Geochemical signatures of pingo ice and its origin in Grøndalen, west Spitsbergen

Pingos are common features in permafrost regions that form by subsurface massive-ice aggradation and create hill-like landforms. Pingos on Spitsbergen have been previously studied to explore their structure, formation timing and connection to springs as well as their role in postglacial landform evo...

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Bibliographic Details
Published in:The Cryosphere
Main Authors: N. Demidov, S. Wetterich, S. Verkulich, A. Ekaykin, H. Meyer, M. Anisimov, L. Schirrmeister, V. Demidov, A. J. Hodson
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2019
Subjects:
Ice
Online Access:https://doi.org/10.5194/tc-13-3155-2019
https://doaj.org/article/1d1a8cdfdf8f4deca8148d271a0e189d