LAST GLACIATION IN THE NORTHERN PART OF THE EASTERN CHUKCHI PENINSULA AND PALEOCEANOGRAPHY OF THE NORTH PACIFIC

dc.contributor.authorLaukhin S.A.
dc.contributor.authorZhimin J.
dc.contributor.authorPushkar V.S.
dc.contributor.authorCherepanova M.V.
dc.date.accessioned2024-11-09T08:38:16Z
dc.date.available2024-11-09T08:38:16Z
dc.date.issued2006
dc.description.abstractThe Last Glaciation covered limited areas in the northeastern Asia. Even in the Kamchatka Peninsula, where valley glaciers were more than 100 km long, the névé line is located at the altitude of 700–800 m on the Kronotskii Peninsula and 1000–1700 m 150–180 km in the western area. The north Yakutian (i.e., cirque type) mechanism of the Sartan Glaciation is assumed for the Chukchi Peninsula. Few researchers assume that valley glaciers in this area are up to 15–20 km long (50 km in rare cases). In this connection, the wide distribution of fresh glacial relief in our map of the Vakarem lowland seems unusual.
dc.identifierhttps://www.elibrary.ru/item.asp?id=13527155
dc.identifier.citationDoklady Earth Sciences, 2006, 411, 9, 1422-1426
dc.identifier.doi10.1134/S1028334X06090194
dc.identifier.issn1028-334X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/46426
dc.titleLAST GLACIATION IN THE NORTHERN PART OF THE EASTERN CHUKCHI PENINSULA AND PALEOCEANOGRAPHY OF THE NORTH PACIFIC
dc.typeСтатья

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