A morphometric approach to reveal the effects of ground-ice thaw on rapid mass movements in northern Iceland
International audience Permafrost degradation is one of the main controlling factors of slope instabilities in glacial and periglacial environments (e.g., Gruber and Haeberli, 2007). In permafrost terrains, ground ice can occur in pores, cavities, voids in soils or rocks, and its thaw can cause slop...
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Bibliographic Details
Main Authors: |
Morino, Costanza,
Conway, Susan J.,
Balme, Matthew R.,
Sæmundsson, Þorsteinn,
Kristinn Helgason, Jón,
Jordan, Colm,
Hillier, John,
Argles, Tom |
Other Authors: |
School of Environment, Earth and Ecosystem Sciences Milton Keynes,
Faculty of Science, Technology, Engineering and Mathematics Milton Keynes,
The Open University Milton Keynes (OU)-The Open University Milton Keynes (OU),
Laboratoire de Planétologie et Géodynamique UMR 6112 (LPG),
Université d'Angers (UA)-Université de Nantes - UFR des Sciences et des Techniques (UN UFR ST),
Université de Nantes (UN)-Université de Nantes (UN)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS),
School of Physical Sciences Milton Keynes,
Icelandic Meteorological Office (IMO),
British Geological Survey Keyworth,
British Geological Survey (BGS) |
Format: | Conference Object
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Language: | English |
Published: |
HAL CCSD
2019
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Subjects: |
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Online Access: | https://hal.archives-ouvertes.fr/hal-02407812
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