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'...
Published in: | Permafrost and Periglacial Processes |
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Format: | Article in Journal/Newspaper |
Language: | unknown |
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Online Access: | https://doi.org/10.1002/ppp.3430030315 |
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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 |