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Landslides are triggered by many extrinsic causative factors such as rainfall, earthquake, blasting and drilling, cloudburst, flash-floods (Anbalagan 1992).
The occurrence of landslides in mountainous regions is subjected to influence of different causative factors and are triggered by rainfall, earthquake shaking, water level change, storm waves and rapid stream erosion etc. [18, 46].
Temporal factors such as rainfall, earthquake, and temperature variations etc. has been considered in landslide hazard mapping studies (Guzzetti et al. 2006; Pradhan et al. 2010; Dahal et al. 2012).
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External environmental factors, such as rainfall, earthquakes and human activities, may all result in landslides.
Landslides can be triggered by different kinds of external stimuli, such as intense rainfall, earthquakes, and even some human activities.
The 27.14 m-long core contains alternating lithotypes that are sedimentary responses to lacustrine organic accumulation, normal to severe rainfalls, earthquakes and volcanism.
However, as far as we know, study about the effect of rainfall during earthquake is scarce in the literature due to the exceptionality of the combined event of rainfall and earthquake.
The extrinsic events like rainfall and earthquake trigger slope.
Historical data of rainfall and earthquake was taken by Muthu et al. [16] for landslide analysis.
Researches focusing on the effect of rainfall on earthquake induced landslides are scarcely found in literatures.
Figure 13 Histogram of specific volume ratio ( R sv ) during actual rainfall without earthquake.
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