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Varieties of mountain soils are found throughout the many ranges in Wyoming, with their greatest concentration in the northwest.
Mountain soils in the Rockies are poorly developed, being extremely thin and young and too deficient in nutrients for most types of agriculture.
Two are widely distributed but of limited extent: alluvial soils, found in the major valleys and coastal plains, and poorly developed, or truncated, mountain soils.
Also significant are the desert soils of Rajasthan, the saline soils in Gujarat, southern Rajasthan, and some coastal areas, and the mountain soils of the Himalayas.
Mountain soils are usually shallow at higher altitudes, partly because the soil has been scraped off by the ice caps that formed on most high mountains throughout the world during the last glacial interval that ended about 10,000 years ago.
Mountain soils play an essential role in ecosystem management.
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Wells was helping Edwin Harp, a debris-flow specialist from the United States Geological Survey, collect "undisturbed" samples by hammering plastic tubes into the mountain soil.
Penicillium oxalicum sp. 68 with the collection number CGMCC 7.328 in China General Microbiological Culture Collection Center was isolated from Chang bai mountain soil (Jilin Province, China).
Hymenobacter swuensis is a gamma-radiation resistant bacterium isolated from mountain soil in South Korea (N 35°51′38″, E 127°44′47″; altitude 1500 m).
At Snodgrass Mountain, soil moisture was overall much lower than at the other sites, and differences between P. leptocoma and P. reflexa habitats were smaller, perhaps accounting for the results obtained.
High-mountain soils develop in particularly sensitive environments.
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