UPSC MainsGEOLOGY-PAPER-II201415 Marks
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Q31.

What do you understand by Landslides? Discuss briefly various types of landslides. Comment upon causes and remedial measures of landslides.

How to Approach

This question requires a multi-faceted answer. Begin by defining landslides and establishing their geological context. Then, systematically categorize different landslide types based on material, movement, and velocity. The core of the answer should focus on the causes – both natural and anthropogenic – and subsequently, detail various remedial measures, categorizing them into preventive and curative approaches. A structured approach using headings and subheadings will enhance clarity. Include examples to illustrate the concepts.

Model Answer

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Introduction

Landslides, also known as mass wasting, represent the downslope movement of soil, rock, and debris under the influence of gravity. They are a significant geological hazard, particularly in mountainous regions, causing substantial economic losses, environmental damage, and loss of life. Recent events like the 2023 Joshimath land subsidence and frequent landslides during the monsoon season in the Himalayan region highlight the increasing vulnerability and the urgent need for understanding and mitigating this hazard. This answer will delve into the definition, types, causes, and remedial measures associated with landslides.

Understanding Landslides

A landslide is defined as the movement of a mass of rock, earth, or debris down a slope. This movement can occur rapidly or slowly, and can be triggered by a variety of factors. The stability of a slope is determined by a balance between the driving forces (gravity) and the resisting forces (shear strength of the material). When the driving forces exceed the resisting forces, a landslide occurs.

Types of Landslides

Landslides are classified based on several criteria, including the type of material involved, the type of movement, and the velocity of movement. Here’s a breakdown of common types:

  • Based on Material:
    • Rockslides: Involve the rapid movement of rocky material.
    • Debris Slides: Composed of a mixture of soil, rock, and vegetation.
    • Earthflows: Slow, viscous flows of fine-grained materials.
    • Mudflows: Rapid flows of water-saturated earth and debris.
  • Based on Type of Movement:
    • Falls: Free fall of rock or debris from a steep slope.
    • Topples: Forward rotation of a mass of rock or soil about a pivot point.
    • Slides: Movement of a mass of material along a defined shear surface. (Rotational and Translational)
    • Spreads: Lateral extension and fracturing of a cohesive mass.
    • Flows: Viscous movement of saturated material.
  • Based on Velocity:
    • Slow Creep: Extremely slow, almost imperceptible movement.
    • Moderate Landslides: Noticeable movement, but not catastrophic.
    • Rapid/Very Rapid Landslides: Extremely fast movement, often catastrophic.

Causes of Landslides

Landslides are rarely caused by a single factor; they are usually the result of a combination of predisposing conditions, triggering events, and amplifying factors.

Natural Causes

  • Geological Factors: Weak or fractured rock formations, unfavorable bedding planes, and the presence of clay layers.
  • Morphological Factors: Steep slopes, narrow valleys, and the removal of vegetation.
  • Hydrological Factors: Intense rainfall, snowmelt, and groundwater saturation.
  • Seismic Activity: Earthquakes can trigger landslides, especially in unstable slopes.

Anthropogenic Causes

  • Deforestation: Removal of vegetation reduces slope stability.
  • Road Construction: Cutting into slopes can destabilize them.
  • Mining Activities: Excavation and blasting can weaken slopes.
  • Urbanization: Increased weight on slopes from buildings and infrastructure.
  • Improper Drainage: Poorly designed drainage systems can lead to water saturation.

Remedial Measures for Landslides

Remedial measures can be broadly categorized into preventive and curative approaches.

Preventive Measures

  • Afforestation: Planting trees and vegetation to stabilize slopes.
  • Retaining Walls: Constructing walls to support slopes.
  • Drainage Control: Implementing effective drainage systems to reduce water saturation.
  • Slope Grading: Reducing the slope angle to increase stability.
  • Terracing: Creating a series of level platforms to reduce slope length.
  • Avoiding Construction on Unstable Slopes: Careful site selection and land-use planning.

Curative Measures

  • Surface Drainage Control: Diverting surface runoff away from the landslide area.
  • Subsurface Drainage: Installing drainage systems to lower the groundwater table.
  • Rock Bolting: Anchoring unstable rock masses to stable ground.
  • Shotcrete: Applying a layer of concrete to the slope surface.
  • Grouting: Injecting cement or chemical mixtures into the ground to improve its strength.
  • Landslide Monitoring: Using sensors and remote sensing techniques to detect early signs of movement.

Conclusion

Landslides pose a significant threat to life and property, particularly in mountainous regions. Understanding the types, causes, and remedial measures is crucial for effective mitigation. A holistic approach combining preventive measures like afforestation and sustainable land-use planning with curative techniques like drainage control and slope stabilization is essential. Continuous monitoring and early warning systems are also vital for minimizing the impact of these devastating natural disasters. Further research and investment in landslide hazard zonation and risk assessment are needed to build resilient communities.

Answer Length

This is a comprehensive model answer for learning purposes and may exceed the word limit. In the exam, always adhere to the prescribed word count.

Additional Resources

Key Definitions

Shear Strength
The internal resistance of a material to deformation or failure due to stress. It is a crucial factor in determining slope stability.
Land Subsidence
The sinking or settling of land surface due to various factors, including groundwater extraction, mining, and natural consolidation of sediments. It can often precede or accompany landslides.

Key Statistics

According to the National Disaster Management Authority (NDMA), approximately 15% of India’s land area is prone to landslides. (Data as of 2021)

Source: NDMA Report on Landslides

The Himalayan region experiences approximately 15% of all landslides in India, despite covering only 4.3% of the country’s land area. (Based on knowledge cutoff 2023)

Source: Geological Survey of India (GSI) reports

Examples

Malin Landslide (2014)

The Malin landslide in Maharashtra in 2014, which claimed over 150 lives, was triggered by heavy rainfall and exacerbated by deforestation and improper land-use practices. It highlighted the vulnerability of settlements in landslide-prone areas.

Frequently Asked Questions

What is landslide hazard zonation?

Landslide hazard zonation is a process of mapping areas based on their susceptibility to landslides. It involves identifying factors that contribute to landslide occurrence and assessing the probability of landslides in different areas. This information is used for land-use planning and disaster mitigation.

Topics Covered

GeologyEnvironmental GeologyGeomorphologyLandslides, Slope Stability, Hazards, Mitigation