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DEHRADUN

Nestled in the mountain ranges of the Himalaya, Dehradun is one of the oldest cities of India and is the Capital of Uttarakhand state and is also known as the ‘Adobe of Drona’, Dehradun has always been an important center for Garhwal rulers which was captured by the British. The headquarters of many National Institutes and Organizations like ONGC, Survey of India, Forest Research Institute, Indian Institute of Petroleum etc are located in the city.

 

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Some of the premier educational and Training Institutes like Indian Miltary Academy, RIMC (Rashtriya Indian Military College), Indira Gandhi National Forest Academy (IGNFA), Lal Bahadur Shahstri National Academy of Administration (LBSNAA)etc are also there in Dehradun. It is a favoured tourist destination as it attracts tourists, pilgrims and enthusiasts from various walks of life to its serene environs. Add to this the abundance of special Basmati rice, tea and leechi gardens which contribute in turning the city into a paradise. The district is named after its chief city Dehra Dun. Dehra appears to be a corruption of dera signifying a temporary abode or camp. During the reign of Aurangzeb, Ram Rai, Guru of the Udasi Sikhs on being ordered by the Mughal king to retire to the wilderness of the Dun, had pitched his tents here in what is now the Khurbura locality of the town and has also built a temple near Dhanawala. Around these two sites, grew up the town popularly known as Dehra. The term dun or doon means the low lands at the foot of a mountain range, and as the bulk of the district lies in such a terrain, it justified the dun part of the name. Another derivation of the term dun is stated to be from Dronashram, hermitage of Guru Dronacharya of Mahabharata fame, who sojourned for a season in the village of Devara, situated near to Dehra to perform his devotions at a lonely spot.

District Boundaries
The district is situated in the north-west corner of the state. It is bounded on the north and to some distance in the north-west by the district of Uttarkashi, In the east by the district Tehri Garhwal and Pauri-Garhwal In the south by the district of Saharanpur(Uttar Pradesh) , At its southern tip touching the boundary of district Haridwar. Its western boundary adjoins the Sirmur(Nahan) district of Himachal Pradesh with the rivers Tons and Yamuna separating the two. Lies between 29 degrees 58' and 31 degrees 2' 30" north latitudes and 77 degrees 34' 45" and 78 degrees 18' 30" east longitudes. Total area of the district is 3088 sq kms. Altitude is 640 mts.(2100 ft) above sea level .

History
According to Skanda Purana, Dun formed part of the region called Kedar Khand. It was included in the kingdom of Ashoka by the end of the 3rd century B.C. It is revealed by history that for centuries the region formed part of the Garhwal kingdom with some interruption from Rohillas. For about two decades till 1815 it was under the occupation of the Gorkhas. In April 1815 Gorkhas were ousted from Garhwal region and Garhwal was annexed by the British. In that year the area now comprising tehsil Dehra Dun was added to district Saharanpur. In 1825, however, it was transferred to the Kumaon Division. In 1828, Dehra Dun and Jaunsar Bhabar were placed under the charge of a separate Deputy Commissioner and in 1829, the Dehra Dun district was transferred from the Kumaon Division to the Meerut Division. In 1842, Dun was attached to Saharanpur district and placed under an officer subordinate to the Collector of the district but since 1871 it is being administered as separate district. In 1968 the district was taken out from Meerut division and included in the Garhwal Division.

Languages
Main languages spoken in the district are Hindu, Sindhi, Punjabi, Garhwali, Kumaoni Urdu & English.

Topography
Dehra Dun can be divided into two distinct tracts i.e. the montane tract and the sub-montane tract. The montane tract covers whole Chakrata tehsil of the district and consists entirely of a succession of mountains and gorges and comprises Jaunsar Bhabar. The mountains are very rough with steep slopes. The most important features of the tract is the ridge which separates the drainage are of Tons on the west from that of Yamuna on the east. Below the montane tract follows the sub-montane tract, which is the famous Dun valley bounded by Shivalik hills in the south and outer scarp of the Himalayas in the north.

Forests
Dehra Dun is distinguished from most other districts in the state by the existence of very large forests chiefly stocked with sal. Forest products play an important role in the economy of the district. Besides, supplying fuel, fodder, bamboos and medicinal herbs, they also yield a variety of products like honey, lac, gum, resin, catechu, wax, horns and hides. The forests account for 1477 sq.kms of area, giving a percentage of 43.70 of the total area of the district. Owing to the variation in altitudes and other aspects, the flora of the district vary from tropical to alpine species. Different types of forests and varying species of shrubs, climbing plants and grasses, depending upon the aspect, altitude and soil condition are found in the district. Sal forest and coniferous forests are predominant in the western part of tehsil Dehra Dun. Chir is the only coniferous species in the old reserved forests of Dehra Dun. Besides other associates of chir, a few deodar trees are also seen in the district. Wide ranges of sal forest occur in this part of the tehsil. Sal is the main timber species and is generally pure towards the Siwalik ridges. A mixture of miscellaneous species are found in the lower parts. In the eastern part of tehsil Dehra Dun, the flora may be divided into a number of Botanical divisions mentioned below :

Moist Siwalik Sal Forests :
These forests are found in the Motichur and Thano forest ranges. Low quality of sal is found in these forests. The main associates of sal are bakli and sain.

Moist Bhabar Doon Sal Forests :
These forests are found in a large areas in Thano and Barkot forest ranges. Sal is pure in the overwood and its typical associates are sain and dhauri. the underwood growth includes karaunda and chameli.

West gangetic Moist Deciduous Forests :
These are found in the Kansro, Barkot, Motichur and Thano forest ranges. These are closed forests from medium to good height. The main associates of sal are safed siris, jhingan, bohera and dhauri.

Dry Siwalik Sal Forests :
These forests are found on the higher slopes of Siwaliks. In Chakrata tehsil they occur near the junction of the Tons and the Yamuna rivers in the neighborhood of Kalsi. Sal is the predominant species mixed with other associates viz. bakli, sain, haldu, jhingan etc. Besides the above many other types of forests occur in small belts in the plain of the district.

Rivers, Canales and Waterways
The Siwalik (outer and lower ranges of Himalayas) lies at its feet, the outer- scrap of the Himalayas bound it on the north and the scared Ganga and the Yamuna skirt in on the east and the west respectively. The Ganga enters the district in the eastern Dun at Tapoban and meandering south-west goes to Hardwar via Raiwala near Rishikesh. The Yamuna enters the district in Jaunsar and flows southwards for about 32 kms on the south-east border of the district. Besides Ganga and yamuna, the other rivers that flow in the district are Asan, Suswa, Tons, Rispana, Bindal and Amalava.

Climate & Rainfall in Dehradun District
The Climate of the district is generally temperate. It varies greatly from tropical to severe cold depending upon the altitude of the area. The district being hilly, temperature variations due to difference in elevation are considerable. In the hilly regions, the summer is pleasant, but in the Doon, the heat is often intense, although not to such degree as in the plains of the adjoining district. The temperature drops below freezing point not only at high altitude but even at places like Dehradun during the winters, when the higher peaks are also under snow. The area receives an average annual rainfall of 2073.3 mm. Most of the annual rainfall in the district is received during the months from June to September, July and August being rainiest. Climate Data of Doon Valley for all the months is as under on the basis of mean of last 25 years.