Characteristics of soils from the Quartermain Mountain area, Antarctica ...

Soil-forming processes and soil development rates are compared and contrasted on glacial deposits in two adjacent and coeval valleys of the Quartermain Mountains, which are important because they display Miocene glacial stratigraphy and some of the oldest landforms in the McMurdo Dry Valleys. More t...

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Bibliographic Details
Main Author: Bockheim, James G
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2007
Subjects:
Ice
IPY
Online Access:https://dx.doi.org/10.1594/pangaea.807625
https://doi.pangaea.de/10.1594/PANGAEA.807625
id ftdatacite:10.1594/pangaea.807625
record_format openpolar
spelling ftdatacite:10.1594/pangaea.807625 2024-09-09T19:11:50+00:00 Characteristics of soils from the Quartermain Mountain area, Antarctica ... Bockheim, James G 2007 application/zip https://dx.doi.org/10.1594/pangaea.807625 https://doi.pangaea.de/10.1594/PANGAEA.807625 en eng PANGAEA https://dx.doi.org/10.1111/j.1468-0459.2007.00315.x Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 International Polar Year 2007-2008 IPY article Collection Supplementary Publication Series of Datasets 2007 ftdatacite https://doi.org/10.1594/pangaea.80762510.1111/j.1468-0459.2007.00315.x 2024-08-01T10:51:31Z Soil-forming processes and soil development rates are compared and contrasted on glacial deposits in two adjacent and coeval valleys of the Quartermain Mountains, which are important because they display Miocene glacial stratigraphy and some of the oldest landforms in the McMurdo Dry Valleys. More than 100 soil profiles were examined on seven drift sheets ranging from 115 000 to greater than 11.3 million years in age in Beacon Valley and Arena Valley. Although the two valleys contain drifts of similar age, they differ markedly in ice content of the substrate. Whereas Arena Valley generally has 'dry-frozen' permafrost in the upper 1 m and minimal patterned ground, Beacon Valley contains massive ice buried by glacial drift and ice-cored rock glaciers and has ice-cemented permafrost in the upper 1 m and considerable associated patterned ground. Arena Valley soils have twice the rate of profile salt accumulation than Beacon Valley soils, because of lower available soil water and minimal cryoturbation. The ... : Data extracted in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150 ... Article in Journal/Newspaper Antarc* Antarctica Ice International Polar Year IPY McMurdo Dry Valleys permafrost DataCite McMurdo Dry Valleys Beacon Valley ENVELOPE(160.650,160.650,-77.817,-77.817) Quartermain Mountains ENVELOPE(160.750,160.750,-77.850,-77.850) Arena Valley ENVELOPE(160.983,160.983,-77.833,-77.833)
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic International Polar Year 2007-2008 IPY
spellingShingle International Polar Year 2007-2008 IPY
Bockheim, James G
Characteristics of soils from the Quartermain Mountain area, Antarctica ...
topic_facet International Polar Year 2007-2008 IPY
description Soil-forming processes and soil development rates are compared and contrasted on glacial deposits in two adjacent and coeval valleys of the Quartermain Mountains, which are important because they display Miocene glacial stratigraphy and some of the oldest landforms in the McMurdo Dry Valleys. More than 100 soil profiles were examined on seven drift sheets ranging from 115 000 to greater than 11.3 million years in age in Beacon Valley and Arena Valley. Although the two valleys contain drifts of similar age, they differ markedly in ice content of the substrate. Whereas Arena Valley generally has 'dry-frozen' permafrost in the upper 1 m and minimal patterned ground, Beacon Valley contains massive ice buried by glacial drift and ice-cored rock glaciers and has ice-cemented permafrost in the upper 1 m and considerable associated patterned ground. Arena Valley soils have twice the rate of profile salt accumulation than Beacon Valley soils, because of lower available soil water and minimal cryoturbation. The ... : Data extracted in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150 ...
format Article in Journal/Newspaper
author Bockheim, James G
author_facet Bockheim, James G
author_sort Bockheim, James G
title Characteristics of soils from the Quartermain Mountain area, Antarctica ...
title_short Characteristics of soils from the Quartermain Mountain area, Antarctica ...
title_full Characteristics of soils from the Quartermain Mountain area, Antarctica ...
title_fullStr Characteristics of soils from the Quartermain Mountain area, Antarctica ...
title_full_unstemmed Characteristics of soils from the Quartermain Mountain area, Antarctica ...
title_sort characteristics of soils from the quartermain mountain area, antarctica ...
publisher PANGAEA
publishDate 2007
url https://dx.doi.org/10.1594/pangaea.807625
https://doi.pangaea.de/10.1594/PANGAEA.807625
long_lat ENVELOPE(160.650,160.650,-77.817,-77.817)
ENVELOPE(160.750,160.750,-77.850,-77.850)
ENVELOPE(160.983,160.983,-77.833,-77.833)
geographic McMurdo Dry Valleys
Beacon Valley
Quartermain Mountains
Arena Valley
geographic_facet McMurdo Dry Valleys
Beacon Valley
Quartermain Mountains
Arena Valley
genre Antarc*
Antarctica
Ice
International Polar Year
IPY
McMurdo Dry Valleys
permafrost
genre_facet Antarc*
Antarctica
Ice
International Polar Year
IPY
McMurdo Dry Valleys
permafrost
op_relation https://dx.doi.org/10.1111/j.1468-0459.2007.00315.x
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.80762510.1111/j.1468-0459.2007.00315.x
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