Surface lowering of ice-cored moraine by wandering lakes.

Lakes wander when steep ice scarps retreat due to collapse and melt. Rates of wander are c.1.3m yr -1 . Rates of lowering due to lake wander on Flanders Moraine (Vestfold Hills, Antarctica) are c.0.05m yr -1 , which is comparable to rates from elsewhere attributed to different processes.-from Author

Bibliographic Details
Main Author: Pickard, J.
Format: Article in Journal/Newspaper
Language:English
Published: 1983
Subjects:
Vestfold Hills
Vestfold
Flanders Moraine
Wandering Lakes
Antarc*
Antarctica
Journal of Glaciology
Online Access:https://researchers.mq.edu.au/en/publications/0ff414c1-e770-4a0b-bf78-5c7e489515d4
http://www.scopus.com/inward/record.url?scp=0021046453&partnerID=8YFLogxK
id ftmacquarieunicr:oai:https://researchers.mq.edu.au:publications/0ff414c1-e770-4a0b-bf78-5c7e489515d4
record_format openpolar
spelling ftmacquarieunicr:oai:https://researchers.mq.edu.au:publications/0ff414c1-e770-4a0b-bf78-5c7e489515d4 2023-05-15T13:51:16+02:00 Surface lowering of ice-cored moraine by wandering lakes. Pickard, J. 1983 https://researchers.mq.edu.au/en/publications/0ff414c1-e770-4a0b-bf78-5c7e489515d4 http://www.scopus.com/inward/record.url?scp=0021046453&partnerID=8YFLogxK eng eng info:eu-repo/semantics/restrictedAccess Pickard , J 1983 , ' Surface lowering of ice-cored moraine by wandering lakes. ' , Journal of Glaciology , vol. 29 , no. 102 , pp. 338-342 . article 1983 ftmacquarieunicr 2022-04-14T14:09:55Z Lakes wander when steep ice scarps retreat due to collapse and melt. Rates of wander are c.1.3m yr -1 . Rates of lowering due to lake wander on Flanders Moraine (Vestfold Hills, Antarctica) are c.0.05m yr -1 , which is comparable to rates from elsewhere attributed to different processes.-from Author Article in Journal/Newspaper Antarc* Antarctica Journal of Glaciology Macquarie University Research Portal Vestfold Hills Vestfold Flanders Moraine ENVELOPE(78.433,78.433,-68.638,-68.638) Wandering Lakes ENVELOPE(-107.335,-107.335,59.950,59.950)
institution Open Polar
collection Macquarie University Research Portal
op_collection_id ftmacquarieunicr
language English
description Lakes wander when steep ice scarps retreat due to collapse and melt. Rates of wander are c.1.3m yr -1 . Rates of lowering due to lake wander on Flanders Moraine (Vestfold Hills, Antarctica) are c.0.05m yr -1 , which is comparable to rates from elsewhere attributed to different processes.-from Author
format Article in Journal/Newspaper
author Pickard, J.
spellingShingle Pickard, J.
Surface lowering of ice-cored moraine by wandering lakes.
author_facet Pickard, J.
author_sort Pickard, J.
title Surface lowering of ice-cored moraine by wandering lakes.
title_short Surface lowering of ice-cored moraine by wandering lakes.
title_full Surface lowering of ice-cored moraine by wandering lakes.
title_fullStr Surface lowering of ice-cored moraine by wandering lakes.
title_full_unstemmed Surface lowering of ice-cored moraine by wandering lakes.
title_sort surface lowering of ice-cored moraine by wandering lakes.
publishDate 1983
url https://researchers.mq.edu.au/en/publications/0ff414c1-e770-4a0b-bf78-5c7e489515d4
http://www.scopus.com/inward/record.url?scp=0021046453&partnerID=8YFLogxK
long_lat ENVELOPE(78.433,78.433,-68.638,-68.638)
ENVELOPE(-107.335,-107.335,59.950,59.950)
geographic Vestfold Hills
Vestfold
Flanders Moraine
Wandering Lakes
geographic_facet Vestfold Hills
Vestfold
Flanders Moraine
Wandering Lakes
genre Antarc*
Antarctica
Journal of Glaciology
genre_facet Antarc*
Antarctica
Journal of Glaciology
op_source Pickard , J 1983 , ' Surface lowering of ice-cored moraine by wandering lakes. ' , Journal of Glaciology , vol. 29 , no. 102 , pp. 338-342 .
op_rights info:eu-repo/semantics/restrictedAccess
_version_ 1766255038970200064

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