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364
GUJRĀT DLSTRICT
and Siālkot. The northern corner is crossed by the Pabbi Hills, a low
range, pierced by the Jhelum at Mong Rāsul, which forms a con
tinuation of the Salt Range. These hills consist o
Physical
aspects. a friable Tertiary sandstone and conglomerate, pre-
senting a chaos of rock, naked or clothed with roug
scrub, and deeply scored with precipitous ravines. Their highest poin
has an elevation of 1,400 feet above sea-level, or about 6oo feet abov
the surrounding plain. Immediately below and surrounding these hills,
a high and undulating submontane plateau extends across the north
of the District from the Jhelum eastwards, till it terminates in a pre
cipitous bank 100 to Zoo feet in height, which almost overhangs th
waters of the Taw! and Chenāb. At the foot of the plateau a bel
of upland crosses the District, ending in a high bank, beneath which
lies a strip of lowland about 8 miles in width, which forms the wide
valley of the Chenāb. A similar narrow belt of lowland fringes th
Jhelum. The surface of the doāb thus descends in a series of step
towards the south and west, and a section of the line along the gran
trunk road shows a rise of 111 feet from the Chenāb to the Jhelu
in a distance of 34 miles. Besides the great boundary rivers, th
Jhelum and Chenāb, the District is intersected by numerous hil
torrents rising in the Outer Himalayas or the Pabb! Hills, the chie
being the Bhimbar, Bhandar, Dalli, Dabnli, Doara, and Bakal. Mos
of these streams, although unmanageable torrents in the rains, eithe
dry up entirely during the dry season, or find their way into the Chenā
by insignificant channels.
The greater part of the District lies on the Indo-Gangetic alluvium
but beds of Siwalik (Upper Tertiary) age are found in the Pabb! o
Kharian Hills, which are composed of an enormous accumulatio
of sandstones, sands, conglomerates, and clays. The sandstones a
highly fossiliferous, and have yielded great numbers of mammalia
bones and teeth, including species of EQuus, Bos, Elephas, an
Cervus.
None of the submontane Districts, except Sialkot, has a scantie
flora than Gujrāt, but the low Pabb! range supports a few stunte
trees and shrubs of kinds abundant in the neighbouring Salt Rang
and dry Outer Himalaya. In the broken country at the north-cas
corner, and on the bank of the Chenab farther to the south, ther
is a good deal of scrub, chiefly Acacia modesta and reed jungle. Th
dhāk (Butea frondosa) is fairly common, while the kikar (Acaci~
arabica) and horse-radish-tree (Moringa pteryg-osperma) occur also, th
first being fully naturalized in the northern part.
Wolves are found in the Pabbi Hills and hyenas are occasional)
met with ; nilgai and antelope are rare, but `ravine deer' (India
gazelle) are not at all uncommon on the hills. Wild hog are numerou
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