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Cryoturbation occurs to varying degrees in most Gelisols ([[permafrost]] [[soil|soils]]). The cause of crytoturbation lies in way in which the repeated freezing of the soil during [[autumn]] causes the formation of [[ice wedges]] at the most easily erodible parts of the parent rock. If the parent rock is hard, this can cause quite deep erosion of the rock over many years. As this process continues, during the [[summer]] when an ''active layer'' forms in the soil this eroded material can easily move both from the soil surface downward and from the permafrost table upward. |
Cryoturbation occurs to varying degrees in most Gelisols ([[permafrost]] [[soil|soils]]). The cause of crytoturbation lies in way in which the repeated freezing of the soil during [[autumn]] causes the formation of [[ice wedges]] at the most easily erodible parts of the parent rock. If the parent rock is hard, this can cause quite deep erosion of the rock over many years. As this process continues, during the [[summer]] when an ''active layer'' forms in the soil this eroded material can easily move both from the soil surface downward and from the permafrost table upward. |
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As this process occurs, the upper soil material gradually dries out (because the soil moisture moves from the warm surface layer to the colder layer at the top of the permafrost) so that it forms a granular structure with many very distinctive crystalline shapes (such as [[ice lenses]]. Separation of coarse from fine soil materials produces distinctive ''patterned ground'' with different types of soil. |
As this process occurs, the upper soil material gradually dries out (because the soil moisture moves from the warm surface layer to the colder layer at the top of the permafrost) so that it forms a granular structure with many very distinctive crystalline shapes (such as [[ice lenses]]). Separation of coarse from fine soil materials produces distinctive ''patterned ground'' with different types of soil. |
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The extent of cryoturbation in Gelisols varies considerably: it occurs much more on exposed sites (where '''Turbels''' dominate everywhere) than in sheltered sites such as valleys (where '''Orthels''' not significantly affected by cryoturbation form). |
The extent of cryoturbation in Gelisols varies considerably: it occurs much more on exposed sites (where '''Turbels''' dominate everywhere) than in sheltered sites such as valleys (where '''Orthels''' not significantly affected by cryoturbation form). |
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InGelisols, cryoturbation refers to the mixing of materials from various horizons of the soil right down to the parent rock.
Cryoturbation occurs to varying degrees in most Gelisols (permafrost soils). The cause of crytoturbation lies in way in which the repeated freezing of the soil during autumn causes the formation of ice wedges at the most easily erodible parts of the parent rock. If the parent rock is hard, this can cause quite deep erosion of the rock over many years. As this process continues, during the summer when an active layer forms in the soil this eroded material can easily move both from the soil surface downward and from the permafrost table upward.
As this process occurs, the upper soil material gradually dries out (because the soil moisture moves from the warm surface layer to the colder layer at the top of the permafrost) so that it forms a granular structure with many very distinctive crystalline shapes (such as ice lenses). Separation of coarse from fine soil materials produces distinctive patterned ground with different types of soil.
The extent of cryoturbation in Gelisols varies considerably: it occurs much more on exposed sites (where Turbels dominate everywhere) than in sheltered sites such as valleys (where Orthels not significantly affected by cryoturbation form).
Pedology (soil study)
Soil classification
