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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Published in:ARCTIC
Main Author: Ingólfsson, Ólafur
Format: Article in Journal/Newspaper
Language:English
Published: The Arctic Institute of North America 1985
Subjects:
Online Access:https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65187
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spelling 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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