UPSC MainsGeneral Studies Paper IGeographyPractice question

Vulnerability of Himalayan Ecology to Disasters

Recent instances of extreme monsoon precipitation and subsequent landslides in the Himalayan region highlight the growing vulnerability of its fragile ecology. Evaluate the geographical factors contributing to these disasters and discuss their impact on local human settlements.

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How to approach

Begin by contextualizing the acute vulnerability of the Himalayan region with recent instances of intense precipitation and landslides. Evaluate the primary geological, geomorphological, and climatological factors driving slope failure and disaster vulnerability. Then, discuss the multidimensional impact on local settlements, including infrastructure, livelihoods, and displacement, concluding with sustainable and eco-sensitive mitigation pathways.

Model answer

285 words

Introduction

Recent events such as widespread highway washouts in Himachal Pradesh and flash floods in Uttarakhand underscore the acute vulnerability of the Himalayan ecosystem to extreme monsoonal precipitation. The region's inherent fragility, exacerbated by changing precipitation dynamics and rapid development, turns high-intensity rainfall events into catastrophic mass-wasting disasters.

Geographical Factors Contributing to Disasters

  • Tectonic Instability: The ongoing collision of the Indian and Eurasian plates creates active and volatile fault zones, notably the Main Central Thrust (MCT) and Main Boundary Thrust (MBT), resulting in heavily sheared, fractured, and seismically weak rock strata.
  • Geomorphological Features: Steep slope gradients paired with deep vertical incision by antecedent rivers like the Sutlej and Teesta severely reduce the shear strength of mountain slopes, leaving loose surface materials prone to gravitational failure.
  • Climatological Dynamics: Orographic uplift of moisture-laden monsoonal winds triggers concentrated, localized cloudbursts. Rapid percolation of torrential rain into unconsolidated regolith causes a sharp rise in pore-water pressure, precipitating sudden, massive debris flows and mudslides.

Impact on Local Human Settlements

  • Infrastructure Failure and Subsidence: Indiscriminate vertical hill-cutting for road widening and unscientific construction around fragile slopes induce slope instability and ground subsidence, as witnessed in Joshimath, cutting off vital connectivity lifelines.
  • Economic Devastation: Debris flows and flash floods obliterate terraced agricultural land, wash away livestock, and disrupt pilgrimage and tourism corridors, severely destabilizing mountain economies.
  • Social and Psychological Toll: Frequent disasters trigger distress out-migration from vulnerable hamlets and impose a heavy psychological toll on isolated communities living under the constant threat of slope collapses and river blockades.

Conclusion

To build climate-resilient Himalayan habitats, policy must pivot toward carrying-capacity-based regional planning, strict enforcement of eco-sensitive zoning, and the adoption of bio-engineering techniques for slope stabilization as outlined in the National Disaster Management Authority guidelines.

Key facts to remember

definition
Pore-Water Pressure

The pressure of groundwater held within the gaps between soil or rock particles. During extreme rainfall, a sharp increase in pore-water pressure reduces the effective stress and shear strength of slope materials, triggering sudden landslides.

case study
Joshimath Land Subsidence

Joshimath, Uttarakhand, experienced severe land subsidence and structural fissures caused by unscientific slope modification, overburden on glacial moraine deposits, and inadequate drainage networks under heavy seepage conditions.

scheme
NDMA Guidelines on Landslide Management (2009)

Framework providing policy directions for hazard zonation mapping, early warning systems, slope stabilization through bio-engineering, and regulation of developmental projects in hilly terrains.

Frequently asked questions

Why are the Himalayas more susceptible to landslides than the Western Ghats?

Unlike the geologically stable, denuded peninsular rocks of the Western Ghats, the Himalayas are young fold mountains characterized by ongoing tectonic activity, fractured rock strata, steeper slope angles, and high seismic vulnerability.