When landslides occur on the slopes of a river valley, the sliding mass may reach the bottom of the valley and cause partial or complete blockage of the river channel. This accumulated mass of landslide debris resulting in the blockage of a river is commonly termed as a Landslide dam.
1. Falls: It happens due to the abrupt movements of masses of geologic materials, such as rocks and boulders that become detached from steep slopes or cliffs.
2. Topples: It happens due to the forward rotation of a unit or units about some pivotal point, below or low in the unit, under the actions of gravity and forces exerted by adjacent units or by fluids in cracks
3. Slides: In this types, rocks, debris or soil slide through slope forming material.
4. Spread: It usually occur on very gentle slopes or flat terrain.
The major causes of landslides are –
1. Rainfall and Snowfall-
2. Earthquakes and Volcanic Eruptions-
3. Mining, Quarrying and Road cutting-
4. Loading by construction of houses-
5. Deforestation-
In India, this hazard affects at least 15% of the land area of the country ( approx 0.49 million square Km.) It is very frequent in geodynamical active domains in the Himalayan and Arakan- Yoma belt of the Northeastern parts of the country as well as in the relatively stable domains of the Meghalaya Plateau, Western Ghats, and Nilgiri Hills.
The Nilgiri Hills located at the convergence of Eastern and the Western Ghats bear the innumerable scars of the landslides due to their location in a zone of high intensity and protracted rainfall where the overburden is sensitive to over-saturation.
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