Differentiate the causes of landslides in the Himalayan region and Western Ghats. (UPSC 2021, 10 Marks, )

Himalayan क्षेत्र और पश्चिमी घाट में भूस्खलन के कारणों में अंतर करें।

Introduction

Landslides are geological hazards that pose a significant threat to various regions globally. The Himalayas and the Western Ghats, both prominent mountain ranges in India, exhibit different frequencies of landslide occurrences. However, landslides are more frequent in the Himalayas as compared to the Western Ghats.

Explanation

Causes of Landslides in the Himalayan region vs the Western Ghats

Aspect

Himalayan Region

Western Ghats

Geological Characteristics

Young and actively rising mountains

Older, more stable geological features

Tectonic Activity

High seismicity and ongoing tectonic processes

Lower seismic activity, more stable tectonics

Main Triggering Factors

Tectonic activity, seismic events

Intense rainfall, tropical cyclones

Lithology

Loose and fragmented rocks

Weathered and less consolidated rocks. Varied lithology with more resistant rocks.

Slope Gradient

Steeper slopes in many areas

Generally gentler slopes

Glacial Activities

Glacial activities contributing to instability 

Absence of glacial activities

Vegetation Cover

Sparse vegetation at higher altitudes

Dense and diverse vegetation cover

Human Activities

Deforestation, road construction

Agriculture, urbanization

Land Use Patterns

Limited agriculture at high altitudes

Extensive agriculture and settlements

Previous History of Landslides

History of catastrophic landslides

Frequent but generally smaller events

Risk and Vulnerability

High risk due to rapid terrain changes

Moderate risk, but localized impact

Preventive Measures

Structural interventions, early warning systems

Afforestation, land-use planning

Conclusion

The frequency of landslides in the Himalayas is influenced by a combination of tectonic, geological, and environmental factors. The Western Ghats, with their older geological formations and less dynamic geological processes, experience fewer landslides.

Understanding these distinctions is crucial for implementing effective mitigation strategies in both regions, considering the potential consequences on human settlements and the environment.