Evolution of an englacial volcano: Brown Bluff, Antarctica
Marine shallow-water to emergent volcanoes have been described in detail, but comparable englacial centres are not well documented. Brown Bluff is a Pleistocene, shallow water, alkali basaltic volcano whose deposits were ponded within an englacial lake, enclosed by ice >400 m thick. Its evolution...
Published in: | Bulletin of Volcanology |
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Format: | Article in Journal/Newspaper |
Language: | unknown |
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Springer
1994
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Online Access: | http://nora.nerc.ac.uk/id/eprint/517380/ https://doi.org/10.1007/BF00302837 |