Sedimentological characteristics of debris flow Deposits within ice−cored moraine of Ebbabreen, central Spitsbergen
The Ebbabreen ice−cored moraine area is covered with a sediment layer of up to 2.5 m thick, which mostly consists of massive diamicton. Due to undercutting by lateral streams, debris flow processes have been induced in marginal parts of this moraine. It was recognized that the sedimentology of depos...
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| Format: | Article |
| Language: | English |
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Polish Academy of Sciences
2015-06-01
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| Series: | Polish Polar Research |
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| Online Access: | http://www.degruyter.com/view/j/popore.2015.36.issue-2/popore-2015-0006/popore-2015-0006.xml?format=INT |