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Abstract

Quaternary sediments in the southwestern Nordenskiöld Land are described with particular emphasis put on distribution of erratics against their basset matrices. Results confirm previous suppositions on directions of past glacial advances from east westwards. The latter separated by sea submergences, caused translocations of the rock material. This process was most intensive in upstreams of large mountain valleys.

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Authors and Affiliations

Andrzej Musiał
Jacek Drecki
Bogdan Horodyski
Krzysztof Kossobudzki

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