Sedimentological characteristics of debris flow Deposits within ice−cored moraine of Ebbabreen, central Spitsbergen
Abstract 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...
| Published in: | Polish Polar Research |
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| Format: | Article in Journal/Newspaper |
| Language: | unknown |
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Walter de Gruyter GmbH
2015
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| Online Access: | http://dx.doi.org/10.1515/popore-2015-0006 http://content.sciendo.com/view/journals/popore/36/2/article-p125.xml https://www.degruyter.com/view/j/popore.2015.36.issue-2/popore-2015-0006/popore-2015-0006.pdf |