Periglacial landforms in the central French Pyrenees: spatial/chronological analyses and promotion
This thesis of climatic geomorphology aims to characterize the past and present periglacial stage in the Western part of the central French Pyrenees. It is based on the relationships between the regional climatic characteristics (freezing/thawing cycles in the ambient air and in the ground, quantity...
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Format: | Doctoral or Postdoctoral Thesis |
Language: | French |
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HAL CCSD
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Online Access: | https://tel.archives-ouvertes.fr/tel-00564112 https://tel.archives-ouvertes.fr/tel-00564112/document https://tel.archives-ouvertes.fr/tel-00564112/file/THESE.pdf |
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ftccsdartic:oai:HAL:tel-00564112v1 2023-05-15T16:37:48+02:00 Periglacial landforms in the central French Pyrenees: spatial/chronological analyses and promotion Les formes périglaciaires dans les Pyrénées centrales françaises : analyse spatiale, chronologique et valorisation Feuillet, Thierry Littoral, Environnement, Télédétection, Géomatique (LETG - Nantes) Université de Caen Normandie (UNICAEN) Normandie Université (NU)-Normandie Université (NU)-École pratique des hautes études (EPHE) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Brest (UBO)-Université de Rennes 2 (UR2) Université de Rennes (UNIV-RENNES)-Université de Rennes (UNIV-RENNES)-Centre National de la Recherche Scientifique (CNRS)-Institut de Géographie et d'Aménagement Régional de l'Université de Nantes (IGARUN) Université de Nantes (UN)-Université de Nantes (UN) Université de Nantes Pascal Bertran 2010-11-12 https://tel.archives-ouvertes.fr/tel-00564112 https://tel.archives-ouvertes.fr/tel-00564112/document https://tel.archives-ouvertes.fr/tel-00564112/file/THESE.pdf fr fre HAL CCSD tel-00564112 https://tel.archives-ouvertes.fr/tel-00564112 https://tel.archives-ouvertes.fr/tel-00564112/document https://tel.archives-ouvertes.fr/tel-00564112/file/THESE.pdf info:eu-repo/semantics/OpenAccess https://tel.archives-ouvertes.fr/tel-00564112 Géographie. Université de Nantes, 2010. Français geomorphology periglacial permafrost Pyrénées géomorphologie périglaciaire pergélisol environnement géomorphosites [SHS.GEO]Humanities and Social Sciences/Geography [SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/Geomorphology info:eu-repo/semantics/doctoralThesis Theses 2010 ftccsdartic 2021-12-26T00:27:47Z This thesis of climatic geomorphology aims to characterize the past and present periglacial stage in the Western part of the central French Pyrenees. It is based on the relationships between the regional climatic characteristics (freezing/thawing cycles in the ambient air and in the ground, quantity and rhythm of snow precipitations) and geomorphic consequences of this climate (patterned grounds, solifluction landforms, permafrost landforms). Thus, the first part focuses on the climate and on the altitudinal definition of the landforms under consideration. It reveals that regional periglacial landforms are staging in a large belt between 1 900 and 3 200 m a.s.l., in which mean annual air temperatures vary between 5°C and -3°C. freezing/thawing cycles fluctuate between 60 and 130 per year and our numerical modelling indicates that the ground freezing can exceed one meter in depth whatever elevation during snow-free time. The second part deals with spatial and paleoenvironmental variability of the periglacial level. In a first step, it is shown on the basis of multivariate analyses that the landforms staging vary on each slope according to local parameters (exposure, lithology, moisture, vegetal cover). Recently deglaciated areas are the most favourable to the development of forms because of the fine-rich deposits occurrence and high moisture. In a second step, the analysis focuses on the evolution of the periglacial landscapes since the Lateglacial. The observations of inherited landforms and radiocarbon dating show some favourable phases to periglacial dynamics (Younger Dryas, mid-Holocene, Little Ice Age). Finally, the third part describes activities dedicated to the promotion and diffusion of these results in the Pyrenees national park. For that, we evaluated 30 geomorphosites of the periglacial belt. Didactic panels and a web site were created to propose to the public at large easy to read presentations of the most remarkable geomorphosites. Cette thèse de géomorphologie climatique a pour objectif de ... Doctoral or Postdoctoral Thesis Ice permafrost pergélisol Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) |
institution |
Open Polar |
collection |
Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) |
op_collection_id |
ftccsdartic |
language |
French |
topic |
geomorphology periglacial permafrost Pyrénées géomorphologie périglaciaire pergélisol environnement géomorphosites [SHS.GEO]Humanities and Social Sciences/Geography [SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/Geomorphology |
spellingShingle |
geomorphology periglacial permafrost Pyrénées géomorphologie périglaciaire pergélisol environnement géomorphosites [SHS.GEO]Humanities and Social Sciences/Geography [SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/Geomorphology Feuillet, Thierry Periglacial landforms in the central French Pyrenees: spatial/chronological analyses and promotion |
topic_facet |
geomorphology periglacial permafrost Pyrénées géomorphologie périglaciaire pergélisol environnement géomorphosites [SHS.GEO]Humanities and Social Sciences/Geography [SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/Geomorphology |
description |
This thesis of climatic geomorphology aims to characterize the past and present periglacial stage in the Western part of the central French Pyrenees. It is based on the relationships between the regional climatic characteristics (freezing/thawing cycles in the ambient air and in the ground, quantity and rhythm of snow precipitations) and geomorphic consequences of this climate (patterned grounds, solifluction landforms, permafrost landforms). Thus, the first part focuses on the climate and on the altitudinal definition of the landforms under consideration. It reveals that regional periglacial landforms are staging in a large belt between 1 900 and 3 200 m a.s.l., in which mean annual air temperatures vary between 5°C and -3°C. freezing/thawing cycles fluctuate between 60 and 130 per year and our numerical modelling indicates that the ground freezing can exceed one meter in depth whatever elevation during snow-free time. The second part deals with spatial and paleoenvironmental variability of the periglacial level. In a first step, it is shown on the basis of multivariate analyses that the landforms staging vary on each slope according to local parameters (exposure, lithology, moisture, vegetal cover). Recently deglaciated areas are the most favourable to the development of forms because of the fine-rich deposits occurrence and high moisture. In a second step, the analysis focuses on the evolution of the periglacial landscapes since the Lateglacial. The observations of inherited landforms and radiocarbon dating show some favourable phases to periglacial dynamics (Younger Dryas, mid-Holocene, Little Ice Age). Finally, the third part describes activities dedicated to the promotion and diffusion of these results in the Pyrenees national park. For that, we evaluated 30 geomorphosites of the periglacial belt. Didactic panels and a web site were created to propose to the public at large easy to read presentations of the most remarkable geomorphosites. Cette thèse de géomorphologie climatique a pour objectif de ... |
author2 |
Littoral, Environnement, Télédétection, Géomatique (LETG - Nantes) Université de Caen Normandie (UNICAEN) Normandie Université (NU)-Normandie Université (NU)-École pratique des hautes études (EPHE) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Brest (UBO)-Université de Rennes 2 (UR2) Université de Rennes (UNIV-RENNES)-Université de Rennes (UNIV-RENNES)-Centre National de la Recherche Scientifique (CNRS)-Institut de Géographie et d'Aménagement Régional de l'Université de Nantes (IGARUN) Université de Nantes (UN)-Université de Nantes (UN) Université de Nantes Pascal Bertran |
format |
Doctoral or Postdoctoral Thesis |
author |
Feuillet, Thierry |
author_facet |
Feuillet, Thierry |
author_sort |
Feuillet, Thierry |
title |
Periglacial landforms in the central French Pyrenees: spatial/chronological analyses and promotion |
title_short |
Periglacial landforms in the central French Pyrenees: spatial/chronological analyses and promotion |
title_full |
Periglacial landforms in the central French Pyrenees: spatial/chronological analyses and promotion |
title_fullStr |
Periglacial landforms in the central French Pyrenees: spatial/chronological analyses and promotion |
title_full_unstemmed |
Periglacial landforms in the central French Pyrenees: spatial/chronological analyses and promotion |
title_sort |
periglacial landforms in the central french pyrenees: spatial/chronological analyses and promotion |
publisher |
HAL CCSD |
publishDate |
2010 |
url |
https://tel.archives-ouvertes.fr/tel-00564112 https://tel.archives-ouvertes.fr/tel-00564112/document https://tel.archives-ouvertes.fr/tel-00564112/file/THESE.pdf |
genre |
Ice permafrost pergélisol |
genre_facet |
Ice permafrost pergélisol |
op_source |
https://tel.archives-ouvertes.fr/tel-00564112 Géographie. Université de Nantes, 2010. Français |
op_relation |
tel-00564112 https://tel.archives-ouvertes.fr/tel-00564112 https://tel.archives-ouvertes.fr/tel-00564112/document https://tel.archives-ouvertes.fr/tel-00564112/file/THESE.pdf |
op_rights |
info:eu-repo/semantics/OpenAccess |
_version_ |
1766028100415520768 |