Landslide Prone Areas is a key topic under Geography for UPSC Civil Services Examination. Key points include: Approximately 12.6% of India's land area (0.42 million sq. km) is prone to landslides, with the Himalayas and Western Ghats being most vulnerable.. Primary causes include gravitational forces, heavy rainfall, earthquakes, and hydrological factors like increased pore water pressure.. Anthropogenic activities (deforestation, unscientific construction) and climate change exacerbate landslide risk.. Understanding this topic is essential for both UPSC Prelims and Mains preparation.
Landslide Prone Areas is a Medium-level topic in UPSC Geography. It is tested in both Prelims (factual MCQs) and Mains (analytical answer writing). Previous year UPSC questions have frequently covered aspects of Landslide Prone Areas, making it essential for comprehensive IAS preparation.
To prepare Landslide Prone Areas for UPSC: (1) Study the comprehensive notes covering all key concepts on Vaidra. (2) Practice previous year questions on this topic. (3) Connect it with current affairs using daily updates. (4) Revise using key takeaways and mind maps available for Geography. (5) Write practice answers linking Landslide Prone Areas to related GS Paper topics.

Landslides are a significant geological hazard in India, affecting a substantial portion of its landmass. These events involve the movement of a mass of rock, debris, or earth down a slope.
India's diverse topography, coupled with specific geological and climatic conditions, makes it highly susceptible to landslides.
As per the Landslide Atlas of India, approximately 0.42 million sq. km, which accounts for about 12.6% of India's total land area, is identified as prone to landslides.
The vulnerability to landslides is not uniform across India but is concentrated in specific geographical belts. These regions are characterized by fragile geology, steep slopes, and intense weather patterns.
UPSC Insight: Remember the relative proportions and specific regions. Questions often ask about geographical distribution and causative factors. Mapping these regions in your mind can help in answer articulation for GS Paper I Geography.
The fundamental trigger for any landslide is the force of gravity. When the downward pull of gravity on a slope material exceeds the internal strength (shear strength) of that material, a landslide occurs.
Gravitational Forces: This is the overarching principle. When the inherent strength of materials like rocks, sand, silt, and clay is overcome by gravitational pull, the slope fails, leading to downhill movement.
Beyond gravity, several natural factors act as catalysts, reducing the stability of slopes and making them prone to failure.
Rainfall is a critical natural factor, especially in monsoon-dominated regions. Heavy or prolonged precipitation significantly alters the properties of slope materials.
Earthquakes are potent triggers, particularly in tectonically active zones like the Himalayas. Seismic vibrations can instantaneously destabilize slopes.
Earthquakes destabilize slopes by intense ground shaking, which weakens the integrity of geomaterials. This shaking can lead to liquefaction in saturated soils or cause fractures in rock masses, precipitating landslides.
Beyond direct rainfall, other hydrological processes contribute to slope instability. The movement and presence of water within the slope material are crucial.
Water seepage through porous materials within a slope increases the pore water pressure. This elevated pressure reduces the effective normal stress within the soil or rock, thereby significantly weakening the overall shear strength of the slope and making it susceptible to failure.


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