Kinnaur situated in Trans Himalayan zone of Himalayas is a mountainous
district having high mountain ranges considered to be a sedimentary wedge
between colliding plate margins enclosing deep narrow valleys/gorges of River
Satluj and its numerous tributaries.
The district has unique climatic
conditions. Winters are severe with heavy snowfall causing Glaciers and
Avalanches. Summers are mild with rainy season in most of the Kapla and Nichar
Sub-Divisions of the district. Pooh Sub-Division of this district forms part of
‘Indian Cold Desert’ and receives
scanty rainfall as it falls in rain-shadow zone of Himalayas.
The unique Geo-tectonic, Geological, Geomorphologic and Climatic
conditions of the District makes it vulnerable/susceptible to various kinds of
natural hazards/disasters which have been compounded by increasing human
interventions with the nature. There is need to identify and delineate the
Hazard Risk zones of the District (areas vulnerable to various hazards) which
will provide the necessary information to work on micro-level and to map the
active and dormant processes of the hazards.
The disasters, which generally occur in this district and its various
areas prone/vulnerable to various kinds of disasters, are as under:
Hazard Type
|
Name of Sub-Division & Hazard
Vulnerability
|
Kalpa
|
Pooh
|
Nichar
|
Earthquakes
|
Moderate
|
Very High
|
Moderate
|
Floods
|
High
|
Very High
|
High
|
GLOFs
|
Moderate
|
Very High
|
Very High
|
Landslides
|
High
|
High
|
High
|
Forest Fires
|
High
|
Low
|
High
|
Domestic Fires
|
Moderate
|
Moderate
|
Moderate
|
Road Accidents
|
Moderate
|
Moderate
|
Moderate
|
Avalanches
|
Moderate
|
High
|
Low
|
Cloud Bursts
|
Low
|
-NA-
|
Moderate
|
Wind Storm
|
Moderate
|
High
|
Moderate
|
Drought
|
Moderate
|
High
|
Moderate
|
Fires are quite
frequent during the summers due to usage of inflammable material for house
construction and wood for fuel. Due to the dryness and absence of moisture
forests easily catch fire too. Floods are common during the rains. Cloud bursts
are short and devastating while heavy continuous rains flood low lying
habitations and saturate the strata leading to land slide and subsidence.
Flooded natural drainage channels cause heavy erosion. During the
dry season drought situations arise. Due to the mountainous terrain natural
sources dry up as groundwater level falls. District Kinnaur located on the
folds of the Himalayas lies in the earthquake Zone IV and is highly prone to
earthquakes.
Important/ Vulnerable Locations in District Kinnaur (Source:
GREF-2010)
|
S. No.
|
Name of
Spot
|
Type of
Trouble
|
1
|
Pangi Nallah
|
Landslide/Shooting Boulders
|
2
|
Umidhang area
|
Landslide/Shooting Boulders
|
3
|
Rally
|
Landslide/Shooting Boulders
|
4
|
Rally
|
Avalanche Point
|
5
|
Laldhang
|
Landslide/Shooting Boulders
|
6
|
Powari Slide
|
Landslide/Shooting Boulders
|
7
|
Powari Slide
|
Avalanche Point
|
8
|
Rehaldhang Area
|
Landslide/Shooting Boulders, Avalanche Point
|
9
|
Jangi
|
Avalanche Point
|
10
|
Spillow
|
Sinking Area
|
11
|
Nesang
|
Landslide Area
|
12
|
Bhagat Nallah
|
Avalanche Point
|
13
|
Tinku Nallah
|
Avalanche Point
|
14
|
Yangthang
|
Sinking Area
|
15
|
Malling Nallah
|
Sinking/ Landslide Area
|