See also:SIRMUR, or SARMOR (also called NAHAN, after the See also:chief See also:town)
, a native See also:state of See also:India, within the See also:Punjab
.
It occupies the See also:lower ranges of the See also:Himalaya, between See also:Simla and See also:Mussoorie
.
See also:Area 1198 sq. m
.
The state is bounded on the N. by the See also:- HILL
- HILL (0. Eng. hyll; cf. Low Ger. hull, Mid. Dutch hul, allied to Lat. celsus, high, collis, hill, &c.)
- HILL, A
- HILL, AARON (1685-175o)
- HILL, AMBROSE POWELL
- HILL, DANIEL HARVEY (1821-1889)
- HILL, DAVID BENNETT (1843–1910)
- HILL, GEORGE BIRKBECK NORMAN (1835-1903)
- HILL, JAMES J
- HILL, JOHN (c. 1716-1775)
- HILL, MATTHEW DAVENPORT (1792-1872)
- HILL, OCTAVIA (1838– )
- HILL, ROWLAND (1744–1833)
- HILL, SIR ROWLAND (1795-1879)
hill states of Balsan and Jubbal, on the E. by the See also:British See also:district of See also:Dehra Dun, from which it is separated by the See also:rivers Tons and See also:Jumna, on the S.W. by See also:Umballa district, and on the N.W. by the states of See also:Patiala and See also:Keonthal
.
Except a very small See also:tract about Nahan, the See also:chief See also:town and See also:residence of the See also:raja, on the See also:south-western extremity, where a few streams rise and flow south-westward to the Saraswati and Ghaggar rivers, the whole of See also:Sirmur lies in the See also:basin of the Jumna, which receives from this tract the Giri and its feeders the Jalal and the Palur
.
The Tons, the See also:great western See also:arm of the stream called lower down the Jumna, flows along the eastern boundary of Sirmur, and on the right See also:side receives from it the two small streams Minus and Nairai
.
The See also:surface generally declines in See also:elevation from See also:north to south; the chief elevations on the See also:northern frontier (Chor See also:peak and station) are about 12,000 ft. above the See also:sea
.
The valley of the Khiarda Dun, which forms the See also:southern See also:part of the state, is bounded on the S. by the Siwalik range, the hills of which are of See also:recent formation and abound in fossil remains of large vertebrate animals
.
Though the rocks of Sirmur consist of formations usually metalliferous, the yield of See also:mineral See also:wealth is small
.
The forests are very dense, so much so that the sportsman finds difficulty in making his way through them in See also:search of See also:deer and
See also:Sirsa was part of the territory conquered from the See also:Mahrattas 1 from the leaves
.
The leaves are put into the See also:machine at one side
in 1803, when it was almost entirely uninhabited
.
It required reconquering from the Bhattis in 1818; but it did not come under British See also:administration until 1837
.
During the See also:Mutiny of 1857 Sirsa was for a See also:- TIME (0. Eng. Lima, cf. Icel. timi, Swed. timme, hour, Dan. time; from the root also seen in " tide," properly the time of between the flow and ebb of the sea, cf. O. Eng. getidan, to happen, " even-tide," &c.; it is not directly related to Lat. tempus)
- TIME, MEASUREMENT OF
- TIME, STANDARD
time wholly lost to British See also:rule
.
On the restoration of See also:- ORDER
- ORDER (through Fr. ordre, for earlier ordene, from Lat. ordo, ordinis, rank, service, arrangement; the ultimate source is generally taken to be the root seen in Lat. oriri, rise, arise, begin; cf. " origin ")
- ORDER, HOLY
order the district was administered by Punjab officials, and in the following See also:year, with the See also:remainder of the See also:Delhi territory, it was formally annexed to that See also:province
.
In 1884 it was sub-divided between the districts of See also:Hissar and See also:Ferozepur
.
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