Present and past geocryogenic processes in Mexico

Abstract Periglacial processes and landforms are described from the Cordillera Neovolcánica of central Mexico. Inactive rock glaciers are related to different late‐glacial and Holocene phases of permafrost conditions. Active discontinuous permafrost occurs above c . 4600 m ASL and appears to be from...

Full description

Bibliographic Details
Published in:	Permafrost and Periglacial Processes
Main Author:	Heine, Klaus
Format:	Article in Journal/Newspaper
Language:	English
Published:	Wiley 1994
Subjects:	Ice permafrost Permafrost and Periglacial Processes
Online Access:	http://dx.doi.org/10.1002/ppp.3430050102 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.3430050102 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.3430050102

id	crwiley:10.1002/ppp.3430050102
record_format	openpolar
spelling	crwiley:10.1002/ppp.3430050102 2024-06-02T08:07:58+00:00 Present and past geocryogenic processes in Mexico Heine, Klaus 1994 http://dx.doi.org/10.1002/ppp.3430050102 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.3430050102 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.3430050102 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Permafrost and Periglacial Processes volume 5, issue 1, page 1-12 ISSN 1045-6740 1099-1530 journal-article 1994 crwiley https://doi.org/10.1002/ppp.3430050102 2024-05-03T11:33:48Z Abstract Periglacial processes and landforms are described from the Cordillera Neovolcánica of central Mexico. Inactive rock glaciers are related to different late‐glacial and Holocene phases of permafrost conditions. Active discontinuous permafrost occurs above c . 4600 m ASL and appears to be from the Little Ice Age. The lower limit of late‐glacial rock glaciers is situated 500 and 600 m lower than during the Little Ice Age. Article in Journal/Newspaper Ice permafrost Permafrost and Periglacial Processes Wiley Online Library Permafrost and Periglacial Processes 5 1 1 12
institution	Open Polar
collection	Wiley Online Library
op_collection_id	crwiley
language	English
description	Abstract Periglacial processes and landforms are described from the Cordillera Neovolcánica of central Mexico. Inactive rock glaciers are related to different late‐glacial and Holocene phases of permafrost conditions. Active discontinuous permafrost occurs above c . 4600 m ASL and appears to be from the Little Ice Age. The lower limit of late‐glacial rock glaciers is situated 500 and 600 m lower than during the Little Ice Age.
format	Article in Journal/Newspaper
author	Heine, Klaus
spellingShingle	Heine, Klaus Present and past geocryogenic processes in Mexico
author_facet	Heine, Klaus
author_sort	Heine, Klaus
title	Present and past geocryogenic processes in Mexico
title_short	Present and past geocryogenic processes in Mexico
title_full	Present and past geocryogenic processes in Mexico
title_fullStr	Present and past geocryogenic processes in Mexico
title_full_unstemmed	Present and past geocryogenic processes in Mexico
title_sort	present and past geocryogenic processes in mexico
publisher	Wiley
publishDate	1994
url	http://dx.doi.org/10.1002/ppp.3430050102 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.3430050102 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.3430050102
genre	Ice permafrost Permafrost and Periglacial Processes
genre_facet	Ice permafrost Permafrost and Periglacial Processes
op_source	Permafrost and Periglacial Processes volume 5, issue 1, page 1-12 ISSN 1045-6740 1099-1530
op_rights	http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi	https://doi.org/10.1002/ppp.3430050102
container_title	Permafrost and Periglacial Processes
container_volume	5
container_issue	1
container_start_page	1
op_container_end_page	12
_version_	1800753125583224832

Present and past geocryogenic processes in Mexico

Similar Items