MORPHOLOGY, FREQUENCY AND MAGNITUDE OF ACTIVE-LAYER DETACHMENT SLIDES, FOSHEIM PENINSULA, ELLESMERE ISLAND, N.W.T.
Hundreds of active-layer detachment slides are present on the Fosheim Peninsula both above and below the marine limit within a 50 km radius of Eureka These landslides occur in silty or sandy materials on slopes from 2->40 ° and range up to 700 m in length and 150 m in width. Length distributions...
Main Author: | |
---|---|
Other Authors: | |
Format: | Text |
Language: | English |
Subjects: | |
Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.518.7450 http://pubs.aina.ucalgary.ca/cpc/cpc5-111.pdf |
id |
ftciteseerx:oai:CiteSeerX.psu:10.1.1.518.7450 |
---|---|
record_format |
openpolar |
spelling |
ftciteseerx:oai:CiteSeerX.psu:10.1.1.518.7450 2023-05-15T16:05:57+02:00 MORPHOLOGY, FREQUENCY AND MAGNITUDE OF ACTIVE-LAYER DETACHMENT SLIDES, FOSHEIM PENINSULA, ELLESMERE ISLAND, N.W.T. Antoni G. Lewkowicz The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.518.7450 http://pubs.aina.ucalgary.ca/cpc/cpc5-111.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.518.7450 http://pubs.aina.ucalgary.ca/cpc/cpc5-111.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://pubs.aina.ucalgary.ca/cpc/cpc5-111.pdf text ftciteseerx 2016-01-08T09:59:25Z Hundreds of active-layer detachment slides are present on the Fosheim Peninsula both above and below the marine limit within a 50 km radius of Eureka These landslides occur in silty or sandy materials on slopes from 2->40 ° and range up to 700 m in length and 150 m in width. Length distributions are positively skewed and modal values are 20-40 m. Typical scar depths are 03-0.5 m and since these represent the position of the thaw front in mid- to late summer, slope failure occurs at this time. Minimum estimates of downslope movement of soil materials by active-layer detachment sliding in three locations range &om 6 to 60 mm yr l for the upper 0.5 m of the active layer. These rates correspond to volumetric transport of 30-300 cm3 cm-1 yrl and indicate that this geomorphic process is at least as important as solifluction. Unequal responses at three sites to a particularly warm period in the summer of 1988 suggest that where active-layer detachment slides are already common, climatic warming might initially induce additional failures. More frequent external triggers will not affect long-term activity rates, however, unless internal slope processes such as weathering and moisture migration are also influenced by climatic change. Sur la Pdninsule Fosheim, au-dessus et au-dessous de la limite marine se trouvent des centaines de ruptures du mollisol B l'indrieur d'un rayon de 50 lun de Eureka. Ces glissernents de terrain se produisent Text Ellesmere Island Fosheim Peninsula Unknown Ellesmere Island Eureka ENVELOPE(-85.940,-85.940,79.990,79.990) Fosheim Peninsula ENVELOPE(-83.749,-83.749,79.669,79.669) |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
ftciteseerx |
language |
English |
description |
Hundreds of active-layer detachment slides are present on the Fosheim Peninsula both above and below the marine limit within a 50 km radius of Eureka These landslides occur in silty or sandy materials on slopes from 2->40 ° and range up to 700 m in length and 150 m in width. Length distributions are positively skewed and modal values are 20-40 m. Typical scar depths are 03-0.5 m and since these represent the position of the thaw front in mid- to late summer, slope failure occurs at this time. Minimum estimates of downslope movement of soil materials by active-layer detachment sliding in three locations range &om 6 to 60 mm yr l for the upper 0.5 m of the active layer. These rates correspond to volumetric transport of 30-300 cm3 cm-1 yrl and indicate that this geomorphic process is at least as important as solifluction. Unequal responses at three sites to a particularly warm period in the summer of 1988 suggest that where active-layer detachment slides are already common, climatic warming might initially induce additional failures. More frequent external triggers will not affect long-term activity rates, however, unless internal slope processes such as weathering and moisture migration are also influenced by climatic change. Sur la Pdninsule Fosheim, au-dessus et au-dessous de la limite marine se trouvent des centaines de ruptures du mollisol B l'indrieur d'un rayon de 50 lun de Eureka. Ces glissernents de terrain se produisent |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Antoni G. Lewkowicz |
spellingShingle |
Antoni G. Lewkowicz MORPHOLOGY, FREQUENCY AND MAGNITUDE OF ACTIVE-LAYER DETACHMENT SLIDES, FOSHEIM PENINSULA, ELLESMERE ISLAND, N.W.T. |
author_facet |
Antoni G. Lewkowicz |
author_sort |
Antoni G. Lewkowicz |
title |
MORPHOLOGY, FREQUENCY AND MAGNITUDE OF ACTIVE-LAYER DETACHMENT SLIDES, FOSHEIM PENINSULA, ELLESMERE ISLAND, N.W.T. |
title_short |
MORPHOLOGY, FREQUENCY AND MAGNITUDE OF ACTIVE-LAYER DETACHMENT SLIDES, FOSHEIM PENINSULA, ELLESMERE ISLAND, N.W.T. |
title_full |
MORPHOLOGY, FREQUENCY AND MAGNITUDE OF ACTIVE-LAYER DETACHMENT SLIDES, FOSHEIM PENINSULA, ELLESMERE ISLAND, N.W.T. |
title_fullStr |
MORPHOLOGY, FREQUENCY AND MAGNITUDE OF ACTIVE-LAYER DETACHMENT SLIDES, FOSHEIM PENINSULA, ELLESMERE ISLAND, N.W.T. |
title_full_unstemmed |
MORPHOLOGY, FREQUENCY AND MAGNITUDE OF ACTIVE-LAYER DETACHMENT SLIDES, FOSHEIM PENINSULA, ELLESMERE ISLAND, N.W.T. |
title_sort |
morphology, frequency and magnitude of active-layer detachment slides, fosheim peninsula, ellesmere island, n.w.t. |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.518.7450 http://pubs.aina.ucalgary.ca/cpc/cpc5-111.pdf |
long_lat |
ENVELOPE(-85.940,-85.940,79.990,79.990) ENVELOPE(-83.749,-83.749,79.669,79.669) |
geographic |
Ellesmere Island Eureka Fosheim Peninsula |
geographic_facet |
Ellesmere Island Eureka Fosheim Peninsula |
genre |
Ellesmere Island Fosheim Peninsula |
genre_facet |
Ellesmere Island Fosheim Peninsula |
op_source |
http://pubs.aina.ucalgary.ca/cpc/cpc5-111.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.518.7450 http://pubs.aina.ucalgary.ca/cpc/cpc5-111.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766401865469132800 |