GDALDEM(1)
β¨ GDALDEM(1) β¨
okay so this is gdaldem from the GDAL manual, and bestie, itβs literally the glow-up tool for DEMs β analyzing and visualizing them, no cap. Letβs get into it π
π NAME π
gdaldem β tools to analyze and visualize DEMs.
π¦ SYNOPSIS π¦
The basic shape is giving:
gdaldem <mode> <input> <output> <options>
Generate a shaded relief map from any GDAL-supported elevation raster:
gdaldem hillshade input_dem output_hillshade
[-z ZFactor (default=1)] [-s scale* (default=1)]
[-az Azimuth (default=315)] [-alt Altitude (default=45)]
[-alg Horn|ZevenbergenThorne] [-combined | -multidirectional | -igor]
[-compute_edges] [-b Band (default=1)] [-of format] [-co "NAME=VALUE"]* [-q]
Generate a slope map from any GDAL-supported elevation raster:
gdaldem slope input_dem output_slope_map
[-p use percent slope (default=degrees)] [-s scale* (default=1)]
[-alg Horn|ZevenbergenThorne]
[-compute_edges] [-b Band (default=1)] [-of format] [-co "NAME=VALUE"]* [-q]
Generate an aspect map from any GDAL-supported elevation raster, outputs a 32-bit float raster with pixel values from 0-360 indicating azimuth:
gdaldem aspect input_dem output_aspect_map
[-trigonometric] [-zero_for_flat]
[-alg Horn|ZevenbergenThorne]
[-compute_edges] [-b Band (default=1)] [-of format] [-co "NAME=VALUE"]* [-q]
Generate a color relief map from any GDAL-supported elevation raster:
gdaldem color-relief input_dem color_text_file output_color_relief_map
[-alpha] [-exact_color_entry | -nearest_color_entry]
[-b Band (default=1)] [-of format] [-co "NAME=VALUE"]* [-q]
where color_text_file contains lines of the format "elevation_value red green blue"
Generate a Terrain Ruggedness Index (TRI) map from any GDAL-supported elevation raster:
gdaldem TRI input_dem output_TRI_map
[-alg Wilson|Riley]
[-compute_edges] [-b Band (default=1)] [-of format] [-q]
Generate a Topographic Position Index (TPI) map from any GDAL-supported elevation raster:
gdaldem TPI input_dem output_TPI_map
[-compute_edges] [-b Band (default=1)] [-of format] [-q]
Generate a roughness map from any GDAL-supported elevation raster:
gdaldem roughness input_dem output_roughness_map
[-compute_edges] [-b Band (default=1)] [-of format] [-q]
π DESCRIPTION π
okay so the big vibe check first: gdaldem generally assumes that x, y and z units are identical. If x (east-west) and y (north-south) units are identical, but z (elevation) units are different, the scale (-s) option can be used to set the ratio of vertical units to horizontal.
For LatLong projections near the equator, where units of latitude and units of longitude are similar, elevation (z) units can be converted to be compatible by using scale=370400 (if elevation is in feet) or scale=111120 (if elevation is in meters). For locations not near the equator, it would be best to reproject your grid using gdalwarp before using gdaldem.
<mode> β where <mode> is one of the seven available modes:
hillshadeβ generate a shaded relief map from any GDAL-supported elevation raster.slopeβ generate a slope map from any GDAL-supported elevation raster.aspectβ generate an aspect map from any GDAL-supported elevation raster.color-reliefβ generate a color relief map from any GDAL-supported elevation raster.TRIβ generate a map of Terrain Ruggedness Index from any GDAL-supported elevation raster.TPIβ generate a map of Topographic Position Index from any GDAL-supported elevation raster.roughnessβ generate a map of roughness from any GDAL-supported elevation raster.
The following general options are available:
input_demβ the input DEM raster to be processed.output_xxx_mapβ the output raster produced.-of <format>β select the output format. New in version 2.3.0: if not specified, the format is guessed from the extension (previously wasraster.gtiff). Use the short format name.-compute_edgesβ do the computation at raster edges and near nodata values.-b <band>β select an input band to be processed. Bands are numbered from 1.-co <NAME=VALUE>β many formats have one or more optional creation options that can be used to control particulars about the file created. For instance, the GeoTIFF driver supports creation options to control compression, and whether the file should be tiled. The creation options available vary by format driver, and some simple formats have no creation options at all. A list of options supported for a format can be listed with the--formatscommand line option but the documentation for the format is the definitive source of information on driver creation options. Seeraster_driversformat specific documentation for legal creation options for each format.-qβ suppress progress monitor and other non-error output.
β οΈ For all algorithms, exceptcolor-relief, a nodata value in the target dataset will be emitted if at least one pixel set to the nodata value is found in the3x3window centered around each source pixel. The consequence is that there will be a1-pixelborder around each image set with nodata value. If-compute_edgesis specified,gdaldemwill compute values at image edges or if a nodata value is found in the3x3window, by interpolating missing values.
π¨ MODES
Okay bestie, this is the fun part β gdaldem has a whole little wardrobe of modes and each one is giving a different main-character terrain analysis vibe. Let's go through them one by one, no skips. π
hillshade
This one outputs an 8-bit raster with a nice shaded relief effect. It's genuinely so useful for visualizing your terrain β like, it makes your DEM look like an actual mountain range instead of soup. β¨
You can optionally specify:
- the azimuth and altitude of the light source
- a vertical exaggeration factor
- a scaling factor to account for differences between vertical and horizontal units
The value 0 is used as the output nodata value.
The following specific options are available:
-alg Horn|ZevenbergenThorneβ picks which algorithm does the math. The literature suggests Zevenbergen & Thorne is more suited to smooth landscapes, whereas Horn's formula performs better on rougher terrain.-z <factor>β vertical exaggeration, used to pre-multiply the elevations.-s <scale>β ratio of vertical units to horizontal. If the horizontal unit of the source DEM is degrees (e.g. Lat/Long WGS84 projection), you can usescale=111120if the vertical units are meters (orscale=370400if they are in feet).-az <azimuth>β azimuth of the light, in degrees.0if it comes from the top of the raster,90from the east, ... The default value,315, should rarely be changed as it is the value generally used to generate shaded maps. (Iconic default behavior, honestly.)-alt <altitude>β altitude of the light, in degrees.90if the light comes from above the DEM,0if it is raking light.-combinedβ combined shading, a combination of slope and oblique shading.-multidirectionalβ multidirectional shading, a combination of hillshading illuminated from225deg,270deg,315deg, and360deg azimuth.
New in version 2.2.
-igorβ shading which tries to minimize effects on other map features beneath. Can't be used with-altoption. π«
New in version 3.0.
Multidirectional hillshading applies the formula of http://pubs.usgs.gov/of/1992/of92-422/of92-422.pdf.
Igor's hillshading uses formula from Maperitive http://maperitive.net/docs/Commands/GenerateReliefImageIgor.html.
slope
This command will take a DEM raster and output a 32-bit float raster with slope values. You have the option of specifying the type of slope value you want: degrees or percent slope. In cases where the horizontal units differ from the vertical units, you can also supply a scaling factor.
The value -9999 is used as the output nodata value.
The following specific options are available:
-alg Horn|ZevenbergenThorneβ same deal as hillshade: the literature suggests Zevenbergen & Thorne is more suited to smooth landscapes, whereas Horn's formula performs better on rougher terrain.-pβ if specified, the slope will be expressed as percent slope. Otherwise, it is expressed as degrees.-sβ ratio of vertical units to horizontal. If the horizontal unit of the source DEM is degrees (e.g. Lat/Long WGS84 projection), you can usescale=111120if the vertical units are meters (orscale=370400if they are in feet).
aspect
This command outputs a 32-bit float raster with values between 0Β° and 360Β° representing the azimuth that slopes are facing. The definition of the azimuth is such that: 0Β° means that the slope is facing the North, 90Β° it's facing the East, 180Β° it's facing the South and 270Β° it's facing the West (provided that the top of your input raster is north oriented). The aspect value -9999 is used as the nodata value to indicate undefined aspect in flat areas with slope=0.
The following specifics options are available:
-alg Horn|ZevenbergenThorneβ yep, same line again: Zevenbergen & Thorne for smooth landscapes, Horn for rougher terrain.-trigonometricβ return trigonometric angle instead of azimuth. Thus0Β°means East,90Β°North,180Β°West,270Β°South.-zero_for_flatβ return0for flat areas withslope=0, instead of-9999.
By using those 2 options, the aspect returned by gdaldem aspect should be identical to the one of GRASS r.slope.aspect. Otherwise, it's identical to the one of Matthew Perry's aspect.cpp utility. π§
color-relief
This command outputs a 3-band (RGB) or 4-band (RGBA) raster with values computed from the elevation and a text-based color configuration file, containing the association between various elevation values and the corresponding wished color. By default, the colors between the given elevation values are blended smoothly and the result is a nice colorized DEM. π The -exact_color_entry or -nearest_color_entry options can be used to avoid that linear interpolation for values that don't match an index of the color configuration file.
The following specifics options are available:
color_text_fileβ text-based color configuration file.-alphaβ add an alpha channel to the output raster.-exact_color_entryβ use strict matching when searching in the color configuration file. If none matching color entry is found, the"0,0,0,0"RGBA quadruplet will be used.-nearest_color_entryβ use the RGBA quadruplet corresponding to the closest entry in the color configuration file.
The color-relief mode is the only mode that supports VRT as output format. In that case, it will translate the color configuration file into appropriate LUT elements. Note that elevations specified as percentage will be translated as absolute values, which must be taken into account when the statistics of the source raster differ from the one that was used when building the VRT. β οΈ
The text-based color configuration file generally contains 4 columns per line: the elevation value and the corresponding Red, Green, Blue component (between 0 and 255). The elevation value can be any floating point value, or the nv keyword for the nodata value. The elevation can also be expressed as a percentage: 0% being the minimum value found in the raster, 100% the maximum value.
An extra column can be optionally added for the alpha component. If it is not specified, full opacity (255) is assumed.
Various field separators are accepted: comma, tabulation, spaces, ':'.
Common colors used by GRASS can also be specified by using their name, instead of the RGB triplet. The supported list is: white, black, red, green, blue, yellow, magenta, cyan, aqua, grey/gray, orange, brown, purple/violet and indigo.
GMT .cpt palette files are also supported (COLOR_MODEL = RGB only).
Note: the syntax of the color configuration file is derived from the one supported by GRASSr.colorsutility. ESRI HDR color table files (.clr) also match that syntax. The alpha component and the support of tab and comma as separators are GDAL specific extensions. π
For example:
3500 white
2500 235:220:175
50% 190 185 135
700 240 250 150
0 50 180 50
nv 0 0 0 0
To implement a "round to the floor value" mode, the elevation value can be duplicate with a new value being slightly above the threshold. For example to have red in [0,10], green in ]10,20] and blue in ]20,30]:
0 red
10 red
10.001 green
20 green
20.001 blue
30 blue
TRI
This command outputs a single-band raster with values computed from the elevation. TRI stands for Terrain Ruggedness Index, which measures the difference between a central pixel and its surrounding cells. ποΈ
The value -9999 is used as the output nodata value.
The following option is available:
-alg Wilson|Rileyβ starting with GDAL 3.3, the Riley algorithm (see Riley, S.J., De Gloria, S.D., Elliot, R. (1999): A Terrain Ruggedness that Quantifies Topographic Heterogeneity. Intermountain Journal of Science, Vol.5, No.1-4, pp.23-27) is available and the new default value. This algorithm uses the square root of the sum of the square of the difference between a central pixel and its surrounding cells. This is recommended for terrestrial use cases.
The Wilson (see Wilson et al 2007, Marine Geodesy 30:3-35) algorithm uses the mean difference between a central pixel and its surrounding cells. This is recommended for bathymetric use cases.
TPI
This command outputs a single-band raster with values computed from the elevation. TPI stands for Topographic Position Index, which is defined as the difference between a central pixel and the mean of its surrounding cells (see Wilson et al 2007, Marine Geodesy 30:3-35).
The value -9999 is used as the output nodata value.
There are no specific options. (A low-maintenance icon, honestly. π )
roughness
This command outputs a single-band raster with values computed from the elevation. Roughness is the largest inter-cell difference of a central pixel and its surrounding cell, as defined in Wilson et al (2007, Marine Geodesy 30:3-35).
The value -9999 is used as the output nodata value.
There are no specific options either. Slay, simple.
π§© C API
This utility is also callable from C with GDALDEMProcessing().
New in version 2.1.
π AUTHORS
Matthew Perry perrygeo@gmail.com, Even Rouault even.rouault@spatialys.com, Howard Butler hobu.inc@gmail.com, Chris Yesson chris.yesson@ioz.ac.uk
Derived from code by Michael Shapiro, Olga Waupotitsch, Marjorie Larson, Jim Westervelt: U.S. Army CERL, 1993. GRASS 4.1 Reference Manual. U.S. Army Corps of Engineers, Construction Engineering Research Laboratories, Champaign, Illinois, 1-425.
π SEE ALSO
Documentation of related GRASS utilities:
https://grass.osgeo.org/grass79/manuals/r.slope.aspect.html
https://grass.osgeo.org/grass79/manuals/r.relief.html
https://grass.osgeo.org/grass79/manuals/r.colors.html
β¨ AUTHOR
Matthew Perry <perrygeo@gmail.com>, Even Rouault <even.rouault@spatialys.com>, Howard Butler <hobu.inc@gmail.com>, Chris Yesson <chris.yesson@ioz.ac.uk>
π COPYRIGHT
1998-2026
That's the whole page bestie, you made it to the end!! π«Ά This edition is dated Jan 08, 2026 and it's the GDALDEM(1) man page β go forth and shade some hills. ππ₯
π¦ where this page comes from
- epel 9: gdal3.4 3.4.3-5.el9 Β· MIT
- π girlified by deepseek-ai/DeepSeek-V4.1-Flash-1017 on : a language model's rewrite of the original, under its terms