Karst processes and phenomena in the perennially frozen carbonate rocks of the middle Lena River basin

V. B. Spektor and V. V. Spektor

Permafrost and Periglacial Processes, 2009, vol. 20, issue 1, 71-78

Abstract: Various karst processes and karst phenomena at scales from the macro to the micro occur in the cryolithozone of the middle Lena River basin. Karst processes have a warming impact on the enclosing perennially cryotic rocks and favour the formation of intra‐permafrost taliks at depths ranging from a few to several tens of metres. Copyright © 2009 John Wiley & Sons, Ltd.

Date: 2009
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Persistent link: https://EconPapers.repec.org/RePEc:wly:perpro:v:20:y:2009:i:1:p:71-78

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