An extensive late Holocene glacier advance of Kotlujokull, central south Iceland

This paper presents data on an extensive late Holocene advance of Kotlujokull, a southeastern outlet glacier from the ice cap Myrdalsjokull, central south Iceland. During the advance, basal till was deposited on top of a volcanic ash layer resting on lava hummocks. Remnants of this landscape are now...

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Published in:Quaternary Science Reviews
Main Authors: Schomacker, Anders, Kruger, J, Larsen, G
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2003
Subjects:
Online Access:https://lup.lub.lu.se/record/306968
https://doi.org/10.1016/S0277-3791(03)00090-8
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spelling ftulundlup:oai:lup.lub.lu.se:9f90146f-1f2e-4da1-8a06-f18a8e0c7bf4 2023-05-15T16:21:26+02:00 An extensive late Holocene glacier advance of Kotlujokull, central south Iceland Schomacker, Anders Kruger, J Larsen, G 2003 https://lup.lub.lu.se/record/306968 https://doi.org/10.1016/S0277-3791(03)00090-8 eng eng Elsevier https://lup.lub.lu.se/record/306968 http://dx.doi.org/10.1016/S0277-3791(03)00090-8 wos:000183932500005 scopus:0038757922 Quaternary Science Reviews; 22(14), pp 1427-1434 (2003) ISSN: 0277-3791 Geology contributiontojournal/article info:eu-repo/semantics/article text 2003 ftulundlup https://doi.org/10.1016/S0277-3791(03)00090-8 2023-02-01T23:32:31Z This paper presents data on an extensive late Holocene advance of Kotlujokull, a southeastern outlet glacier from the ice cap Myrdalsjokull, central south Iceland. During the advance, basal till was deposited on top of a volcanic ash layer resting on lava hummocks. Remnants of this landscape are now seen 3.5-5.5 km in front of Kotlujokull as a fragment surrounded by the Myrdalssandur. Electron microprobe analysis of the volcanic ash shows that it is silicic and originates from the volcano Katla underneath Myrdalsjokull. A C-14 AMS date on a twig fragment sampled in the upper part of the volcanic ash layer provides a maximum age of the till of 1610 +/- 40 yr BP, and this is supported by tephrochronological and geochemical analyses of the volcanic ash. It is concluded that Kotlujokull must have advanced more than 5.5 km from its present position after 1.6 kyr 13P. This advance is much more extensive than the Little Ice Age (LIA) advance and took place in a relatively cold period also identified in the Greenland ice cores and the diatom record in the seas surrounding Iceland. In the proglacial environment in front of the Icelandic ice caps, the preservation potential of older end-moraines is strongly restricted due to intense glaciofluvial erosion. Therefore, the LIA end-moraines have in many cases been interpreted as marking the outermost Holocene glacier front position. This study as well as other recent results stresses the fact that the "LIA glacial maximum" in Iceland may not be identical to the Holocene glacial maximum, and that far more case studies with well-constrained dating control are needed. (C) 2003 Elsevier Science Ltd. All rights reserved. Article in Journal/Newspaper glacier glacier Greenland Greenland ice cores Ice cap Iceland Katla Lund University Publications (LUP) Greenland Katla ENVELOPE(-19.062,-19.062,63.631,63.631) Quaternary Science Reviews 22 14 1427 1434
institution Open Polar
collection Lund University Publications (LUP)
op_collection_id ftulundlup
language English
topic Geology
spellingShingle Geology
Schomacker, Anders
Kruger, J
Larsen, G
An extensive late Holocene glacier advance of Kotlujokull, central south Iceland
topic_facet Geology
description This paper presents data on an extensive late Holocene advance of Kotlujokull, a southeastern outlet glacier from the ice cap Myrdalsjokull, central south Iceland. During the advance, basal till was deposited on top of a volcanic ash layer resting on lava hummocks. Remnants of this landscape are now seen 3.5-5.5 km in front of Kotlujokull as a fragment surrounded by the Myrdalssandur. Electron microprobe analysis of the volcanic ash shows that it is silicic and originates from the volcano Katla underneath Myrdalsjokull. A C-14 AMS date on a twig fragment sampled in the upper part of the volcanic ash layer provides a maximum age of the till of 1610 +/- 40 yr BP, and this is supported by tephrochronological and geochemical analyses of the volcanic ash. It is concluded that Kotlujokull must have advanced more than 5.5 km from its present position after 1.6 kyr 13P. This advance is much more extensive than the Little Ice Age (LIA) advance and took place in a relatively cold period also identified in the Greenland ice cores and the diatom record in the seas surrounding Iceland. In the proglacial environment in front of the Icelandic ice caps, the preservation potential of older end-moraines is strongly restricted due to intense glaciofluvial erosion. Therefore, the LIA end-moraines have in many cases been interpreted as marking the outermost Holocene glacier front position. This study as well as other recent results stresses the fact that the "LIA glacial maximum" in Iceland may not be identical to the Holocene glacial maximum, and that far more case studies with well-constrained dating control are needed. (C) 2003 Elsevier Science Ltd. All rights reserved.
format Article in Journal/Newspaper
author Schomacker, Anders
Kruger, J
Larsen, G
author_facet Schomacker, Anders
Kruger, J
Larsen, G
author_sort Schomacker, Anders
title An extensive late Holocene glacier advance of Kotlujokull, central south Iceland
title_short An extensive late Holocene glacier advance of Kotlujokull, central south Iceland
title_full An extensive late Holocene glacier advance of Kotlujokull, central south Iceland
title_fullStr An extensive late Holocene glacier advance of Kotlujokull, central south Iceland
title_full_unstemmed An extensive late Holocene glacier advance of Kotlujokull, central south Iceland
title_sort extensive late holocene glacier advance of kotlujokull, central south iceland
publisher Elsevier
publishDate 2003
url https://lup.lub.lu.se/record/306968
https://doi.org/10.1016/S0277-3791(03)00090-8
long_lat ENVELOPE(-19.062,-19.062,63.631,63.631)
geographic Greenland
Katla
geographic_facet Greenland
Katla
genre glacier
glacier
Greenland
Greenland ice cores
Ice cap
Iceland
Katla
genre_facet glacier
glacier
Greenland
Greenland ice cores
Ice cap
Iceland
Katla
op_source Quaternary Science Reviews; 22(14), pp 1427-1434 (2003)
ISSN: 0277-3791
op_relation https://lup.lub.lu.se/record/306968
http://dx.doi.org/10.1016/S0277-3791(03)00090-8
wos:000183932500005
scopus:0038757922
op_doi https://doi.org/10.1016/S0277-3791(03)00090-8
container_title Quaternary Science Reviews
container_volume 22
container_issue 14
container_start_page 1427
op_container_end_page 1434
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