Thaw depressions and thaw lakes – a review
DOI:
https://doi.org/10.26485/BP/1969/19/4Keywords:
thermokarst, permafrost, ground iceAbstract
This paper reviews the current state of knowledge on thaw depressions and thaw lakes in North American permafrost regions. The formation of these features is a result of thermokarst processes, where the thawing of ground ice leads to a decrease in ground volume and the formation of surface depressions. Thaw depressions commonly evolve into lakes, which are abundant and widespread throughout the Arctic.
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