Rangelands of the desert Southwest can be in a degraded condition and lacking perennial vegetation, which can lead to exposed soil and erosion.
Where can I obtain soil surveys?
A soil survey is the systematic description, classification, and mapping of soils in an area. They are published by the USDA Natural Resources Conservation Service (NRCS), formerly known as the Soil Conservation Service.
NRCS soil surveys are available from several sources:
- Some are on the NRCS website.
- Published soil surveys can be found at some libraries or borrowed through interlibrary loan.
- Surveys might be available from the state NRCS offices.
- Online GIS data of the Gridded Soil Survey Geographic Database is here.
- The USGS Libraries have a majority of the soil surveys in our collection, available to the public through interlibrary loan.
The USGS does have a low-density soil map for the conterminous U.S. (geochemical and mineralogical data) and a National Geochemical Database for soil that includes a small number of sites in Alaska and outside the U.S.
Related Content
Does the USGS have reports on the background levels of elements in soils and other surficial materials?
The following USGS products will be helpful in determining the background levels of various elements in soils and other surficial materials: Geochemical and Mineralogical Data for Soils of the Conterminous United States (2013) Data for samples collected at three intervals (0-5 cm surficial soils, A-Horizon soils, and C-Horizon soils) across the entire conterminous U.S. These data provide the best...
How are harmful elements and compounds in plants, soils, rocks, and sediments regulated?
Regulatory limits for safe levels of elements in water and foodstuffs are established by the U.S. Environmental Protection Agency (EPA) and the U.S. Food and Drug Administration (FDA). However, there are generally no regulatory limits that scientists can refer to when dealing with plants, soils, rocks, and sediments. Therefore, to determine whether a plant, soil, rock, or sediment contains a 'high...
What are some benefits of volcanic eruptions?
Over geologic time, volcanic eruptions and related processes have directly and indirectly benefited mankind: Volcanic materials ultimately break down and weather to form some of the most fertile soils on Earth, cultivation of which has produced abundant food and fostered civilizations. The internal heat associated with young volcanic systems has been harnessed to produce geothermal energy . Most...
Rangelands of the desert Southwest can be in a degraded condition and lacking perennial vegetation, which can lead to exposed soil and erosion.
On the Colorado Plateau, mature biocrusts are bumpy and dark-colored due to the presence of lichens, mosses, and high densities of cyanobacteria and other organisms. Disturbed biocrusts are lighter in color, looking more like the underlying sand than undisturbed ones, and are less capable of stabilizing soils or providing soil fertility.
On the Colorado Plateau, mature biocrusts are bumpy and dark-colored due to the presence of lichens, mosses, and high densities of cyanobacteria and other organisms. Disturbed biocrusts are lighter in color, looking more like the underlying sand than undisturbed ones, and are less capable of stabilizing soils or providing soil fertility.
Many human activities can be unintentionally harmful to biological crusts. The biocrusts are no match for the compressional stress caused by footprints of livestock or people or tracks from vehicles.
Many human activities can be unintentionally harmful to biological crusts. The biocrusts are no match for the compressional stress caused by footprints of livestock or people or tracks from vehicles.
Biocrusts provide soil stability and prevent erosion. Soil is the foundation where plants live; if soil is not stable, native plants can have difficulty growing.
Biocrusts provide soil stability and prevent erosion. Soil is the foundation where plants live; if soil is not stable, native plants can have difficulty growing.
USGS scientist Sasha Reed studies sites where different climate conditions are being mimicked to determine effect on biocrusts.
USGS scientist Sasha Reed studies sites where different climate conditions are being mimicked to determine effect on biocrusts.
USGS researchers collecting a soil sample for rare earth elements at the Roy Creek prospect, Alaska. Jamey Jones is holding the bag while Erin Todd shovels soil into the bag.
USGS researchers collecting a soil sample for rare earth elements at the Roy Creek prospect, Alaska. Jamey Jones is holding the bag while Erin Todd shovels soil into the bag.
Amount of soil (about 200 mg) from which Geomyces destructans was cultured. This shows the small amount of soil needed to harbor live fungus and the threat that humans might pose in moving it around from cave to cave on their gear, boots, and clothing.
Amount of soil (about 200 mg) from which Geomyces destructans was cultured. This shows the small amount of soil needed to harbor live fungus and the threat that humans might pose in moving it around from cave to cave on their gear, boots, and clothing.
Soil core obtained from existing goose grazing lawn along the Smith River in the Teshekpuk Lake Special Area of the National Petroleum Reserve - Alaska. The buried layer of peat beneath goose grazing lawn demonstrates that vegetation change has occurred in this area.
Soil core obtained from existing goose grazing lawn along the Smith River in the Teshekpuk Lake Special Area of the National Petroleum Reserve - Alaska. The buried layer of peat beneath goose grazing lawn demonstrates that vegetation change has occurred in this area.
Every year, billions of tons of fine desert dust from the Saharan Desert are transported thousands of miles through the atmosphere to the Americas, Europe and the Near East. Living microorganisms and chemical contaminants such as pesticides and metals are carried along with the dust.
Every year, billions of tons of fine desert dust from the Saharan Desert are transported thousands of miles through the atmosphere to the Americas, Europe and the Near East. Living microorganisms and chemical contaminants such as pesticides and metals are carried along with the dust.
JoAnn Holloway(USGS) and Ron Wiederholt(NDSU) collecting soil samples.
JoAnn Holloway(USGS) and Ron Wiederholt(NDSU) collecting soil samples.
Jim Crowley taking spectral measurements of arid soil with a field spectrometer.
Jim Crowley taking spectral measurements of arid soil with a field spectrometer.
Soil mineralogy and geochemistry along a north-south transect in Alaska and the relation to source-rock terrane
Geochemical and mineralogical maps, with interpretation, for soils of the conterminous United States
USGS microbiome research
Hyperspectral surveying for mineral resources in Alaska
The geochemical atlas of Alaska, 2016
Geochemical and mineralogical maps for soils of the conterminous United States
Long-term soil monitoring at U.S. Geological Survey reference watersheds
Mapping grasslands suitable for cellulosic biofuels in the Greater Platte River Basin, United States
Phosphorus and groundwater: Establishing links between agricultural use and transport to streams
The Alaska Geochemical Database: v. 1.0 - Geologic Materials
Biochar for soil fertility and natural carbon sequestration
Health effects of energy resources
Related Content
- FAQ
Does the USGS have reports on the background levels of elements in soils and other surficial materials?
The following USGS products will be helpful in determining the background levels of various elements in soils and other surficial materials: Geochemical and Mineralogical Data for Soils of the Conterminous United States (2013) Data for samples collected at three intervals (0-5 cm surficial soils, A-Horizon soils, and C-Horizon soils) across the entire conterminous U.S. These data provide the best...
How are harmful elements and compounds in plants, soils, rocks, and sediments regulated?
Regulatory limits for safe levels of elements in water and foodstuffs are established by the U.S. Environmental Protection Agency (EPA) and the U.S. Food and Drug Administration (FDA). However, there are generally no regulatory limits that scientists can refer to when dealing with plants, soils, rocks, and sediments. Therefore, to determine whether a plant, soil, rock, or sediment contains a 'high...
What are some benefits of volcanic eruptions?
Over geologic time, volcanic eruptions and related processes have directly and indirectly benefited mankind: Volcanic materials ultimately break down and weather to form some of the most fertile soils on Earth, cultivation of which has produced abundant food and fostered civilizations. The internal heat associated with young volcanic systems has been harnessed to produce geothermal energy . Most...
- Multimedia
Dry, cracked soil (RAMPS)
Rangelands of the desert Southwest can be in a degraded condition and lacking perennial vegetation, which can lead to exposed soil and erosion.
Rangelands of the desert Southwest can be in a degraded condition and lacking perennial vegetation, which can lead to exposed soil and erosion.
BiocrustOn the Colorado Plateau, mature biocrusts are bumpy and dark-colored due to the presence of lichens, mosses, and high densities of cyanobacteria and other organisms. Disturbed biocrusts are lighter in color, looking more like the underlying sand than undisturbed ones, and are less capable of stabilizing soils or providing soil fertility.
On the Colorado Plateau, mature biocrusts are bumpy and dark-colored due to the presence of lichens, mosses, and high densities of cyanobacteria and other organisms. Disturbed biocrusts are lighter in color, looking more like the underlying sand than undisturbed ones, and are less capable of stabilizing soils or providing soil fertility.
Footprint damage to biocrustsMany human activities can be unintentionally harmful to biological crusts. The biocrusts are no match for the compressional stress caused by footprints of livestock or people or tracks from vehicles.
Many human activities can be unintentionally harmful to biological crusts. The biocrusts are no match for the compressional stress caused by footprints of livestock or people or tracks from vehicles.
Biocrusts provide soil stability and prevent erosionBiocrusts provide soil stability and prevent erosionBiocrusts provide soil stability and prevent erosion. Soil is the foundation where plants live; if soil is not stable, native plants can have difficulty growing.
Biocrusts provide soil stability and prevent erosion. Soil is the foundation where plants live; if soil is not stable, native plants can have difficulty growing.
USGS scientist Sasha Reed studys outdoor biocrust testing sitesUSGS scientist Sasha Reed studys outdoor biocrust testing sitesUSGS scientist Sasha Reed studies sites where different climate conditions are being mimicked to determine effect on biocrusts.
USGS scientist Sasha Reed studies sites where different climate conditions are being mimicked to determine effect on biocrusts.
Taking soil samplesUSGS researchers collecting a soil sample for rare earth elements at the Roy Creek prospect, Alaska. Jamey Jones is holding the bag while Erin Todd shovels soil into the bag.
USGS researchers collecting a soil sample for rare earth elements at the Roy Creek prospect, Alaska. Jamey Jones is holding the bag while Erin Todd shovels soil into the bag.
Soil in Test TubeAmount of soil (about 200 mg) from which Geomyces destructans was cultured. This shows the small amount of soil needed to harbor live fungus and the threat that humans might pose in moving it around from cave to cave on their gear, boots, and clothing.
Amount of soil (about 200 mg) from which Geomyces destructans was cultured. This shows the small amount of soil needed to harbor live fungus and the threat that humans might pose in moving it around from cave to cave on their gear, boots, and clothing.
Soil Core Sample #1Soil core obtained from existing goose grazing lawn along the Smith River in the Teshekpuk Lake Special Area of the National Petroleum Reserve - Alaska. The buried layer of peat beneath goose grazing lawn demonstrates that vegetation change has occurred in this area.
Soil core obtained from existing goose grazing lawn along the Smith River in the Teshekpuk Lake Special Area of the National Petroleum Reserve - Alaska. The buried layer of peat beneath goose grazing lawn demonstrates that vegetation change has occurred in this area.
USGS Public Lecture Series: Out of Africa--Dust in the WindUSGS Public Lecture Series: Out of Africa--Dust in the WindUSGS Public Lecture Series: Out of Africa--Dust in the WindEvery year, billions of tons of fine desert dust from the Saharan Desert are transported thousands of miles through the atmosphere to the Americas, Europe and the Near East. Living microorganisms and chemical contaminants such as pesticides and metals are carried along with the dust.
Every year, billions of tons of fine desert dust from the Saharan Desert are transported thousands of miles through the atmosphere to the Americas, Europe and the Near East. Living microorganisms and chemical contaminants such as pesticides and metals are carried along with the dust.
Soil SamplingJoAnn Holloway(USGS) and Ron Wiederholt(NDSU) collecting soil samples.
JoAnn Holloway(USGS) and Ron Wiederholt(NDSU) collecting soil samples.
Arid SoilsJim Crowley taking spectral measurements of arid soil with a field spectrometer.
Jim Crowley taking spectral measurements of arid soil with a field spectrometer.
- Publications
Filter Total Items: 13
Soil mineralogy and geochemistry along a north-south transect in Alaska and the relation to source-rock terrane
Soils collected along a predominately north-south transect in Alaska were used to evaluate regional differences in the soil mineralogy and geochemistry in the context of a geotectonic framework for Alaska. The approximately 1,395-kilometer-long transect followed the Dalton, Elliott, and Richardson Highways from near Prudhoe Bay to Valdez. Sites were selected with a site spacing of approximately 10AuthorsBronwen Wang, Chad P. Hults, Dennis D. Eberl, Laurel G. Woodruff, William F. Cannon, Larry P. GoughGeochemical and mineralogical maps, with interpretation, for soils of the conterminous United States
Between 2007 and 2013, the U.S. Geological Survey conducted a low-density (1 site per 1,600 square kilometers, 4,857 sites) geochemical and mineralogical survey of soils in the conterminous United States. The sampling protocol for the national-scale survey included, at each site, a sample from a depth of 0 to 5 centimeters, a composite of the soil A horizon, and a deeper sample from the soil C horAuthorsDavid B. Smith, Federico Solano, Laurel G. Woodruff, William F. Cannon, Karl J. EllefsenUSGS microbiome research
Microbiomes are the communities of microorganisms (for example, bacteria, viruses, and fungi) that live on, in, and around people, plants, animals, soil, water, and the atmosphere. Microbiomes are active in the functioning of diverse ecosystems, for instance, by influencing water quality, nutrient acquisition and stress tolerance in plants, and stability of soil and aquatic environments. MicrobioAuthorsChristina A. Kellogg, M. Camille HopkinsHyperspectral surveying for mineral resources in Alaska
Alaska is a major producer of base and precious metals and has a high potential for additional undiscovered mineral resources. However, discovery is hindered by Alaska’s vast size, remoteness, and rugged terrain. New methods are needed to overcome these obstacles in order to fully evaluate Alaska’s geology and mineral resource potential. Hyperspectral surveying is one method that can be used to raAuthorsRaymond F. Kokaly, Garth E. Graham, Todd M. Hoefen, Karen D. Kelley, Michaela R. Johnson, Bernard E. HubbardThe geochemical atlas of Alaska, 2016
A rich legacy of geochemical data produced since the early 1960s covers the great expanse of Alaska; careful treatment of such data may provide significant and revealing geochemical maps that may be used for landscape geochemistry, mineral resource exploration, and geoenvironmental investigations over large areas. To maximize the spatial density and extent of data coverage for statewide mapping ofAuthorsGregory K. Lee, Douglas B. Yager, Jeffrey L. Mauk, Matthew Granitto, Paul Denning, Bronwen Wang, Melanie B. WerdonGeochemical and mineralogical maps for soils of the conterminous United States
The U.S. Geological Survey began sampling in 2007 for a low-density (1 site per 1,600 square kilometers, 4,857 sites) geochemical and mineralogical survey of soils in the conterminous United States as part of the North American Soil Geochemical Landscapes Project. The sampling protocol for the national-scale survey included, at each site, a sample from a depth of 0 to 5 centimeters, a composite ofAuthorsDavid B. Smith, William F. Cannon, Laurel G. Woodruff, Federico Solano, Karl J. EllefsenLong-term soil monitoring at U.S. Geological Survey reference watersheds
Monitoring the environment by making repeated measurements through time is essential to evaluate and track the health of ecosystems (fig. 1). Long-term datasets produced by such monitoring are indispensable for evaluating the effectiveness of environmental legislation and for designing mitigation strategies to address environmental changes in an era when human activities are altering the environmeAuthorsMichael R. McHale, Jason Siemion, Gregory B. Lawrence, Alisa MastMapping grasslands suitable for cellulosic biofuels in the Greater Platte River Basin, United States
Biofuels are an important component in the development of alternative energy supplies, which is needed to achieve national energy independence and security in the United States. The most common biofuel product today in the United States is corn-based ethanol; however, its development is limited because of concerns about global food shortages, livestock and food price increases, and water demand inAuthorsBruce K. Wylie, Yingxin GuPhosphorus and groundwater: Establishing links between agricultural use and transport to streams
Phosphorus is a highly reactive element that is essential for life and forms a variety of compounds in terrestrial and aquatic ecosystems. In water, phosphorus may be present as the orthophosphate ion (PO43-) and is also present in all life forms as an essential component of cellular material. In natural ecosystems, phosphorus is derived from the erosion of rocks and is conserved for plant growthAuthorsJoseph L. Domagalski, Henry JohnsonThe Alaska Geochemical Database: v. 1.0 - Geologic Materials
What is the AGDB?: The Alaska Geochemical Database (AGDB) is a new, comprehensive compilation of geologic, spatial, descriptive, mineralogical, and analytical geochemical data for samples collected in Alaska and surrounding waters by the U.S. Geological Survey (USGS) from 1962 to 2009. Data for geologic materials (rocks, minerals and mineral separates, soils, lake sediments, bulk stream sediments,AuthorsJeanine M. Schmidt, Matthew GranittoBiochar for soil fertility and natural carbon sequestration
Biochar is charcoal (similar to chars generated by forest fires) that is made for incorporation into soils to increase soil fertility while providing natural carbon sequestration. The incorporation of biochar into soils can preserve and enrich soils and also slow the rate at which climate change is affecting our planet. Studies on biochar, such as those cited by this report, are applicable to bothAuthorsC.E. Rostad, D.W. RutherfordHealth effects of energy resources
Energy resources (coal, oil, and natural gas) are among the cornerstones of modern industrial society. The exploitation of these resources, however, is not without costs. Energy materials may contain harmful chemical substances that, if mobilized into air, water, or soil, can adversely impact human health and environmental quality. In order to address the issue of human exposure to toxic substanceAuthorsWilliam Orem, Calin Tatu, Nikola Pavlovic, Joseph Bunnell, Allan Kolker, Mark Engle, Ben Stout - News