YUKON EXPLORATION AND GEOLOGY 2003 107 Permafrost and landslide activity:
Five case studies of recent landslides in southwestern Yukon Territory illustrate the role of permafrost in landslide processes of the region. In the Marshall Creek basin, permafrost degradation after recent forest fires caused numerous debris flows near the valley bottom. Similarly, on Haeckel Hill...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.556.3289 2023-05-15T16:37:23+02:00 YUKON EXPLORATION AND GEOLOGY 2003 107 Permafrost and landslide activity: Crystal A. Huscroft Panya S. Lipovsky Jeffrey D. Bond The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.556.3289 http://publications.gc.ca/collections/Collection/R71-41-2003E(9).pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.556.3289 http://publications.gc.ca/collections/Collection/R71-41-2003E(9).pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://publications.gc.ca/collections/Collection/R71-41-2003E(9).pdf text ftciteseerx 2016-01-08T11:47:32Z Five case studies of recent landslides in southwestern Yukon Territory illustrate the role of permafrost in landslide processes of the region. In the Marshall Creek basin, permafrost degradation after recent forest fires caused numerous debris flows near the valley bottom. Similarly, on Haeckel Hill, fire-related deepening of the active layer has facilitated active layer detachment slides on upper hillside slopes. In the Kluane Range, the interface between frozen and unfrozen ground appears to control the depth of movement for active layer detachment slides and debris flows along Silver Creek. The failure mechanism on Mount Sumanik is controlled by a frozen substrate, which contributes to a reduction in drainage and elevated pore-water pressure. Lastly, thawing of segregated ice has caused a thaw slump of fine-grained sediment in lacustrine terraces along Takhini River. RÉSUMÉ Cinq études de glissements de terrain récents illustrent le rôle du pergélisol dans les processus de glissement dans la région. Dans le bassin du ruisseau Marshall, la dégradation du pergélisol après des feux de forêt récents a provoqué de nombreuses coulées de débris dans le fond de la vallée. Dans une situation analogue, sur la colline Haeckel, le creusement du mollisol causé par le feu a fait Text Ice permafrost pergélisol Yukon Unknown Yukon Le Fond ENVELOPE(-55.815,-55.815,51.067,51.067) Takhini ENVELOPE(-135.094,-135.094,60.738,60.738) Silver Creek ENVELOPE(-138.401,-138.401,61.040,61.040) Takhini River ENVELOPE(-135.854,-135.854,59.999,59.999) Haeckel Hill ENVELOPE(-135.280,-135.280,60.768,60.768) Marshall Creek ENVELOPE(-137.340,-137.340,60.795,60.795) Mount Sumanik ENVELOPE(-135.327,-135.327,60.747,60.747) |
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ftciteseerx |
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English |
description |
Five case studies of recent landslides in southwestern Yukon Territory illustrate the role of permafrost in landslide processes of the region. In the Marshall Creek basin, permafrost degradation after recent forest fires caused numerous debris flows near the valley bottom. Similarly, on Haeckel Hill, fire-related deepening of the active layer has facilitated active layer detachment slides on upper hillside slopes. In the Kluane Range, the interface between frozen and unfrozen ground appears to control the depth of movement for active layer detachment slides and debris flows along Silver Creek. The failure mechanism on Mount Sumanik is controlled by a frozen substrate, which contributes to a reduction in drainage and elevated pore-water pressure. Lastly, thawing of segregated ice has caused a thaw slump of fine-grained sediment in lacustrine terraces along Takhini River. RÉSUMÉ Cinq études de glissements de terrain récents illustrent le rôle du pergélisol dans les processus de glissement dans la région. Dans le bassin du ruisseau Marshall, la dégradation du pergélisol après des feux de forêt récents a provoqué de nombreuses coulées de débris dans le fond de la vallée. Dans une situation analogue, sur la colline Haeckel, le creusement du mollisol causé par le feu a fait |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Crystal A. Huscroft Panya S. Lipovsky Jeffrey D. Bond |
spellingShingle |
Crystal A. Huscroft Panya S. Lipovsky Jeffrey D. Bond YUKON EXPLORATION AND GEOLOGY 2003 107 Permafrost and landslide activity: |
author_facet |
Crystal A. Huscroft Panya S. Lipovsky Jeffrey D. Bond |
author_sort |
Crystal A. Huscroft |
title |
YUKON EXPLORATION AND GEOLOGY 2003 107 Permafrost and landslide activity: |
title_short |
YUKON EXPLORATION AND GEOLOGY 2003 107 Permafrost and landslide activity: |
title_full |
YUKON EXPLORATION AND GEOLOGY 2003 107 Permafrost and landslide activity: |
title_fullStr |
YUKON EXPLORATION AND GEOLOGY 2003 107 Permafrost and landslide activity: |
title_full_unstemmed |
YUKON EXPLORATION AND GEOLOGY 2003 107 Permafrost and landslide activity: |
title_sort |
yukon exploration and geology 2003 107 permafrost and landslide activity: |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.556.3289 http://publications.gc.ca/collections/Collection/R71-41-2003E(9).pdf |
long_lat |
ENVELOPE(-55.815,-55.815,51.067,51.067) ENVELOPE(-135.094,-135.094,60.738,60.738) ENVELOPE(-138.401,-138.401,61.040,61.040) ENVELOPE(-135.854,-135.854,59.999,59.999) ENVELOPE(-135.280,-135.280,60.768,60.768) ENVELOPE(-137.340,-137.340,60.795,60.795) ENVELOPE(-135.327,-135.327,60.747,60.747) |
geographic |
Yukon Le Fond Takhini Silver Creek Takhini River Haeckel Hill Marshall Creek Mount Sumanik |
geographic_facet |
Yukon Le Fond Takhini Silver Creek Takhini River Haeckel Hill Marshall Creek Mount Sumanik |
genre |
Ice permafrost pergélisol Yukon |
genre_facet |
Ice permafrost pergélisol Yukon |
op_source |
http://publications.gc.ca/collections/Collection/R71-41-2003E(9).pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.556.3289 http://publications.gc.ca/collections/Collection/R71-41-2003E(9).pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766027684088905728 |