material models with perturbations to the regional seismic model and with perturbations to the deep sedimentary basins. Simple perturbations to the regional seismic velocity model and to the seismic velocities of the sedimentary basin result in small improvements in the observed misfit but do not indicate a significantly improved material model. Unresolved differences between the observed and synthetic seismograms are likely due to un-modeled heterogeneities and incorrect basin geometries in the WCVM. These differences suggest that ground motion prediction accuracy from deterministic modeling varies across the region and further efforts to improve the WCVM are needed.

## Citation Information

## Related Content

                  -              Connect           

#### Morgan P Moschetti, PhD

##### Research Geophysicist

Earthquake Hazards Program

mmoschetti@usgs.gov

303-273-8464

## Related Content

#### Morgan P Moschetti, PhD

##### Research Geophysicist

Earthquake Hazards Program

mmoschetti@usgs.gov

303-273-8464

### Contact

#### Geologic Hazards Science Center

1711 Illinois St.Golden, CO80401United States

303-273-8500

### Explore Search

                  - Natural Hazards
                  - United States
                  - Wasatch Front
                  - Utah

View All **
```

[Congressional Bills 114th Congress]
[From the U.S. Government Publishing Office]
[H.R. 4726 Introduced in House (IH)]

<DOC>

114th CONGRESS
  2d Session
                                H. R. 4726

To prohibit the obligation of funds to pay the salary of the Secretary 
 of Homeland Security until a biometric entry and exit data system has 
            been fully implemented, and for other purposes.

_______________________________________________________________________

                    IN THE HOUSE OF REPRESENTATIVES

                             March 10, 2016

    Mr. Graves of Missouri introduced the following bill; which was 
             referred to the Committee on Homeland Security

_______________________________________________________________________

                                 A BILL

 
To prohibit the obligation of funds to pay the salary of the Secretary 
 of Homeland Security until a biometric entry and exit data system has 
            been fully implemented, and for other purposes.

    Be it enacted by the Senate and House of Representatives of the 
United States of America in Congress assembled,

SECTION 1. SHORT TITLE.

    This Act may be cited as the ``Preventing Illegal Visa Overstays 
Act of 2016''.

SEC. 2. NO PAYMENT OF SALARY TO THE SECRETARY OF HOMELAND SECURITY 
              UNTIL FULL IMPLEMENTATION OF THE ENTRY AND EXIT DATA 
              SYSTEM.

    Beginning on the date of enactment of this Act, no funds made 
available in any fiscal year may be obligated to pay the salary of the 
Secretary of Homeland Security. The limitation provided under the 
previous sentence shall no longer apply beginning on the date that the 
entry and exit data system (as such term is defined in section 7208(b) 
of the Intelligence Reform and Terrorism Prevention Act of 2004 (8 
U.S.C. 1365b(b))) has been fully implemented.
                                 <all>
```
## Breadcrumb

-  Publications 
-  Articles 

#           Microhabitat and biology of *Sphaerium striatinum* in a central New York stream      

      May 9, 2017    

In many lotic systems, drastic declines in freshwater bivalve populations, including fingernail clams (Sphaeriidae), have created concerns about biodiversity and future ecosystem services. We examined the local occurrence of the historically common fingernail clam, Sphaerium striatinum, in a central New York stream. We sampled the density of sphaeriids and measured the associated habitat variables (substrate, depth, water flow) to test within-stream multivariate benthic microhabitat association. Size distribution, density, and diel feeding periodicity were measured as focal aspects of fingernail clam biology and ecology. S. striatinum tended to be found in microhabitats that had harder substrates and faster flow. The Labrador Creek fingernail clam local population had positive indicators (size distribution, density). There was significant diel periodicity in feeding behavior. The clams fed most actively during the 0400–0800 h periods. This kind of behavioral periodicity can indicate a significant ecological interaction between predators and bivalve prey. Increased understanding of the behavioral ecology of small native freshwater bivalves in an unimpacted headwater stream is a fundamental building block for development of overall ecological conservation goals for freshwater bivalves and their lotic habitats.

## Citation Information

## Related Content

                  -              Connect           

#### Dawn Elaine Dittman, PhD

##### Research Ecologist

Great Lakes Science Center

ddittman@usgs.gov

607-753-9391

#### James H Johnson, PhD

##### Scientist Emeritus

Great Lakes Science Center

jhjohnson@usgs.gov

607-753-9391

## Related Content

#### Dawn Elaine Dittman, PhD

##### Research Ecologist

Great Lakes Science Center

ddittman@usgs.gov

607-753-9391

#### James H Johnson, PhD

##### Scientist Emeritus

Great Lakes Science Center

jhjohnson@usgs.gov

607-753-9391

### Contact

####               Great Lakes Science Center          

1451 Green RoadAnn Arbor, MI48105United States

734-994-3331

734-994-8780

### Explore Search

                  - United States
                  - New York

View All **
## Breadcrumb

-  Publications 
-  Articles 

#           Mapped versus actual burned area within wildfire perimeters: Characterizing the unburned      

      November 1, 2012    

For decades, wildfire studies have utilized fire occurrence as the primary data source for investigating the causes and effects of wildfire on the landscape. Fire occurrence data fall primarily into two categories: ignition points and perimeter polygons which are used to calculate a ‘burned area’ for a fire. However, understanding the relationships between climate and fire or between fire and its ecological effects requires an understanding of the burn heterogeneity across the landscape and the area within fire perimeters that remains unburned. This research characterizes unburned areas within fire perimeters, which provide ecological refugia and seed source for post-fire regeneration. We utilized differenced Normalized Burn Ratio (dNBR) data to examine the frequency, extent, and spatial patterns of unburned area in three national parks across the western US (Glacier, Yosemite, and Yukon-Charley Rivers). We characterized unburned area within fire perimeters by fire size and severity, characterized distance to an unburned area across the burned portion of the fire, and investigated patch dynamics of unburned patches within the fire perimeter. From 1984 through 2009, the total area within the fire perimeters that was classified as unburned from dNBR was 37% for Yosemite, 17% for Glacier, and 14% for Yukon-Charley. Variation in unburned area between fires was highest in Yosemite and lowest in Yukon-Charley. The unburned proportion significantly decreased with increasing fire size and severity across all three parks. Unburned patch size increased with size of fire perimeter, but patches decreased in density. There were no temporal trends in unburned area found. These results raise questions about the validity of relationships found between external forcing agents, such as climate, and ‘burned area’ values derived solely from polygon fire perimeters.

## Citation Information

### Study Area

### Contact

####               Northern Rocky Mountain Science Center (NOROCK) Headquarters          

2327 University WaySuite 2Bozeman, MT59715United States

406-994-7544

406-994-6556

### Explore Search

                  - United States
                  - Alaska
                  -  Montana
                  -  Wyoming
                  - Yosemite National Park
                  -  Glacier National Park
                  -  Yukon-Charley Rivers National Preserve

View All **