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...
Published in: | The Cryosphere |
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Main Authors: | , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Copernicus Publications
2019
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Subjects: | |
Online Access: | https://doi.org/10.5194/tc-13-3155-2019 https://www.the-cryosphere.net/13/3155/2019/tc-13-3155-2019.pdf https://doaj.org/article/1d1a8cdfdf8f4deca8148d271a0e189d |