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Osini is an old rural village that was abandoned in 1951 because of a severe landslide.
Formerly in pasture, this area sustained severe landslide damage during Cyclone Bola in March 1988.
Therefore, slope dimension optimization and stabilization are required on the tailing dumps at Enyigba to prevent severe landslide occurrence.
The study area experienced frequent severe landslide events triggered by heavy rainfalls in July 1990, June 2001, and July 2012 (Miyabuchi and Daimaru 2004; Saito et al. 2016).
The study area has frequently experienced severe landslide events triggered by heavy rainfalls in the past three decades (Miyabuchi and Daimaru 2004; Saito et al. 2016).
The results indicated that rock fragment content, soil pH value, bulk density, inorganic carbon, and base saturation increased following landslide deposition and that severe landslide deposition caused more substantial increases.
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Whole villages disappeared as a result of such severe landslides (Shahrivar and Nadim 2005).
Satellite images and aerial-photography following the Wenchuan earthquake show that a broad area experienced severe landsliding in association with the main earthquake and aftershocks.
While severe landslides have occurred recently (in Vaima and Marae in 2010, many villages in 2015), they are not that frequent On an island with three large dormant volcanic mountains, landslides are common and communities understand the risk.
The width of this severe landsliding zone varies along the strike, from ~ 25 30 km wide in the southwestern section of the earthquake region, to ~ 3 5 in the northeastern section.
Many of the existing main roads (expressways, national highways and prefectural roads) were cleared, and then repaired immediately after the earthquake-tsunami damage, with a few exceptions that were damaged by severe landslides caused by the quake or the fall of bridges caused by the tsunami.
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