Zagłębienia i jeziora termokrasowe – przegląd
DOI:
https://doi.org/10.26485/BP/1969/19/4Słowa kluczowe:
procesy termokrasowe, wieczna zmarzlina, lód gruntowyAbstrakt
Artykuł przedstawia przegląd obecnego stanu wiedzy na temat zagłębień i jezior termokrasowych w regionach występowania wiecznej zmarzliny w Ameryce Północnej. Formowanie się tych form terenu jest wynikiem procesów termokrasowych, gdzie topnienie lodu gruntowego prowadzi do zmniejszenia objętości gruntu i powstawania zagłębień na powierzchni. Zagłębienia termokrasowe powszechnie przekształcają się w jeziora, które są liczne i szeroko rozpowszechnione w całej Arktyce.
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