Quetta-Pishin
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==History== | ==History== | ||
In former times Pishm was known as Fushanj and Pashang. The | In former times Pishm was known as Fushanj and Pashang. The | ||
− | ancient name of Quetta was Shal, a term by | + | ancient name of Quetta was Shal, a term by which it is still known |
among the people of the country, and which Rawhn- | among the people of the country, and which Rawhn- | ||
son traces back to the tenth century. The District | son traces back to the tenth century. The District | ||
was held in turns by the Ghazmvids, Ghonds, and Mongols, and | was held in turns by the Ghazmvids, Ghonds, and Mongols, and | ||
towards the end of the fifteenth century was conferred by the ruler | towards the end of the fifteenth century was conferred by the ruler | ||
− | of Herat on Shah Beg Arghun, who, | + | of Herat on Shah Beg Arghun, who, however, had shortly to give |
way before the using power of the Mughals. The Aiti-i-Akbarl | way before the using power of the Mughals. The Aiti-i-Akbarl | ||
mentions both Shal and Pishm as supplying military service and | mentions both Shal and Pishm as supplying military service and | ||
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More than 84 per cent of the people are Muhammadans of the | More than 84 per cent of the people are Muhammadans of the |
Revision as of 19:38, 28 May 2014
This article has been extracted from THE IMPERIAL GAZETTEER OF INDIA , 1908. OXFORD, AT THE CLARENDON PRESS. |
Note: National, provincial and district boundaries have changed considerably since 1908. Typically, old states, ‘divisions’ and districts have been broken into smaller units, and many tahsils upgraded to districts. Some units have since been renamed. Therefore, this article is being posted mainly for its historical value.
Contents |
Quetta-Pishin
A highland District of Baluchistan, lying be- tween 29 52' and 31 18' N. and 66 15' and 67 48' E , with an area of 5,127 square miles. It is bounded on the noith and west by Afghanistan , on the east by Zhob and Sibi Districts , and on the south by the Bolan Pass and the Mastung nidbat of the Kalat State.
Physical aspects
The District consists of a series of valleys of con- i=iderable length but medium width, forming the catchment area of the Pishm Lora, and enclosed on all sides by the mountains of the TOBA-KAKAR and CENTRAL BRAHUI ranges The valleys vaiy in elevation from 4,500 to 5,500 feet, and the mountains from about 8,000 to 11,500 feet On the north he the Toba hills, containing the fine plateau of Loe Toba and Tablna. This range sends out the Khwaja Amran offshoot south- ward to form the western boundary of the District under the name of the Sarlath. On the east a barrier is formed by the mass of Zarghun (11,738 feet), with the ranges of Takatu (n,375 feet) and Murdar (10,398 feet). Directly to the south lie the Chiltan and Mashelakh hills. Besides the PISHIN LORA, \\hich, with its tributaries, drains the greater part of the District, the only river of impoitance is the Kadanai on the north, which drains the Toba plateau and eventually joins the Helmand in Afghanistan. The District is subject to earthquakes. Severe shocks occurred in Decembei, 1892, and in March, 1902
Two different systems of hill ranges meet in the neighbourhood of Quelta, giving rise to a complicated geological structure. The principal rock formations belong to the Permo-Carbomferous , Upper Trias; Lia^ Middle Jurassic (masbive limestone), neocomian (belemmte beds); Upper Cretaceous (Dunghan) , Deccan trap; middle eocene (Khojak shales, Ghazij, and Splntangi) 3 oligocene (Upper Nan) , middle and upper miocene (Lower, Middle, and Upper Siwaliks) , and a vast accumulation of sub-recent and recent formations.
Except parts of the Toba, Zarghun, and Mashelakh langes, the hills are almost entirely bare of trees. In the valleys are orchards of apricot, almond, peach, pear, pomegranate, and apple trees, protected by belts of poplar, willow, and slnjid (Elaeagnus angustifoha). The plane (chinar) gives grateful shade in Quetta In spring the hill-sides become covered for a little while with irises, red and yellow tulips, and many Astragali. In the undergrsound water-channels maiden-hair fern is found. The valley basins are covered with a scrub jungle of Artemisia and Halo\ylon GriffithiL In parts Tamarix gallic a covers the ground, and salsolaceous plants are frequent. The grasses are chiefly species of Bromus, Poa, and Hordenm. On the Khwaja Amran range wild rhubarb (Rheum Euiodi} is found in years of good rainfall.
The 'reserved' forests in Zarghun foim a welcome breeding ground for mountain sheep and mdrkhor^ but elsewhere they are decreasing in numbers The leopard is found occasionally A few hares are met with in the valleys. Wolves sometimes cause damage to the flocks in winter, and foxes are fairly abundant. Ducks are plentiful in the irrigation tanks in Pishm Chikor and MSI abound in years of good lamfall.
The climate is dry ; dust-storms are common in the spring and summer months, especially in that part of the Chaman subdivision which borders on the Registan or sandy desert. The seasons are well marked, the spring commencing towards the end of March, the summer in June, the autumn in September, and the winter in December Only in July and August is the day temperature high ] the nights are always cool. The mean temperature in summer is 78 and in winter 40. The higher elevations are covered with snow in winter, when piercing winds blowing off the hills reduce the temperature below freezing-point. The total annual rain and snowfall vanes from less than 7 inches in Chaman to io| in Quetta. Most of it is received between December and March.
History
In former times Pishm was known as Fushanj and Pashang. The ancient name of Quetta was Shal, a term by which it is still known among the people of the country, and which Rawhn- son traces back to the tenth century. The District was held in turns by the Ghazmvids, Ghonds, and Mongols, and towards the end of the fifteenth century was conferred by the ruler of Herat on Shah Beg Arghun, who, however, had shortly to give way before the using power of the Mughals. The Aiti-i-Akbarl mentions both Shal and Pishm as supplying military service and revenue to Akbar. From the Mughals they passed with Kandahar to the Safavids. On the rise of the Ghilzai power in Kandahar at the beginning of the eighteenth century, simultaneously with that of the Brahms in Kalat, Quetta and Pishm became the battle-ground between Afghan and Brahui, until Nadir Shah handed Quetta over to the Biahuis about 1740. The Durranis and their successois continued to hold possession of Pishm and Shorarud till the final transfer of these places to the British in 1879 On the advance of the Army of the Indus m 1839, Captain Bean was appointed the first Political Agent in Shal, and the country was managed by him on behalf of Shah Shuja-ul-mulk. In March, 1842, General England was advancing on Kandahar with treasure for General Nott when he was worsted in an encounter at Haikalzai m Pishin, but the disgrace was wiped out at the same place a month later. The country was evacuated in 1842 and handed over to Kalat. After Sir Robert Sandeman's mission to Kalat in 1876, the fort at Quetta was occupied by his escort and the country was managed on behalf of the Khan up to 1883, when it was leased to the British Government for an annual rent of Rs 25,000 It was formed, with Pishln and Shorarud, into a single administrative charge in 1883 Up to 1888 Old Chaman was the most advanced post on the frontier , but, on the extension of the railroad across the Khwaja Amran, the terminus was fixed at its present site, 7 miles from that place. The boundary with Afghanistan was finally demarcated in 1895-6
Many mounds containing pottery are to be found throughout the District. In the Quetta tahsil the most ancient karez are known to the people of the country as Gabri^ i. e. Zoroastrian, While the present arsenal at Quetta was being excavated in 1886, a bronze or copper statuette of Hercules was unearthed, which was 2\ feet high and held in its left hand the skin of the Nemcan lion,
The number of towns is three, the largest being QULITA, and of villages 329 The population was 78,662 in 1891 and 114,087 in 1901, an increase of 45 per cent. The following table gives statistics of area, &c , by tafalls in 1901 .
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Tahsil<span lang="EN-US" /> |
Area India square miles |
Numbers Towns, |
Villages |
Population |
Population Per separe mile |
Chaman<span lang="EN-US" /> Pishin<span lang="EN-US" /> |
2,236 2717 |
1 1 1 |
4 271 47 7 |
16,437 31,753 1,062 |
13 19 83 2 |
Quetta Shorarud<span lang="EN-US" /> |
340 634 |
3 |
329 |
114,087 |
22 |