
Gelisol - Wikipedia
Gelisols are an order in USDA soil taxonomy. They are soils of very cold climates which are defined as containing permafrost within two meters (6 ft 7 in) of the soil surface.
Gelisol | Permafrost, Cryosols, Tundra | Britannica
Gelisols are perennially frozen soils of the Arctic and Antarctic regions, but they are also found at extremely high elevations in the lower latitudes. They are fragile, easily eroded soils, and their location near the polar ice caps makes them important indicators of the …
Gelisols - Natural Resources Conservation Service
Gelisols are soils that have permafrost near the soil surface and/or have evidence of cryoturbation (frost churning) and/or ice segregation.
Gelisols | Soil & Water Systems | University of Idaho
Gelisols (from Latin gelare, "to freeze") are soils of very cold climates that contain permafrost within two meters of the surface. These soils are limited geographically to the high-latitude polar regions and localized areas at high mountain elevations.
5.12 - Gelisols | Soil Genesis and Development, Lesson 5 - Soil ...
Gelisols are soils with permafrost within 2 meters of the surface. These soils generally have limited profile development. Most of the soil forming processes in these soils occur near the surface, sometimes resulting in significant accumulation of organic matter.
The Twelve Soil Orders - Rangelands Gateway
Gelisols are soils of very cold climates that contain permafrost within 2 meters of the surface. These soils are limited geographically to the high-latitude polar regions and localized areas at high mountain elevations.
Gelisols: Part II. Classification and Related Issues
Jul 2, 2013 · Gelisols, most notably those with ice-cemented permafrost, have unique morphological properties caused by patterned ground formation, cryoturbation, and cryostructures caused by freeze–thaw cycles.
Gelisols - SpringerLink
Jan 1, 2014 · Gelic materials are mineral or organic soil materials that have evidence of cryoturbation (frost churning), ice segregation in the active layer, or the upper part of the permafrost. Low soil temperatures cause soil-forming processes such as decomposition of organic materials to proceed very slowly.
Gelisols: Part I. Cryogenesis and State Factors of Formation
May 8, 2013 · Gelisols are soils affected by permafrost. It was the 12th order added to Soil Taxonomy, the U.S. soil classification system. They are classified as Cryosols in both of the World Reference Base and the Canadian System of Soil Classification, and Cryozem in the Russian soil classification system.
Soil Orders | Soil & Water Systems | University of Idaho
Learn about the twelve soil orders from the Department of Soils and Water Systems as part of the College of Agricultural and Life Sciences at the University of Idaho.
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