Glaciovolcanic edifices. Correlation of passage zone with ice sheet slope at Bláfjall tuya, NE-Iceland
Bláfjall tuya in northern Iceland was formed in a volcanic eruption within a Pleistocene ice sheet. It is located well north of the old ice divide, where ice flow was predominantly from south to north. The elongated structure of the tuya is oriented parallel to the flow of the ancient glacier. Bláfj...
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| Format: | Thesis |
| Language: | English |
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2023
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| Online Access: | http://hdl.handle.net/1946/43329 |