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خاک سره
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خاک سره

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thumb|Garland-like solifluction formed in the Swiss National Park thumb|Possible solifluction lobes in Acidalia Planitia on Mars as seen by [[HiRISE]] thumb|Solifluction sheets near Eagle Summit (Alaska)|Eagle Summit, [[Alaska]] Solifluction is a collective name for gradual processes in which a mass moves down a slope ("mass wasting") related to freeze-thaw activity. This is the standard modern meaning of solifluction, which differs from the original meaning given to it by Johan Gunnar Andersson in 1906.

Wikidata facts

Subclass of
landform
Show 2 more facts
Commons category
Solifluctions
different from
soil liquefaction
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