The cause of cryoturbation lies in the 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.
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This paleosol has been largely modified by periglacial processes and development of ice wedges periodically during the Pleistocene These deeply weathered sediments are unfossiliferous and characterized by the presence of weathering products like kaolinite and montmorillonite.
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An "'ice wedge "'is a crack in the ground formed by a narrow or thin piece of ice that measures up to 3 4 meters in length at ground level and extends downwards into the ground up to several meters.
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Terms synonymous with clastic dike include : " clastic intrusion, sandstone dike, fissure fill, soft-sediment deformation, fluid escape structure, seismite, injectite, liquefaction feature, neptunian dike ( passive fissure fills ), paleoseismic indicator, pseudo ice wedge cast, sedimentary insertion, sheeted clastic dike, synsedimentary filling, tension fracture, hydraulic injection dike ", and " tempestite ".
35.
"' Periglaciation "'( adjective : " periglacial, " also referring to places at the edges of geomorphic processes that result from seasonal thawing of snow in areas of permafrost, the runoff from which refreezes in ice wedges and other structures . " Periglacial " suggests an environment located on the margin of past glaciers.
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