IMHE OpenIR  > Journal of Mountain Science  > Journal of Mountain Science-2007  > Vol4 No.3
Enveloping relief surfaces of landslide terrain
Pachauri, A. K.; Chatterjee, Abhirup; Gaur, Reeta
Corresponding AuthorPachauri, AK
2007-09
Source PublicationJOURNAL OF MOUNTAIN SCIENCE
ISSN1672-6316
Volume4Issue:3Pages:203–208
AbstractTwo relief surfaces that envelop the rock fall region in a part of Garhwal Himalayas around Chamoli have been identified. Relative relief and absolute relief have been analyzed and the enveloping surfaces recorded at two levels of relief in the landscape. All landslide activity lies within these surfaces. The lower enveloping surface (800 m) dips due south by 7-8 degrees, due to an elevation rise of loo meters within 12 km from south to north, i.e., a gradient of 8 percent. The nature of the surface is smooth. The upper enveloping surface (> 2500 m) is almost parallel to the lower one but its surface is undulatory due to landslides and denudation. The area has been a seismically active region and has undergone seismic activity up until recently, as evidenced by the Chamoli earthquake Of 29(th) March 1999. The effects of earthquakes are seen at higher levels in the form of landslide imprints on the terrain.
KeywordRelief Landslide Terrain Himalayas
Language英语
Document Type期刊论文
Identifierhttp://ir.imde.ac.cn/handle/131551/6081
CollectionJournal of Mountain Science_Journal of Mountain Science-2007_Vol4 No.3
Recommended Citation
GB/T 7714
Pachauri, A. K.,Chatterjee, Abhirup,Gaur, Reeta. Enveloping relief surfaces of landslide terrain[J]. JOURNAL OF MOUNTAIN SCIENCE,2007,4(3):203–208.
APA Pachauri, A. K.,Chatterjee, Abhirup,&Gaur, Reeta.(2007).Enveloping relief surfaces of landslide terrain.JOURNAL OF MOUNTAIN SCIENCE,4(3),203–208.
MLA Pachauri, A. K.,et al."Enveloping relief surfaces of landslide terrain".JOURNAL OF MOUNTAIN SCIENCE 4.3(2007):203–208.
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