1:250,000 USGS DEM
The following document was taken from http://edc.usgs.gov/Webglis/glisbin/guide.pl/glis/hyper/guide/usgs_dem.
For information on the dataset on this Adirondack Park CD-ROM called 'dem250k' refer to the sections of this document under the heading 'Small Scale' which discuss the 1-degree (30 arc-second), or 1:250000-scale DEM data.
The data was downloaded from USGS, merged and clipped to the vicinity of the Adirondack Park and projected in ArcInfo GRID from UTM meters, Zone 18, NAD27 to NAD83.
Background
The USGS Digital Elevation Model
(DEM) data files are
digital representations of
cartographic information in a raster
form. DEMs consist of a sampled array of elevations for a number
of ground positions at regularly spaced intervals. These digital
cartographic/geographic data files are produced by the U.S.
Geological Survey (USGS) as
part of the National Mapping Program and are sold in 7.5-minute,
15-minute, 2-arc-second (also known as 30-minute), and 1-degree units. The 7.5- and 15-minute
DEMs are included in the large scale category while 2-arc-second DEMs fall
within the intermediate scale category and 1-degree DEMs fall within the
small scale category.
- Large scale
- The DEM data for 7.5-minute units correspond to the USGS
1:24,000 and 1:25,000 scale topographic quadrangle map series for
all of the United States and its territories. Each
7.5-minute DEM is based on 30- by 30-meter data spacing with the
Universal Transverse Mercator (UTM) projection. Each 7.5- by
7.5-minute block provides the same coverage as the standard USGS
7.5-minute map series.
The 7.5-minute Alaska DEM data correspond to the USGS 1:24,000 and
1:25,000 scale topographic quadrangle map series of Alaska by unit size.
The unit sizes in Alaska vary depending on the latitudinal location of
the unit. The 7.5-minute Alaska DEM data consist of a regular array of
elevations referenced horizontally to the geographic (latitude/longitude)
coordinate system of the North American 1927 Datum (NAD 27) or the North
American 1983 Datum (NAD 83). The spacing between elevations along
profiles is 1 arc second in latitude by 2 arc seconds of longitude.
Syrup Creek, Idaho DEM (44.8KB)
The 15-minute DEM data correspond to the USGS 1:63,360 scale topographic
quadrangle map series of Alaska by unit size. The unit sizes in Alaska vary
depending on the latitudinal location of the unit. The 15-minute
DEM data consist of a regular array of elevation referenced
horizontally to the geographic (latitude/longitude) coordinate
system of NAD 27. The spacing
between elevations along profiles is 2 arc seconds of latitude
by 3 arc seconds of longitude.
Seward, Alaska DEM (58.8KB)
- Intermediate scale
- The 2-arc-second DEM data cover 30-minute by 30-minute areas which
correspond to the east half or west half of the USGS 30- by
60-minute topographic quadrangle map series for the conterminous
United States and Hawaii. Each 2-arc-second unit is produced and
distributed as four 15- by 15-minute cells. The spacing of
elevations along and between each profile is 2 arc seconds.
Sheridan, Wyoming DEM (80.9KB)
- Small scale
- The 1-degree DEM (3- by 3-arc-second data spacing) provides
coverage in 1- by 1-degree blocks for all of the contiguous
United States, Hawaii, and most of Alaska. The
basic elevation model is produced by or for the Defense Mapping
Agency (DMA), but is distributed by the USGS,
in DEM data record format. In reformatting the product, the
USGS does not change the basic elevation information. The 1-degree
DEMs are also referred to as 3-arc-second or 1:250,000 scale
DEM data.
Yellowstone DEM (31.8KB)
- The EROS Data Center (EDC) also concatenated the 1- by 1-degree blocks for the contiguous United States in the Land Analysis System (LAS)
environment using the elevation data from the photographic
sources. This is referred to as the 1-degree DEM mosaic data set.
Nine strips of concatenated imagery comprise the data
set.
Extent of Coverage
- Large scale
- The UTM-based 7.5-minute DEM data are available for much of the
contiguous United States, Hawaii, and Puerto Rico. Data availability for
the contiguous United States may be viewed on a status coverage
map.
The geographic-based 15-minute Alaska DEM data are available for most
of Alaska.
- The 7.5-minute DEM data are available for portions of Alaska.
- Intermediate scale
- The 2-arc-second DEM data are available for portions of the
contiguous United States and Hawaii.
- Small scale
- The 1-degree DEM data are available for all of the contiguous
United States, Hawaii, and most of Alaska. The concatenated
images (1-degree mosaic data) cover only the contiguous United States.
Acquisition
Processing Steps
- Large scale
- The 7.5-minute DEM data are produced in 7.5- by 7.5-minute
blocks either from digitized cartographic
map contour overlays or from scanned National Aerial Photography
Program (NAPP) photographs.
- Four processes have been used to generate DEM data for
7.5-minute units. The first three processes have been
discontinued:
- The Gestalt Photo Mapper II (GPM2) is an automated
photogrammetric system designed to produce orthophotos, digital
terrain data, and contours in subunits known as patches.
- Manual profiling from photogrammetric stereomodels uses
stereoplotters equipped with three-axis electronic digital
profile recording modules for scanning stereomodels along
successive terrain profiles.
- Elevations are recorded by stereomodel digitizing
of contours, in which digital contours are acquired on stereoplotters
equipped with three-axis digital recording modules.
- Interpolation from digital line graph (DLG)
hypsographic and hydrographic data.
All data now being generated use this process.
- The 15-minute Alaska DEM data are produced to match the
spatial format of the 1:63,360-scale source contours. The
primary process used for production of Alaska DEMs is to combine
digitized hypsographic and hydrographic data from 1:63,360-scale
graphics. Processing can include all of the scanning,
resampling, and contour interpolation programs previously
mentioned. If derived from hypsography overlays, data production
for this series is classified according to Level 2 specifications.
- Intermediate scale
- The
USGS uses two processes to collect the digital elevation data
for production
of 2-arc-second DEMs: (1) derivation from DLG contours of any map
series 7.5 minutes to 30 by 60 minutes (1:24,000 scale to
1:100,000 scale); and (2) resampling from digital elevation models
with a source spacing equal to or less than a 2-arc-second
sampling interval (if the data are resampled from preexisting
DEMs, they are arbitrarily archived as Level 1). The DEM data for
this series are tested according to Level 2 accuracy
specifications.
- Small scale
- The majority of the 1-degree
DEMs are produced by DMA from cartographic
and photographic sources. Elevation data from cartographic
sources are collected from any map series 7.5 minutes through
1 degree (1:24,000 scale through 1:250,000 scale). The topographic
features (e.g., contours, drain lines,
ridge lines, lakes, and spot elevations) are first digitized
and then processed into the required matrix form and interval
spacing.
- Elevation data from photographic sources are
collected by using manual and automated correlation
techniques. Elevations along a profile are
collected at 80 to 100 percent of the eventual point spacing.
The raw elevations are weighted with additional information such
as drainage, ridge, water,
and spot heights during the interpolation process in which
final elevations are determined for the required matrix form and
interval spacing.
- The DEMs distributed within the Department of Defense cover
1- by 1-degree blocks and are called Digital Terrain Elevation Data
Level 1 (DTED-1). In reformatting the DMA product
to create the DEMs, the USGS restructures the header records
and data but does not change the basic elevation information.
- The DMA 1-degree DTED-1 data and the USGS-distributed
1-degree DEMs are gridded by using the World Geodetic System
1972 (WGS 72) or World Geodetic System 1984
(WGS 84). All 1-degree
DEMs were converted to WGS 84.
- The EDC concatenated the 1- by
1-degree blocks for the contiguous United States in the
LAS environment using the elevation data
from the photographic sources. The starting line and sample of
each 1- by 1-degree image was calculated from the projection
coordinates, contained in the data descriptor record, to
form nine strips of data. The coordinates of each strip, along
with their number of lines (rows) and samples (columns), are:
strip coordinate range line/sample
1 50N 125W / 31N 113W 22801/14401
2 50N 117W / 31N 106W 22801/13201
3 50N 110W / 28N 100W 26401/12001
4 50N 104W / 25N 95W 30001/10801
5 50N 99W / 25N 90W 30001/10801
6 50N 94W / 29N 83W 25201/13201
7 50N 87W / 24N 79W 31201/ 9601
8 50N 83W / 24N 75W 31201/ 9601
9 50N 79W / 33N 66W 20401/15601
Data Characteristics
- Large scale
- Each 7.5-minute unit of DEM coverage (based on the 7.5-minute quadrangle) consists of a regular array of elevations referenced horizontally in the UTM projection coordinate system. Elevation units are in meters or feet relative to National Geodetic Vertical Datum of 1929 (NGVD 29) in the continental U.S. and local mean sea level in Hawaii and Puerto Rico. The data are ordered from south to north in profiles that are ordered from west to east.
- These horizontally referenced data may be NAD 27, NAD 83, Old Hawaiian Datum (OHD), or Puerto Rico Datum (PRD) of 1940.
- The 7.5-minute Alaska DEMs consist of a regular array of elevations referenced horizontally to the geographic (latitude/longitude) coordinate system of NAD 27 or NAD 83. The data are ordered from south to north in profiles that are ordered from west to east. The unit of coverage corresponds to four basic quadrangle sizes for 1:63,360 scale graphics (depending on latitude):
- Cell size limits
- 7.5 by 18 minutes -- State of Alaska north of 68°N latitude
- 7.5 by 15 minutes -- Between 62°N and 68°N latitude
- 7.5 by 11.25 minutes -- Between 59°N and 62°N latitude
- 7.5 by 10 minutes -- State of Alaska south of 59°N latitude
- The 15-minute Alaska DEMs consist of a regular array of elevations referenced horizontally to the geographic (latitude/longitude) coordinate system of NAD 27 or NAD 83. The data are ordered from south to north in profiles that are ordered from west to east. Elevation units are in meters or feet relative to NGVD 29. The unit of coverage corresponds to four basic quadrangle sizes for 1:63,360-scale graphics (depending on latitude):
- Cell size limits
- 15 by 36 minutes -- State of Alaska north of 68°N latitude
- 15 by 30 minutes -- Between 62°N and 68°N latitude
- 15 by 2.5 minutes -- Between 59°N and 62°N latitude
- 15 by 20 minutes -- State of Alaska south of 59°N latitude
- Intermediate scale
- The 2-arc-second DEM data consist of a regular array of elevations referenced horizontally to the geographic (latitude/longitude) coordinate system of NAD 27 or
NAD 83. The unit of coverage is a 30- by 30-minute block. Saleable units are four
15-minute DEMs covering a 30- by 30-minute area. Elevation data on the integer
minute lines (all four sides) correspond to the same profiles on the surrounding
eight blocks. Elevations are in meters or feet relative to NGVD 29.
- Small scale
- The 1-degree DEM consists of a regular array of elevations referenced horizontally on the geographic
(latitude/longitude) coordinate system of the WGS 72 (converted to WGS 84). The information content is
approximately equivalent to that which can be derived from contour information represented on 1:250,000 scale
maps.The unit of coverage is a 1- by 1-degree block. Elevation data on the integer degree lines (all four sides) overlap with
the corresponding profiles on the surrounding eight blocks.
- Elevations are in meters relative to NGVD 29 in the continental U.S.
and local mean sea level in Hawaii. DEM accuracy information is provided in the
Appendix.
- The 1-degree DEM mosaic data set is characteristically the same as the source 1- by 1-degree DEM unit of coverage.
Spatial Resolution
- Large scale
- The 7.5-minute DEM data are stored as profiles in which the spacing of the elevations along and between each profile is 30 meters. The number of elevations in a profile will vary because of the variable angle between the quadrangle's geographic boundary (neatline) and the UTM coordinate system. DEM data of low-relief terrain or generated from contour maps with intervals of 10 feet or less are recorded in feet while DEM data of moderate to high-relief terrain or generated from maps with terrain contour intervals greater than 10 feet are generally recorded in meters.
UTM Meter Grid for 7.5 DEM
- The 15-minute DEM data are collected with a 2- by 3-arc-second spacing in
latitude, and longitude, respectively. The first and last data points
along a profile are at the integer degrees of latitude. Elevation data on
the quadrangle neatlines (all four sides) share edge profiles with the
surrounding eight quadrangles.
- Intermediate scale
- Spacing of the elevations along each profile is 2 arc seconds. The first
and last data points are at the integer 15 minutes of latitude. A
15-minute profile will, therefore, contain 451 elevations.
- Small scale
- Spacing of elevations along and between each profile of 1-degree DEMs is 3 arc seconds with 1,201 elevations per profile. The exception is DEM data in Alaska, where the profile spacing varies depending on the latitudinal location of the DEM. Latitudes between 50 and 70 degrees north have spacings at 6 arc seconds with 601 profiles per 1-degree unit and latitudes greater than 70 degrees north have spacings at 9 arc seconds with 401 profiles per 1-degree unit.
- The 1-degree mosaic data set spacing of elevation and profile data is the same as the data of conterminous U.S. 1-degree DEM data set.
Arc Second Grid for 1-degree DEM
DEM Accuracy
The method of determining DEM accuracy involves computation of the root-mean-square error (RMSE) for linearly interpolated elevations in the DEM and corresponding true elevations from the
published maps. Test points are well distributed and representative of the
terrain. Collection of test point data and comparison of the DEM to the
quadrangle hypsography are conducted by USGS quality-control groups.
- Large scale
- The vertical accuracy of 7.5-minute DEMs is equal to or better than 15 meters. A minimum of 28 test points per DEM is required (20 interior points and 8 edge points). The accuracy of the 7.5-minute DEM data, together with the
data spacing, adequately support computer applications that analyze
hypsographic features to a level of detail similar to manual interpretations
of information as printed at map scales not larger than 1:24,000 scale.
Accuracy of the 15-minute DEMs is equal to or better than one-half of a contour
interval of the 15-minute topographic quadrangle map. The accuracy of the
15-minute DEM data, together with the data spacing, adequately support
computer applications that analyze hypsographic features to a level of
detail similar to manual interpretations of information as printed at map
scales not larger than 1:63,360 scale. The plotting of contours from the
15-minute Alaska DEMs at scales larger than 1:63,360, or reliance on the
elevation heights without incorporating the National Map Accuracy Standard
(NMAS) horizontal error tolerance, will lead to less reliable results.
- Intermediate scale
- The 2-arc-second DEM accuracy is equal to or better than one-half of a contour interval of the 30- by 60-minute topographic quadrangle map. The accuracy
of the 2-arc-second DEM data, together with the data spacing, adequately
support computer applications that analyze hypsographic features to a level
of detail similar to manual interpretations of information as printed at
map scales not larger than 1:100,000 scale. The plotting of contours from
2-arc-second DEM data at scales larger than 1:100,000, or reliance on the
elevation heights without incorporating the NMAS horizontal error
tolerance, will lead to less reliable results.
- Small scale
- The 1-degree mosaic data set spacing of elevation and profile data is the same as the 1-degree DEM contiguous U.S. data. The accuracy of the 1-degree
DEM data, together with the data spacing, adequately support computer
applications that analyze hypsographic features to a level of detail
similar to manual interpretations of information as printed at map scales
not larger than 1:250,000 scale. The plotting of contours from the 1-degree DEM
at scales larger than 1:250,000, or reliance on the elevation heights
without incorporating the NMAS horizontal error tolerance, will lead to
less reliable results.
- For general information on accuracy, see Horizontal Positional Accuracy and Vertical Positional Accuracy.
Data Organization
A DEM file is organized into three logical records:
contains information defining the general
characteristics of the DEM, including DEM
name, boundaries, units of measurement,
minimum and maximum elevations, projection
parameters, and number of type B records.
Each DEM file has one Type A record.
contains profiles of elevation data and
associated header information. Each profile
has a Type B record.
contains statistics on the accuracy of the
data.
Examples of a DEM record format may be found in the
Appendix.
Entity and Attribute Information
A digital elevation model is composed of
integer values
representing a gridded form of a topographic map hypsography overlay.
Additional information on DEM specifications can be found in the USGS National
Mapping Program's Standards for Digital Elevation Model (DEMs) and in the USGS
publication titled "Digital Elevation Models -- Data Users Guide 5."
Classification Levels
DEM data are organized in three classification levels. Level-1 DEMs are
elevation data sets in a standardized format. The intent is to reserve
this level for 7.5-minute DEMs which are created by scanning National High Altitude Photography (NHAP)/NAPP
photography. A vertical RMSE of 7 meters is the desired accuracy
standard. A RMSE of 15 meters is the maximum permitted.
Level-2 DEMs are elevation data sets that have been processed or smoothed
for consistency and edited to remove identifiable systematic errors. DEM
data derived from hyposographic and hydrographic data digitizing, either
photogrammetrically or from existing maps, are entered into the Level-2
category. A RMSE of one-half contour interval is the maximum permitted.
Level-3 DEMs are derived from DLG data by incorporating selected elements
from both hypsography (contours, spot elevations) and hydrography (lakes,
shorelines, drainage). A RMSE of one-third of the contour interval is the
maximum permitted.
Digital Elevation Model Caveats
- Large scale
- The majority of the 7.5-minute DEMs produced to date are categorized as
Level-1 DEMs.
- Intermediate scale
- All 2-arc-second DEMs derived from contours are Level 2. All 2-arc-second DEMs
derived for 7.5-minute DEMs are Level 1.
- Small scale
- All 1-degree DMA DTED-1 data have been classified as Level 3.
A more detailed description of the DEM accuracy and classification levels
may be found in the USGS publication titled "Digital Elevation Models -- Data Users Guide 5."
Data Availability
Procedures for Obtaining Data
To place orders and to obtain additional information regarding technical
details and pricing schedules, contact:
Customer Services, EROS Data Center
Earth Science Information
Centers (ESICs)
A Data Users Guide is provided with each mailed order. Data Users Guides
and Technical Instructions also may be ordered separately for a nominal
fee.
- Large and Intermediate scale
- The data are available now (at the cost of
reproduction) through a semi-anonymous FTP account at the EDC, on 3480 magnetic tape, 8mm cartridges, or CD-Recordable. The data also are available in SDTS format through anonymous FTP at no cost. (only SDTS format)
SDTS FTP Instructions
- To access the account for the 7.5 MIN DEM data:
- FTP to edcftp.cr.usgs.gov
- Enter "anonymous" at the Name prompt.
- Enter your complete e-mail address at the Password prompt.
- Change (cd) to the "pub/data/DEM" subdirectory.
- Set the file transfer mode to binary by typing the word "binary".
- Use the "get" or "mget" commands to download the 00README and data
files.
- The 00README file located in the "pub/data/DEM" subdirectory contains
an explanation of the directory structure.
- Small scale
- The data are available at no charge through an anonymous File Transfer Protocol (FTP) account at the
EDC.
- FTP Instructions
- To access the account:
- FTP to edcftp.cr.usgs.gov
- Enter "anonymous" at the Name prompt.
- Enter your complete e-mail address at the
- Password prompt.
- Change (cd) to the "pub/data/DEM/250"
- subdirectory.
- Set the file transfer mode to binary by
- typing the word "binary".
- Use the "get" and "mget" commands to
- download the 00README or data files.
- The 00README file located under the
- "/pub/data/DEM/250" subdirectory
- contains an explanation of the directory
- structure and instructions for
- uncompressing data files.
- The files are also available sorted by state,
or can be selected from an
index map.
The data are available on 3480 magnetic tape, 8mm cartridges, or
CD-Recordable.
The mosaic data set is available as a set of three 8mm cartridges in
raster,
compressed LAS format.
Online requests for these data can be placed via the USGS
Global Land Information System
(GLIS) interactive query system. The GLIS system contains metadata and
online samples of Earth science data. With GLIS, you may review metadata,
determine product availability, and place online requests for products.
- The 1-degree DEM files are written as ANSI-standard ASCII characters in
fixed-block format. The 1-degree DEM mosaic data set is in the LAS format.
(See Data Availability).
Applications and Related Data Sets
The DEM files may be used in the generation of graphics such as isometric
projections displaying slope, direction of slope (aspect), and terrain
profiles between designated points. They may also be combined with other
data types such as stream location data and weather data to assist in
forest fire control or they may be combined with remote sensing data to aid
in the classification of vegetation. Applications include: (1) modeling
terrain gravity data for use in locating energy resources, (2) determining
the volume of proposed reservoirs, (3) calculating the amount of material
removed during strip mining, (4) determining landslide probability, and (5)
developing parameters for hydrologic models.
Further information regarding additional data sets may be obtained by
contacting:
ESIC
References
- Large scale
- U.S. Geological Survey, 1992, US GeoData, [brochure]: [Reston,
Virginia],
U.S. Geological Survey, 2 p. [fold out, oversized]
- U.S. Geological Survey, 1992, US GeoData data users guides and
associated
documentation, order form: [Reston, Virginia], U.S. Geological Survey, 2
p.
- U.S. Geological Survey, 1993, Digital elevation models -- data users guide 5: Reston, Virginia, U.S. Geological Survey, 48 p.
- U.S. Geological Survey, 1993, US GeoData digital elevation model,
factsheet:
[Reston, Virginia], U.S. Geological Survey, 2 p.
- U.S. Geological Survey, 1994, Cartographic technical instructions,
price
list: [Reston, Virginia], U.S. Geological Survey, 2 p.
- U.S. Geological Survey, 1994, US GeoData available through the
Internet, factsheet: [Reston, Virginia], U.S. Geological Survey, 2 p.
- Intermediate scale
- U.S. Geological Survey, 1993, Digital elevation models
--data users guide 5: Reston, Virginia, U.S. Geological Survey, 48 p.
- Small scale
- U.S. Geological Survey, 1993, Digital elevation models
--data users guide 5: Reston, Virginia, U.S. Geological Survey, 48 p.
Appendix
A soft copy in ASCII text format of the individual records is available at:
<URL:ftp://www-nmd.er.usgs.gov/pub/ti/DEM/demstnds/pt2_apps_dem.txt>
DEM Accuracy
General Information
The accuracy of a DEM is dependent upon its source and the spatial resolution, that is grid spacing,
of the data profiles. One factor influencing DEM accuracy is source data scale and resolution. A
dependency exists between the scale of the source materials and the level of grid refinement
possible. The source resolution is also a factor in determining the level of content that may be
extracted during digitization. For example, 1:250,000-scale topographic maps are the primary
source of 1-degree DEMs.
Another factor is the horizontal and vertical dimension of the DEM. Horizontal accuracy of DEM
data is dependent upon the horizontal spacing of the elevation matrix. Within a standard DEM,
most terrain features are generalized by being reduced to grid nodes spaced at regular intersections
in the horizontal plane. This generalization reduces the ability to recover positions of specific
features less than the internal spacing during testing and results in a de facto filtering or smoothing
of the surface during gridding.
Vertical accuracy of DEM data is dependent upon the spatial resolution (horizontal grid spacing),
quality of the source data, collection and processing procedures, and digitizing systems. As with
horizontal accuracy, the entire process, beginning with project authorization, compilation of the
source data sets, and the final gridding process, must satisfy accuracy criteria customarily applied
to each system. Each source data set must qualify to be used in the next step of the process. Errors
have the effect of compounding for each step of the process. Production personnel are directed to
account for each production step leading to the final DEM.
SDTS Format
The Spatial Data Transfer Standard (SDTS) distribution format is designed
as a mechanism for the transfer of spatial data between various computer
systems. The SDTS format is designed to transfer data with complete content
transfer (no loss of information). Data quality reports provide complete
metadata and documentation of processing. The SDTS is a
FIPS standard intended to work
between various platforms and various data models. There is limited software
available at this time which can accommodate the SDTS-formatted data.
For more in-depth information on SDTS, refer to the SDTS technical
documentation (available online).