Table of Contents
ToggleLandslides are the downward movement of rock, soil, and debris down a slope under the direct influence of gravity
It is a major disaster in hilly and mountainous regions. Landslides often occur due to heavy rainfall, earthquakes, slope instability, deforestation, road construction, mining and unplanned development in fragile regions.
In India, landslides are common in the Himalayan region, North-East India, Western Ghats, Eastern Ghats and some parts of the Nilgiris. They cause loss of life, damage to roads, houses, bridges, hydropower projects, forests and agricultural land.
The Indian subcontinent, with diverse physiographic, seismic, tectonic and climatological conditions is subjected to varying degree of landslide hazards; the Himalayas including Northeastern mountains ranges being the worst affected, followed by a section of Western Ghats and the Vindhyas.
Removal of vegetation and toe erosion have also triggered slides.
Torrential rainfall on the deforested slopes is the main factor in Peninsular India namely in Western Ghat and Nilgiris. Human intervention by way of slope modification has added to this effect
Structural Measures
Non-Structural Measures

Landslides are a serious disaster risk in India’s hilly and mountainous regions. Their impact is increasing due to climate change, unplanned development, deforestation and fragile geology. Effective landslide management requires a shift from post-disaster relief to risk reduction through hazard mapping, slope stabilisation, safe construction, ecological protection, early warning and community preparedness.
Q1. Discuss the structural and non-structural measures for landslide risk reduction.
(250 words, 15 marks)
Q2. Unplanned development in hill areas has increased landslide vulnerability in India. Analyse.
(250 words, 15 marks)
Q3. Explain the significance of landslide hazard zonation mapping in disaster risk reduction.
(150 words, 10 marks)
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