The landslide formed a Type VI landslide dam, with an estimated height of 25 m dam, and a lake length of 1.5 to 1.7 km (Lu et al. 1998).
Massive landslides formed this 10km (six-mile) coastal strip with its dense scrub, wild woodland and open ground.
Landslides forming natural dams across rivers have been described from a number of mountain environments [1 3].
Peat landslides form a distinct suite of slope failures that are characteristic of landscapes where organic soils dominate.
According to GIS analysis of the distribution of shallow landslides formed in Ichinomiya during the July 2012 heavy rainfall event, landslide frequency is greatest at slope angles between 30 and 40° (Geographical Survey and Photography, Japan 2012).
Paudel et al. (2003, 2008) and Miyabuchi et al. (2011) reported that the soils on the slopes consisted of different layers, and the slip surfaces of most landslides formed between upper blackish and lower brownish tephra layers.
This Kimmeridge Clay has resulted in a series of landslides, forming West Weares and East Weares.
Landslides formed due to the quake included 47 falls and topples, nine slides, and three lateral spreads.
At the next elections, in 1956, Bandaranaike won by a landslide and formed a leftwing coalition.
Consequently, the landslide immediately formed a dam.
Such interactions are responsible for "landslide-tectonized" forms and transformation of rock avalanches into debris flows.
