LANDSLIDES TRIGGERED BY THE 2015 GORKHA, NEPAL EARTHQUAKE

The 25 April 2015 Gorkha Mw 7.8 earthquake in central Nepal caused a large number of casualties and serious property losses, and also induced numerous landslides. Based on visual interpretation of high-resolution optical satellite images pre- and post-earthquake and field reconnaissance, we delineat...

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Main Author: C. Xu
Format: Article
Language:English
Published: Copernicus Publications 2018-04-01
Series:The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences
Online Access:https://www.int-arch-photogramm-remote-sens-spatial-inf-sci.net/XLII-3/1989/2018/isprs-archives-XLII-3-1989-2018.pdf
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spelling doaj-4b6c6565eddd4862851429862187d7412020-11-25T01:45:11ZengCopernicus PublicationsThe International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences1682-17502194-90342018-04-01XLII-31989199310.5194/isprs-archives-XLII-3-1989-2018LANDSLIDES TRIGGERED BY THE 2015 GORKHA, NEPAL EARTHQUAKEC. Xu0Institute of Geology, China Earthquake Administration, ChinaThe 25 April 2015 Gorkha Mw 7.8 earthquake in central Nepal caused a large number of casualties and serious property losses, and also induced numerous landslides. Based on visual interpretation of high-resolution optical satellite images pre- and post-earthquake and field reconnaissance, we delineated 47,200 coseismic landslides with a total distribution extent more than 35,000&thinsp;km<sup>2</sup>, which occupy a total area about 110&thinsp;km<sup>2</sup>. On the basis of a scale relationship between landslide area (A) and volume (V), V = 1.3147&thinsp;&times;&thinsp;A<sup>1.2085</sup>, the total volume of the coseismic landslides is estimated to be about 9.64&thinsp;&times;&thinsp;10<sup>8</sup>&thinsp;m<sup>3</sup>. Calculation yields that the landslide number density, area density, and volume density are 1.32&thinsp;km<sup>&minus;2</sup>, 0.31&thinsp;%, and 0.027&thinsp;m, respectively. The spatial distribution of these landslides is consistent with that of the mainshock and aftershocks and the inferred causative fault, indicating the effect of the earthquake energy release on the pattern on coseismic landslides. This study provides a new, more detailed and objective inventory of the landslides triggered by the Gorkha earthquake, which would be significant for further study of genesis of coseismic landslides, hazard assessment and the long-term impact of the slope failure on the geological environment in the earthquake-scarred region.https://www.int-arch-photogramm-remote-sens-spatial-inf-sci.net/XLII-3/1989/2018/isprs-archives-XLII-3-1989-2018.pdf
collection DOAJ
language English
format Article
sources DOAJ
author C. Xu
spellingShingle C. Xu
LANDSLIDES TRIGGERED BY THE 2015 GORKHA, NEPAL EARTHQUAKE
The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences
author_facet C. Xu
author_sort C. Xu
title LANDSLIDES TRIGGERED BY THE 2015 GORKHA, NEPAL EARTHQUAKE
title_short LANDSLIDES TRIGGERED BY THE 2015 GORKHA, NEPAL EARTHQUAKE
title_full LANDSLIDES TRIGGERED BY THE 2015 GORKHA, NEPAL EARTHQUAKE
title_fullStr LANDSLIDES TRIGGERED BY THE 2015 GORKHA, NEPAL EARTHQUAKE
title_full_unstemmed LANDSLIDES TRIGGERED BY THE 2015 GORKHA, NEPAL EARTHQUAKE
title_sort landslides triggered by the 2015 gorkha, nepal earthquake
publisher Copernicus Publications
series The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences
issn 1682-1750
2194-9034
publishDate 2018-04-01
description The 25 April 2015 Gorkha Mw 7.8 earthquake in central Nepal caused a large number of casualties and serious property losses, and also induced numerous landslides. Based on visual interpretation of high-resolution optical satellite images pre- and post-earthquake and field reconnaissance, we delineated 47,200 coseismic landslides with a total distribution extent more than 35,000&thinsp;km<sup>2</sup>, which occupy a total area about 110&thinsp;km<sup>2</sup>. On the basis of a scale relationship between landslide area (A) and volume (V), V = 1.3147&thinsp;&times;&thinsp;A<sup>1.2085</sup>, the total volume of the coseismic landslides is estimated to be about 9.64&thinsp;&times;&thinsp;10<sup>8</sup>&thinsp;m<sup>3</sup>. Calculation yields that the landslide number density, area density, and volume density are 1.32&thinsp;km<sup>&minus;2</sup>, 0.31&thinsp;%, and 0.027&thinsp;m, respectively. The spatial distribution of these landslides is consistent with that of the mainshock and aftershocks and the inferred causative fault, indicating the effect of the earthquake energy release on the pattern on coseismic landslides. This study provides a new, more detailed and objective inventory of the landslides triggered by the Gorkha earthquake, which would be significant for further study of genesis of coseismic landslides, hazard assessment and the long-term impact of the slope failure on the geological environment in the earthquake-scarred region.
url https://www.int-arch-photogramm-remote-sens-spatial-inf-sci.net/XLII-3/1989/2018/isprs-archives-XLII-3-1989-2018.pdf
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