The glacially sculptured landscape in Dronning Maud Land, Antarctica, formed by wet‐based mountain glaciation and not by the present ice sheet
The glacial landscape beneath the Maudheimvidda ice sheet in East Antarctica was most probably formed during a more temperate phase of Antarctic glaciation than the present. Overdeepened glacial cirques and U‐shaped valleys are found in the Heimefrontfjella and Vestfjella mountain ranges. These glac...
Published in: | Boreas |
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Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Wiley
1994
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Subjects: | |
Online Access: | http://dx.doi.org/10.1111/j.1502-3885.1994.tb00594.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1994.tb00594.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1994.tb00594.x |