Glaciers in the Polar Urals, Russia, were not much larger during the Last Global Glacial Maximum than today

Autor: Mangerud, Jan, Gosse, John, Matiouchkov, Alexei, Dolvik, Tore

Publikováno v: In Quaternary Science Reviews 2008 27(9):1047-1057

Late Weichselian (Valdaian) and Holocene vegetation and environmental history of the northern Timan Ridge, European Arctic Russia

Autor: Paus, Aage ^*, Svendsen, John Inge, Matiouchkov, Alexei

Publikováno v: In Quaternary Science Reviews 2003 22(21):2285-2302

Age and extent of the Barents and Kara ice sheets in Northern Russia

Autor: Mangerud, Jan, Svendsen, John Inge, Astakhov, Valery I., Andreicheva, Ludmila, Funder, Svend, Henriksen, Mona, Hufthammer, Anne Karin, Indrelid, Svein, Matiouchkov, Alexei, Murray, Andrew, Paus, Aage, Pavlov, Pavel, Tveranger, Jan, Ulvedal, Per

Publikováno v: Mangerud, J, Svendsen, J I, Astakhov, V I, Andreicheva, L, Funder, S, Henriksen, M, Hufthammer, A K, Indrelid, S, Matiouchkov, A, Murray, A, Paus, A, Pavlov, P, Tveranger, J & Ulvedal, P 1999, ' Age and extent of the Barents and Kara ice sheets in Northern Russia ', Boreas, vol. 28, no. 1, pp. 46-80 . https://doi.org/10.1111/j.1502-3885.1999.tb00206.x

The youngest ice marginal zone between the White Sea and the Ural mountains is the W-E trending belt of moraines called the Varsh-Indiga-Markhida-Harbei-Halmer-Sopkay, here calledthe Markhida line. Glacial elements show that it was deposited by the K

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b06b6b75a011cde891d6fd12ba633a00
https://doi.org/10.1111/j.1502-3885.1999.tb00206.x

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