Holocene emergence and shoreline delevelling, southern Eureka Sound, High Arctic Canada
This paper is a reconstruction of postglacial relative sea level change and shoreline delevelling in southern Eureka Sound, High Arctic Canada. Postglacial emergence of up to 150 m is recorded in this area by raised marine deltas, beaches and washing limits that date from the early Holocene. Marine...
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Les Presses de l'Université de Montréal
1999
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Online Access: | http://id.erudit.org/iderudit/004827ar https://doi.org/10.7202/004827ar |
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fterudit:oai:erudit.org:004827ar 2023-05-15T15:02:07+02:00 Holocene emergence and shoreline delevelling, southern Eureka Sound, High Arctic Canada Ó Cofaigh, Colm 1999 http://id.erudit.org/iderudit/004827ar https://doi.org/10.7202/004827ar en eng Les Presses de l'Université de Montréal Érudit Géographie physique et Quaternaire vol. 53 no. 2 (1999) http://id.erudit.org/iderudit/004827ar doi:10.7202/004827ar Tous droits réservés © Les Presses de l'Université de Montréal, 1999 text 1999 fterudit https://doi.org/10.7202/004827ar 2022-09-24T23:12:12Z This paper is a reconstruction of postglacial relative sea level change and shoreline delevelling in southern Eureka Sound, High Arctic Canada. Postglacial emergence of up to 150 m is recorded in this area by raised marine deltas, beaches and washing limits that date from the early Holocene. Marine limit is metachronous and formed successively with glacier retreat. Marked contrasts in the form of relative sea level curves and rate of initial emergence are recorded from the study area. In Blind Fiord, relative sea level fell continuously following deglaciation. Initial emergence was characterised by rates of ≥ 5 m/century. This contrasts with curves from Starfish and Irene bays, where the rate of initial emergence was ≤ 1 m/century. Isobases drawn on the 8.5 ka shoreline for greater Eureka Sound demonstrate that a cell of highest emergence (≥ 130 m asl) extends along the length of the channel, and closes in the vicinity of the entrance to Norwegian Bay. This pattern confirms a distinct loading centre over Eureka Sound during the Last Glacial Maximum, and is compatible with independent glacial geological evidence indicating that the thickest ice was centred over the channel during the Late Wisconsinan. Cet article présente une reconstitution des changements du niveau marin relatif et de ces conséquences sur le littoral au postglaciaire. Les deltas marins soulevés, les plages et les limites de l'érosion par les vagues qui datent du début de l'Holocène attestent d'une émersion des terres de plus de 150 m dans la région. La limite marine est métachrone et s'est établie successivement au retrait glaciaire. Des contrastes forts dans les courbes du niveau marin relatif et le taux d'émrersion inital ont été enregistrés dans la région à l'étude. Dans le Blind Fiord, le niveau marin relatif s'est abaissé de façon continue après la déglaciation. L'émersion initiale s'élevait à ≥ 5 m/siècle. Ce taux contraste avec les courbes de Starfish Bay et de Irene Bay, où le taux d'émersion initial était de ≤ 1 m/siècle. Les iso- ... Text Arctic Eureka Sound glacier* Irene Bay Norwegian Bay Norwegian Bay Érudit.org (Université Montréal) Arctic Blind Fiord ENVELOPE(-86.266,-86.266,78.235,78.235) Canada Eureka ENVELOPE(-85.940,-85.940,79.990,79.990) Eureka Sound ENVELOPE(-84.999,-84.999,79.002,79.002) Irene Bay ENVELOPE(-81.781,-81.781,79.002,79.002) Norwegian Bay ENVELOPE(-91.535,-91.535,77.584,77.584) Starfish Bay ENVELOPE(-84.499,-84.499,78.202,78.202) Géographie physique et Quaternaire 53 2 235 247 |
institution |
Open Polar |
collection |
Érudit.org (Université Montréal) |
op_collection_id |
fterudit |
language |
English |
description |
This paper is a reconstruction of postglacial relative sea level change and shoreline delevelling in southern Eureka Sound, High Arctic Canada. Postglacial emergence of up to 150 m is recorded in this area by raised marine deltas, beaches and washing limits that date from the early Holocene. Marine limit is metachronous and formed successively with glacier retreat. Marked contrasts in the form of relative sea level curves and rate of initial emergence are recorded from the study area. In Blind Fiord, relative sea level fell continuously following deglaciation. Initial emergence was characterised by rates of ≥ 5 m/century. This contrasts with curves from Starfish and Irene bays, where the rate of initial emergence was ≤ 1 m/century. Isobases drawn on the 8.5 ka shoreline for greater Eureka Sound demonstrate that a cell of highest emergence (≥ 130 m asl) extends along the length of the channel, and closes in the vicinity of the entrance to Norwegian Bay. This pattern confirms a distinct loading centre over Eureka Sound during the Last Glacial Maximum, and is compatible with independent glacial geological evidence indicating that the thickest ice was centred over the channel during the Late Wisconsinan. Cet article présente une reconstitution des changements du niveau marin relatif et de ces conséquences sur le littoral au postglaciaire. Les deltas marins soulevés, les plages et les limites de l'érosion par les vagues qui datent du début de l'Holocène attestent d'une émersion des terres de plus de 150 m dans la région. La limite marine est métachrone et s'est établie successivement au retrait glaciaire. Des contrastes forts dans les courbes du niveau marin relatif et le taux d'émrersion inital ont été enregistrés dans la région à l'étude. Dans le Blind Fiord, le niveau marin relatif s'est abaissé de façon continue après la déglaciation. L'émersion initiale s'élevait à ≥ 5 m/siècle. Ce taux contraste avec les courbes de Starfish Bay et de Irene Bay, où le taux d'émersion initial était de ≤ 1 m/siècle. Les iso- ... |
format |
Text |
author |
Ó Cofaigh, Colm |
spellingShingle |
Ó Cofaigh, Colm Holocene emergence and shoreline delevelling, southern Eureka Sound, High Arctic Canada |
author_facet |
Ó Cofaigh, Colm |
author_sort |
Ó Cofaigh, Colm |
title |
Holocene emergence and shoreline delevelling, southern Eureka Sound, High Arctic Canada |
title_short |
Holocene emergence and shoreline delevelling, southern Eureka Sound, High Arctic Canada |
title_full |
Holocene emergence and shoreline delevelling, southern Eureka Sound, High Arctic Canada |
title_fullStr |
Holocene emergence and shoreline delevelling, southern Eureka Sound, High Arctic Canada |
title_full_unstemmed |
Holocene emergence and shoreline delevelling, southern Eureka Sound, High Arctic Canada |
title_sort |
holocene emergence and shoreline delevelling, southern eureka sound, high arctic canada |
publisher |
Les Presses de l'Université de Montréal |
publishDate |
1999 |
url |
http://id.erudit.org/iderudit/004827ar https://doi.org/10.7202/004827ar |
long_lat |
ENVELOPE(-86.266,-86.266,78.235,78.235) ENVELOPE(-85.940,-85.940,79.990,79.990) ENVELOPE(-84.999,-84.999,79.002,79.002) ENVELOPE(-81.781,-81.781,79.002,79.002) ENVELOPE(-91.535,-91.535,77.584,77.584) ENVELOPE(-84.499,-84.499,78.202,78.202) |
geographic |
Arctic Blind Fiord Canada Eureka Eureka Sound Irene Bay Norwegian Bay Starfish Bay |
geographic_facet |
Arctic Blind Fiord Canada Eureka Eureka Sound Irene Bay Norwegian Bay Starfish Bay |
genre |
Arctic Eureka Sound glacier* Irene Bay Norwegian Bay Norwegian Bay |
genre_facet |
Arctic Eureka Sound glacier* Irene Bay Norwegian Bay Norwegian Bay |
op_relation |
Géographie physique et Quaternaire vol. 53 no. 2 (1999) http://id.erudit.org/iderudit/004827ar doi:10.7202/004827ar |
op_rights |
Tous droits réservés © Les Presses de l'Université de Montréal, 1999 |
op_doi |
https://doi.org/10.7202/004827ar |
container_title |
Géographie physique et Quaternaire |
container_volume |
53 |
container_issue |
2 |
container_start_page |
235 |
op_container_end_page |
247 |
_version_ |
1766334098338480128 |