Investigation of pingos in Kuganguaq delta on Disko Island ...

The growth and collapse history of two pingos located approximately 18 m a.s.l, and 35 m a.s.l. in Kuganguag, Disko lsland, west-central Greenland were examined. The pingos of this area were formed on Tertiary basalt rocks. One of the pingos is located in the middle of an alluvial fan, the other is...

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Main Authors: Yoshikawa, Kenji, Nakamura, Toshio, Igarashi, Yaeko
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2011
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.767446
https://doi.pangaea.de/10.1594/PANGAEA.767446
id ftdatacite:10.1594/pangaea.767446
record_format openpolar
spelling ftdatacite:10.1594/pangaea.767446 2024-09-15T18:09:04+00:00 Investigation of pingos in Kuganguaq delta on Disko Island ... Yoshikawa, Kenji Nakamura, Toshio Igarashi, Yaeko 2011 application/zip https://dx.doi.org/10.1594/pangaea.767446 https://doi.pangaea.de/10.1594/PANGAEA.767446 en eng PANGAEA Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Geological sample article Collection Supplementary Publication Series of Datasets 2011 ftdatacite https://doi.org/10.1594/pangaea.767446 2024-08-01T10:50:55Z The growth and collapse history of two pingos located approximately 18 m a.s.l, and 35 m a.s.l. in Kuganguag, Disko lsland, west-central Greenland were examined. The pingos of this area were formed on Tertiary basalt rocks. One of the pingos is located in the middle of an alluvial fan, the other is on a river bed. Both have already collapsed. The pingo on the river bed had already collapsed at least 3545±60 year BP (14C dating from base of the pond sediments in the pingo crater). Both pingos formed after the sea's retreat as permafrost developed in the newly exposed delta bottom. ... : Supplement to: Yoshikawa, Kenji; Nakamura, Toshio; Igarashi, Yaeko (1996): Growth and collapse history of Pingos, Kuganguaq, Disko Island, Greenland. Polarforschung, 64(3), 109-113 ... Article in Journal/Newspaper Greenland permafrost DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Geological sample
spellingShingle Geological sample
Yoshikawa, Kenji
Nakamura, Toshio
Igarashi, Yaeko
Investigation of pingos in Kuganguaq delta on Disko Island ...
topic_facet Geological sample
description The growth and collapse history of two pingos located approximately 18 m a.s.l, and 35 m a.s.l. in Kuganguag, Disko lsland, west-central Greenland were examined. The pingos of this area were formed on Tertiary basalt rocks. One of the pingos is located in the middle of an alluvial fan, the other is on a river bed. Both have already collapsed. The pingo on the river bed had already collapsed at least 3545±60 year BP (14C dating from base of the pond sediments in the pingo crater). Both pingos formed after the sea's retreat as permafrost developed in the newly exposed delta bottom. ... : Supplement to: Yoshikawa, Kenji; Nakamura, Toshio; Igarashi, Yaeko (1996): Growth and collapse history of Pingos, Kuganguaq, Disko Island, Greenland. Polarforschung, 64(3), 109-113 ...
format Article in Journal/Newspaper
author Yoshikawa, Kenji
Nakamura, Toshio
Igarashi, Yaeko
author_facet Yoshikawa, Kenji
Nakamura, Toshio
Igarashi, Yaeko
author_sort Yoshikawa, Kenji
title Investigation of pingos in Kuganguaq delta on Disko Island ...
title_short Investigation of pingos in Kuganguaq delta on Disko Island ...
title_full Investigation of pingos in Kuganguaq delta on Disko Island ...
title_fullStr Investigation of pingos in Kuganguaq delta on Disko Island ...
title_full_unstemmed Investigation of pingos in Kuganguaq delta on Disko Island ...
title_sort investigation of pingos in kuganguaq delta on disko island ...
publisher PANGAEA
publishDate 2011
url https://dx.doi.org/10.1594/pangaea.767446
https://doi.pangaea.de/10.1594/PANGAEA.767446
genre Greenland
permafrost
genre_facet Greenland
permafrost
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.767446
_version_ 1810446470866796544