Should Glaciers Be Considered Permafrost?

This commentary critically evaluates concepts of extending the term permafrost to any parts of an active glacier. The whole mass of any glacier is at zero centigrade or below (cryotic), except for non-ice inclusions at the glacier surface. Therefore, if glacial ice is considered a monomineral rock,...

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Bibliographic Details
Published in:Geosciences
Main Author: Maciej Dąbski
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2019
Subjects:
Ice
Online Access:https://doi.org/10.3390/geosciences9120517
Description
Summary:This commentary critically evaluates concepts of extending the term permafrost to any parts of an active glacier. The whole mass of any glacier is at zero centigrade or below (cryotic), except for non-ice inclusions at the glacier surface. Therefore, if glacial ice is considered a monomineral rock, then any glacier constitutes a perennially cryotic ground (i.e., permafrost), according to the purely thermal definition. However, extending the term permafrost to active glaciers introduces misconceptions, rather than a clarification of important geological terms.