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Publication Date
January 1985
Abstract
Ground temperature measurements show that open taliks occurring at Vardeborgsletta are probably caused by the heat of circulating water from great depths. The absence of permafrost has allowed the ground water to circulate, and large-scale karst features have developed in a limestone area. Karst processes are also active today, and dolines and ponds with sinking drainage occur.
Keywords
High-Alpine Environments, Stone, Ice
Document Type
Article
Notes
Polar Research, Vol. 3, no. 2 (1985-01-01).
Identifier
K26-00065
Recommended Citation
Salvigsen, Otto and Elgersma, Anne, "Large-scale karst features and open taliks at Vardeborgsletta, outer Isfjorden, Svalbard" (1985). KIP Articles. 2940.
https://digitalcommons.usf.edu/kip_articles/2940