Chamoli disaster due to avalanche
- June 30, 2021
- Posted by: OptimizeIAS Team
- Category: DPN Topics
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Chamoli disaster due to avalanche
Subject : Geography
Context : The flash flood on February 7 in Chamoli district, Uttarakhand, that claimed at least 72 lives with at least 200 missing was due to a large mass of snow, ice and rock avalanche along with a hanging mass of rock crashing into the RaunthiGarh valley floor.
Concept :
Glacial Lake Outburst Flood (GLOF)
- A GLOF is a type of outburst flood that occurs when the dam containing a glacial lake fails.
- An event similar to a GLOF, where a body of water contained by a glacier melts or overflows the glacier, is called a jökulhlaup.
- The dam can consist of glacier ice or a terminal moraine.
- Failure can happen due to various factors such as:
Erosion, a buildup of water pressure
Avalanche of rock or heavy snow
Earthquake or volcanic eruptions under the ice or
Displacement of water in a glacial lake when a large portion of an adjacent glacier collapses into it.
Avalanche
- Avalanche is a rapid downslope movement of a large detached mass of snow, ice, and associated debris such as rocks and vegetation.
- Small avalanches, or Sluffs, occur in large numbers, while large avalanches that may encompass slopes a kilometer or more in length with millions of tons of snow, occur infrequently but cause most of the damage.
- Humans have been exposed to the threat of sliding snow for as long as they have inhabited mountainous regions.
Types of Avalanches:
- Loose snow avalanches-formed in snow with little internal cohesion among individual snow crystals.
- Slab avalanches-Originate in snow with sufficient internal cohesion to enable a snow layer, or layers, to react mechanically as a single entity.
- Wet snow avalanches-These move more slowly than dry ones and are seldom accompanied by dust clouds.
- Direct action avalanches –These are the immediate result of a single snowstorm. They usually involve only fresh snow.
- Climax avalanches-Result of a series of snowstorms or a culmination of weather influences. Their fall is not necessarily associated with a current storm or weather situation.