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SIWALIK HILLS

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Originally appearing in Volume V25, Page 164 of the 1911 Encyclopedia Britannica.
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SIWALIK HILLS , a name given to the See also:

foot-hills of the Hima-Iayas in See also:Dehra Dun See also:district of the See also:United Provinces of See also:India and in Nahan See also:state and See also:Hoshiarpur district of the See also:Punjab. The range runs parallel with the Himalayan See also:system from See also:Hardwar on the See also:Ganges to the See also:banks of the See also:Beas, with a length of 200 M. and an See also:average width of 10 m. The See also:elevation varies from 2000 to 3500 ft. Geologically speaking the Siwaliks belong to the See also:tertiary deposits of the See also:outer Himalayas, and are chiefly composed of See also:low See also:sandstone and See also:conglomerate hills, the solidified and upheaved detritus of the See also:great range in their See also:rear The inter-mediate valley lying between the outer hills and the See also:Mussoorie mountains is known as the Dehra Dun (or Dehra valley) and contains a considerable See also:Eurasian See also:colony and some See also:British See also:tea-planters. The See also:principal pass is that of Mohan by which the See also:main road from See also:Saharanpur to Dehra and Mussoorie traverses the range. The Siwalik formation (distinguished for its extraordinary See also:wealth of palaeontological remains) is found on the See also:North-See also:West Frontier occupying much the same position relatively to the Suliman range as it does to the Himalayas, i.e. it faces the plains and becomes the outermost See also:wall of the hills.

End of Article: SIWALIK HILLS

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