Late Weichselian Glacial Geology of the Lower Borgarfjördur Region, Western Iceland: a Preliminary Report
Morphological and lithostratigraphical investigations have revealed two successive glacial advances of Late Weichselian age in the lower Borgarfjördur region, Western Iceland. Studies of the Melabakkar-Ásbakkar coastal cliffs have disclosed a complex of glaciomarine sediments and tills, accompanied...
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The Arctic Institute of North America
1985
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ftunivcalgaryojs:oai:journalhosting.ucalgary.ca:article/65187 2023-05-15T14:19:15+02:00 Late Weichselian Glacial Geology of the Lower Borgarfjördur Region, Western Iceland: a Preliminary Report Ingólfsson, Ólafur 1985-01-01 application/pdf https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65187 eng eng The Arctic Institute of North America https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65187/49101 https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65187 ARCTIC; Vol. 38 No. 3 (1985): September: 167–260; 210-213 1923-1245 0004-0843 Coast changes Deglaciation Glacial deposits Glacial geology Glacier variations Glaciers Mollusks Pleistocene epoch Radiocarbon dating Sea level Sediments (Geology) Shorelines Stratigraphy Iceland info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion research-article 1985 ftunivcalgaryojs 2022-03-22T21:22:19Z Morphological and lithostratigraphical investigations have revealed two successive glacial advances of Late Weichselian age in the lower Borgarfjördur region, Western Iceland. Studies of the Melabakkar-Ásbakkar coastal cliffs have disclosed a complex of glaciomarine sediments and tills, accompanied by glaciofluvial deposits from ice marginal sources. A brief description is given for each of the major lithostratigraphical units, and a depositional model for the sequence is outlined. The first glacial advance occurred some time shortly after 12 000 radiocarbon years before present (BP), and the second one around 11 000 BP. By 10 000 BP the glaciers had retreated from the lowlands and the sea transgressed to 60 m above present sea level, where extensive marine terraces were formed.Key words: Borgarfjördur, western Iceland, Melabakkar-ásbakkar, glacial geology, glacia chronology, Late Weichselian Mots clés: Borgarfjördur, ouest de l'Icelande, Melabakkar-ásbakkar, géologie glaciale, chronologie glaciaire, Weichsel supérieur Article in Journal/Newspaper Arctic glacier Iceland University of Calgary Journal Hosting Melabakkar ENVELOPE(-22.025,-22.025,64.415,64.415) ARCTIC 38 3 |
institution |
Open Polar |
collection |
University of Calgary Journal Hosting |
op_collection_id |
ftunivcalgaryojs |
language |
English |
topic |
Coast changes Deglaciation Glacial deposits Glacial geology Glacier variations Glaciers Mollusks Pleistocene epoch Radiocarbon dating Sea level Sediments (Geology) Shorelines Stratigraphy Iceland |
spellingShingle |
Coast changes Deglaciation Glacial deposits Glacial geology Glacier variations Glaciers Mollusks Pleistocene epoch Radiocarbon dating Sea level Sediments (Geology) Shorelines Stratigraphy Iceland Ingólfsson, Ólafur Late Weichselian Glacial Geology of the Lower Borgarfjördur Region, Western Iceland: a Preliminary Report |
topic_facet |
Coast changes Deglaciation Glacial deposits Glacial geology Glacier variations Glaciers Mollusks Pleistocene epoch Radiocarbon dating Sea level Sediments (Geology) Shorelines Stratigraphy Iceland |
description |
Morphological and lithostratigraphical investigations have revealed two successive glacial advances of Late Weichselian age in the lower Borgarfjördur region, Western Iceland. Studies of the Melabakkar-Ásbakkar coastal cliffs have disclosed a complex of glaciomarine sediments and tills, accompanied by glaciofluvial deposits from ice marginal sources. A brief description is given for each of the major lithostratigraphical units, and a depositional model for the sequence is outlined. The first glacial advance occurred some time shortly after 12 000 radiocarbon years before present (BP), and the second one around 11 000 BP. By 10 000 BP the glaciers had retreated from the lowlands and the sea transgressed to 60 m above present sea level, where extensive marine terraces were formed.Key words: Borgarfjördur, western Iceland, Melabakkar-ásbakkar, glacial geology, glacia chronology, Late Weichselian Mots clés: Borgarfjördur, ouest de l'Icelande, Melabakkar-ásbakkar, géologie glaciale, chronologie glaciaire, Weichsel supérieur |
format |
Article in Journal/Newspaper |
author |
Ingólfsson, Ólafur |
author_facet |
Ingólfsson, Ólafur |
author_sort |
Ingólfsson, Ólafur |
title |
Late Weichselian Glacial Geology of the Lower Borgarfjördur Region, Western Iceland: a Preliminary Report |
title_short |
Late Weichselian Glacial Geology of the Lower Borgarfjördur Region, Western Iceland: a Preliminary Report |
title_full |
Late Weichselian Glacial Geology of the Lower Borgarfjördur Region, Western Iceland: a Preliminary Report |
title_fullStr |
Late Weichselian Glacial Geology of the Lower Borgarfjördur Region, Western Iceland: a Preliminary Report |
title_full_unstemmed |
Late Weichselian Glacial Geology of the Lower Borgarfjördur Region, Western Iceland: a Preliminary Report |
title_sort |
late weichselian glacial geology of the lower borgarfjördur region, western iceland: a preliminary report |
publisher |
The Arctic Institute of North America |
publishDate |
1985 |
url |
https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65187 |
long_lat |
ENVELOPE(-22.025,-22.025,64.415,64.415) |
geographic |
Melabakkar |
geographic_facet |
Melabakkar |
genre |
Arctic glacier Iceland |
genre_facet |
Arctic glacier Iceland |
op_source |
ARCTIC; Vol. 38 No. 3 (1985): September: 167–260; 210-213 1923-1245 0004-0843 |
op_relation |
https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65187/49101 https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65187 |
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ARCTIC |
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