Southern limit of relict rock glaciers, Central Apennines, Italy

Abstract Relict rock glaciers have been identified in the Maiella Mountain massif, Central Apennines (42° N). They are located at elevations of 2500–2300 m a.s.l. and probably mark the uppermost and southernmost limit of Pleistocene discontinuous alpine permafrost in the Apennine peninsula.

Bibliographic Details
Published in:Permafrost and Periglacial Processes
Main Authors: Dramis, Francesco, Kotarba, Adam
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1992
Subjects:
permafrost
Permafrost and Periglacial Processes
Online Access:http://dx.doi.org/10.1002/ppp.3430030315
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.3430030315
https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.3430030315
id crwiley:10.1002/ppp.3430030315
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spelling crwiley:10.1002/ppp.3430030315 2024-06-02T08:13:02+00:00 Southern limit of relict rock glaciers, Central Apennines, Italy Dramis, Francesco Kotarba, Adam 1992 http://dx.doi.org/10.1002/ppp.3430030315 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.3430030315 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.3430030315 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Permafrost and Periglacial Processes volume 3, issue 3, page 257-260 ISSN 1045-6740 1099-1530 journal-article 1992 crwiley https://doi.org/10.1002/ppp.3430030315 2024-05-03T11:11:09Z Abstract Relict rock glaciers have been identified in the Maiella Mountain massif, Central Apennines (42° N). They are located at elevations of 2500–2300 m a.s.l. and probably mark the uppermost and southernmost limit of Pleistocene discontinuous alpine permafrost in the Apennine peninsula. Article in Journal/Newspaper permafrost Permafrost and Periglacial Processes Wiley Online Library Permafrost and Periglacial Processes 3 3 257 260
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract Relict rock glaciers have been identified in the Maiella Mountain massif, Central Apennines (42° N). They are located at elevations of 2500–2300 m a.s.l. and probably mark the uppermost and southernmost limit of Pleistocene discontinuous alpine permafrost in the Apennine peninsula.
format Article in Journal/Newspaper
author Dramis, Francesco
Kotarba, Adam
spellingShingle Dramis, Francesco
Kotarba, Adam
Southern limit of relict rock glaciers, Central Apennines, Italy
author_facet Dramis, Francesco
Kotarba, Adam
author_sort Dramis, Francesco
title Southern limit of relict rock glaciers, Central Apennines, Italy
title_short Southern limit of relict rock glaciers, Central Apennines, Italy
title_full Southern limit of relict rock glaciers, Central Apennines, Italy
title_fullStr Southern limit of relict rock glaciers, Central Apennines, Italy
title_full_unstemmed Southern limit of relict rock glaciers, Central Apennines, Italy
title_sort southern limit of relict rock glaciers, central apennines, italy
publisher Wiley
publishDate 1992
url http://dx.doi.org/10.1002/ppp.3430030315
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.3430030315
https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.3430030315
genre permafrost
Permafrost and Periglacial Processes
genre_facet permafrost
Permafrost and Periglacial Processes
op_source Permafrost and Periglacial Processes
volume 3, issue 3, page 257-260
ISSN 1045-6740 1099-1530
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/ppp.3430030315
container_title Permafrost and Periglacial Processes
container_volume 3
container_issue 3
container_start_page 257
op_container_end_page 260
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