Introduction

Abstract Environmental reconstructions utilising the evidence of relic or fossil periglacial features are necessarily based on the nature and present distribution of comparable active features. The most critical features are those indicative of permafrost, because of the negative mean annual tempera...

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Bibliographic Details
Published in:Journal of Quaternary Science
Main Authors: French, Hugh M., Koster, Eduard A.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1988
Subjects:
Washburn
permafrost
Online Access:http://dx.doi.org/10.1002/jqs.3390030102
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjqs.3390030102
https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.3390030102
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spelling crwiley:10.1002/jqs.3390030102 2024-06-02T08:12:58+00:00 Introduction French, Hugh M. Koster, Eduard A. 1988 http://dx.doi.org/10.1002/jqs.3390030102 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjqs.3390030102 https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.3390030102 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Journal of Quaternary Science volume 3, issue 1, page 1-2 ISSN 0267-8179 1099-1417 journal-article 1988 crwiley https://doi.org/10.1002/jqs.3390030102 2024-05-03T11:18:06Z Abstract Environmental reconstructions utilising the evidence of relic or fossil periglacial features are necessarily based on the nature and present distribution of comparable active features. The most critical features are those indicative of permafrost, because of the negative mean annual temperatures required for permafrost, whereas many other cold climate features are much less informative as to temperature implications. (Washburn, Geocryology, 1980, 279). Article in Journal/Newspaper permafrost Wiley Online Library Washburn ENVELOPE(-86.133,-86.133,-77.617,-77.617) Journal of Quaternary Science 3 1 1 2
institution Open Polar
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op_collection_id crwiley
language English
description Abstract Environmental reconstructions utilising the evidence of relic or fossil periglacial features are necessarily based on the nature and present distribution of comparable active features. The most critical features are those indicative of permafrost, because of the negative mean annual temperatures required for permafrost, whereas many other cold climate features are much less informative as to temperature implications. (Washburn, Geocryology, 1980, 279).
format Article in Journal/Newspaper
author French, Hugh M.
Koster, Eduard A.
spellingShingle French, Hugh M.
Koster, Eduard A.
Introduction
author_facet French, Hugh M.
Koster, Eduard A.
author_sort French, Hugh M.
title Introduction
title_short Introduction
title_full Introduction
title_fullStr Introduction
title_full_unstemmed Introduction
title_sort introduction
publisher Wiley
publishDate 1988
url http://dx.doi.org/10.1002/jqs.3390030102
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjqs.3390030102
https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.3390030102
long_lat ENVELOPE(-86.133,-86.133,-77.617,-77.617)
geographic Washburn
geographic_facet Washburn
genre permafrost
genre_facet permafrost
op_source Journal of Quaternary Science
volume 3, issue 1, page 1-2
ISSN 0267-8179 1099-1417
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/jqs.3390030102
container_title Journal of Quaternary Science
container_volume 3
container_issue 1
container_start_page 1
op_container_end_page 2
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