This glossary of geographical terms is drawn extensively from "An Album of Map Projections", U.S. Geological Survey Professional Paper 1453, by John P. Snyder and Philip M. Voxland.
Because the purpose of this glossary is to assist in understanding and using Mapping Toolbox™ features, it includes some terms specific to the toolbox, and gives some other terms shades of meaning beyond their general definitions.
Two points on opposite sides of a planet.
1/3600th of a degree (1 second) of latitude or longitude.
The conceptual placement of a projection system in relation to the Earth's axis (direct, normal, polar, equatorial, oblique, and so on).
In vector geodata, a quantitative or qualitative descriptor of a spatial entity. An attribute can describe a real-world quality (such as population or land area), or a graphic quality (such as patch color or line weight). Attributes are frequently coded as numbers or strings in character-coded or binary tabular data files, with one or more attribute per map feature.
(Attribute specification) A cell array structure that specifies
attributes of geodata to be included in a KML file and defines label
strings and format strings for each attribute. Used with
See Map axes.
The angle a line makes with a meridian, taken clockwise from north.
A projection on which the azimuth or direction from a given central point to any other point is shown correctly. When a pole is the central point, all meridians are spaced at their true angles and are straight radii of concentric circles that represent the parallels. Also called a zenithal projection.
The measurement of water depths of oceans, seas, lakes, and other bodies of water.
A late 18th/early 19th century mathematician, astronomer, and sailor who "wrote the book" on navigation. John Hamilton Moore's The Practical Navigator was the leading navigational text when Bowditch first went out to sea, and had been for many years. Early in his first voyage, however, Bowditch began noticing errors in Moore's book, which he recorded and later used in preparing an American edition of Moore's work. The revisions were to such an extent that Bowditch was named the principal author, and the title was changed to The New American Practical Navigator, published in 1802. In 1868, the U.S. Navy bought the copyright to the book, which is still commonly referred to as "Bowditch" and considered the "bible" of navigation.
The locus of points that lie within a specified distance from a map feature.
The art or practice of making charts or maps. See Map.
Geospatial data in which raster pixel values (or vector data attributes) are categorical indices, usually coded as integers. The meanings of the categories are usually stored in a separate table. Examples are geocodes, land use categories, and indexed color images. See Numerical geodata.
The meridian passing through the center of a projection, often a straight line about which the projection is symmetrical.
A projection in which the Earth is projected geometrically from the center of the Earth onto a plane or other surface. The Gnomonic and Central Cylindrical projections are examples.
A map portraying regions of homogeneous classified attribute values, changing abruptly at region boundaries, and colored or shaded according to their attribute values. Thematic political maps are usually choropleth maps.
Curves that are not elementary forms such as circles, ellipses, hyperbolas, parabolas, and sine curves, such as rivers, coastlines, and administrative boundaries.
A projection formed by connecting two or more projections along common lines such as parallels of latitude, necessary adjustments being made to achieve fit. The Goode Homolosine projection is an example.
A projection on which all angles at each point are preserved, except at a finite number of singular points (e.g., the poles in a Mercator projection). Also called an orthomorphic projection.
A projection resulting from the conceptual projection of the Earth onto a tangent or secant cone, which is then cut lengthwise and laid flat. When the axis of the cone coincides with the polar axis of the Earth, all meridians are straight equidistant radii of concentric circular arcs representing the parallels, but the meridians are spaced at less than their true angles. Mathematically, the projection is often only partially geometric.
A linear scale that remains the same along a particular line on a map, although that scale may not be the same as the stated or nominal scale of the map.
All points that are at the same height above or below a reference datum; generally applied to continuous, single-valued surfaces only, such as elevation, temperature, or magnetic field strength.
See Normal aspect.
A linear scale having exactly the same value as the stated or nominal scale of the map, or a scale factor of 1.0. Also called true scale.
A projection resulting from the conceptual projection of the Earth onto a tangent or secant cylinder, which is then cut lengthwise and laid flat. When the axis of the cylinder coincides with the axis of the Earth, the meridians are straight, parallel, and equidistant, while the parallels of latitude are straight, parallel, and perpendicular to the meridians. Mathematically, the projection is often only partially geometric.
A raster data set consisting of an array of values posted or sampled at specific geographic points. Mapping Toolbox data grids can be implicit (regular) or explicit (irregular, or geolocated), depending on the uniformity of the grid. See Regular data grid, Geolocated data grid.
A base reference level for establishing the vertical dimension of elevation for the earth's surface. A datum defines sea level and incorporates an ellipsoid; thus one can reference a coordinate system to a datum or to a specified ellipsoid, but not both at the same time.
A base measuring point ("0.0 point") used as the origin of rectangular coordinate systems for mapping or for maintaining excavation provenience. Two examples are the North American Datum of 1927 (NAD27) and the North American Datum of 1983 (NAD83). Earth-centered coordinate systems, such as WGS84, combine horizontal and vertical datums.
From "deduced reckoning," the estimation of geographic position based on course, speed, and time.
Elevation data in the form of a data grid, generally a regular (implicit) one. DEM also refers to the five primary types of digital elevation models produced by the U.S. Geological Survey; Mapping Toolbox functions can read 30-meter and 10-meter DEMs as well as 3-second DEMs.
The arc length distance along a parallel of a point from a given meridian.
A simple geometric form capable of being flattened without stretching. Many map projections can be grouped by a particular developable surface: cylinder, cone, or plane.
See Normal aspect.
A Mapping Toolbox data structure for mapped objects dating from Version 1 of the product. The structures can contain line, patch, text, regular data grid, geolocated data grid, and light objects; vector data always has coordinates in latitude and longitude. In Version 2 of the toolbox, display structures were superseded by geostructs and mapstructs. See Geographic data structure. Most vector display structures can be converted to geographic data structures.
A variation of the area or linear scale on a map from that indicated by the stated map scale, or the variation of a shape or angle on a map from the corresponding shape or angle on the Earth.
Degrees-minutes angle notation of the form ddd° mm'. There
are 60 seconds in a minute, and 60 minutes in a degree. In DM notation,
degrees are always integer, but minutes can be fractional. Certain Mapping Toolbox functions
represent DM angles as column vectors,
Degrees-minutes-seconds angle notation of the form ddd°
mm' ss''. There are 60 seconds in a minute, and 60 minutes in a degree.
In DMS notation, degrees and minutes are always integer, but seconds
can be fractional. Certain Mapping Toolbox functions represent
DMS angles as column vectors,
[degrees minutes seconds].
Digital Terrain Elevation Data; a raster data format used by various terrain data products, based on specifications originating in the United States Department of Defense. DTED® files sample terrain elevation in a geographic grid at specific "levels" of spatial resolution; sampling intervals are approximately one kilometer for Level 0, 100 meters for Level 1, 30 meters for Level 2, and so on. High level DTED files are not generally available to the public. Mapping Toolbox software imports all levels of DTED data.
The distance of a point eastward from the origin in the units of the coordinate system for the defined projection. Paired with Northings.
When used to represent the Earth, a solid geometric figure formed by rotating an ellipse about its minor (shorter) axis. Also called spheroid.
A vector describing a specific ellipsoid model. The ellipsoid vector has the form
ellipsvec = [semimajor-axis eccentricity]
Elevation of a point above a reference ellipsoid, as measured along a normal to the ellipsoid.
A projection on which the areas of all regions are shown in the same proportion to their true areas. Shapes may be greatly distorted. Also called an equivalent or authalic projection.
The great circle straddling a planet at a latitude of 0°, perpendicular to its polar axis and midway along it, dividing the northern and southern hemispheres.
An aspect of an azimuthal projection on which the center of projection or origin is some point along the Equator. For cylindrical and pseudocylindrical projections, this aspect is usually called conventional, direct, normal, or regular rather than equatorial.
A projection that maintains constant scale along all great circles from one or two points. When the projection is centered on a pole, the parallels are spaced in proportion to their true distances along each meridian.
The value of the easting assigned to the projection origin. Easting values increase to the east.
The value of the northing assigned to the projection origin. Northing values increase to the north.
A cylindrical projection on which, in normal aspect, the pole is shown as a line rather than as a point. For example, the Miller projection is flat-polar.
See Map frame.
Having no distortion of shape, area, or linear scale. On a flat map, this condition can exist only at certain points or along certain lines.
A minimum-distance curve on a curved surface, independent of the choice of a coordinate system. On a sphere a geodesic is equivalent to a great circle arc.
A data grid defined with separate latitude, longitude, and value matrices, allowing irregular sampling, nonrectangular shapes, and noncardinal orientations. Satellite imagery swaths are often represented as geolocated data grids. See Data grid, Regular data grid.
Geospatial data. See Geospatial.
The figure of the earth less its topography, defined as an equipotential surface with respect to gravity, more or less corresponding to mean sea level. It is approximately an oblate ellipsoid, but not exactly so because local variations in gravity create minor hills and dales. Empirically determined geoids are used to define datums and to compute orbital mechanics.
Spherical 2-D coordinate tuples (latitudes, longitudes) that specify point locations for unprojected geodata. The analogous term for geodata projected to a rectangular coordinate system is map coordinates.
A Mapping Toolbox data structure for vector data comprised
of a MATLAB® structure array with one element per vector geographic
feature. It includes a mandatory
at least two coordinate array fields. The field names are
Y (for mapstructs),
Lon (for geostructs),
and optional attribute fields.
Identifying objects and locations by name, identifier, or coordinates to describe where they are located on the Earth's surface.
Spatial data, concepts, and techniques that specifically refer to geographic space or phenomena, and not just to arbitrary coordinate systems or abstract space frames.
A Mapping Toolbox geographic data structure for vector geodata with coordinates in latitude and longitude. See Geographic data structure.
An extension of the TIFF image file format with additional tags containing parameters for image georeferencing and projected map coordinate system definition.
A system, usually computer based, for the input, storage, retrieval, analysis, and display of interpreted geographic data.
Generally, a nonazimuthal projection developed before 1700 on which a hemisphere is enclosed in a circle, and meridians and parallels are simple curves or straight lines.
A network of lines representing a subset of the Earth's parallels and meridians (or plane coordinates) used as a reference grid on globes and maps. Generally synonymous with map grid, except that many map grids are rulings at regular intervals in projected coordinates. See Map grid, National grid (U.S.), and National grid (U.K.). The vertices of the graticule grid are precisely projected, and the map data contained in any grid cell is warped to fit the resulting quadrilateral. A finer graticule grid results in a higher projection fidelity at the expense of greater computational requirements.
Any circle on the surface of a sphere, especially when the sphere represents the Earth, formed by the intersection of the surface with a plane passing through the center of the sphere. It is the shortest path between any two points along the circle and therefore important for navigation. All meridians and the Equator are great circles on the Earth taken as a sphere.
The science of measurement, description, and mapping of the surface waters of the Earth, especially with reference to their use in navigation. The term also refers to those parts of a map collectively that represent surface waters and drainage.
The scientific study of the waters of the Earth, especially with relation to the effects of precipitation and evaporation upon the occurrence and character of ground water.
A graphic means of representing terrain or other scalar attributes using a sequence of colors or tints indexed to elevation.
The scientific study of the Earth's topological configuration above sea level, especially the measurement and mapping of land elevation.
A small-scale map used to help locate a map containing a region or feature of interest in a tiled geospatial database, map series, plat book, or atlas.
A circle or ellipse useful in illustrating the distortions of
a given map projection. Indicatrices are constructed by projecting
infinitesimally small circles on the Earth onto a map and giving them
visible dimensions. Their axes lie in the directions of and are proportional
to the maximum and minimum scales at their point locations. Often
called a Tissot indicatrix after the originator of the concept. Mapping Toolbox Tissot
indicatrices can be displayed using the
and indicatrices for all supported projections are provided.
A projection designed to reduce peripheral distortion by making use of separate sections joined at certain points or along certain lines, usually the Equator in the normal aspect, and split along lines that are usually meridians. There is normally a central meridian for each section. No Mapping Toolbox projections are of this type, but the user can separate data into sections and project these independently to achieve this effect.
A file format and dialect of XML used to georeference geographic locations and describe their attributes and relations, including hyperlinks, for display in earth browsers.
Mapping at a scale larger than about 1:75,000, although this limit is somewhat flexible. Includes cadastral, utility, and some topographic maps.
The complement of the elevation angle of the celestial North Pole, which depends on normal to the Earth's equipotential surface (geoid) at a given point (positive if the point is north of Equator, negative if it is south). It can be thought of as the angle that a plumb line makes with the equatorial plane.
Intermediate forms of latitude that are mathematically constructed (normally by transferring latitudes first from an ellipsoid to a sphere, and then to a plane) in order to achieve desired map projection properties. Types include conformal (for constructing conformal maps), authalic (for constructing equal-area maps), and rectifying (for constructing equidistant maps).
The angle at which a line connecting the surface of a sphere or reference ellipsoid to its center intersects the equatorial plane (positive if the point is north of Equator, negative if it is south). One of the two common geographic coordinates of a point on the Earth.
The angle made by a perpendicular to a given point on the surface of a sphere or ellipsoid representing the Earth and the plane of the Equator (positive if the point is north of Equator, negative if it is south). Also called geographic latitude. One of the two common geographic coordinates of a point on the Earth.
Line segments connecting waypoints.
See Map legend.
The form taken by a system of projection when the parameters of the formulas defining that projection are allowed to reach limits that cause it to be identical with another separately defined projection.
A binary data grid consisting entirely of 1s and 0s. An example
of a logical data grid can be created with the
by performing a logical test for positive elevations (
Each entry in the data grid contains a 1 if it is above sea level,
or a 0 if it is at or below sea level.
The angle made by the plane of a meridian passing through a given point on the Earth's surface and the plane of the (prime) meridian passing through Greenwich, England, east or west to 180 (positive if the point is east, negative if it is west). One of the two common geographic coordinates of a point on the Earth. Paired with Latitude.
See Rhumb line.
A diagrammatic or pictorial representation of a planet's surface or part of it, showing the geographical distributions, positions, etc., of natural or artificial features such as roads, towns, relief, land cover, rainfall, populations, etc. Maps represent geospatial data visually.
A Handle Graphics® axes object augmented with additional
properties, including a projection type, projection parameters, map
latitude and longitude limits and so forth. Many Mapping Toolbox display
functions require that a map axes first be defined. Others create
a map axes if necessary (e.g.,
or assume that your coordinate data are in a projected map coordinate
Orthogonal planar 2-D coordinate tuples that specify point locations for projected geodata. The analogous term for unprojected geodata is geographic coordinates. Also called grid coordinates and plane coordinates.
A projected rectangle or quadrangle enclosing a geographic data displayed on a Mapping Toolbox map axes.
A symbolized network of lines, or graticule, representing parallels and meridians or plane coordinates. Plane coordinate grids are almost always rectangular with uniform spacing. Azimuthal map grids are organized as polar coordinates. See Graticule.
A vector or raster geographic data set read into the Map Viewer, for example, roads, rivers, municipal boundaries, topographic grids, or orthophoto images. Map layers are "stacked" from top to bottom, and can be reordered and hidden by the user.
A key to symbolism used on a map, usually containing swatches of symbols with descriptions, and can include notes on projection, provenance, scale, units of distance, etc.
A Mapping Toolbox geographic data structure for vector geodata with coordinates in projected (x,y) coordinates. See Geographic data structure.
See Data grid.
A reference line on the Earth's surface formed by the intersection of the surface with a plane passing through both poles and some third point on the surface. This line is identified by its longitude. When the Earth is regarded as a sphere, this line is half a great circle; on the Earth regarded as an ellipsoid, it is half an ellipse.
A projection having the least possible total error of any projection in the designated classification, according to a given mathematical criterion. Usually, this criterion calls for the minimum sum of squares of deviations of linear scale from true scale throughout the map ("least squares").
A metric grid based on the Transverse Mercator Projection developed by Ordnance Survey in 1936 for use in Great Britain. Sometimes abbreviated "OSGB36," it is the de facto standard projection for display of UK based mapping.
A metric grid based on the Transverse Mercator Projection, adopted by the Federal Geographic Data Committee (FGDC) in 2001 for use in the United States. It is an evolving standard intended to unify georeferencing across the U.S., but is not yet as widely used as other countries' national grids.
The stated scale at which a map projection is constructed. Scale is never completely constant across the extent of a map, although in some maps (especially at large scales) it can vary by minuscule amounts.
A form of a projection that provides the simplest graticule and calculations. It is the polar aspect for azimuthal projections, the aspect having a straight Equator for cylindrical and pseudocylindrical projections, and the aspect showing straight meridians for conic projections. Also called conventional, direct, or regular aspect.
The distance of a point northward from the origin, in the units of the coordinate system for the defined projection. Paired with Eastings.
Geospatial data in which raster pixel values (or vector data
attributes) are cardinal, ratio, or ordinal numeric measurements or
computed values. For example, the
topo data set
contains numerical geodata. Each value in its data grid is an average
elevation in meters for the geographic area covered by that cell. See Categorical geodata.
An aspect of a projection on which the axis of the Earth is rotated so it is neither aligned with nor perpendicular to the conceptual axis of the map projection.
A projection on which the surface of the Earth taken as a sphere is transformed onto a solid other than the sphere and then projected orthographically and obliquely onto a plane for the map.
A specific azimuthal projection or a type of projection in which the Earth is projected geometrically onto a surface by means of parallel projection lines.
Elevation above a datum defined by a geoid representing mean sea level.
See Conformal projection.
A small circle on the surface of the Earth, formed by the intersection of the surface of the reference sphere or ellipsoid with a plane parallel to the plane of the Equator. This line is identified by its latitude, which can be defined in several ways. The Equator (a great circle) is usually also treated as a parallel. See entries for Latitude.
A parallel that is equally distant from but on the opposite side of the Equator. For example, for lat 30°N (or +30°), the parallel of opposite sign is lat 30° S (or -30°). Also called latitude of opposite sign.
A projection produced by projecting straight lines radiating from a selected point (or from infinity) through points on the surface of a sphere or ellipsoid and then onto a tangent or secant plane. Other perspective maps are projected onto a tangent or secant cylinder or cone by using straight lines passing through a single axis of the sphere or ellipsoid. Also called geometric projection.
A projection resulting from the conceptual projection of the Earth onto a tangent or secant plane. Usually, a planar projection is the same as an azimuthal projection. Mathematically, the projection is often only partially geometric.
A map representing only the horizontal positions of features (without their elevations).
An aspect of a projection, especially an azimuthal one, on which the Earth is viewed from directly above a pole. This aspect is called transverse for cylindrical or pseudocylindrical projections.
An extremity of a planet's axis of rotation. The North Pole is a singular point at 90°N for which longitude is ambiguous. The South Pole has the same characteristics and is located at 90°S.
A specific projection or member of a class of projections that are constructed like conic projections but with different cones for each parallel. In the normal aspect, all the parallels of latitude are nonconcentric circular arcs, except for a straight Equator, and the centers of these circles lie along a central axis.
A coordinate system defined for a particular map projection and associated parameters, which normally is planar with well-defined coordinate origin, handedness, nominal scale, and units of distance. While map scale can vary at different coordinate locations, a linear projected coordinate system has constant units of distance.
A systematic representation of a curved 3-D surface such as
the Earth onto a flat 2-D plane. Each map projection has specific
properties that make it useful for specific purposes. For a list of Mapping Toolbox map
The values of constants as applied to a map projection for a specific map; examples are the values of the scale, the latitudes of the standard parallels, and the central meridian. The required parameters vary with the projection.
A projection that, in the normal aspect, has concentric circular arcs for parallels and on which the meridians are equally spaced along the parallels, like those on a conic projection, but on which meridians are curved.
A projection that, in the normal aspect, has straight parallel lines for parallels and on which the meridians are (usually) equally spaced along parallels, as they are on a cylindrical projection, but on which the meridians are curved.
A region bounded by parallels north and south, and meridians east and west.
A georeferenced array or grid of values corresponding to specific geographic points, usually regularly and rectangularly sampled in either geographic or map space. Values can be continuous or categorical. In the case of georeferenced multiband images, raster geodata can take the form of 3- and higher dimensional arrays.
The determination of geographic position by calculation.
A 3-by-2 matrix defining the scaling, orientation, and placement of raster map data on the globe or in planar map coordinates. The matrix specifies an affine transformation that ties (geolocates) the row and column subscripts of an image or regular data grid to 2-D map coordinates or to geographic coordinates (longitude and geodetic latitude). See Referencing vector.
A three-component vector defining the geographic placement and
unit cell size for raster map data. A referencing vector has the form
north-latitude west-longitude], with latitude and longitude
limits specified in degrees.
A referencing vector specifies an affine transformation with rows and columns aligned to latitude and longitude, respectively, and the same data spacing in both latitude and longitude. As such, it is more specific than a referencing matrix. Note that a referencing vector can always be transformed to a referencing matrix, but only certain referencing matrices can be transformed to referencing vectors. See Referencing matrix.
A small-scale map of an area covering at least 5 or 10 degrees of latitude and longitude but less than a hemisphere.
See Normal aspect.
A data grid with equally spaced grid points in either latitude-longitude or map coordinates, defined with a referencing matrix or vector, and limited to a rectangular shape and cardinal orientation. See Data grid, Geolocated data grid, Referencing matrix.
A projection on which the direction or azimuth from every point on the map to a given central point is shown correctly with respect to a vertical line parallel to the central meridian. The reverse of an azimuthal projection.
A complex curve (a spherical helix) on a planet's surface that crosses every meridian at the same oblique angle; a navigator can proceed between any two points along a rhumb line by maintaining a constant heading. A rhumb line is a straight line on the Mercator projection. Also called a loxodrome.
The ratio of the distance on a map or globe to the corresponding distance on the Earth; usually stated in the form 1:5,000,000, for example. A given region will appear smaller on a small-scale map than on a large-scale map.
The ratio of the scale at a particular location and direction on a map to the nominal scale of the map. At a standard parallel, or other standard line, the scale factor is 1.0.
A secant cone or cylinder intersects the sphere or ellipsoid along two separate lines; these lines are parallels of latitude if the axes of the geometric figures coincide. A secant plane intersects the sphere or ellipsoid along a line that is a parallel of latitude if the plane is at right angles to the axis.
A cell array in which the first element is a predicate function
and the remaining elements list the names of attributes in a shapefile.
shaperead has an option to screen out
any feature in the shapefile for which a predicate returns false when
applied to the subset of attributes corresponding to the list in the
Shading added to a map or image that makes it appear to have three-dimensional aspects. This type of enhancement is commonly done to satellite images and thematic maps utilizing digital topographic data to provide the appearance of terrain relief.
A widely used file format for vector geodata designed by Environmental Systems Research Institute. Shapefiles encode coordinates for points, multipoints, lines (polylines), or polygons along with tabular attributes.
Certain points on most but not all conformal projections at which conformality fails, such as the poles on the normal aspect of the Mercator projection.
An aspect of a projection on which the axis of the Earth is rotated, so it is neither aligned with nor perpendicular to the conceptual axis of the map projection, and tilted, so the poles are at an angle to the conceptual axis of the map projection.
A circle on the surface of a sphere, formed by the intersection with a plane. Parallels of latitude are small circles on the Earth taken as a sphere. Mapping Toolbox great circles, including the Equator and all meridians, are treated as special, limiting cases of small circles. Mapping Toolbox functions generalize the concept of small circle with computations for two other types of curve: the locus of points on an ellipsoid at a given distance (as measured along a geodesic) from a central point, or the locus of points on a sphere or ellipsoid at a given distance from a central point, as measured along a rhumb line.
Mapping at a scale smaller than about 1:1,000,000, although the limiting scale sometimes has been made as large as 1:250,000.
A self-documenting geospatial file formatting standard adopted by the U.S. government and others. SDTS can encode locations, attributes, topological relationships, data quality, and other metadata. Note that Mapping Toolbox software can read the SDTS Raster Profile, but does not currently support SDTS vector data.
In the normal aspect of a projection, a parallel of latitude along which the scale is as stated for that map. There are one or two standard parallels on most cylindrical and conic map projections and one on many polar stereographic projections.
A set of commensurate coordinate systems commonly used for utility and surveying applications in the lower 48 United States. Each state contains one or more zones. Coordinates for zones elongated north-to-south are based on Transverse Mercator projections, while zones elongated east-to-west use Lambert Conformal Conic.
A specific azimuthal projection or type of projection in which the Earth is projected geometrically onto a surface from a fixed (or moving) point on the opposite face of the Earth.
In cartography, a mapping between geospatial objects or numerical or categorical values and cartographic symbols. The choice of graphic symbols, their size, density, shape, contrast, color, and pattern are principal aspects of symbolization.
(Symbol specification) A cell array structure that defines symbolism characteristics for points, lines, and polygons with respect to attributes and their values, or as a default symbolization regardless of attributes.
A cone or cylinder that just touches the sphere or ellipsoid along a single line. This line is a parallel of latitude if the axes of the geometric figures coincide.
A map designed to portray primarily a particular subject, such as population, railroads, or croplands.
A map that usually represents the vertical positions or elevations of features as well as their horizontal positions.
Graticule of meridians and parallels on a projection after the Earth has been turned with respect to the projection so that the Earth's axis no longer coincides with the conceptual axis of the projection. Used for oblique and transverse aspects of many projections.
An aspect of a map projection on which the axis of the Earth is rotated so that it is at right angles to the conceptual axis of the map projection. For azimuthal projections, this aspect is usually called equatorial rather than transverse.
See Correct scale.
Data representing geospatial objects as sequences of geographic
or projected coordinate points that are implicitly connected if they
represent linear or areal shapes. In Mapping Toolbox and other
software, such geodata is often represented by two vectors, one with
latitudes, another with longitudes. Objects can be segmented by inserting
NaNs at the same locations in both vectors. Such pairs of coordinate
vectors can also be represented as the
values in a geographic data structure array.
The portion of a surface that is visible from a given point on or above it; derived from the concept of a watershed.
Points through which a trip, track, or transit passes, usually corresponding to course or speed changes.
An Earth-centered datum, used as a definition of DMA (now NGA) DEMs. The WGS 72 datum was the result of an extensive effort extending over approximately three years to collect selected satellite, surface gravity, and astrogeodetic data available throughout 1972. This data was combined using a unified WGS solution (a large-scale least squares adjustment).
The WGS 84 was developed as a replacement for the WGS 72 by the military mapping community as a result of new and more accurate instrumentation and a more comprehensive control network of ground stations. The newly developed satellite radar altimeter was used to deduce geoid heights from oceanic regions between 70° north and south latitude. Geoid heights were also deduced from ground-based Doppler and ground-based laser satellite-tracking data, as well as surface gravity data. The ellipsoid associated with WGS 84 is GRS 80.
A small text file used to georeference different raster image formats, developed to incorporate imagery into ESRI's ArcView software.
See Azimuthal projection.