Investigation of pingos in Kuganguaq delta on Disko Island

Fuente: PANGAEA
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Hauptverfasser: Yoshikawa, Kenji, Nakamura, Toshio, Igarashi, Yaeko
Format: Dataset Open Access
Sprache:en
Veröffentlicht: PANGAEA 2011
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author Yoshikawa, Kenji
Nakamura, Toshio
Igarashi, Yaeko
author_facet Yoshikawa, Kenji
Nakamura, Toshio
Igarashi, Yaeko
collection Datos científicos de ciencias marinas y ambientales
contents 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.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_767446
institution PANGAEA
language en
publishDate 2011
publisher PANGAEA
record_format pangaea
spellingShingle Investigation of pingos in Kuganguaq delta on Disko Island
Yoshikawa, Kenji
Nakamura, Toshio
Igarashi, Yaeko
Delta_Pingo; Disko Island, West Greenland; Fan_Pingo; Geological sample; GEOS
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.
title Investigation of pingos in Kuganguaq delta on Disko Island
topic Delta_Pingo; Disko Island, West Greenland; Fan_Pingo; Geological sample; GEOS
url https://doi.org/10.1594/PANGAEA.767446