Age determinations from northwest Russia ...

The last glacial maximum (LGM) of the Scandinavian ice sheet in the Arkhangelsk region has been identified morphologically as ridges and hummocks in an otherwise flat topography. Stratigraphically the limit is marked by the presence of till above Mikhulinian (last interglacial) sediments inside the...

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Main Authors: Larsen, Eiliv, Lyså, Astrid, Demidov, Igor, Funder, Svend, Houmark-Nielsen, Michael, Kjær, Kurt Henrik, Murray, Andrew Sean
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1999
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.727408
https://doi.pangaea.de/10.1594/PANGAEA.727408
id ftdatacite:10.1594/pangaea.727408
record_format openpolar
spelling ftdatacite:10.1594/pangaea.727408 2024-09-15T17:54:42+00:00 Age determinations from northwest Russia ... Larsen, Eiliv Lyså, Astrid Demidov, Igor Funder, Svend Houmark-Nielsen, Michael Kjær, Kurt Henrik Murray, Andrew Sean 1999 application/zip https://dx.doi.org/10.1594/pangaea.727408 https://doi.pangaea.de/10.1594/PANGAEA.727408 en eng PANGAEA https://dx.doi.org/10.1111/j.1502-3885.1999.tb00209.x Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Outcrop sample QUEEN_Exped Quaternary Environment of the Eurasian North QUEEN article Collection Supplementary Publication Series of Datasets 1999 ftdatacite https://doi.org/10.1594/pangaea.72740810.1111/j.1502-3885.1999.tb00209.x 2024-08-01T10:58:30Z The last glacial maximum (LGM) of the Scandinavian ice sheet in the Arkhangelsk region has been identified morphologically as ridges and hummocks in an otherwise flat topography. Stratigraphically the limit is marked by the presence of till above Mikhulinian (last interglacial) sediments inside the ridges and by the absence of till outside the ridges. During the LGM, ice flowed into the region from the north and northwest forming a lobe in the Dvina--Vaga depression. The continuation northward, northeast of Arkhangelsk, is still somewhat uncertain, but evidence suggests that the outer margin of the Scandinavian ice sheet was situated in the Mezen drainage basin. Luminescence and radiocarbon dates suggest that the maximum position was attained after some 17 ka ago, and that deglaciation started close to 15 ka ago. This age for the maximum position is younger than the maximum position in the western peripheral areas of the Scandinavian ice sheet. This may be accounted for by initial ice build-up in the west ... : Supplement to: Larsen, Eiliv; Lyså, Astrid; Demidov, Igor; Funder, Svend; Houmark-Nielsen, Michael; Kjær, Kurt Henrik; Murray, Andrew Sean (1999): Age and extent of the Scandinavian ice sheet in northwest Russia. Boreas, 28(1), 115-132 ... Article in Journal/Newspaper Arkhangelsk dvina Ice Sheet Mezen Mezen' Northwest Russia DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Outcrop sample
QUEEN_Exped
Quaternary Environment of the Eurasian North QUEEN
spellingShingle Outcrop sample
QUEEN_Exped
Quaternary Environment of the Eurasian North QUEEN
Larsen, Eiliv
Lyså, Astrid
Demidov, Igor
Funder, Svend
Houmark-Nielsen, Michael
Kjær, Kurt Henrik
Murray, Andrew Sean
Age determinations from northwest Russia ...
topic_facet Outcrop sample
QUEEN_Exped
Quaternary Environment of the Eurasian North QUEEN
description The last glacial maximum (LGM) of the Scandinavian ice sheet in the Arkhangelsk region has been identified morphologically as ridges and hummocks in an otherwise flat topography. Stratigraphically the limit is marked by the presence of till above Mikhulinian (last interglacial) sediments inside the ridges and by the absence of till outside the ridges. During the LGM, ice flowed into the region from the north and northwest forming a lobe in the Dvina--Vaga depression. The continuation northward, northeast of Arkhangelsk, is still somewhat uncertain, but evidence suggests that the outer margin of the Scandinavian ice sheet was situated in the Mezen drainage basin. Luminescence and radiocarbon dates suggest that the maximum position was attained after some 17 ka ago, and that deglaciation started close to 15 ka ago. This age for the maximum position is younger than the maximum position in the western peripheral areas of the Scandinavian ice sheet. This may be accounted for by initial ice build-up in the west ... : Supplement to: Larsen, Eiliv; Lyså, Astrid; Demidov, Igor; Funder, Svend; Houmark-Nielsen, Michael; Kjær, Kurt Henrik; Murray, Andrew Sean (1999): Age and extent of the Scandinavian ice sheet in northwest Russia. Boreas, 28(1), 115-132 ...
format Article in Journal/Newspaper
author Larsen, Eiliv
Lyså, Astrid
Demidov, Igor
Funder, Svend
Houmark-Nielsen, Michael
Kjær, Kurt Henrik
Murray, Andrew Sean
author_facet Larsen, Eiliv
Lyså, Astrid
Demidov, Igor
Funder, Svend
Houmark-Nielsen, Michael
Kjær, Kurt Henrik
Murray, Andrew Sean
author_sort Larsen, Eiliv
title Age determinations from northwest Russia ...
title_short Age determinations from northwest Russia ...
title_full Age determinations from northwest Russia ...
title_fullStr Age determinations from northwest Russia ...
title_full_unstemmed Age determinations from northwest Russia ...
title_sort age determinations from northwest russia ...
publisher PANGAEA
publishDate 1999
url https://dx.doi.org/10.1594/pangaea.727408
https://doi.pangaea.de/10.1594/PANGAEA.727408
genre Arkhangelsk
dvina
Ice Sheet
Mezen
Mezen'
Northwest Russia
genre_facet Arkhangelsk
dvina
Ice Sheet
Mezen
Mezen'
Northwest Russia
op_relation https://dx.doi.org/10.1111/j.1502-3885.1999.tb00209.x
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.72740810.1111/j.1502-3885.1999.tb00209.x
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