2020
DOI: 10.1007/s10346-019-01339-9
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The effect of topography on landslide kinematics: a case study of the Jichang town landslide in Guizhou, China

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Cited by 59 publications
(21 citation statements)
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“…A large earthquake (magnitude > 6) can trigger landslides of shallow soil, as well as large, deep rock landslides [51]. A landslide's initiation is controlled by different failure mechanisms associated with material types, topography, and geotechnical features [52][53][54]. Landslides in bedrock are especially strongly influenced by their structure and preaccumulated failure, which consequently result in complex failure mechanisms compared with soil landslides [55].…”
Section: Performance Of Rock Landslide Predictionmentioning
confidence: 99%
“…A large earthquake (magnitude > 6) can trigger landslides of shallow soil, as well as large, deep rock landslides [51]. A landslide's initiation is controlled by different failure mechanisms associated with material types, topography, and geotechnical features [52][53][54]. Landslides in bedrock are especially strongly influenced by their structure and preaccumulated failure, which consequently result in complex failure mechanisms compared with soil landslides [55].…”
Section: Performance Of Rock Landslide Predictionmentioning
confidence: 99%
“…e upper part of the Shuicheng landslide was steep with an average dip angle of 28°, while the lower part was slightly gentler with an average dip angle of 10°. ere were multiple gentle slopes and terraces in the trailing edge and central area of the landslide, which conducted to the collection of rainwater [38]. In addition, the narrow gullies on both sides of the landslide formed a favorable circulation channel for the sliding body.…”
Section: Topography and Landformmentioning
confidence: 99%
“…e study area is located in the middle of the Weining northwest trending structure deformation zone in the Liupanshui fault depression of the Yangtze platform [38]. e exposed strata mainly include the Carboniferous (C), Permian (P), and Triassic (T).…”
Section: Geological Conditionsmentioning
confidence: 99%
“…In addition, soil movement can also be caused by human activities, such as water extraction, mining activities, cutting slopes for road construction, and others (Bateson et al, 2015;Hearn et al, 2020;Persichillo et al, 2017). In addition, ground movements due to landslides can cause topographic changes (Dehghani & Javadi, 2013;Guo et al, 2020). Therefore, monitoring and mapping ground movements such as landslides are necessary to minimize the risk of landslides and other ground movements (Crosetto et al, 2018;Skrzypczak et al, 2021).…”
Section: Introductionmentioning
confidence: 99%