Why landslide can destroy the houses and block down the road
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Landslides occur when the slope (or a portion of it) undergoes some processes that change its condition from stable to unstable. This is essentially due to a decrease in the shear strength of the slope material, to an increase in the shear stress borne by the material, or to a combination of the two. A change in the stability of a slope can be caused by a number of factors, acting together or alone. Natural causes of landslides include:
saturation by rain water infiltration, snow melting, or glaciers melting;
rising of groundwater or increase of pore water pressure (e.g. due to aquifer recharge in rainy seasons, or by rain water infiltration);[2]
increase of hydrostatic pressure in cracks and fractures;[2][3]
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