Oodaaq Ø and other short-lived islets north of Greenland

Abstract In 1978, a small island was discovered north of Kaffeklubben Ø, until then considered the most northern island on Earth. This island was named Oodaaq Ø. It was visited again in 1979, and in 1980 it was seen from Kaffeklubben Ø by members of the Sirius sledge patrol. Sirius searched for Ooda...

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Published in:Polar Record
Main Authors: Bennike, Ole, Shea, Jeff
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2019
Subjects:
Online Access:http://dx.doi.org/10.1017/s0032247419000135
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0032247419000135
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spelling crcambridgeupr:10.1017/s0032247419000135 2024-03-03T08:45:01+00:00 Oodaaq Ø and other short-lived islets north of Greenland Bennike, Ole Shea, Jeff 2019 http://dx.doi.org/10.1017/s0032247419000135 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0032247419000135 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Polar Record volume 55, issue 1, page 14-24 ISSN 0032-2474 1475-3057 General Earth and Planetary Sciences Ecology Geography, Planning and Development journal-article 2019 crcambridgeupr https://doi.org/10.1017/s0032247419000135 2024-02-08T08:42:25Z Abstract In 1978, a small island was discovered north of Kaffeklubben Ø, until then considered the most northern island on Earth. This island was named Oodaaq Ø. It was visited again in 1979, and in 1980 it was seen from Kaffeklubben Ø by members of the Sirius sledge patrol. Sirius searched for Oodaaq Ø again from 1981 to 1984 but did not find it. During the period from 1996 to 2008, the region was visited regularly and a number of new islets were discovered: the 1996 ATOW Island, KMS Island, 2001 RTOW Island, 83-42 Island, Stray Dog West Island and the 2008 Island. The islets are composed of gravel. We believe the area with islets is shallow, being a continuation of a coastal plain to the south. We suggest that the sea floor in the area is irregular and that the islets form by floes of sea ice that bulldoze material from the sea floor up above sea level. In some cases, perhaps all, the islets disappear when sea ice floes bulldoze sediment back below sea level. Alternatively, the so-called islets are just accumulations of gravel on sea ice. Article in Journal/Newspaper Greenland Kaffeklubben ø Oodaaq ø Polar Record Sea ice Cambridge University Press Greenland Sirius ENVELOPE(163.250,163.250,-84.133,-84.133) The Islets ENVELOPE(-55.448,-55.448,51.600,51.600) West Island ENVELOPE(68.711,68.711,-49.348,-49.348) Polar Record 55 1 14 24
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic General Earth and Planetary Sciences
Ecology
Geography, Planning and Development
spellingShingle General Earth and Planetary Sciences
Ecology
Geography, Planning and Development
Bennike, Ole
Shea, Jeff
Oodaaq Ø and other short-lived islets north of Greenland
topic_facet General Earth and Planetary Sciences
Ecology
Geography, Planning and Development
description Abstract In 1978, a small island was discovered north of Kaffeklubben Ø, until then considered the most northern island on Earth. This island was named Oodaaq Ø. It was visited again in 1979, and in 1980 it was seen from Kaffeklubben Ø by members of the Sirius sledge patrol. Sirius searched for Oodaaq Ø again from 1981 to 1984 but did not find it. During the period from 1996 to 2008, the region was visited regularly and a number of new islets were discovered: the 1996 ATOW Island, KMS Island, 2001 RTOW Island, 83-42 Island, Stray Dog West Island and the 2008 Island. The islets are composed of gravel. We believe the area with islets is shallow, being a continuation of a coastal plain to the south. We suggest that the sea floor in the area is irregular and that the islets form by floes of sea ice that bulldoze material from the sea floor up above sea level. In some cases, perhaps all, the islets disappear when sea ice floes bulldoze sediment back below sea level. Alternatively, the so-called islets are just accumulations of gravel on sea ice.
format Article in Journal/Newspaper
author Bennike, Ole
Shea, Jeff
author_facet Bennike, Ole
Shea, Jeff
author_sort Bennike, Ole
title Oodaaq Ø and other short-lived islets north of Greenland
title_short Oodaaq Ø and other short-lived islets north of Greenland
title_full Oodaaq Ø and other short-lived islets north of Greenland
title_fullStr Oodaaq Ø and other short-lived islets north of Greenland
title_full_unstemmed Oodaaq Ø and other short-lived islets north of Greenland
title_sort oodaaq ø and other short-lived islets north of greenland
publisher Cambridge University Press (CUP)
publishDate 2019
url http://dx.doi.org/10.1017/s0032247419000135
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0032247419000135
long_lat ENVELOPE(163.250,163.250,-84.133,-84.133)
ENVELOPE(-55.448,-55.448,51.600,51.600)
ENVELOPE(68.711,68.711,-49.348,-49.348)
geographic Greenland
Sirius
The Islets
West Island
geographic_facet Greenland
Sirius
The Islets
West Island
genre Greenland
Kaffeklubben ø
Oodaaq ø
Polar Record
Sea ice
genre_facet Greenland
Kaffeklubben ø
Oodaaq ø
Polar Record
Sea ice
op_source Polar Record
volume 55, issue 1, page 14-24
ISSN 0032-2474 1475-3057
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s0032247419000135
container_title Polar Record
container_volume 55
container_issue 1
container_start_page 14
op_container_end_page 24
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