Kishtwar National Park
The National Park encompasses the catchments of Kiar, Nath and Kibar
Nalas, all of which drain south-west into Marwa River which joins the
Chenab River just above Kishtwar Town. The terrain is generally rugged
and steep, with narrow valleys bounded by high ridges opening in their
upper glacial parts. The area lies in the Central Crystalline belt of
the Great Himalayas. Rocks are strongly folded in places and composed
mainly of granite, gneiss and schist, with the occasional bed of marble.
The shallow, slightly alkaline soils are mostly alluvial with gravel
deposits (Kurt,1976;Bacha, 1986).There are permanent settlements but some 1,115 families of nomadic
graziers, with 25,000 head of livestock, and an unspecified number of
families from nearby villages, with 10,000 head, have grazing rights in
the national park. Some agriculture is practised in peripheral areas.
(Bacha, 1986).

The influence of the monsoon is weak. Mean annual rainfall at palmar and Sirshi (1,761 m), located near the periphery of the national park, is 827 mm and 741 mm, respectively, precipitation is maximal and in excess of 100 mm per month in March and April, and again in July and August.Most snow fall in December and January when the whole area becomes snowbound. Mean maximum and minimum temperatures recorded at Sirshi are 130 and -70 in January and 350c and 110c in July respectively (Kurt, 1976;Bacha,1986).
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