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Crioturbația

Crioturbația este un proces important care se petrece în stratul activ al permafrostului, în care diferite materiale de pe straturile orizontale ale solului se amestecă între ele, din cauza înghețării și dezghețării continue.

Materialul multicolor se plasează într-un strat caracteristic și texturat.

Crioturbația © Brentwood Higman & Andrew Mattox

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