Subglacial Meltwater Channels at Cape Jones, Obruchev Hills, Antarctica
Subglacial curved and winding meltwater channels, and Sichelwannen are recorded from Cape Jones in the Obruchev Hills. Such channels, sometimes referred to as Pāforms, may have a variety of origins. After briefly considering the origins, it is deduced that those at Cape Jones were formed subglaciall...
Published in: | Australian Geographical Studies |
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Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Wiley
1989
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Subjects: | |
Online Access: | http://dx.doi.org/10.1111/j.1467-8470.1989.tb00605.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1467-8470.1989.tb00605.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1467-8470.1989.tb00605.x |