Characterization, Geometry, Temporal Evolution and Controlling Mechanisms of the Jettan Rock-Slide, Northern Norway
The Jettan rockslide is an active topmost part of a large instability in paragneiss along the fjord Storfjorden in Northern Norway. It has deep back fractures in the top part with sliding planes at 45–50 m depth. The sliding planes seem to be controlled largely by SW-NE trending regional faults dipp...
Main Authors: | , , , |
---|---|
Other Authors: | , , , , , , |
Format: | Book Part |
Language: | English |
Published: |
Springer Science+Business Media
2015
|
Subjects: | |
Online Access: | https://curis.ku.dk/portal/da/publications/characterization-geometry-temporal-evolution-and-controlling-mechanisms-of-the-jettan-rockslide-northern-norway(16e91c78-6c37-47fd-bb9f-88356fa6356c).html https://doi.org/10.1007/978-3-319-09057-3_40 |
id |
ftcopenhagenunip:oai:pure.atira.dk:publications/16e91c78-6c37-47fd-bb9f-88356fa6356c |
---|---|
record_format |
openpolar |
spelling |
ftcopenhagenunip:oai:pure.atira.dk:publications/16e91c78-6c37-47fd-bb9f-88356fa6356c 2024-05-19T07:41:51+00:00 Characterization, Geometry, Temporal Evolution and Controlling Mechanisms of the Jettan Rock-Slide, Northern Norway Blikra, Lars Harald Christiansen, Hanne Hvidtfeldt Kristensen, Lene Lovisolo, Mario Lollino, Giorgio Giordan, Daniele Crosta, Giovanni B. Corominas, Jordi Azzam, Rafig Wasowski, Janusz Sciarra, Nicola 2015 https://curis.ku.dk/portal/da/publications/characterization-geometry-temporal-evolution-and-controlling-mechanisms-of-the-jettan-rockslide-northern-norway(16e91c78-6c37-47fd-bb9f-88356fa6356c).html https://doi.org/10.1007/978-3-319-09057-3_40 eng eng Springer Science+Business Media info:eu-repo/semantics/closedAccess Blikra , L H , Christiansen , H H , Kristensen , L & Lovisolo , M 2015 , Characterization, Geometry, Temporal Evolution and Controlling Mechanisms of the Jettan Rock-Slide, Northern Norway . in G Lollino , D Giordan , G B Crosta , J Corominas , R Azzam , J Wasowski & N Sciarra (eds) , Engineering Geology for Society and Territory : Landslide Processes . vol. 2 , Springer Science+Business Media , pp. 273-278 . https://doi.org/10.1007/978-3-319-09057-3_40 bookPart 2015 ftcopenhagenunip https://doi.org/10.1007/978-3-319-09057-3_40 2024-04-25T00:45:02Z The Jettan rockslide is an active topmost part of a large instability in paragneiss along the fjord Storfjorden in Northern Norway. It has deep back fractures in the top part with sliding planes at 45–50 m depth. The sliding planes seem to be controlled largely by SW-NE trending regional faults dipping steeply downslope towards NW. The displacements vary from about 2 cm–5 cm/year. The active movements demonstrate a systematic seasonal trend with displacements initiating during snowmelt in mid-May, decreasing during the late autumn and early winter and with low deformations until spring. The top part of the rockslide sectors has discontinuous permafrost, while sporadic permafrost is documented to exist in the open fractures in the lower parts. The seasonal changes is thought to be controlled by changing shear strength of the brecciated sliding planes due to either raising ice temperatures within the detachment zones and/or variations in water infiltration from local ice bodies to the unsaturated sliding zones. Book Part Ice Northern Norway permafrost University of Copenhagen: Research 273 278 Cham |
institution |
Open Polar |
collection |
University of Copenhagen: Research |
op_collection_id |
ftcopenhagenunip |
language |
English |
description |
The Jettan rockslide is an active topmost part of a large instability in paragneiss along the fjord Storfjorden in Northern Norway. It has deep back fractures in the top part with sliding planes at 45–50 m depth. The sliding planes seem to be controlled largely by SW-NE trending regional faults dipping steeply downslope towards NW. The displacements vary from about 2 cm–5 cm/year. The active movements demonstrate a systematic seasonal trend with displacements initiating during snowmelt in mid-May, decreasing during the late autumn and early winter and with low deformations until spring. The top part of the rockslide sectors has discontinuous permafrost, while sporadic permafrost is documented to exist in the open fractures in the lower parts. The seasonal changes is thought to be controlled by changing shear strength of the brecciated sliding planes due to either raising ice temperatures within the detachment zones and/or variations in water infiltration from local ice bodies to the unsaturated sliding zones. |
author2 |
Lollino, Giorgio Giordan, Daniele Crosta, Giovanni B. Corominas, Jordi Azzam, Rafig Wasowski, Janusz Sciarra, Nicola |
format |
Book Part |
author |
Blikra, Lars Harald Christiansen, Hanne Hvidtfeldt Kristensen, Lene Lovisolo, Mario |
spellingShingle |
Blikra, Lars Harald Christiansen, Hanne Hvidtfeldt Kristensen, Lene Lovisolo, Mario Characterization, Geometry, Temporal Evolution and Controlling Mechanisms of the Jettan Rock-Slide, Northern Norway |
author_facet |
Blikra, Lars Harald Christiansen, Hanne Hvidtfeldt Kristensen, Lene Lovisolo, Mario |
author_sort |
Blikra, Lars Harald |
title |
Characterization, Geometry, Temporal Evolution and Controlling Mechanisms of the Jettan Rock-Slide, Northern Norway |
title_short |
Characterization, Geometry, Temporal Evolution and Controlling Mechanisms of the Jettan Rock-Slide, Northern Norway |
title_full |
Characterization, Geometry, Temporal Evolution and Controlling Mechanisms of the Jettan Rock-Slide, Northern Norway |
title_fullStr |
Characterization, Geometry, Temporal Evolution and Controlling Mechanisms of the Jettan Rock-Slide, Northern Norway |
title_full_unstemmed |
Characterization, Geometry, Temporal Evolution and Controlling Mechanisms of the Jettan Rock-Slide, Northern Norway |
title_sort |
characterization, geometry, temporal evolution and controlling mechanisms of the jettan rock-slide, northern norway |
publisher |
Springer Science+Business Media |
publishDate |
2015 |
url |
https://curis.ku.dk/portal/da/publications/characterization-geometry-temporal-evolution-and-controlling-mechanisms-of-the-jettan-rockslide-northern-norway(16e91c78-6c37-47fd-bb9f-88356fa6356c).html https://doi.org/10.1007/978-3-319-09057-3_40 |
genre |
Ice Northern Norway permafrost |
genre_facet |
Ice Northern Norway permafrost |
op_source |
Blikra , L H , Christiansen , H H , Kristensen , L & Lovisolo , M 2015 , Characterization, Geometry, Temporal Evolution and Controlling Mechanisms of the Jettan Rock-Slide, Northern Norway . in G Lollino , D Giordan , G B Crosta , J Corominas , R Azzam , J Wasowski & N Sciarra (eds) , Engineering Geology for Society and Territory : Landslide Processes . vol. 2 , Springer Science+Business Media , pp. 273-278 . https://doi.org/10.1007/978-3-319-09057-3_40 |
op_rights |
info:eu-repo/semantics/closedAccess |
op_doi |
https://doi.org/10.1007/978-3-319-09057-3_40 |
container_start_page |
273 |
op_container_end_page |
278 |
op_publisher_place |
Cham |
_version_ |
1799481456886546432 |