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...

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Bibliographic Details
Published in:Boreas
Main Authors: HOLMLUND, PER, NÄSLUND, JENS‐OVE
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1994
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