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Source: http://164.214.2.59/GandG/tm83581/toc.htm NIMA Geodesy and Geophysics DEFENSE MAPPING AGENCY
TECHNICAL MANUAL 8358.1 DATUMS, ELLIPSOIDS, GRIDS, AND
GRID REFERENCE SYSTEMS Abstract: This manual describes the basic principles of the Military Grid Reference System and the non-standard reference systems. It describes the method for determining references on maps and charts at scales of 1:1,000,000 and larger. It contains identifications for the grid zone designations and for the 100,000 meter squares of the Universal Transverse Mercator Grid and the Universal Polar Steriographic Grid. It also contains the specifications and grid identifications for the various non-standard grids. It provides diagrams and textual information for delineating geodetic datums and ellipsoids. Subject Terms: Position location, military grid, geodetic datum, coordinate reference system, ellipsoid, spheroid, graticule, chart, projection. TABLE OF CONTENTS FRONT MATTER FOREWORD LIST OF FIGURES LIST OF TABLES CHAPTER 1 GENERAL 1-1 - Authority 1-2 - References 1-3 - Purpose 1-4 - Scope 1-5 - Utilization 1-6 - Definitions 1-7 - Reference Systems 1-8 - Standard and Nonstandard Grids 1-9 - Multiple Grids 1-10 - Overlapping Grids 1-11 - Extended Grids 1-12 - Grid and Datum Related Marginal Notes 1-13 - Supercession CHAPTER 2 DATUMS, ELLIPSOIDS, PROJECTIONS AND MILITARY GRIDS 2-1 - General 2-2 - Horizontal Datums 2-3 - Transforming Coordinates from one Horizontal Datum to Another Horizontal Datum 2-4 - Ellipsoids 2-5 - Projections 2-6 - Military Grids 2-7 - Transforming Coordinates from one Grid System to Another Grid System CHAPTER 3 THE U. S. MILITARY GRID REFERENCE SYSTEM (MGRS) 3-1 - General Description 3-2 - The Grid Zone Designation 3-3 - 100,000-Meter Square Identification 3-4 - The Military Grid Reference 3-5 - MGRS Application CHAPTER 4 THE NONSTANDARD GRID SYSTEMS IN CURRENT USE PAGE 4-1 - Nonstandard Grids on Maps and Charts 4-2 - Diagrams of Nonstandard Grids CHAPTER 5 GEOGRAPHIC COORDINATE REFERENCES 5-1 - Use 5-2 - The Geographic Reference 5-3 - Geographic Coordinates on Maps and Charts 5-4 - The World Geographic Reference System CHAPTER 6 PORTRAYAL OF GRIDS ON MAPS AT 1:100,000 SCALE AND LARGER 6-1 - General 6-2 - The Major Grid 6-3 - Multiple Major Grids 6-4 - Overlapping Grids 6-5 - Secondary Grids 6-6 - The Declination Diagram (One Grid) 6-7 - The Declination Diagram (More Than One Grid) 6-8 - The Grid Reference Box CHAPTER 7 PORTRAYAL OF GRIDS ON MAPS AT 1:250,000 AND 1:500,000 SCALE 7-1 - General 7-2 - The Major Grid 7-3 - Multiple Major Grids 7-4 - Overlapping and Extended Grids 7-5 - Secondary Grids 7-6 - Grid Declination 7-7 - Magnetic Dechnotion 7-8 - The Grid Reference Box CHAPTER 8 PORTRAYAL OF GRIDS ON MAPS AT 1:1,000,000 SCALE 8-1 - General 8-2 - The Major Grid 8-3 - Multiple Major Grids 8-4 - Overlapping, Extended, and Secondary Grids 8-5 - Grid and Magnetic Declinations 8-6 - The Grid Reference Box CHAPTER 9 GRIDS ON NAUTICAL CHARTS AT 1:75,000 SCALE AND LARGER 9-1 - General 9-2 - The Major Grid on Combat Charts and Amphibious Assault Charts 9-3 - The Major Grid on Mine Warfare Charts 9-4 - The Major Grid on Harbor, Approach, and Coastal Charts 9-5 - Multiple Major Grids on Combat Charts and Amphibious Assault Charts 9-6 - Multiple Major Grids on Harbor, Approach, and Coastal Charts 9-7 - Overlapping Grids on Combat Charts, Amphibious Assault Charts, and Mine Warfare Charts 9-8 - Overlapping Grids on Harbor, Approach, and Coastal Charts 9-9 - Secondary Grids 9-10 - The Declination Note 9-11 - The Grid Reference Box 9-12 - World Geodetic System (WGS) Datum Note CHAPTER 10 GRIDS ON NAUTICAL CHARTS AT SCALES SMALLER THAN 175,000 10-1 - General 10-2 - The Major Grid 10-3 - Multiple Grids 10-4 - Secondary Grids 10-5 - The Grid Reference Box (or Notes) 10-6 - World Geodetic System (WGS) Datum Note CHAPTER 11 GRIDS ON AERONAUTICAL CHARTS AT 1-500,000 SCALE AND LARGER 11-1 - General 11-2 - The Major Grid 11-3 - Grid Declination 11-4 - Magnetic Declination 11-5 - The Grid Reference Box APPENDIXES A - Table of Mil Equivalents *B - 100,000-Meter Square Identifications of the Military Grid Reference System (Graphics), Figures B-1 through B-4 *C - Guide To Geodetic Status Of Large Scale Mapping *D -Index to Preferred Grids, Datums and Ellipsoids Specified for New Mapping * Requires periodic update and revision.
Abstract: This manual describes the basic principles of the Military Grid Reference System and the non-standard reference systems. It describes the method for determining references on maps and charts at scales of 1:1,000,000 and larger. It contains identifications for the grid zone designations and for the 100,000 meter squares of the Universal Transverse Mercator Grid and the Universal Polar Steriographic Grid. It also contains the specifications and grid identifications for the various non-standard grids. It provides diagrams and textual information for delineating geodetic datums and ellipsoids. Subject Terms: Position location, military grid, geodetic datum, coordinate reference system, ellipsoid, spheroid, graticule, chart, projection.
DEFENSE MAPPING AGENCY MISSION: To enhance national security and support the Office of the Secretary of Defense, the Joint Chiefs of Staff, Unified and Specified Commands, Military Departments, and other users, by producing and distributing timely and tailored mapping, charting, and geodetic products, services, and training, and advising on such matters. To provide nautical charts and marine navigational data to worldwide merchant marine and private vessel operators. To maintain liaison with civil agencies and other national and international scientific and other mapping, charting, and geodetic activities. DEFENSE MAPPING AGENCY
FAIRFAX, VIRGINIA 22031-2137
DEFENSE MAPPING AGENCY TECHNICAL MANUAL 8358.1 DATUMS, ELLIPSOIDS, GRIDS, AND GRID REFERENCE SYSTEMS FOREWORD This manual states current authoritative guidance for the use and portrayal of grids and grid reference systems information as applicable to maps and charts compiled for the United States Department of Defense (DoD). This publication contains no copyrighted material and has been approved for public release. Distribution is unlimited. DoD users may order copies from the Defense Mapping Agency Combat Support Center, ATTN: PMSR, Washington, D.C. 20315-0020. All other requests should be directed to the National Technical Information Center, Cameron Station, Alexandria, VA 22314-6145.                                            STANLEY O. SMITH
LIST OF FIGURES 1 Defining Parameters of Ellipsoids 2 Mercator Projection 3 Transverse Mercator Projection 4 Secant Condition of Transverse Mercator Projection; Typical 6-degree Projection Zone 5 Polar Stereographic Projection 6 Lambert Conformal Conic Projection 7 Grid Zone Designations of the Military Grid Reference System 8 Basic Plan of the 100,000-meter Square Identifications of the U.S. Military Grid Reference System, Between 84'N. and 80's. 9 Method of Reading a U.S. Military Grid Reference from a 1:250,000 Scale Map 10 Method of Reading a U.S. Military Grid Reference from a Large Scale Map 11 Normal Lettering Plan of the 500,000 - 100,000-unit squares of the British Grid System 12 World Geographic Reference (GEOREF) System 13 The Major Grid as Shown a 1:50,000 Scale Map 14 The Major Grid as Shown on a 1:100,000 Scale Map 15 Two Major Grids (in this case, Zones of the UTM) Separated 16 Three Major Nonstandard Grids as Shown on a Large Scale Map 17 Major and Overlapping Grids as Shown on a Large Scale 18 Overlapping Grid in Combination with Two Major Grids Separated by a Grid Junction as Shown on a Large Scale Map 19 Major and Secondary (Obsolete) Grids as Shown on a Large Scale Map 20 The Declination Diagram and Accompanying Notes with True North Appearing as the Center Prong 21 The Declination Diagram and Accompanying Notes with True North Appearing as an Outside Prong 22 The Declination Data when a Sheet Contains an Overlapping rid and/or More Than One Major Grid 23 Grid Reference Boxes Most Commonly Used on Maps at Coles of 1:100,000 and Larger 24 Methods of Showing Grid Zone Designations and 100,000- meter Squares of the UTM in the Grid Reference Boxes of Large Scale Maps 25 Methods of Showing 100,000-unit, and Larger, Square Identifications of Nonstandard Grids in the Grid Reference Boxes of Large Scale Maps 26 Treatment for the Major Grid in UTM Areas as Shown on a 1:250,000 Map 27 Treatment for the Major Grid in UTM Areas as Shown on Maps Smaller than 1:250,000 Scale and Larger than 1:1,000,000 28 Two Major UTM Grid Zones Separated by a Grid Junction as Shown on a 1:250,000 Scale Map 29 Three Major Nonstandard Grids Separated by Grid Junctions 30 Two Major Grids (UTM) Separated by an Ellipsoid Junction as Shown on a 1:250,000 Scale Map 31 Treatment when Grid Falls within More than One UTM Grid Zone Designation Area as Shown on a 1:250,000 Scale Map 32 Major and Secondary (Obsolete) Grids as Shown on a 1:250,000 Scale Map 33 Grid Reference Boxes Most Commonly Used on Maps at 1:250,000 and 1:500,000 Scale 34 Treatment for the Major Grid in UTM Areas as Shown on Maps at 1:1,000,000 Scale 35 Two Major Grids (in this case, Zones of the UTM) Separated by a Grid Junction, as Shown on a Map at 1:1,000,000 Scale 36 Three Major Nonstandard Grids as Shown on a Map at 1:1,000,000 Scale 37 Grid Reference Box for 1:1,000,000 Scale Map 38 The Major Grid as Shown on Combat, Amphibious Assault Charts 39 Two Major Grids (in this case, Zones of the UTM) Separated by a Grid Junction as Shown on Combat, Amphibious Assault Charts 40 Treatment for the Major Grid on Mine Warfare Charts at 1:75,000 Scale and Larger 41 Treatment for the Major Grid on Harbor and Approach Charts at 1:75,000 Scale and Larger 42 Treatment for the Multiple Major Grids on Harbor and Approach Charts at 1:75,000 scale and Larger 43 Grid Reference Boxes Commonly Used on Nautical Charts at Scales of 1:75,000 and Larger 44 Treatment for the Major Grid on Nautical Charts at Scales Smaller than 1:75,000 45 Treatment for Multiple Grids on Nautical Charts at Scales Smaller than 1:75,000 46 Treatment for Major and Secondary Grids on Nautical Charts at Scales Smaller than 1:75,000 47 Grid Reference Box Commonly Used on Aeronautical Charts at 1:500,000 Scale and Larger LIST OF TABLES 1 Geodetic Datums Used in Map Production 2 Molodenskiy Transformation Constants to Convert from Local Datum to WGS 84 3 Characteristics of Projections 4 Grid Unit Intervals for Various Scale Topographic Maps 5 Dimensions of Grid Zone Designation Areas 6 Specifications for Secondary Grids 7 Corner Labeling on Topographic Maps 8 The Equivalents of 40 Kilometers when Measured Along a Given Parallel of Latitude Expressed in Degrees, Minutes, and Seconds of Longitude 9 Maximum Acceptable Deviation of the Constructed Grid from the True Grid CHAPTER I GENERAL 1-1 AUTHORITY.
This document is issued under the authority delegated by DoD Directive 5105.40, subject: Defense Mapping Agency (DMA), 12 December 1988. 1-2 REFERENCES.
1-2.1 The DMA TM 83581 series replaces the DA TM 5-241 series of manuals. 1-2.2 JCS-MOP 88, Position Reference Procedures, 8 May 1981. 1-2.3 STANAG 2211, subject: Geodetic Datums, Ellipsoids, Grids, and Grid References. 1-2.4 STANAG 3676, subject: Marginal Information on Land Maps and Aeronautical Charts. 1-2.5 QSTAG 544, subject: Geodetic Datums, Spheroids, Grids, and Grid References. 1-2.6 IHO Circular Letter 9, International Horizontal Datum for Chart Reference, 15 March 1983. 1-2.7 IHO Circular Letter 28, Transformation Notes, WGS-84, 15 July 1988. 1-2.8 IHO Circular Letter 46, International Horizontal Datum for Chart Reference, 16 December 1983. 1-2.9 IHO Circular Letter 18, Indication on Charts of Relationship of Horizontal Datum to Worldwide and Other Datums, 17 May 1984. 1-2.10 IHO Circular Letter 46, Indication on Charts of Relationship of Horizontal Datum to Worldwide and Other Datums, 14 December 1984. 1-2.11 DMA TM 83581.2 The Universal Grids: Universal Transverse Mercator (UTM) and Universal Polar Stereographic (UPS). 1-2.12 DMA TR 8350.2 (and supplements) Department of Defense World Geodetic System 1984. 1-3 PURPOSE.
1-3.1 This manual provides guidance to DoD Mapping, Charting and Geodesy (MC&G) production elements, product users, and system developers on the application of datums, ellipsoids, grids, and grid reference systems within the DoD. 1-3.2 It describes the standard methods for selecting and portraying grids or maps and charts at scales of 1:1,000,000 and larger. Descriptions are based on the following categories. 1-3.2.1 Topographic Maps. 1-3.2.2 Hydrographic Charts. 1-3.2.3 Aeronautical Charts. 1-4 SCOPE.
1-4.1 This manual specifies the use of geodetic datums, ellipsoids, grids and grid reference systems used in the production of maps and charts for the DoD. The Universal Transverse Mercator an d Universal Polar Stereographic grids, the Military Grid Reference System, and nonstandard grid reference systems are described. 1-4.2 Detailed instructions and formats for grid depictions and labeling, grid margin data, declination data, etc. are contained in the DMA product specifications for approved topographic, hydrographic, and' aeronautical products. 1-5 UTILIZATION.
1-5.1 TM 83581.1 is to be used by DoD MC&G production elements, product users, and DoD system developers in the application of datums, ellipsoids, grids, and grid reference systems. 1-5.2 Users are cautioned that the information contained herein applies to current and future MC&G production, and does not necessarily apply to products that are currently available through the DoD supply system. 1-6 DEFINITIONS.
1-6.1 Major Grid. The primary grid or grids on a map or chart. 1-6.2 Military Grid Reference System (MGRS). The alphanumeric position reporting system used by U.S. military. A full description is provided in Chapter 3. 1-6.3 Nonstandard Grids. Grids other than UTM and UPS, such as Ceylon Belt, India Zone IIA, West Malaysian RSO (Metric) Grid, etc. 1-6.4 Operational Grid. A grid in current operational use. Generally this would be the preferred grid but could be a previously prescribed grid. 1-6.5 Overlapping Grid. A major grid from a neighboring area primarily intended to facilitate military surveying anti fire-control. 1-6.6 Preferred Grid. The grid designated by the DoD for production of new maps, charts, and digital geographic data; and shown on the "Index to Preferred Grids, Datums, and Ellipsoids Specified for New Mapping" (Appendix D). 1-6.7 Prescribed Grid. The grid that is locally prescribed, by the country of origin or military commander. 1-6.8 Primary Grid. The major, or principal, grid on a map or chart. 1-6.9 Secondary Grid. Any grid, other than the primary grid, required for combined operations application. Tick marks along the neat lines are the preferred method of portrayal. Such grids should remain on the maps or charts so long as the secondary grid remains in use. 1-6.10 Standard Grids. The Universal Transverse Mercator (UTM) grid and the Universal Polar Stereographic (UPS) grid. 1-6.11 World Geographic Reference System (GEOREF). A worldwide position reference system that may be applied to any map or chart graduated in latitude and longitude regardless of projection. It provides a method of expressing positions in a form suitable for reporting and plotting. The primary use is for interservice and interallied reporting of aircraft and air target positions. 1-6.12 Other Key Terms. 1-6.12.1 Bleeding Edge. That edge of a map or chart on which cartographic detail is extended beyond the neatline to the edge of the sheet. 1-6.12.2 Coordinate Reference Notation Grid coordinates are given in terms of linear in meters. Geographic coordinates are given in terms of angular measurement, usually in degrees, minutes, and seconds but occasionally in grads. 1-6-12.3 Datum. As used in this manual, datum refers to the geodetic or horizontal datum. The classical datum is defined by a minimum of five elements giving the position of the origin (two elements), the orientation of the network (one element), and the parameters of a reference ellipsoid (two elements). More recent definitions express the position and orientation as functions of the deviations in the meridian and in the prime vertical, the geoid-ellipsoid separation, and the parameters of a reference ellipsoid. The World Geodetic System is a geocentric system that provides a basic reference frame and geometric figure for the earth, models the earth gravimetrically, and provides the means for relating positions on various datums to an earth-centered, earth fixed coordinate system. 1-6.12.4 Easting. Eastward (that is left to right) reading of grid values on a map. 1-6.12.5 Ellipsoid. An ellipsoid is a mathematical figure generated by the revolution of of an ellipse about one of its axes. The ellipsoid that approximates the geoid is an ellipse rotated about its minor axis, or an oblate spheroid. 1-6.12.6 False Easting. A value assigned to the origin of eastings, in a grid coordinate system, to avoid the convenience of using negative coordinates. 1-6.12.7 False Northing. A value assigned to the origin of northings, in a grid coordinate system, to avoid the inconvenience of using negative coordinates. 1-6.12.8 Geoid. The equipotential surface in the gravity field of the Earth which approximates the undisturbed mean sea level extended continuously through the continents. The direction of gravity is perpendicular to the geoid at every point. The geoid is the surface of reference for astronomic observations and for geodetic leveling. 1-6.12.9 Graticule. A network of lines representing parallels of latitude and meridians of longitude forming a map projection. 1-6.12.10 Grid. Two sets of parallel lines intersecting at right angles and forming squares; a rectangular Cartesian coordinate system that is superimposed on maps, charts, and other similar representations of the earth's surface in an accurate and consistent manner to permit identification of ground locations with respect to other locations and the computation of direction and distance to other points. 1-6.12.11 Isogonic Line. A line drawn on a map or chart joining points of equal magnetic declination for a given time. The line connecting points of zero declination is the agonic line. Lines connecting points of equal annual change are isopors. The Magnetic Variation chart for the current 5-year epoch is available from the DMACSC. 1-6.12.12 Loxodrome. A line on the surface of the Earth cutting all meridians at the same angle, a rhumb line. 1-6.12.13 Map Projection. An orderly system of lines on a plane representing a corresponding system of imaginary lines on an adopted terrestrial datum surface. A map projection may be derived by geometrical construction or by mathematical analysis. 1-6.12.14 Neatline. The lines that bound the body of a map, usually parallels and meridians (but may be conventional or arbitrary grid lines); also called sheet lines. 1-6.12.15 Northing. Northward (that is from bottom to top) reading of grid values on a map. 1-6.12.16 Spheroid. A mathematical figure closely approaching the geoid in form and size. Ellipsoid will be used in this manual. 1-7 REFERENCE SYSTEMS.
1-7.1 Rectangular grid reference systems are usually shown on military maps and chart at scales of 1:1,000,000 and larger. Maps and charts at all scales show the geographic graticule. Maps and aeronautical charts at 1:250,000 scale and smaller show the GEOREF. 1-7.2 The Military Grid Reference System is described in Chapter 3. 1-7.3 Grid reference systems used with operational nonstandard grids are described in Chapter 4. 1-7.4 The geographic coordinates are described in Chapter 5. 1-8 STANDARD AND NONSTANDARD GRIDS.
1-8.1 The standard grid for polar areas north of 84ï¿½ north, and south of 80ï¿½ south, is the Universal Polar Stereographic (UPS) grid. 1-8.2 Between 84ï¿½north and 80ï¿½ south, the standard grid is the Universal Transverse Mercator (UTM) grid. Other grid systems are being phased out. The long term objective is to convert the mapping of all areas of the world to UTM and UPS grids. 1-8.3 Normally, grids are not portrayed on maps at scales smaller than 1:1,000,000. 1-9 MULTIPLE GRIDS.
The use of military grids presents complex conditions in junction areas, i.e., grid zone junctions within a grid system, grid junctions between various grid systems, datum junctions, and junctions between ellipsoids. Despite this complexity, these conditions lend themselves to a uniform graphical treatment of the grids with differences in grid orientation and grid color, labels, and values. The treatment of grids under various junction conditions is prescribed in later chapters of this manual. 1-10 OVERLAPPING GRIDS.
Maps at scales of 1:100,000 and larger, falling within approximately 40 kilometers of a grid junction, datum junctions or ellipsoid junction, usually show the adjacent (overlapping) grid by ticks and values around the neatline. In some instances, a coordinate conversion note may be used instead of an overlapping grid. 1-11 EXTENDED GRIDS.
An extended grid is form of overlapping grid used on city maps. It provides total coverage of a map on a single grid when a portion of the map falls on an adjacent grid. The major grid is extended to cover the adjacent area and is shown by full lines. 1-12 GRID AND DATUM RELATED MARGINAL NOTES.
Marginal notes on maps and charts should include projection, ellipsoid, grid zone or belt, horizontal datum, and magnetic declination data. Specific treatment of these items on each product is covered in the various product specifications. 1-13 SUPERCESSION.
This document supercedes DMA 8358.1, Preliminary Edition. CHAPTER 2
DATUMS, ELLIPSOIDS, PROJECTIONS
AND MILITARY GRIDS 2-1 GENERAL.
2-1.1 The Earth is not a sphere, but an ellipsoid, flattened slightly at the poles and bulging somewhat at the Equator. The ellipsoid is used as a surface of reference for the mathematical reduction of geodetic and cartographic data. 2-1.2 A map projection is the systematic drawing of lines representing the meridians and parallels (the graticule) on a flat surface. Different projections have unique characteristics and serve differing purposes. They are depicted by projecting the graticule of the ellipsoid onto a plane; the intersections of the graticule are computed in terms of the ellipsoid. 2-1.3 U.S. Military maps use the sexagesimal system of angular measurement (the division of a full circle into 360ï¿½) for designating the values of the graticule. A degree is divided into 60 minute, and each minute into 60 seconds. Parallels are numbered north and south from Oï¿½ at the equator to 90ï¿½ at the poles. Meridians are numbered east and west from Oï¿½ at the prime meridian to a common 180ï¿½ meridian. The prime meridian used for U.S. Military mapping and charting is related to the Bureau International de I'Heure defined Zero Meridian, located near Greenwich, England. Some foreign produced maps may use the centesimal (decimal) system of angular measurement (the division of a full circle into 400 grads). A grad (or gon) is divided into 100 centigrade (grad minutes), and each centigrad into 100 deci-milligrads (grad seconds). Other prime meridians may be used in non-U.S. mapping. 2-1.4 Grids are applied to maps to provide a rectangular system for referencing and making measurements. There is a definite relationship between the grid and the graticule so that a corresponding geographic position can be determined for each grid position. 2-2 HORIZONTAL DATUMS
The identification, pertinent descriptive information, parameters, and attendant explanatory footnotes for some geodetic datums currently in use are contained in table 1. The datums preferred for use in the production of new and revised topographic maps, joint operations graphics, and selected large scale nautical charts are shown in Appendix D which also graphically depicts their areas of application. 2-3 TRANSFORMING COORDINATES FROM ONE HORIZONTAL DATUM TO ANOTHER HORIZONTAL DATUM.
2-3.1 Coordinates may be transformed from one geodetic datum to another geodetic datum by using the Abridged Molodenskiy Datum Transformation Formulas: where      Phi = geodetic latitude.
Lambda  = geodetic longitude
H = the distance of a point above or below the ellipsoid measured along the
ellipsoid normal through the point.
Table 1 (page 1): Geodetic Datums Used in Map Production Table 1 (page 2): Geodetic Datums Used in Map Production Table 1: (page 3 - footnotes): FOOTNOTES-GEODETIC DATUMS FOR MAP PRODUCTION The World Geodetic System (WGS) is not referenced to a single datum point. represents an ellipsoid whose placement, orientation, and dimensions best fit the Earth's equipotential surface which coincides with the geoid. The system was developed from a worldwide distribution of terrestrial gravity measurements and geodetic satellite observations. Several different ellipsoids have been used in conjunction with the various date WGS determinations. The dimensions of the WGS 72 Ellipsoid are: a = 6,378,135 meters f = 1/298.26 The dimensions of the WGS 84 Ellipsoid are: a = 6,378,137 meters
f = 1/298.25722 3563 This datum is not defined in terms of an origin. It results from a retriangulation of the area to a number of points whose latitude and longitude were known with respect to Greenwich. The dimensions of the Clarke 1880 Ellipsoid adopted by different countries vary in accordance with which of Clarke's original dimensions are used: (a, b) or (a, f), or which foot-meter relationship is used to convert the units from feet to meters. In the area referenced to Arc 1950 datum, the dimensions adopted are: Semimajor axis: a = 6,378,249.145326 meters
Semiminor axis: b = 6,356,514.966721 meters The above figures yield: Flattening: f = 1/293.4663076 In the areas of Merchich and Voirol datum, the dimensions adopted are: a = 6,378,249.2 meters
b = 6,356,515.0 meters and f = 1/293.46598 The values adopted by the Department of Defense are: a = 6,378,249.145 meters f = 1/293.465 The above figures yield: b = 6,356,514.8696 meters Dimensions of the War Office Ellipsoid derived by G. T. McCaw (1924) are: a = 6,378,300.58 meters f = 1/296. Local Astro refers to several independently determined datum origins or to areas where maps are positioned by a network of astronomic positions that are not interconnected. Table 1: Geodetic Datums Used in Map Production - End 2-3.2 Table 2 (Molodenskiy Transformation Constants to convert from local datum to WGS 84) lists the Delta X, Delta Y, Delta Z, Delta a, and Delta f to transform coordinates from the various datums shown in Appendix D to WGS 84. Values for a and f are listed with figure 1. 2-3.3 The direction of the transformation may be reversed by changing the signs of Delta X, Delta Y, Delta Z, Delta a, and Delta f. Note also that Rm and Rn must be computed with respect to the input ellipsoid. 2-3.4 Transformation procedures and constants are published in DMA TR 8350.2, Department of Defense World Geodetic System 1984. 2-4 ELLIPSOIDS.
2-4.1 Several ellipsoids are presently used in U.S. Military mapping. The goal is to eventually refer all positions to the World Geodetic System (WGS), which has a specific set of defining parameters, or to a WGS compatible ellipsoid. Ellipsoids may be defined by a combination of algebraically related dimensions such as the semi-major and semi- minor axes or the semi-major axis and the flattening. Figure 1 illustrates the defining elements and lists the dimensions of the ellipsoids used by the Defense Mapping Agency. 2-4.2 Appendix D (index of Preferred Grids, Datums, and Ellipsoids Specified for New Mapping) identifies the extent of currently effective ellipsoids. 2-5 PROJECTIONS
2-5.1 The projections used as the framework of all U.S. Military maps and charts have a common characteristic in that they are conformal. Conformality indicates that small areas retain their true shape; angles closely approximate their true values; and, at any point, the scale is the same in all directions. 2-5.2 Certain projections are prescribed for U.S. Military topographic mapping and charting that shows military grids: 2-5.2.1 Maps at scales of 1:500,000 and larger for areas between 80ï¿½ south and 84ï¿½ north, and some hydrographic charts at 1:50,000 and larger, are based on the Transverse Mercator Projection. Table 2 (page 1): Molodenskiy Transformation Constants to Convert from Local Datum to WGS 84 Table 2 (page 2): Molodenskiy Transformation Constants to Convert from Local Datum to WGS 84 Table 2 (page 3): Molodenskiy Transformation Constants to Convert from Local Datum to WGS 84 Figure 1. Defining Parameters of Ellipsoids 2-5.2.2 Maps at 1:1,000,000 scale between 80ï¿½ south and 84ï¿½ north, some hydrographic charts, and aeronautical charts at 1:500,000 between 80ï¿½ south and 80ï¿½ north, are based on the Lambert Conformal Conic Projection. 2-5.2.3 Maps at 1:1,000,000 scale and larger of the polar regions (south of 80ï¿½ south and north of 84ï¿½ north), some hydrographic charts smaller than 1:50,000 and at latitude between 70ï¿½ and the poles, and aeronautical charts at 1:500,000 north of 80ï¿½ north or south of 80ï¿½ south, are base, on the Polar Stereographic Projection. 2-5.2.4 Coastal charts at 1:75,000 scale and smaller are based on the Mercator Projection. 2-5.2.5 General maps at scales smaller than 1:1,000,000 are based on projections individually selected to conform with the intended use of the map. Because of their variety, complexity, and limited use, such projections are not described in this manual. 2-5.2.6 Maps produced by coproducing nations in non-U.S. areas of responsibility may be based on other projections such as the Transverse Mercator Projection, the Lambert Conical Orthomorphic Projection (Lambert Conformal Conic Projection), Laborde Projection, New Zealand Map Grid Projection, the Rectified Skew Orthomorphic Projection, etc. 2-5.3 The following paragraphs contain concepts of some of the prescribed projections; in practice, however, the projections are reduced to a plane surface by use of mathematical formulas. (See Chapter 1 for references to mathematical tables.) Figures 2, 3, 4, 5, and 6 are provided as an aid in the, understanding of these concepts. 2-5.4 The Mercator Projection is not normally used for military topographic maps; however, it is used extensively for naval ocean navigation and bathymetric charts. Its description also serves as a basis for understanding the Transverse Mercator Projection. The Mercator Projection can be visualized as an ellipsoid projected onto a cylinder with tangency established at the Equator and with the polar axis of the ellipsoid in coincidence with the cylinder axis as shown in figure 2. The origins of the projection lines vary and are about three-quarters of the way back along the diameters in the equatorial plane. When the cylinder is opened and flattened, a distortion appears in the polar regions, in as much as the line representing the Equator is the true distance and each parallel is represented by a line as long as the Equator. The poles are infinitely distant from the Equator and can not be shown on the projection. Distortion becomes more pronounced as the distance north and south of the Equator increases. For example, the map scale at 60ï¿½ north and 60ï¿½ south is approximately twice that at the Equator. 2-5.5 A Transverse Mercator Projection is a Mercator Projection where the cylinder has been rotated or transversed 90ï¿½. The ellipsoid and cylinder are thus tangent along a meridian. By projecting the surface of the ellipsoid onto the cylinder, as shown in figure 3, in the same manner as for the Mercator Projection, the Transverse Mercator Projection is developed on the surface of the cylinder, which is then opened and flattened. 2-5.5.1 Distortion - The east and west extremities appear distorted at the outer edges when projected onto a cylinder. The two shaded areas of figure 3 show the varying distortion of two equivalent geographic areas on the some projection. Note that both areas extend 15ï¿½in longitude within the 30ï¿½ to 45ï¿½ south latitude bond. The area bounded by the 30ï¿½ and 45ï¿½ east meridians is greatly magnified in comparison to the area bounded by the 90ï¿½ and 105ï¿½ east meridians. When a meridian is tangent to the cylinder of projection, there is no distortion along that meridian. Distances along the tangent meridians are true distances, and all distances within 3ï¿½ of the meridians are relatively accurate. Therefore, to minimize distortion, the Transverse Mercator Projection, for military purposes, uses 60 longitudinal zones, each zone 6ï¿½ wide. For example, a zone centered on 3ï¿½ (central meridian) is bounded by the Oï¿½ and 6ï¿½ meridians, and a zone centered on 9ï¿½ is bounded by the 6ï¿½ and 12ï¿½ meridians. Figure 2. Mercator Projection Figure 3. Transverse Mercator Projection Figure 4. Secant Condition of Transverse Mercator Projection; Typical 6-degree Projection Zone 2-5.5.2 Secant condition - The cylinder of projection is modified by reducing its elliptical dimensions and making it secant to the ellipsoid, intersecting the ellipsoid along lines parallel to the central meridian (fig. 4). For the Universal Transverse Mercator grid this condition establishes, in one 6ï¿½ zone, two lines of secancy approximately 180,000 meters east and west of the central meridian. These lines of seconcy, in effect, allow a more congruous relationship between ellipsoid and map distances than that of the central meridian tangency. Since the central meridian of all zones is given a false easting value of 500,000 meters east (mE), the secant lines have coordinates of approximately 320,000 mE and 680,000 mE respectively. Figure 4 also gives a schematic representation of the scale distortion in any 6ï¿½ zone. Note that the scale of the projection at the lines of secancy is exact. 2-5.5.3 Scale factor - For Most military operations, map and ground distances are assumed to be equivalent. However, in certain geodetic and artillery operations, where long distances are involved and accuracy of results is essential, it is necessary to correct for the difference between distances on the map and distances on the ground. This is done by the use of scale factors from prepared tables or by formula. For the Transverse Mercator Projection, the scale factor is 1.00000 (unity) at the lines of secancy, decreasing inwardly to 0.9996 at the central meridian, and increasing outwardly to about 1.0010 near the zone boundaries at The equator. 2-5.6 The Polar Stereographic Projection, a conformal azimuthal projection, is similar in both the northern and southern polar regions. The projection is developed on a plane tangent at a pole with the projection lines originating from the opposite pole. The plane is perpendicular to the minor axis, as shown in figure 5. For use with the Universal Polar Stereographic grid, a scale factor of 0.994 is applied at the origin (pole) to lower the plane of projection to intersect the sphere at approximately 81ï¿½07' latitude. This arbitrary geometry is applied to reduce the maximum scale distortion of the tangent projection. As shown in figure 5, the scale is exact (unity scale factor) at approximately 81'07' latitude. The scale factor decreases to 0.994 at the pole, increases to 1.0016076 at 80ï¿½00' and attains its maximum value of 1.0023916 at 79ï¿½30'. The scale factor is constant along any given parallel. 2-5.7 The Lambert Conformal Conic Projection can be visualized as the projection of the ellipsoid onto a cone whose axis coincides with the polar axis of the ellipsoid as in figure 6. Usually, the cone is secant to the ellipsoid, intersecting along two parallels of latitude. These two parallels are called standard parallels. Meridians appear as straight lines radiating from a point beyond the mapped areas. Parallels appear as arcs of concentric circles which are centered at the point from which the meridians radiate. None of the parallels appear in exactly the projected positions; they are mathematically adjusted to produce the property of conformality. This adjustment is slight if the standard parallels are sufficiently close together. 2-5.8 The characteristics of prescribed projections are tabulated in table 3. Figure 5. Polar Stereographic Projection Figure 6. Lambert Conformal Conic Projection Table 3. Characteristics of Projections 2-6 MILITARY GRIDS
2-6.1 Military grids consist of parallel lines intersecting at right angles and forming a regular series of squares. The north-south lines are called eastings and the east-west lines northings. Each grid line is one of an even-interval selection of measurement units. The interval is selected in accordance with the map scale. The unit intervals shown on military map scales are: MAP SCALES
1,000 or 10,000
100,000 with ticks at 10,000
Table 4. Grid Unit Intervals for Various Scale Topographic Maps. 2-6.2 The grids preferred for military maps are: 2-6.2.1 Universal Transverse Mercator (UTM) grid for areas between 80ï¿½ south and 84ï¿½ north. 2-6.2.2 Universal Polar Stereographic (UPS) grid for the polar regions south of 80ï¿½ south and north of 84ï¿½ north. 2-6.2.3 Other grids for certain parts of the world as shown in Appendix D. These grids are being progressively replaced by the UTM grid, with the intent to eventually cover all military mapping of the world with a universal metric grid system. 2-6.2.4 Area of application for the various other grids are given in Appendix D. A general description of the grids and numbering systems is given in Chapter 4. 2-6.3 Specifications for the Universal Grid Systems follow: 2-6.3.1 Universal Transverse Mercator (UTM) Grid. Projection: Transverse Mercator (Gauss-Kruger type) in zones 6ï¿½ wide. Ellipsoid:
Longitude of Origin: Central meridian (CM) of each projection zone (3ï¿½, 9ï¿½, 15ï¿½, 21ï¿½, 27ï¿½, 33ï¿½, 39ï¿½, 45ï¿½, 51ï¿½, 57ï¿½, 63ï¿½, 69ï¿½, 75ï¿½, 81ï¿½, 87ï¿½, 93ï¿½, 99ï¿½, 105ï¿½, 111ï¿½, 117ï¿½, 123ï¿½, 129ï¿½, 135ï¿½, 141ï¿½, 147ï¿½, 153ï¿½, 159ï¿½, 165ï¿½, 171ï¿½, 177ï¿½, E and W). Latitude of Origin: Oï¿½ (the Equator). Unit: Meter. False Northing: 0 meters at the Equator for the Northern Hemisphere; 10,000,000 meters at the Equator for the Southern Hemisphere. False Easting: 500,000 meters at the CM of each zone. Scale Factor at the Central Meridian: 0.9996. Grid Zone Designations: See Chapter 3 and Appendix B. Latitude Limits of System: From 80ï¿½S to 84ï¿½N. Limits of Projection Zones: The zones are bounded by meridians, the longitudes of which are multiples of 6ï¿½ east and west of the prime meridian. Overlap: On large-scale maps and trig lists, the data for each zone, datum, or ellipsoid overlaps the adjacent zone, datum, or ellipsoid a minimum of 40 kilometers. The UTM grid extends to 80ï¿½30'S and 84ï¿½30'N, providing a 30-minute overlap with the UPS grid. 2-6.3.2 Universal Polar Stereographic (UPS) Grid. Projection: Polar Stereographic. Ellipsoid: World Geodetic System 1984 Longitude of Origin: Oï¿½ and 180ï¿½E-W. Latitude of Origin: 90ï¿½N and 90ï¿½S. Unit: Meter. False Northing: 2,000,000 meters. False Easting: 2,000,000 meters. Scale Factor at the Origin: 0.994. Grid Zone Designations: See Chapter 3 and Appendix B. Limits of System:
North Zone: Polar area north of 84ï¿½N.
South Zone: Polar area south of 8Oï¿½S.
Overlap: The UPS grid extends to 83ï¿½30'N and 79ï¿½30'S, providing a 30-minute overlap with the UTM grid. 2-6.4 Formulas for constructing UTM and UPS grids are contained in DMA TM 8358.2. 2-7 TRANSFORMING COORDINATES FROM ONE GRID SYSTEM TO ANOTHER GRID SYSTEM.
Coordinates may be transformed from one grid system to another grid system, for instance, between a Lambert grid and a UTM grid or between different grid zones. The preferred procedure is to transform the grid coordinates from the first grid system to geographic positions. Then transform the geographic positions to grid coordinates of the second grid system. Note: This procedure does not change the datum. See paragraph 2-3 for the procedure to use when changing from one datum to another datum. CHAPTER 3 THE U.S. MILITARY GRID REFERENCE SYSTEM (MGRS) 3-1 GENERAL DESCRIPTION
3-1.1 The U.S. Military Grid Reference System (MGRS) is designed for use with the UTM and UPS grids. 3-1.2 For convenience, the world is generally divided into 6ï¿½ by 8ï¿½ geographic areas, each of which is given a unique identification, called the Grid Zone Designation (fig. 7). These areas are covered by a pattern of 100,000-meter squares. Each square is identified by two letters called tie 100,000-meter square identification. This identification is unique within the area covered by the Grid Zone Designation. Exceptions to this general rule have been made in the post to preserve the 100,000-meter identifications on mapping that already exists. Appendix B shows the method for finding the 100,000-meter square identifications. 3-1.3 A reference keyed to a gridded map of any scale is made by giving the 100,000- meter square identification together with the numerical location. Numerical references within the 100,000-mater square are given to the desired accuracy in terms of the easting (E) and northing (N) grid coordinates for the point. The Grid Zone Designation usually is prefixed to the identification when references are made in more than one grid zone designation area. 3-2 THE GRID NORTH DESIGNATION.
3.2.1 An MGRS position location uses the standard military practice of reading "right (easting) and up (northing)". In each portion of a military grid reference (grid zone designation, 100,000-meter square identification, and grid coordinates), the first part provides the easting component and the second part provides the northing component. 3.2.2 The MGRS is on alphanumeric version of a numerical UTM or UPS grid coordinate. 3-2.2.1 For that portion of the world where the UTM grid is specified (80ï¿½ south to 84ï¿½ north), the UTM grid zone number is the first element of a Military Grid reference. This number sets the zone longitude limits. Zone 32 has been widened to 9ï¿½ (at the expense of zone 31) between latitudes 56ï¿½ and 64ï¿½ to accommodate southwest Norway. Similarly, between 72ï¿½ and 84ï¿½, zones 33 and 35 have been widened to 12ï¿½ to accommodate Svalbard. To compensate for these 12ï¿½ wide zones, zones 31 and 37 are widened to 9ï¿½ and zones 32, 34, and 36 are eliminated. 3-2.2.2 The next element is a letter which designates a latitude bond. Beginning at 80ï¿½ south and proceeding northward, twenty bands are lettered C through X, omitting I and O. The bands are all 8ï¿½ wide except for bond X which Is 12ï¿½ wide. Thus, in the UTM portion of the MGRS, the first three characters designate one of the 1197 areas with the dimensions as shown in Table 5. 3-2.2.3 In the Polar regions, there is no zone number. A single letter designates the semicircular area and hemisphere. Since the letters A, B, Y, and Z are used only in the Polar regions, their presence in an MGRS, with the omission of a zone number, designates that the coordinates are UPS. Figure 7. Grid Zone Designations of the Military Grid Reference System 3-2.3 The grid zones are divided into a pattern of 100,000-meter grid squares forming a matrix of rows and columns. Each row and each column is sequentially lettered such that two letters provide, a unique identification, within approximately 9ï¿½, for each 100,000- meter grid square. Appendix B provides the location and identification of the grid zones and 100,000-meter grid squares. Latitude
Table 5. Dimensions of Grid Zone Designation Areas. 3-2.3.1 For many years efforts hove been made to reduce the complexity of grid reference systems by standardization to a single world-wide grid reference system. This effort is continuing and will generate additional changes to Appendixes B and D. 3-2.3.2 The remainder of this chapter describes the determination of the 100,000-meter square identification, and the military grid reference. 3-3 100,000-METER SQUARE IDENTIFICATION.
3-3.1 The 100,000-meter columns, including partial columns along zone, datum, and ellipsoid junctions, are lettered alphabetically, A through Z (with I and O omitted), north and south of the Equator, starting at the 180ï¿½ meridian and proceeding easterly for 18ï¿½. The alphabetical sequence repeats at 18ï¿½ intervals. 3-3.2 To prevent ambiguity of identifications along ellipsoid junctions changes in the order of the row letters are necessary. The row alphabet (second letter) is shifted ten letters. This decreased the maximum distance in which the 100,000-meter square identification is repeated. 3-3.3 The 100,000-meter row lettering is based on a 20-letter alphabetical sequence (A through V with I and O omitted). This alphabetical sequence is read from south to north, and repeated at 2,000,000-meter intervals from the Equator. 3-3.3.1 The row letters in each odd numbered 6ï¿½ grid zone are read in an A through V sequence from south to north. 3-3.3.2 In each even-numbered 6ï¿½ grid zone, the some lettering sequence is advanced five letters to F, continued sequentially through V and followed by A through V. 3-3.3.3 The advancement or staggering of row letters for the even-numbered zones lengthens the distance between 100,000-meter squares of the same identification. 3-3.4 Users are cautioned that deviations from the preceding rules were mode in the past. These deviations were an attempt to provide unique grid references within a complicated and disparate world-wide mapping system. 3-3.5 Determination of 100,000-meter grid square identification is further complicated by the use of different ellipsoids. Figure 8 shows the basic lettering system. Appendix B provides detailed guidance for finding the correct identification in each ellipsoid area. Figure 8. Basic Plan of the 100,000-meter Square Identifications of the U.S. Military Grid Reference System, Between 84ï¿½N and 80ï¿½S 3-4 THE MILITARY GRID REFERENCE.
3-4.1 The MGRS coordinate for a position consists of a group of letters and numbers which include the following elements: 3-4.1.1 The Grid Zone Designation. 3-4.1.2 The 100,000-meter square letter identification. 3-4.1.3 The grid coordinates (also referred to as rectangular coordinates); the numerical portion of the reference expressed to a desired refinement. 3-4.2 A reference is written as an entity without spaces, parentheses, dashes, or decimal points. Examples
(Locating a point within the Grid Zone Designation)
(Locating a point within a 100,000-meter square)
18SUU80
(Locating a point within a 10,000-meter square)
18SUU8401
(Locating a point within a 1,000-meter square)
18SUU836014
(Locating a point within a 100-meter square)
3-4.3 To satisfy special needs, a reference can be given to a 10-meter square and a 1-meter square as: 18SUU83630143
(Locating a point within a 10-meter square)
18SUU8362601432
(Locating a point within a 1-meter square)
3-5 MGRS APPLICATION.
3-5.1 All elements of a grid reference need not be used. Their use depends upon the size of the area of Activities, the type of military operations, and the scale of the map to which the reference is keyed. The military area commander usually designates the elements of the grid references to be used. The following paragraphs provide guidance for the use of Grid Zone Designations and 100,000-meter square identifications. 3-5.1.1 For military operations spanning large geographical areas, the Grid Zone Designation is usually given (such as IBS). This designation will alleviate ambiguity between identical references that may occur when reporting to a station outside the area. The Grid Zone Designation is always used in giving references on 1:1,000,000 scale and 1:500,000 scale maps. 3-5.1.2 For operational areas of lesser extent, but exceeding 100,000 meters, the 100,000-meter square identification is used (such as UU80). The 100,000-meter square identification is uses in reporting references on the 1:250,000 and larger scale maps to avoid ambiguity between identical references which occur every 100,000 motors, and near grid zone junctions and ellipsoid junctions. Figure 9. Method of Reading a U.S. Military Grid Reference from a 1:250,000 Scale Map 3-5.1.3 For small and localized operational areas, the Grid Zone Designations and 100,000-meter square identifications are not used, unless reporting falls within the parameters explained in preceding paragraphs. In the instance of local report only the numerical part of the grid reference is used (such as 836014). This condition applies to 1:100,000 scale maps and larger. 3-5.1.4 Topographic maps at scales 1:500,000 and larger provide a grid reference box with the elements and instructions for making a complete grid reference. Figure 10. Method of Reading a U.S. Military Grid Reference from a Large Scale Map 3.5.2 The numerical part of a grid reference always contains an even number of digits. The first half of the total number of digits represents the easting, and second half the northing. The standard military practice of reading "right (easting) and up (northing)" is employed. 3-5.2.1 To read the easting coordinate, locate the first easting (vertical) grid line to the left of the point of reference and read the large digit (or digits), the principal digit labeling the line either in the top or bottom margin or on the line itself. Smaller digits shown as part of a grid number are ignored. Estimate, or scale to the closest tenth of the grid interval, the distance between the easting grid line to the left of the point and the point itself. 3-5.2.2 The reading of the northing coordinate is made in a similar manner. Locate the first northing (horizontal) grid line below the point of reference and read the principal digits labeling the line located in the left or right margin or on the line itself. Then estimate, or scale to the closest tenth of the grid interval, the distance between the northing grid line below the point and the point itself. 3-5.2.3 The numerical part of a point reference taken from a 100,000-meter grid (on maps of 1:1,000,000 scale) is a two-digit number; for example: 80. Reading from left to right, the 8 represents the 10,000 digit of the first easting grid line (or grid tick) to the left of the point; the 0 represents the 10,000 digit of the first northing grid line (or grid tick) below the point. 3-5.2.4 The numerical part of a point reference taken from a 10,000-meter grid (on maps smaller than 1:100,000 scale and larger than 1:1,000,000 scale) is a four-digit number; for example: 8401. Reading from left to right, the 8 represents the 10,000 digit of the first easting grid line to the left of the point, the 4 represents the estimated tenths (nearest 1,000 meters) from the easting grid line to the point, the 0 represents the 10,000 digit of the first northing grid line below the point, and the 1 represents the estimated tenths (nearest 1,000 meters) from the northing grid line to the point. See figure 9. 3-5.2.5 Normally, the numerical part of a point reference taken from a 1,000-meter grid (on maps at scales of 1:100,000 and larger) is a six-digit number; for example: 836014. Reading from left to right, the 83 represents the 10,000 and 1,000 digits of the first easting grid line to the left of the point, the 6 represents the estimated or scaled tenths (nearest 100 meters) from the easting line to the point, the 01 represents the 10,000 and 1,000 digits of the first northing grid line below the point, and the 4 represents the estimated or scaled tenths (nearest 100 meters) from the northing grid line to the point. See figure 10. CHAPTER 4 THE NONSTANDARD SYSTEMS IN CURRENT USE
4-1 NONSTANDARD GRIDS ON MAPS AND CHARTS.
4-1.1 Nonstandard Grids. 4-1.1.1 There is no regular or uniform global plan for the various grids which make up the nonstandard grid systems. Some were originally developed by the native country and later conveniently adopted by the British and U.S. with or without modifications. Others are of British or French origin. The systems were devised or adopted at different times and, except in certain geographic areas, do not have a direct relationship with one another. Primary considerations in the selection of a grid were the projection, ellipsoid, origin, false coordinates for the origin, and limits which would best suit the particular area. Consequently, various projections and ellipsoids have been employed. Nomenclature, sizes, predominant directions, and outlines of the grids vary considerably. This is demonstrated in Appendix D, which illustrates the layout of the nonstandard grids. This displays what is currently specified for new products and maintenance. 4-1.1.2 The nomenclature for the nonstandard grids includes the terms grid, zone, and belt to characterize the systems. 4-1.1.2.1 A grid covers a relatively small area. Its limits consist of combinations of meridians, parallels, loxodomes (rhumb lines), or grid lines. The origin of each grid is arbitrary. It is generally located approximately in the center of the grid and may bear no relation to the origins of other grids or to those of adjacent grids. 4-1.1.2.2 A zone usually is wide in longitude and comparatively narrow in latitude. Its limits, which are regular or in a few cases but irregular in most, consist of parallels and meridians. Each zone has its own origin which, with some few exceptions, falls within the limits of the zone. There is no relation between the origins of the zones, although, in a regional geographic area, those of adjacent zones may be on a common meridian or parallel. 4-1.1.2.3 A belt originally referred to a grid that was extensive in latitude, but narrow in longitude. 4-1.1.3 Each grid, zone, and belt has a name. Where groups of adjacent grids or zones cover a regional geographic area, the some name may be used for each; distinction is preserved by adding either a cardinal point or a number and a letter to the name. 4-1.1.4 The unit of measure is either meters or yards. 4-1.1.5 Normally, a British grid or zone is divided into 500,000-unit squares with each square identified by a letter of the alphabet. In a square composed of twenty-five 500,000- unit squares the letters are arranged alphabetically (the letter I is omitted) in a left to right - top to bottom fashion. Each 500,000-unit is similarly divided into twenty-five 100,000-unit squared, each of which is Identified by a letter following the some plan as for the 500,000-unit squares. The Normal Lettering Plan is illustrated in figure 11. This basic lettering plan is repeated for India Zone IIIA where it exceeds 2,500,000 yards in easting. 4-1.1.6 Among the British grids, deviations from the normal lettering system exist for the Irish Transverse Mercator Grid. Figure 11. Normal Lettering Plan of the 500,000- 100,00-unit squares of the British Grid System 4-1.1.7 No letters are used for the Ceylon Belt, New Zealand Map Grid, Nord Algerie Grid, Nord Maroc Grid, Nord Tunisie Grid, Sud Algerie Grid, Sud Maroc Grid, and Sud Tunisie Grid. 4-1.1.8 The secondary grids are constantly changing. Specifications for those grids currently in this category are given in table 6. Table 6. Specifications for secondary grids. 4-1.1.9 The Gauss-Kruger (GK) projection and grids are the basis for the UTM grid system. Within the scope of this manual, there are three GK systems that may be encountered even though the Defense Mapping Agency uses none of them. The Russian GK grid is discussed in Department of the Army Field Manual No. 34-85, Conversion of Warsaw pact Grids to UTM Grids. General specifications are as follows: Projection: Transverse Mercator in zones 6" wide. Ellipsoid:  Krassovskiy (a = 6,378,245 meters, 1/f = 298.3) (U.S.S.R., China to 1981).
Geodetic Reference System of China 1980 (a = 6,378,140 meters,
1/f = 298.257) (China from 1981).
Bessel (Germany).
Longitude of Origin: Same as the UTM. Latitude of Origin: Same as the UTM. Unit: Meter. False Easting: 500,000 meter at the CM of each zone. However, the zone number is prefixed to the false easting In most cases, i.e. the false easting for the GK zone 7 is 7,500,000 meters. False Northing: Same as the UTM. Scale Factor on Central Meridian: Unity (1). Grid Zone Designations: The zones are numbered eastward from 1 to 60 starting at the Greenwich meridian rather than the 180' meridian. In other words, the UTM and GK zones differ by 30. Row letters are not used with the GK systems Limits of System: The limits north and south are not rigidly defined as with the UTM. However, the limits can be assumed to be similar to the UTM. Overlap: Same as the UTM., 4-1.1.10 The specifications for the nonstandard grids, including the various lettering systems, are shown later in this chapter. 4-1.2 Nonstandard Grids on Maps and Charts. 4-1.2.1 Maps at scales of 1:100,000 and larger are gridded at 1,000-unit intervals. Those at scales 1:250,000 and 1:500,000 are gridded at 10,000-unit intervals. Maps at scales 1:1,000,000 and smaller than 1:500,000 are gridded at 100,000-unit intervals intersected by ticks at 10,000-unit intervals. 4-1.2.2 Each grid line, except on maps at 1:1,000,000 scale, is labeled with its value in the margin and on the line itself. Maps at 1:1,000,000 scale are not labeled on the face of the map. In the margins, the grid values for each line are shown in two sizes of type. The larger digits - the principal digits - are the only digits to be used in determining a grid reference. On the face of the map, the grid lines are labeled with principal digits only. These grid-labeling practices are similar to those of the UTM and UPS grids. 4-1.2.2.1 The number of principal digits labeling the grid lines is dependent upon the particular grid and the interval of the grid lines. 4-1.2.2.2 With grids whose 100,000-unit squares ore identified by letters or numbers, the 10,000-unit or 100,000-unit interval grid lines are labeled with one principal digit only. This represents the 10,000 digit of the grid value. On maps in the same area whose grid lines appear at 1,000-unit intervals, the lines are labeled with two principal digits. These represent the 10,000 and 1,000 digits of the grid value. 4-1.2.2.3 Except the Ceylon Belt, the lines of grids whose 100,000-unit squares are not identified are labeled with two principal digits when the interval is 10,000 and with three principal digits when the interval is 1,000 units. At the 10,000-unit or 100,000- unit interval, the numbers represent the 100,000, 10,000, and 1,000 digits of the grid value. 4-1.2.2.4 With the Ceylon Belt, two principal digits are used, regardless of the interval of the grid lines. On maps gridded at 10,000- or 100,000-yard intervals, the numbers represent the 100,000 and 10,000 digits of the grid value. On maps gridded at 1,000- yard intervals, the numbers represent the 10,000 and 1,000 digits of the grid value. 4-1.2.3 The 100,000- and 500,000-unit square identifications are shown in several ways, depending upon the scale of the map. 4-1.2.3.1 On maps at British origin which are gridded at 10,000-unit intervals, a miniature representation of the 100,000-unit grid lines is printed in the index to adjoining sheets. Within each square is added the 100,000-unit square identification. If the 500,000-unit squares are identified, the identification is added in smaller type just before each 100,000- unit square identification such as sC. Similar identifications appear on the face of the map. These will be found either in the center or at the corners of each 100,000-unit square. Variations in these practices will often be encountered. 4-1.2.3.2 This same, plan is followed on maps of British origin which are gridded at 1,000-unit intervals, although in many cases it will be found that the identifications are omitted from the face of the map. 4-1.2.3.3 On U.S. maps containing nonstandard grids, a miniature representation of the sheet with 100,000-unit grid lines appears in the grid reference box which is part of the marginal data of the sheet. The appropriate 500,000- and 100,000-unit square identifications appear in each square of the miniature. These are written together, with the 500,000-unit square,identification appearing in smaller type, such as sC. Examples are illustrated in figure 27. Similar identifications appear on the face of maps gridded at 10,000-unit intervals. 4-1.3 Referencing Two basic methods for giving grid references are used on maps with nonstandard grid reference systems. These are modified in some instances. The first method, referred to as the normal British grid reference system, is used with grids whose 100,000- unit squares are identified by letters. The second method, referred to as the abnormal grid reference system, is used with grids whose 100,000-unit squares are not identified. 4-1.4 The Normal British Grid Reference System. 4-1.4.1 The instructions contained in this section apply only to those grids which adhere to the normal lettering plan. 4-1.4.2 The normal method for giving a reference based on a British grid is similar to that used for the U,S. Military Grid Reference System. See Figures 10 and 11. A reference consists of a group of letters and numbers which indicate (1) the 500,000-unit square identification, (2) the 100,000-unit square identification, and (3) the grid coordinates - the numerical portion of the reference - expressed to a prescribed refinement. It is desirable to leave a space between letters and numbers. Examples:
(Locating a point within a 10,000-unit square)
NT 6354
(Locating a point within a 1,000-unit square)
NT 632543
(Locating a point within a 100-unit square)
4-1.4.3 The use of the letters of the 500,000- and 100,000-unit square identifications depends on the size of the area of operations. The above examples of reporting are desirable when reporting between 500,000-unit squares so that ambiguity in letter identifications may be avoided. However, when all reporting is within a 500,000-unit square, the 500,000-unit square identification letter may be dropped, and the 100,000-unit square identification is retained to avoid ambiguity in numerical coordinates. When the area of operations is completely localized within a 100,000-unit square, both the 500,000- and 100,000-unit square identifications may be dropped. 4-1.5 Exceptions to the Normal British Grid Reference System. 4-1.5.1 The letter I is used as the 500,000-meter square letter with the Irish Transverse Mercator. 4-1.5.2 No 500,000- and 100,000-meter square letters are used with the New Zealand Map Grid. To avoid ambiguity, references are prefixed with the sheet number. A space separates the sheet number from the numerical reference. Examples:
Z15 894623
(Locating a point within a 1,000-meter square at 1:50,000 scale)
Sht 5 989362
(Locating a point within a 10,000-meter square at 1:250,000 scale)
4-1.6 The Abnormal Grid Reference System. 4-1.6.1 The abnormal grid reference system is used when 100,000-unit squares are not identified, as with the Madagascar grid and the Lambert Grids of northwestern Africa. The reference usually is expressed in terms of grid coordinates only and is determined in the same manner as that used with the normal British grid reference system. The number of digits in the reference depends upon the grid interval and the grid itself. 4-1.6.2 Except for the Ceylon Belt, an abnormal reference taken from a map gridded at 100,000-meter intervals consists of four digits; at 10,000 meters, six digits; and for 1,000-meter intervals, eight digits. Examples:
86324543
4-1.6.3 References based on the Ceylon Belt use four digits on maps gridded at 100,000- yard intervals and six digits for all other grid intervals. Examples:
Reference from map gridded at 100,000-yard intervals.
3524 (Locating a point within a 10,000-yard square)
Reference from map gridded at 10,000-yard intervals.
347241 (Locating a point within a 1,000-yard square)
Reference from map gridded at 1,000-yard intervals.
472413 (Locating C, point within a 100-yard square)
4-1.6.3.1 The Ceylon Belt grid reference system has a distinct disadvantage. Ambiguity between references is possible when six-digit reporting covers an area exceeding 100,000- yards square. 4-1.6.3.2 No official method is provided for preserving a distinction between the references. In practice, various devices have been used, such as prefixing the reference with the scale, name, or number of the map from which the reference was taken. 4-1.6.3.3 On maps prepared by the United States, the grid reference box will contain instructions for preserving distinctions. Normally, this will require prefixing the numerical reference with the sheet number of the map from which the reference was taken. 4-1.7 Unique Reporting. Nonstandard reference systems, unlike the U.S. Military Grid Reference System, make no provisions for worldwide reporting. It may be necessary to identify the general areas in terms of geographic coordinates before giving the grid references for the separate general areas. 4-2 DIAGRAMS OF NONSTANDARD GRIDS.
The following pages show the diagrams and specifications of nonstandard grids used as the primary or secondary grid on maps produced by DMA: Page 4-8 British National Grid Page 4-9 Junction with Irish Transverse Mercator Grid Page 4-10 Ceylon Belt page 4-11 India Zone I Page 4-12 India Zone IIA Page 4-13 India Zone IIB Page 4-14 India Zone IIIA Page 4-15 India Zone IIIB Page 4-16 India Zone IVA Page 4-17 India Zone IVB Page 4-18 Irish Transverse Mercator Grid Page 4-19 Madagascar Grid Page 4-20 Netherlands East Indies Equatorial Zone Page 4-21 New Zealand Map Grid (NZMG) Page 4-22 Nord Algerie Grid Page 4-23 Nord Maroc Grid Page 4-24 Nord Tunisie Grid Page 4-25 Sud Algerie Grid Page 4-26 Sud Maroc Grid Page 4-27 Sud Tunisie Grid Page 4-28 West Malaysian RSO Grid CHAPTER 5 GEOGRAPHIC COORDINATE REFERENCES 5-1 USE.
The use of geographic coordinates as a system of reference is accepted worldwide. It is based on the expression of position by latitude (parallels) and longitude (meridians) in terms of arc (degrees, minutes, and seconds) referred to the Equator (north and south) and a prime meridian (east and west). 5-2 THE GEOGRAPHIC REFERENCE.
The degree of accuracy of a geographic reference is influenced by the map scale and accuracy requirements for plotting and scaling purposes. Examples of references are:
40ï¿½N 132ï¿½E (in degrees of latitude and longitude)
40ï¿½21'N 132ï¿½14' (To minutes of latitude and longitude)
40ï¿½21'12"N 132ï¿½14'18"E (To seconds of latitude and longitude)
40ï¿½21'12.4"N 132ï¿½14'17.7"E (To tenths of seconds of latitude and longitude)
40ï¿½21'12.45"N 132ï¿½14'17.73"E (To hundredths of seconds of latitude and longitude)
5-3 GEOGRAPHIC COORDINATES ON MAPS AND CHARTS.
5-3.1 U.S. military maps and charts include a graticule (parallels and meridians) for plotting and scaling geographic coordinates. Graticule values are shown in the map margin. 5-3.2 On most maps and charts at the scale of 1:1,000,000, the parallels and meridians are shown by intersections or full lines at one-degree intervals. The intersections or lines are labeled in degree values. 5-3.3 On maps and charts at the scale of 1:500,000, parallels and meridians are shown by full lines at 30-minute intervals. The full degree lines are labeled in degree values; the intermediate lines are labeled in minutes only. 5-3.4 On maps and charts at scales of 1:250,000 and larger the graticule may be indicated in the map interior by lines or ticks at prescribed intervals. The following indicates these intervals: Scale
Labeling at Corners1
Labeling of ticks
Table 7. Corner Labeling on Topographic Maps. 1 When departing from standard sheet lines to avoid unnecessary sheets or because of datum changes, corners are labeled to 1 second for 1:250,000 and 1:100,000 scale and to 0.1 second for 1:50,000 to 1:12,500 scale. Figure 12. World Geographic Reference (GEOREF) System. 5-3.5 On Joint Operations Graphics (JOG), between Oï¿½ and 76ï¿½, meridians are shown by full lines at 15-minute intervals with 1-minute ticks. Between 76ï¿½ and 84ï¿½ North and between 76ï¿½ and 80ï¿½ South, meridians are shown by full lines at 30 minute intervals with 1-minute ticks. 5-4 THE WORLD GEOGRAPHIC REFERENCE SYSTEM
5-4.1 The World Geographic Reference System (GEOREF) is a system used for position reporting. It is not a military grid, and therefore does not replace existing military grids. It is an area-designation method used for interservice and interallied position reporting for air defense and strategic air operations. Positions are expressed in a form suitable for reporting and plotting on any map or chart graduated in latitude and longitude regardless of map projection. 5-4.2 The system divides the surface of the earth into quadrangles, the sides of which are specific arc lengths of longitude and latitude; each quadrangle is identified by a simple systematic letter code giving positive identification with no risk of ambiguity. 5-4.2.1 There are 24 longitudinal zones each of 15 degrees width extending eastward from the 180ï¿½ meridian around the globe through 360 degrees of longitude. These zones are lettered from A to Z inclusive (omitting I and O). There are 12 bands of latitude each of 15 degrees height, extending northward from the South Pole. These bands are lettered from A to M inclusive (omitting I) northward from the South Pole. This code divides the earth's surface into 288 15 degree quadrangles, each of which is identified by two letters. The first letter is that of the longitude zone and the second letter that of the latitude band. Thus the major part of the United Kingdom is in the 15 degree quadrangle MK. See figure 12. 5-4.2.2 Each 15 degree quadrangle is sub-divided into 15 one degree zones of longitude, eastward from the western meridian of the quadrangle, these one degree units being lettered from A to Q inclusive (omitting I and O). Each 15 degree quadrangle is also subdivided into 15 one degree bands of latitude northward from the southern parallel of the quadrangle, these bands being lettered from A to Q inclusive (omitting I and O). A one degree quadrangle anywhere on the earth's surface may now be identified by four letters. Salisbury therefore is in the one degree quadrangle MKPG. See figure 12. 5-4.2.3 Each one degree quadrangle is divided into 60 minutes of longitude, numbered eastward from its western meridian, and 60 minutes of latitude, numbered northward from its southern parallel. This direction of numbering is used wherever the one degree quadrangle is located,i.e., it does not vary even though the location may be west of the prime meridian or south of the equator. A unique reference defining the position of a point to an accuracy of one minute in latitude and longitude (i.e., 2 kms or less) can now be given by quoting four letters and four numerals. The four letters identify the one degree quadrangle. The first two numerals are the number of minutes of longitude by which the point lies eastward of the western meridian of the one degree quadrangle, and the last two numerals are the number of minutes of latitude by which the point lies northward of the southern parallel of the one degree quadrangle. if the number of minutes is less than 10 minutes, the first numeral will be a zero and must be written, e.g., 04. The GEOREF of Salisbury Cathedral is MK PG 12 04. See figure 12. 5-4.2.4 Each of the one degree quadrangles may be further divided into decimal parts (1/10 th and 1/100 th) eastward and northward. Thus, four letters and six numerals will define a location to 0.1-minute; four letters and eight numerals will define a location to 0.01-minute. CHAPTER 6 PORTRAYAL OF GRIDS ON MAPS AT 1:100,000 SCALE AND LARGER 6-1 GENERAL.
6-1.1 Requirements for grid data and grid formats on maps prepared for the DoD at 1:100,000 scale and larger are essentially the same for Universal Transverse Mercator grids, Universal Polar Stereographic grids and nonstandard grids. 6-1.2 The grid data for DoD maps usually include the major grid, a declination diagram, a grid reference box, and notes identifying the grid. 6-1.3 The adjacent grid is provided as an overlapping grid when a map lies within approximately 40 kilometers of a grid junction line or a datum junction boundary. A separate declination diagram and notes identifying the overlapping grid appear in the margin for grid junctions, and may or may not appear for datum junctions, depending on grid alignments. 6-1.4 A map may show a secondary grid which occurs in the area. The secondary grid is identified by margin notes. 6-1.5 Normally, no single map of a foreign area in this scale category ever shows more than three grids. When a sheet covers an area which includes more than three grids (either major, overlapping, or secondary), those omitted are the ones which are considered of least military importance. Major grids are never omitted. When choice lies between two overlapping grids, the one retained usually is the one which occurs most frequently on the sheets in the general, area. Domestic maps may show up to five grids. 6-1.6 Specific dimensions, size and style of type, and placement of margin data relating to grids and grid formats at 1:100,000 scale and larger are contained in DMA product specifications. 6-2 THE MAJOR GRID 6-2.1 The major grid is indicated by full lines at 1,000-unit intervals. Every 10,000-unit grid line is accentuated in weight. 6-2.2 Grid numbers appear outside the neatline on all four sides of the sheet, labeling each grid line. Where a grid line coincides with a neatline of the map, the grid line is omitted, but the neatline is labeled in the margin with the values for the grid line. 6-2.3 Basically, all grid lines are labeled with two principal digits which represent the 10,000- and 1,000-unit values of the grid line, respectively. Some variations to this basic labeling are: 6-2.3.1 On all 10,000-unit grid lines, the basic two principal digits are preceded by the 100,000-unit digits. See figures 13 and 14. 6-2.3.2 On sheets with one major grid, only the first grid lines in each direction from the southwest corner are given full coordinate values. See figures 13 and 14. 6-2.3.3 On sheets containing grid zone junctions, junctions of major grids, or datum junctions, the first grid lines in each direction from all four corners are given full coordinate values. See figures 15, 16, and 18. Figure 13. The Major Grid as Shown on a 1:50,000 Scale Map 6-2.3.4 On sheets showing the major and overlapping grids, the first grid line and grid tick in each direction from the southwest corner are given the full coordinate values for both grids. See figure 17. 6-2.3.5 On the Madagascar grid and the Lambert grids of northwest Africa, use three principal digits to represent the 100,000-, 10,000-, and 1,000-meter values of the grid lines. 6-2.4 The grid lines in the map interior contain a pattern of grid value labels (principal digits) designed to assist in position referencing on a folded map. The pattern, referred to as a grid ladder, may appear in either of two forms: 6-2.4.1 One row (easting) and one column (northing) intersecting at the approximate center of the sheet. 6-2.4.2 Two rows (easting) and two columns (northing) intersecting at approximate one- third intervals across the sheet. The principal digits are centered between adjacent horizontal (northing) and vertical (easting) grid lines. The digits may be displaced or omitted if they impair the legibility of important map detail. Omissions are held to a minimum. Grid ladder treatments are illustrated in figures 13 and 14. 6-2.5 The color of the grid values is governed by the grid system. 6-2.5.1 Black (blue for 1:100,000 scale) is used when the major grid is the Universal Transverse Mercator or the Universal Polar Stereographic. 6-2.5.2 With nonstandard grids, the color varies. It may be black, blue, or red-brown. The color to be used with each particular nonstandard grid is specified in Chapter 4. 6-2.6 A note identifying the grid and ellipsoid appears in the lower margin of a sheet. The note is modeled after one of the following:           ELLIPSOID......................................BESSEL
GRID..........................1,000 METER UTM ZONE 53
(BLACK NUMBERED LINES)
ELLIPSOID..............................INTERNATIONAL
GRID...........................1,000 METER MADAGASCAR
(RED-BROWN NUMBERED LINES)
6-2.7 On maps having a land inset for which the grid or grid zone differs from that of the map proper, the appropriate grid note is shown within the inset. 6-2.8 Figures 13 and 14 illustrate the treatment for the major grid on DoD mapping at 1:50,000 and 1:100,000 scales. 6-3 MULTIPLE MAJOR GRIDS.
6-3.1 In certain instances a sheet contains more than one major grid. 6-3.1.1 With the UTM and UPS grids this may occur: 6-3.1.1.1 Where original sheet lines are retained as established by a mapping agency of a foreign country. 6-3.1.1.2 Where a sheet is shifted from the normal position to avoid making additional sheets. 6-3.1.2 With nonstandard grids, this condition occurs more frequently since, in addition to the above cases, grid junctions are sometimes loxodromes or are grid lines. Figure 14. The Major Grid as Shown on a 1:100,000 Scale Map. Figure 15. Two Major Grids (in this case, Zones of UTM) Separated by at Grid Junction as Shown on a Large Scale Map Figure 16. Three Major Nonstandard Grids as Shown on a Large Scale Map Figure 17. Major and Overlapping Grids as Shown on a Large Scale Map Figure 18. Overlapping Grid in Combination with Two Major Grids Separated by a Grid Junction as Shown on a Large Scale Map 6-3.2 Grid, datum, ellipsoid, and zone junctions are indicated by accentuated lines, printed in black (blue for 1:100,000 scale). Labels identifying the junction appear parallel to and on each side of the junction line. The label may be shown more than once to facilitate identification. Each label is printed in the color designated for the particular grid system. When a grid, datum, ellipsoid, or zone junction line is coincident with a neatline, both the junction line and the identifying labels are omitted. If the junction line falls within 2.5 mm (0.10 inch) of the neatline, the junction line is not shown; it is considered as being coincident with the neatline. 6-3.2.1 For nonstandard grids, the label is modeled after the following:         WEST MALAYSIAN RSO GRID
6-3.2.2 The label for a UTM grid junction, or a UPS grid junction, includes the identification of the Grid Zone Designation and is written in MGRS terms as:         UTM GRID ZONE DESIGNATION: 47T
6-3.3 Each grid is shown by full lines Within its own area only, being represented at 1,000-unit intervals with every 10,000-unit line accentuated in weight. 6-3.3.1 On maps bearing two major grids, the extension of either grid into the area of the other (overlapping grid) is shown by outside ticks emanating from the neatline correctly aligned with its respective major grid. The even 10,000-unit ticks are accentuated in weight. 6-3.3.2 On maps bearing three major grids, a similar practice is followed, except that outside ticks are used to indicate the extension of the grid which occupies the major part of the sheet, and inside ticks are used to indicate the extensions of the others. 6-3.4 Grid values appear on all four sides of the sheet labeling each grid line and those grid ticks whose values are multiples of 5,000. Full values appear at each corner, labeling the first grid line in each direction from the corner. 6-3.4.1 For the UTM and UPS grids, the values for the different grids appear in black and blue. Block is reserved for the grid which covers the greater portion of the sheet. If the grid junction divides the sheet equally, black is used for the grid which occurs most frequently on the sheets in the general area. On maps at 1:100,000 scale, blue is used for the dominant grid and red-brown for the other grid. 6-3.4.2 For nonstandard grids, the values appear in the colors designated for the grid system. Where the designated colors are the same, one or more substitutions are made to emphasize distinction, with the order of preference as follows: black, blue, red-brown (or blue, red-brown, black at 1:100,000 scale). 6-3.4.3 Black is used for the UTM or UPS grids when either appears in combination with nonstandard grids. In such cases, if the conventional color for a nonstandard grid is black, a substitution is made for the nonstandard grid with blue, or red-brown being used. On maps at 1:100,000 scale, the order of colors is blue, red-brown, black. 6-3.5 Grid values, expressed in principal digits only, appear on the face of the map labeling each grid line. Refer to figures 15, 16, and 18 for sample treatments of the grid ladder numbers when a sheet contains more than one major grid. 6-3.6 Notes identifying each grid appear in the lower margin of the sheet. The notes are modeled after the following:        ELLIPSOID......................................WORLD GEODETIC SYSTEM
GRID.........................................1,000 METER UTM ZONE 47
(BLACK NUMBERED LINES AND TICKS)
1,000 METER UTM ZONE 48
(BLUE NUMBERED LINES AND TICKS)
6-3.7 When the ellipsoid is not the same for each of the grids shown on the map, the ellipsoids are included with the grid notes. The notes are patterned after the following:        GRID................1,000 METER UTM ZONE 31, INTERNATIONAL ELLIPSOID
1,000 METER UTM ZONE 32, CLARKE 1880 ELLIPSOID
6-3.8 Figures 15 and 16 illustrate the treatments described for sheets containing more than one major grid. 6-4 OVERLAPPING GRIDS.
6-4.1 An overlapping is generally required within approximately 40 kilometers of a grid, zone, or ellipsoid junction. The overlapping grid may be omitted if there are no land bodies within the 40 kilometer overlap area. See table 8. 6-4.2 The overlapping grid is shown by ticks printed in black (blue for 1:100,000 scale) emanating from the neatline correctly aligned with its respective grid and spaced at 1,000- unit intervals. The even 10,000-unit ticks are accentuated in weight. The direction of the ticks from the neatline (i.e., inside or outside) is dependent on the other grids shown on the map. 6-4.2.1 If the sheet contains one major grid, outside ticks are used. 6-4.2.2 If the sheet contains two major grids, inside ticks are used. 6-4.2.3 If a sheet contains two overlapping grids in conjunction with a single major grid, outside ticks are used for the overlapping grid which occurs most frequently on the sheets in the general area. Inside ticks are used for the other. 6-4.3 Values, similar in composition to those labeling the major grid lines, appear on all four sides of the sheet. The first grid tick in each direction from the southwest corner of the sheet whose values are multiples of 5,000 are labeled. 6-4.4 The color of the overlapping grid values is governed by the grid system. Where the prescribed color for two overlapping grids is the same, the color of the grid which occurs more frequently on the sheets in the general area is retained, and a substitution of black, blue, or red-brown, in that order of preference, is made for the other. (The order of preference for 1:100,000 scale is blue, red-brown, or black.) A similar substitution is made when the color of and overlapping grid is the some as the major grid. 6-4.5 Notes identifying overlapping grids appear in the lower margin of each sheet. Table 8. The equivalents of 40 kilometers when measured along a given parallel of latitude expressed in degrees, minutes, and seconds of longitude. 6-4.6 When the ellipsoid is not the same for the overlapping grid and the major grid, the ellipsoids are included with the grid notes. The notes are patterned after the following:      GRIDS....................1,000 METER UTM ZONE 42, WORLD GEODETIC SYSTEM
ELLIPSOID (BLACK NUMBERED LINES)
1,000 METER UTM ZONE 41, INTERNATIONAL
ELLIPSOID (BLUE NUMBERED TICKS)
6-4.7 Figures 17 and 18 illustrate the treatments described for sheets containing major and overlapping grids. 6-5 SECONDARY GRIDS.
6-5.1 Secondary grids are temporary grids whose purpose is to provide a common grid to adjacent maps and on companion maps of different scales. Generally, after one printing of the secondary grid, it will be discontinued. Excepted are those instances where mapping arrangements with cooperating foreign agencies specify the showing of a secondary grid. No more than one secondary grid is shown. 6-5.2 When required, the secondary grid is shown by inside ticks, printed in black (blue for 1:100,000 scale), emanating from the neatline in their correct alignment and spaced at -1,000-unit intervals. The even 10,000-unit ticks are accentuated in weight. 6-5.3 Values, similar in composition to those labeling the major grid lines, appear on all four sides of the sheet. The first grid tick. In each direction from the southwest corner of the sheet is labeled with full values. Thereafter, only those grid ticks whose values are multiples of 5,000 are labeled. If the secondary grid has a prescribed color, the color is used for the numbers unless there is conflict with another grid shown on the map. In that event, substitutions are made in the established order of preference. 6-5.4 A grid note, identifying the secondary grid, appears in the margin of the sheet. 6-5.5 When a secondary grid differs uniformly from the major grid, a coordinate shift note may be used in lieu of showing the secondary grid. The note should be patterned after the following: COORDINATE CONVERSION WGS 84 TO ED
Grid Add 30m.E., Subtract 9m.N.
Geographic:  Add 1.1" Long., Subtract 0.1" Lat.
6-5.6 Figure 19 illustrates the treatment described for sheets containing major and secondary grids. 6-6 THE DECLINATION DIAGRAM (ONE GRID).
6-6.1 A declination diagram appears in the margin of each sheet. The diagram shows the relationship of magnetic north and true north to grid north at the center of the sheet. It also provides information regarding the use of this data. See figures 20 and 21. 6-6.2 The diagram contains three prongs which emanate from a central point. These represent grid north, magnetic north, and true north, and are appropriately labeled. 6-6.2.1 The grid north prong is an extension of an easting (vertical) grid line; the extension is a continuous line, which stops at the central point near the bottom work limits of the sheet. The prong is broken for the letters GN. 6-6.2.2 The magnetic north prong emanates from the central point to the approximate extent of the letters GN. It Is surmounted with a half-arrowhead; a left half-arrowhead is used when magnetic north lies to the west of grid north, while a right half-arrowhead is used when magnetic north lies to the east of grid north. Figure 19. Major and Secondary (Obsolete) Grids as Shown on a Large Scale Map Figure 20. The Declination Diagram and Accompanying Notes with True North Appearing as the Center Prong. 6-6.2.3 The true north prong, surmounted with a five-point star, is shorter in length than the other two prongs. When it occurs as the left or right prong of the diagram, it emanates from the central point. When true north occurs as the middle prong, its characteristic star appears at the approximate height of the magnetic north arrowhead; the prong is shown as an extension from the central point. 6-6.2.4 Angles between the prongs are approximately represented. The magnetic north and true north prongs are plotted within 30 minutes of their given angular position from grid north, except that the magnetic prong is never shown within three degrees of the grid north prong. In maintaining relative symmetry between prongs, the characteristic star of the true north prong must never touch another prong. When there is no declination between prongs, a single prong represents the coincidence, and distinguishing characteristics (star, full arrowhead, or letters GN) of each are shown on the composite prong. Figure 21. The Declination Diagram and Accompanying Notes with True North Appearing as an Outside Prong. 6-6.3 The grid-magnetic angle (G-M Angle) is expressed by a note alongside a dashed arc connecting the grid north and magnetic north prongs. The value of this angle is derived from the latest isogonic data for a standard epoch; i.e., a year that is divisible by five, such as 1990, 1995, etc. The value of the grid-magnetic angle is given to the nearest one-half degree with mil equivalent to the nearest ten mils. See Appendix A for a table of mil equivalents. 6-6.3.1 The grid-magnetic note is modeled after the following: 1990
G-M ANGLE
7 1/2ï¿½ (130 MILS)
6-6.3.2 For sheets with 0ï¿½ grid-magnetic angle the note is shown as follows: 1990
0 (0 MILS)
6-6.3.3 For land insets, grid-magnetic data are shown only when the angle is different from that for the map proper. A diagram is not shown. The grid-magnetic data are shown by a note modeled after the following: GRID TO MAGNETIC DECLINATION
FOR 1990 IS 1 1/2ï¿½ (30 MILS)
WESTERLY OVER THE ENTIRE INSET
6-6.4 The grid convergence is the angle between grid north and true north. The value of the angle is expressed to the nearest full minute, with the mils equivalent to the nearest one-half mil. 6-6.4.1 In the diagram, the grid convergence is indicated by a note alongside a dashed arc which connects the grid north and true north prongs. The convergence angle is given for the center of the sheet and is modeled after the following: GRID CONVERGENCE
1ï¿½ 19' (23 1/2 MILS)
FOR CENTER OF SHEET
6-6.4.2 In land insets, a diagram is not shown. The grid convergence is shown only when the angle is different from that on the map proper. The convergence angle is given for the center of the inset and is modeled after the following: GRID TO TRUE NORTH CONVERGENCE
FOR THE CENTER OF THE INSET IS
1ï¿½ 54' (34 MILS) EASTERLY
6-6.5 Notes appear in conjunction with the diagram explaining the use of the G-M Angle. 6-6.5.1 When the magnetic north prong of the diagram is east of the grid north prong, the notes read as follows: TO CONVERT A
TO A GRID AZIMUTH
ADD G-M ANGLE
GRID AZIMUTH TO A
SUBTRACT G-M ANGLE
6-6.5.2 When the magnetic north prong of the diagram is West of the grid north prong, the notes read as follows: TO CONVERT A
6-6.5.3 When the magnetic north and grid north prongs are coincident, azimuth conversion notes are omitted. 6-6.5.4 Azimuth conversion notes are not shown for insets. 6-6.6 The diagram and related notes are printed in the some color as the grid values. 6-7 THE DECLINATION DIAGRAM (MORE THAN ONE GRID).
6-8.1 A grid reference box appears in the margin of each sheet. The box contains instructions and attendant data to enable the user to compose standard grid references. 6-8.2 The grid system(s) in use on the map dictates the referencing instructions contained in the grid reference box. The grid reference boxes most commonly used on maps, 1:100,000 scale and larger, are illustrated in figure 23. The boxes are subject to modifications. 6-8.3 The grid reference box also contains diagrams identifying applicable grid zone designations and grid square identifications. Figure 22. The Declination Data when a Sheet Contains an Overlapping Grid and/or More Than One Major Grid. 6-8.3.1 For the UTM and UPS grids, the diagrams show the grid zone designation, the l00,000-meter grid lines and their values in abbreviated form, and the 100,000-meter square identifications). Figure 24 illustrates the composition of the diagrams under various conditions. 6-8.3.2 For nonstandard grids, the diagram shows the 100,000-unit square identifications and the values of the 100,000-unit grid lines in abbreviated form. These data are printed in the same color as the grid values to which they pertain. If the grid system identifies larger squares, their identifications are shown in smaller type just preceding the 100,000-unit identifications. The 100,000-unit grid lines and grid junction lines are printed in black (blue at 1:100,000 scale). If a junction is a grid line, its value Is shown in abbreviated form and printed in the same color as the grid values to which it pertains. Loxodromes are not labeled. Figure 25 illustrates the composition of this information under various conditions. Figure 23. Grid Reference Boxes Most Commonly Used on Maps at Scales of 1:100,000 and Larger. Figure 24. Methods of Showing Grid Zone Designations and 100,000-meter Squares of the UTM in the Grid Reference Boxes of Large Scale Maps 6-8.3.3 For sheets that have a land inset whose l00,00-unit square identification letters differ from those of the map proper, the identification letters are shown in the interior of the inset, rather than in the grid reference box. 6-8.4 When more than one major grid appears on a sheet and the method for giving a reference is the same for all the grids, a common reference box is used. 6-8.5 When more than one major grid appears on a sheet and the method for giving a reference varies with the grids, circumstances control the treatment of the grid reference boxes. 6-8.5.1 A grid reference box is shown in the margin for each grid. Over each box appears a note limiting the use of the box to the grid or grids concerned. 6-8.5.1.1 When each box describes the method of referencing for one grid only, the note is printed in the same color as the values for its respective grid and is modeled after the following: USE THIS BOX FOR GIVING REFERENCES ON THE
Figure 25. Methods of Showing 100,000-unit, and Larger, Square Identifications of Nonstandard Grids in the Grid Reference Boxes of the Large Scale Maps. 6-8.5.1.2 When the same system of referencing is used for two grids occurring in the same sheet with a third grid which uses a different reference system, the note for the common reference box is printed in black and modeled after the following: USE THIS BOX FOR GIVING REFERENCES ON THE
6-8.5.2 When all reference boxes cannot be accommodated in the margin, the excess is shown in expanses of open water on the face of the map. When this is not practicable, a note which refers the user to an adjacent sheet is added to a reference box in the margin. The notes are modeled after the following: USE THIS BOX FOR GIVING REFERENCES ON THE
PORTRAYAL OF GRIDS ON MAPS AT 1:250,000 AND 1:500,000 SCALE 7-1 GENERAL.
7-3.1 In certain instances a sheet contains more than one major grid. 7-3.1.1 With the UTM and UPS grids this may occur: 7-3.1.1.1 Where a sheet is shifted from the normal position to avoid making additional sheets. 7-3.1.1.2 In higher latitudes, where sheets may be wide in longitudinal extent. 7-3.1.1.3 At datum junctions. 7-3.1.2 With nonstandard grids, this condition occurs more frequently since grid junctions are sometimes loxodromes or are grid lines not coincident with parallels or meridians. 7-3.2 Grid, datum, ellipsoid, and zone junctions are indicated by accentuated lines printed in blue. Labels may appear on each side of the junction line. The labels may be shown more than once to facilitate identification. Each label is printed in the color designated for the particular grid system. Where a grid, datum, ellipsoid, or zone junction line is coincident with a neatline, both the junction line and the identifying labels are omitted. 7-3.2.1 For nonstandard grids, the label is modeled after the following: BRITISH NATIONAL GRID
7-3.11 In certain cases, a sheet bearing the UTM grid may straddle a parallel which marks the division between different grid zone designations. The grid and corresponding labeling appear as previous described. A continuous line in black indicates the dividing parallel. The proper grid zone designations, printed in the same color as the grid values, appear on each side of the line. The dividing parallel is omitted when it falls within 2.5 mm (0.10inch) of the north or south neatlines. Figure 31 illustrates these principles.
7-4 OVERLAPPING AND EXTENDED GRIDS
7-5.1 Secondary grids are seldom shown on JOGs. As a general rule, secondary grids are no longer required on military topographic maps. Excepted are those instances where mapping arrangements with cooperating foreign agencies specify the showing of a secondary grid. No more than one secondary grid is shown. 7-5.2 When required, the secondary grid is shown by inside ticks, printed in blue, emanating from the neatline in their correct alignment and spaced at 10,000-unit intervals. The even 100,000-unit ticks are accentuated in weight. 7-5.3 Values, similar in composition to those labeling the major grid lines, appear on all four sides of the sheet. The first grid tick in each direction from the southwest corner of the sheet is labeled with full values. Thereafter, only those grid ticks whose values are multiples of 50,000 are labeled. If the secondary grid is a nonstandard grid, prescribed colors are used (para. 7-1.6-2), unless there is conflict with another grid shown on the map. In that event, substitutions are made in the established order of preference. Figure 28. Two Major Grid Zones Separated by a Grid Junction as Shown on a 1:250,000 Scale Map. 7-5.4 A grid note, identifying the secondary grid, appears in the lower margin of the sheet. It is printed In the some color as that used for the values of the grid it identifies and is modeled after the following: BLACK NUMBERED TICKS INSIDE THE NEATLINE
NORTH VARIES FROM 1 1/2ï¿½ (30 MILS)
EDGE TO 2ï¿½ (40 MILS) WESTERLY FOR THE
1 1/2ï¿½ (30 MILS)
1ï¿½ W OVER THE ENTIRE AREA
CHAPTER 8 PORTRAYAL OF GRIDS ON MAPS AT 1:1,000,000 SCALE 8-1 GENERAL.
CHAPTER 9 GRIDS ON NAUTICAL CHARTS AT 1:75,000 SCALE AND LARGER 9-1 GENERAL.
At West edge of chart Grid N. is 0ï¿½ 40'E. of True N.
At East edge of charg Grid N. is 1ï¿½ 15'E. of Ture N.
9-12.1 All nautical charts, Other than Combat Charts, Amphibious Assault Charts, and certain modified facsimiles, are constructed on WGS wherever possible. When the chart is not on the latest World Geodetic System datum, a note is shown in black indicating the correction needed to convert a coordinate to that datum. Example for Combat Chart: COORDINATE CONVERSIONS
Geographic: Subtract 3.5" Long; Subtract 3.0" Lat
9-12.2 When there is insufficient data available or inconsistent deviations result from the available geodetic control, one of the following notes, as appropriate, is shown in place of the WGS correction note: WORLD GEODETIC SYSTEM DATA ADJUSTMENT
this chart cannot be placed on the World Geodetic System (WGS) Datum. 9-12.3 When a Mine Warfare or Harbor, Approach, and Coastal Chart is on WGS, a datum note is shown as follows: DATUM NOTE
Figure 43. Grid Reference Boxes commonly used on Nautical Charts at scales of 1:75,000 and larger. CHAPTER 10 GRIDS ON NAUTICAL CHARTS AT SCALES SMALLER THAN 1:75,000 10-1 GENERAL.
For information relating to the appropriate WGS Datum Note, see Chapter 9 paragraph 9-12. CHAPTER 11 GRIDS ON AERONAUTICAL CHARTS AT 1:500,000 SCALE AND LARGER 11-1 GENERAL.
11-5.1 A grid reference box appears in the margin of each sheet. The box contains step- by-step instructions for composing a grid reference. For examples, see figure 47. The applicable grid zone designation is also identified in the box. 11-5.2 The grid system(s) in use on the map dictates the referencing instructions contained in the grid reference box. 11-5.3 When more than one major grid appears on a sheet and the method for giving a reference is the same for all the grids, a common reference box is used. 11-5.4 When more than one major grid appears on a sheet and the method for giving a reference varies with the grids, circumstances control the treatment of the grid reference boxes. A grid reference box is shown in the margin for each grid, except those falling completely in open water area. At the top of each box appears a note limiting the use of the box to the grid or grids concerned. Figure 47. Grid Reference Box Commonly Used on Aeronautical Charts at 1:5000,000 Scale and Larger. APPENDIX A
TABLE OF MIL
APPENDIX A TABLE OF MIL EQUIVALENTS APPENDIX B 100,000-METER SQUARE IDENTIFICATIONS OF MILITARY GRID REFERENCE SYSTEM TO DETERMINE THE UTM OR UPS 100,000-METER SQUARE MGRS IDENTIFICATION B-1. These instructions provide a method for determining the correct UTM or UPS 100,000- meter square identification for any point in the world. See Chapter 3 for a full explanation of the 100,000-meter square identification. If geographic coordinates are the only coordinates given, they must he transformed to UTM or UPS grid coordinates. The following data are necessary to determine the correct 100,000-meter square letters: B-1.1 For the UPS grid: B-1.1.1 UPS grid coordinates (easting and northing). B-1.1.2 The polar zone in which the coordinates are located. B-1.2 For the UTM grid: B-1.2.1 UTM grid coordinates (easting and northing). B-1.2.2 UTM grid zone B-1.2.3 Geographic coordinates or the 8ï¿½ latitude bond letter which is the Grid Zone Designation letter. B-1.2.4 Ellipsoid and/or datum. B-2 Determine by area, datum, and/or ellipsoid which of the following figures is appropriate: Figure B-1: North of 84ï¿½N. Figure B-2: South of 80ï¿½S. Figure  B-3: Geodetic Reference System (GRS 1980)
Figure B-4: Bessel 1841 B-3 Method of use with the UPS grid: B-3.1 If the coordinates fall in the north Polar region, use figure B-1 to determine the correct square identification letters. If the coordinates fall in the south Polar region, use figure B-2. B-3.2 In figures B-1 and B-2, the easting lines are labeled every 500,000 meters from left to right with the 2,000,000 meter line being coincident with the Oï¿½ and 180ï¿½ line. If the easting is less than 2,000,000 meters the Grid Zone Designation will be Y or A depending on whether the point is in the North or South Polar region. If the easting is greater than 2,000,000 meters the Grid Zone Designation will be Z or B. The northing lines are labeled every 500,000 meters from bottom to top with the 2,000,000 meter line coincident with the 90ï¿½W and 90ï¿½E line. B-3.3 Reduce both easting and northing to the nearest 100,000 meters. B-3.4 Find these grid lines on the figure. B-3.5 The 100,000-meter square will be to the right and above these lines. B-3.6 The procedure is the some for the north Polar region or the south Polar region. Example:  At latitude 86ï¿½46' north, longitude 132ï¿½30' west,
UPS grid coordinates were scaled, E = 1,735,000
N = 2,243,000 in the North Polar area.
Use figure B-1.
The easting is less than 2,000,000 meters, therefore
the grid zone designation is Y.
The coordinates reduced to the nearest 100,000 meters
are: E = 1,700,000 N = 2,200,000.
The 100,000-meter square letters to the right and above
the intersection of these lines are XK.
MGRS to the nearest 1,000 meters is YXK3543
B-4 Method of use with the UTM grid: B-4.1 To determine the 100,000-meter square letters for UTM grid coordinates, first determine which figure, B-3 or B-4, is needed. The ellipsoid identifications are specified on each figure. B-4.2 Locate the zone number in the list at the top of the figure. This identifies the set of designators in which the letters will be found. B-4.3 If the 8ï¿½latitude bond letter is given, it will be used as the grid designation letter. If the geographic coordinates are given, use the latitude of the point to determine the grid zone designation letter from Appendix D. B-4.4 Reduce the easting to the nearest 100,000 meters. Find the 100,000-meter easting grid line within the grid zone identified in paragraph B-4.2. The easting lines are labeled below the figure, from 200,000 meters to 800,000 meters within each zone. B-4.5 Reduce the grid northing by multiples of 2,000,000 meters until the resulting value is between 0 and 2,000,000 meters. Further reduce the grid northing to the nearest 100,000 meters. Find the 100,000-meter northing grid line. The northing lines are labeled at the left side of the figure. B-4.6 The 100,000-meter square will be to the right and above the intersection of the lines found in paragraphs B-4.4 and B-4.5. B-4.7 The procedure is the some for the northern hemisphere or the southern hemisphere. Example:  At latitude 34ï¿½15' north, longitude 88ï¿½36' east,
UTM grid coordinates were scaled, E = 647,000
N = 3,791,000 in UTM zone 45, grid zone
designation letter S.
Grid zone designation is 45S.
The point is referenced to the WGS ellipsoid, therefore
use figure B-3 and set 3 of the zones.
The easting is reduced to 600,000 meters.
For an easting of 600,000 meters start at the column X.
Reduce the northing by 2,000,000 meters and then to the
nearest 100,000 meters, obtaining 1,700,000 and
read across that grid line to the intersection
with the 600,000 meter easting line in zone 45.
this intersection is XT.
MGRS to the nearest 1,000 meters is 45SXT4791.
FIGURE B-1. 100,000 METER SQUARE IDENTIFICATIONS FOR THE MILITARY GRID REFERENCE SYSTEM (Northern Hemisphere) FIGURE B-2. 100,000 METER SQUARE IDENTIFICATIONS FOR THE MILITARY GRID REFERENCE SYSTEM (Southern Hemisphere) FIGURE B-3. USE THIS DIAGRAM FOR: GEODETIC REFERENCE SYSTEM 1980 ELLIPSOID, INTERNATIONAL ELLIPSOID, WORLD GEODETIC SYSTEM 1984 ELLIPSOID IN THE NORTH AND SOUTH HEMISPHERES. FIGURE B-4. USE THIS DIAGRAM FOR BESSEL 1841 ELLIPSOID IN THE NORTH AND SOUTH HEMISPHERES. APPENDIX C
GUIDE TO GEODETIC STATUS OF LARGE SCALE MAPPING GUIDE TO GEODETIC STATUS1
OF LARGE SCALE MAPPING
DATUM CODES
A    Map sheets are on preferred datum.
B    Mapping is being converted to preferred datum.
C    Map sheets are not on preferred datum.
*    Insufficient or unavailable information.
1    Map sheets portray UTM or UPS grid.
2    Map sheets portray a nonstandard preferred grid.
3    Mapping is being converted to a preferred grid.
4    Map sheets portray a non preferred grid.
DATUM/GRID
BAHAMAS; TURKS AND CAICOS
K724S2
K7372
MADEIRAS ISLANDS
P761S2
GUAM, NORTHERN MARIANAS
KIRIBATI AND PHOENIX ISLAND
1This guide provides information concerning unclassified mapping only. It is based on an appraisal of a majority of the maps available in the series. For information regarding map series not listed contact DMA (PR). 2This will be the correct status for these series if the present configuration of Appendix D is approved. APPENDIX D
INDEX TO PREFERRED GRIDS, DATUMS AND ELLIPSOIDS SPECIFIED FOR NEW MAPPING APPENDIX D. This appendix is not available. Point of Contact: DOGIG Phone Numbers: Com. (314)263-4059 DSN 693-4059 Email: gandg@nima.mil [NIMA Home] [Geospatial Sciences Home] [Geospatial Sciences Publications] [Table of Contents] [Feedback]
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