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.