Lake stratigraphy implies an 80 000 yr delayed melting of buried dead ice in northern Russia

Sediment cores from lakes Kormovoye and Oshkoty in the glaciated region of the Pechora Lowland, northern Russia, reveal sediment gravity flow deposits overlain by lacustrine mud and gyttja. The sediments were deposited mainly during melting of buried glacier ice beneath the lakes. In Lake Kormovoye,...

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Veröffentlicht in:	Journal of quaternary science 2003-10, Vol.18 (7), p.663-679
Hauptverfasser:	Henriksen, Mona, Mangerud, Jan, Matiouchkov, Alexei, Paus, Aage, Svendsen, John Inge
Format:	Artikel
Sprache:	eng
Schlagworte:	dead ice deglaciation lake sediments northern Russia Weichselian
Online-Zugang:	Volltext
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