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

Polarpedia terms are created by EDU-ARCTIC Consortium, which holds responsibility for quality of translations in following languages: Polish, French, Danish, Norwegian, German, Russian, Italian, unless indicated otherwise. If you see an error - please contact us: edukacja@igf.edu.pl.
European Union flag This project (EDU-ARCTIC) has received funding from the European Union’s Horizon 2020 research and innovation programme under grant agreement No 710240. The content of the website is the sole responsibility of the Consortium and it does not represent the opinion of the European Commission, and the Commission is not responsible for any use that might be made of information contained.
Designed & hosted by American Systems Sp. z o.o.