Holocene Sea Levels in Southeast Alaska: Preliminary Results

Natural raised marine deposits and archaeological sites recently discovered in southeastern Alaska have been measured relative to mean sea level and radiocarbon dated. Plots of sites on Heceta and Prince of Wales islands are compared to those developed for British Columbia. The Heceta Island curve i...

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Published in:ARCTIC
Main Author: Mobley, Charles M.
Format: Article in Journal/Newspaper
Language:English
Published: The Arctic Institute of North America 1988
Subjects:
Online Access:https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64784
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spelling ftunivcalgaryojs:oai:journalhosting.ucalgary.ca:article/64784 2023-05-15T14:17:51+02:00 Holocene Sea Levels in Southeast Alaska: Preliminary Results Mobley, Charles M. 1988-01-01 application/pdf https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64784 eng eng The Arctic Institute of North America https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64784/48698 https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64784 ARCTIC; Vol. 41 No. 4 (1988): December: 261–336; 261-266 1923-1245 0004-0843 Archaeology Geological time Glacial epoch Palaeogeography Quaternary period Radiocarbon dating Recent epoch Sea level Sediments (Geology) Glaciation Alaska Southeastern British Columbia Northern info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion research-article 1988 ftunivcalgaryojs 2022-03-22T21:21:59Z Natural raised marine deposits and archaeological sites recently discovered in southeastern Alaska have been measured relative to mean sea level and radiocarbon dated. Plots of sites on Heceta and Prince of Wales islands are compared to those developed for British Columbia. The Heceta Island curve is comparable to that of the Queen Charlotte Islands, in which pre-Holocene shorelines were lower than present until about 10,000 B.P. and then rose to a maximum of 15 m asl by 8500 B.P., when gradual emergence began to bring the sea level down to its present position. In contrast, the Prince of Wales Islands data indicate that sea level remained a few metres above its present position between 10,000 and 7000 B.P. - a time when the shores of mainland British Columbia were as much as 15 m below present sea level. Because Holocene sea levels are a function of isostatic rebound due to removal of glacial ice, as well as global sea level changes and tectonic activity, the implication is that whereas Heceta Island underwent processes and magnitudes of glaciation and isostatic rebound similar to the Queen Charlotte Islands, Prince of Wales Island was subjected to a pattern of glaciation and isostatic rebound different from that of the Queen Charlotte Islands and mainland of British Columbia.Key words: Alaska, Alexander Archipelago, archaeology, eustacy, geomorphology, glaciation, Holocene, isostacy, sea level, Quaternary Mots clés: Alaska, archipel Alexander, archéologie, eustatisme, géomorphologie, glaciation, holocène, isostasie, niveau de la mer, quaternaire Article in Journal/Newspaper Archipel Archipelago Arctic Prince of Wales Island Alaska University of Calgary Journal Hosting Prince of Wales Island ENVELOPE(-99.001,-99.001,72.668,72.668) Queen Charlotte ENVELOPE(-132.088,-132.088,53.255,53.255) ARCTIC 41 4
institution Open Polar
collection University of Calgary Journal Hosting
op_collection_id ftunivcalgaryojs
language English
topic Archaeology
Geological time
Glacial epoch
Palaeogeography
Quaternary period
Radiocarbon dating
Recent epoch
Sea level
Sediments (Geology)
Glaciation
Alaska
Southeastern
British Columbia
Northern
spellingShingle Archaeology
Geological time
Glacial epoch
Palaeogeography
Quaternary period
Radiocarbon dating
Recent epoch
Sea level
Sediments (Geology)
Glaciation
Alaska
Southeastern
British Columbia
Northern
Mobley, Charles M.
Holocene Sea Levels in Southeast Alaska: Preliminary Results
topic_facet Archaeology
Geological time
Glacial epoch
Palaeogeography
Quaternary period
Radiocarbon dating
Recent epoch
Sea level
Sediments (Geology)
Glaciation
Alaska
Southeastern
British Columbia
Northern
description Natural raised marine deposits and archaeological sites recently discovered in southeastern Alaska have been measured relative to mean sea level and radiocarbon dated. Plots of sites on Heceta and Prince of Wales islands are compared to those developed for British Columbia. The Heceta Island curve is comparable to that of the Queen Charlotte Islands, in which pre-Holocene shorelines were lower than present until about 10,000 B.P. and then rose to a maximum of 15 m asl by 8500 B.P., when gradual emergence began to bring the sea level down to its present position. In contrast, the Prince of Wales Islands data indicate that sea level remained a few metres above its present position between 10,000 and 7000 B.P. - a time when the shores of mainland British Columbia were as much as 15 m below present sea level. Because Holocene sea levels are a function of isostatic rebound due to removal of glacial ice, as well as global sea level changes and tectonic activity, the implication is that whereas Heceta Island underwent processes and magnitudes of glaciation and isostatic rebound similar to the Queen Charlotte Islands, Prince of Wales Island was subjected to a pattern of glaciation and isostatic rebound different from that of the Queen Charlotte Islands and mainland of British Columbia.Key words: Alaska, Alexander Archipelago, archaeology, eustacy, geomorphology, glaciation, Holocene, isostacy, sea level, Quaternary Mots clés: Alaska, archipel Alexander, archéologie, eustatisme, géomorphologie, glaciation, holocène, isostasie, niveau de la mer, quaternaire
format Article in Journal/Newspaper
author Mobley, Charles M.
author_facet Mobley, Charles M.
author_sort Mobley, Charles M.
title Holocene Sea Levels in Southeast Alaska: Preliminary Results
title_short Holocene Sea Levels in Southeast Alaska: Preliminary Results
title_full Holocene Sea Levels in Southeast Alaska: Preliminary Results
title_fullStr Holocene Sea Levels in Southeast Alaska: Preliminary Results
title_full_unstemmed Holocene Sea Levels in Southeast Alaska: Preliminary Results
title_sort holocene sea levels in southeast alaska: preliminary results
publisher The Arctic Institute of North America
publishDate 1988
url https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64784
long_lat ENVELOPE(-99.001,-99.001,72.668,72.668)
ENVELOPE(-132.088,-132.088,53.255,53.255)
geographic Prince of Wales Island
Queen Charlotte
geographic_facet Prince of Wales Island
Queen Charlotte
genre Archipel
Archipelago
Arctic
Prince of Wales Island
Alaska
genre_facet Archipel
Archipelago
Arctic
Prince of Wales Island
Alaska
op_source ARCTIC; Vol. 41 No. 4 (1988): December: 261–336; 261-266
1923-1245
0004-0843
op_relation https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64784/48698
https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64784
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