Southern limit of relict rock glaciers, Central Apennines, Italy

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. Des restes d'...

Full description

Bibliographic Details
Published in:Permafrost and Periglacial Processes
Main Authors: Francesco Dramis, Adam Kotarba
Format: Article in Journal/Newspaper
Language:unknown
Subjects:
permafrost
pergélisol
Online Access:https://doi.org/10.1002/ppp.3430030315
id ftrepec:oai:RePEc:wly:perpro:v:3:y:1992:i:3:p:257-260
record_format openpolar
spelling ftrepec:oai:RePEc:wly:perpro:v:3:y:1992:i:3:p:257-260 2023-05-15T17:57:26+02:00 Southern limit of relict rock glaciers, Central Apennines, Italy Francesco Dramis Adam Kotarba https://doi.org/10.1002/ppp.3430030315 unknown https://doi.org/10.1002/ppp.3430030315 article ftrepec https://doi.org/10.1002/ppp.3430030315 2020-12-04T13:31:03Z 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. Des restes d'anciens glaciers rocheux ont été identifiés dans le massif montagneux de Maiella, au centre de Appennins (42° N). Ils sont localisés à des altitudes comprises entre 2500 et 2300 m et marquent probablement la limite inférieure et méridionale du pergélisol pléistocène discontinu dans la péninsule italienne. Article in Journal/Newspaper permafrost pergélisol RePEc (Research Papers in Economics) Permafrost and Periglacial Processes 3 3 257 260
institution Open Polar
collection RePEc (Research Papers in Economics)
op_collection_id ftrepec
language unknown
description 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. Des restes d'anciens glaciers rocheux ont été identifiés dans le massif montagneux de Maiella, au centre de Appennins (42° N). Ils sont localisés à des altitudes comprises entre 2500 et 2300 m et marquent probablement la limite inférieure et méridionale du pergélisol pléistocène discontinu dans la péninsule italienne.
format Article in Journal/Newspaper
author Francesco Dramis
Adam Kotarba
spellingShingle Francesco Dramis
Adam Kotarba
Southern limit of relict rock glaciers, Central Apennines, Italy
author_facet Francesco Dramis
Adam Kotarba
author_sort Francesco Dramis
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
url https://doi.org/10.1002/ppp.3430030315
genre permafrost
pergélisol
genre_facet permafrost
pergélisol
op_relation https://doi.org/10.1002/ppp.3430030315
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
_version_ 1766165870220935168

Similar Items