Present‐day periglacial processes and landforms in mountain areas

Abstract This paper outlines recent advances in our understanding of periglacial processes and landforms in mountain areas, as reported in the literature over the last 8 years. Landforms investigated include rockwalls, screes, avalanche paths, bedded slope deposits and patterned ground phenomena. Pr...

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Published in:Permafrost and Periglacial Processes
Main Authors: Lautridou, J. P., Francou, B., Hall, K.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1992
Subjects:
Online Access:http://dx.doi.org/10.1002/ppp.3430030206
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.3430030206
https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.3430030206
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spelling crwiley:10.1002/ppp.3430030206 2024-09-15T18:30:16+00:00 Present‐day periglacial processes and landforms in mountain areas Lautridou, J. P. Francou, B. Hall, K. 1992 http://dx.doi.org/10.1002/ppp.3430030206 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.3430030206 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.3430030206 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Permafrost and Periglacial Processes volume 3, issue 2, page 93-101 ISSN 1045-6740 1099-1530 journal-article 1992 crwiley https://doi.org/10.1002/ppp.3430030206 2024-08-27T04:28:08Z Abstract This paper outlines recent advances in our understanding of periglacial processes and landforms in mountain areas, as reported in the literature over the last 8 years. Landforms investigated include rockwalls, screes, avalanche paths, bedded slope deposits and patterned ground phenomena. Processes subject to quantification include cliff recession, rock displacements on slopes, rock thermal and moisture regimes, frost creep, mass wasting and solution. Laboratory experimentation and modelling studies have also been undertaken. Article in Journal/Newspaper Permafrost and Periglacial Processes Wiley Online Library Permafrost and Periglacial Processes 3 2 93 101
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract This paper outlines recent advances in our understanding of periglacial processes and landforms in mountain areas, as reported in the literature over the last 8 years. Landforms investigated include rockwalls, screes, avalanche paths, bedded slope deposits and patterned ground phenomena. Processes subject to quantification include cliff recession, rock displacements on slopes, rock thermal and moisture regimes, frost creep, mass wasting and solution. Laboratory experimentation and modelling studies have also been undertaken.
format Article in Journal/Newspaper
author Lautridou, J. P.
Francou, B.
Hall, K.
spellingShingle Lautridou, J. P.
Francou, B.
Hall, K.
Present‐day periglacial processes and landforms in mountain areas
author_facet Lautridou, J. P.
Francou, B.
Hall, K.
author_sort Lautridou, J. P.
title Present‐day periglacial processes and landforms in mountain areas
title_short Present‐day periglacial processes and landforms in mountain areas
title_full Present‐day periglacial processes and landforms in mountain areas
title_fullStr Present‐day periglacial processes and landforms in mountain areas
title_full_unstemmed Present‐day periglacial processes and landforms in mountain areas
title_sort present‐day periglacial processes and landforms in mountain areas
publisher Wiley
publishDate 1992
url http://dx.doi.org/10.1002/ppp.3430030206
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.3430030206
https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.3430030206
genre Permafrost and Periglacial Processes
genre_facet Permafrost and Periglacial Processes
op_source Permafrost and Periglacial Processes
volume 3, issue 2, page 93-101
ISSN 1045-6740 1099-1530
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/ppp.3430030206
container_title Permafrost and Periglacial Processes
container_volume 3
container_issue 2
container_start_page 93
op_container_end_page 101
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