Are Rock Avalanches and Landslides Due to Large Earthquakes or Local Topographic Effects? A Case Study of the Lurøy Earthquake of August 31, 1819, A 3D Finite Difference Approach

Bibliographic Details
Main Authors: Kebeasy, T. R. M., Husebye, Eystein S., Hestholm, S.
Format: Book Part
Language:unknown
Published: Springer Netherlands 2008
Subjects:
Online Access:http://dx.doi.org/10.1007/978-1-4020-6815-7_18
http://link.springer.com/content/pdf/10.1007/978-1-4020-6815-7_18.pdf
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spelling crspringernat:10.1007/978-1-4020-6815-7_18 2024-03-10T08:35:48+00:00 Are Rock Avalanches and Landslides Due to Large Earthquakes or Local Topographic Effects? A Case Study of the Lurøy Earthquake of August 31, 1819, A 3D Finite Difference Approach Kebeasy, T. R. M. Husebye, Eystein S. Hestholm, S. 2008 http://dx.doi.org/10.1007/978-1-4020-6815-7_18 http://link.springer.com/content/pdf/10.1007/978-1-4020-6815-7_18.pdf unknown Springer Netherlands NATO Science Series: IV: Earth and Environmental Sciences Earthquake Monitoring and Seismic Hazard Mitigation in Balkan Countries page 271-289 ISSN 1568-1238 ISBN 9781402068133 9781402068157 book-chapter 2008 crspringernat https://doi.org/10.1007/978-1-4020-6815-7_18 2024-02-13T17:12:42Z Book Part Lurøy Springer Nature Lurøy ENVELOPE(12.849,12.849,66.418,66.418) 271 289
institution Open Polar
collection Springer Nature
op_collection_id crspringernat
language unknown
format Book Part
author Kebeasy, T. R. M.
Husebye, Eystein S.
Hestholm, S.
spellingShingle Kebeasy, T. R. M.
Husebye, Eystein S.
Hestholm, S.
Are Rock Avalanches and Landslides Due to Large Earthquakes or Local Topographic Effects? A Case Study of the Lurøy Earthquake of August 31, 1819, A 3D Finite Difference Approach
author_facet Kebeasy, T. R. M.
Husebye, Eystein S.
Hestholm, S.
author_sort Kebeasy, T. R. M.
title Are Rock Avalanches and Landslides Due to Large Earthquakes or Local Topographic Effects? A Case Study of the Lurøy Earthquake of August 31, 1819, A 3D Finite Difference Approach
title_short Are Rock Avalanches and Landslides Due to Large Earthquakes or Local Topographic Effects? A Case Study of the Lurøy Earthquake of August 31, 1819, A 3D Finite Difference Approach
title_full Are Rock Avalanches and Landslides Due to Large Earthquakes or Local Topographic Effects? A Case Study of the Lurøy Earthquake of August 31, 1819, A 3D Finite Difference Approach
title_fullStr Are Rock Avalanches and Landslides Due to Large Earthquakes or Local Topographic Effects? A Case Study of the Lurøy Earthquake of August 31, 1819, A 3D Finite Difference Approach
title_full_unstemmed Are Rock Avalanches and Landslides Due to Large Earthquakes or Local Topographic Effects? A Case Study of the Lurøy Earthquake of August 31, 1819, A 3D Finite Difference Approach
title_sort are rock avalanches and landslides due to large earthquakes or local topographic effects? a case study of the lurøy earthquake of august 31, 1819, a 3d finite difference approach
publisher Springer Netherlands
publishDate 2008
url http://dx.doi.org/10.1007/978-1-4020-6815-7_18
http://link.springer.com/content/pdf/10.1007/978-1-4020-6815-7_18.pdf
long_lat ENVELOPE(12.849,12.849,66.418,66.418)
geographic Lurøy
geographic_facet Lurøy
genre Lurøy
genre_facet Lurøy
op_source NATO Science Series: IV: Earth and Environmental Sciences
Earthquake Monitoring and Seismic Hazard Mitigation in Balkan Countries
page 271-289
ISSN 1568-1238
ISBN 9781402068133 9781402068157
op_doi https://doi.org/10.1007/978-1-4020-6815-7_18
container_start_page 271
op_container_end_page 289
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