To install click the Add extension button. That's it.

The source code for the WIKI 2 extension is being checked by specialists of the Mozilla Foundation, Google, and Apple. You could also do it yourself at any point in time.

4,5
Kelly Slayton
Congratulations on this excellent venture… what a great idea!
Alexander Grigorievskiy
I use WIKI 2 every day and almost forgot how the original Wikipedia looks like.
Live Statistics
English Articles
Improved in 24 Hours
Added in 24 Hours
What we do. Every page goes through several hundred of perfecting techniques; in live mode. Quite the same Wikipedia. Just better.
.
Leo
Newton
Brights
Milds

From Wikipedia, the free encyclopedia

Dras River
Dras River
The confluence of the Dras River with the Suru River
Location
CountryIndia
Union TerritoryLadakh
DistrictKargil
Physical characteristics
Source34°16′20″N 75°31′47″E / 34.272303°N 75.529832°E / 34.272303; 75.529832
 • locationMachoi Glacier near Zojila
 • elevation4,400 m (14,400 ft)
Mouth34°35′41″N 76°07′13″E / 34.5946°N 76.1202°E / 34.5946; 76.1202
 • location
Suru River at Kharul Kargil
 • elevation
3,618 m (11,870 ft)
Length86 km (53 mi)
Discharge 
 • average212 m3/s (7,500 cu ft/s)

The Dras River, also spelt Drass River, is a river in the Kargil district in the Indian union territory of Ladakh. It originates below the Zoji La pas in the Great Himalayan range and flows northeast towards Kargil, where it joins the Suru River. The Shingo River, which flows in a parallel direction in Pakistan-administered Baltistan, also joins the Drass River. The combined river is alternatively called Suru, Drass and Shingo by various local groups.

The Drass River valley is traversed by the National Highway 1D that connects Srinagar in Kashmir with Leh in Ladakh. It represents a historic trade route.

YouTube Encyclopedic

  • 1/3
    Views:
    391
    6 728
    439
  • Drass to Kargil
  • Kargil war memorial - Drass Sector
  • Sainik School Bijapur, Col MB Ravindranath, VrC, 403, Adl, Capturing Tololing, 4590, 17 Nov, 2016

Transcription

Course

The Dras River is 86 km (53 mi) long and flows entirely in the Dras Valley. Its source lies in the Machoi Glacier near Zojila Pass, the gateway to Ladakh, 26 km (16 mi) east of Sonamarg and 120 km (75 mi) east of Srinagar, the summer capital (May - October) of Jammu and Kashmir.[1][2] The Machoi Glacier is also the source of the Sind River, which flows through the neighbouring Kashmir Valley in the opposite direction to the Dras River.[3] The Dras River flows northeast, fed by many glacial streams. NH 1D, a national highway connecting Srinagar with Ladakh (Kargil and Leh), runs parallel to the river. The river forms the Dras Valley at Dras,[2] where it is joined by two tributaries, the Mashko Nala and Gamru Nala, which originate in the glaciers of Mashko Valley.[3] In the Dras Valley, the road connecting Dras and Gurais runs parallel to the river.

The confluence of Dras (left) and Shingo Rivers

The Shingo River joins the Dras River at Latoo near Kaksar, and doubles the flow of the river. The Shingo River originates in the Chota Deosai Plains north of Minimarg (Astore District, Gilgit-Baltistan) and flows east.[4][2]

The combined Dras and Shingo rivers join the Suru River at Kharul, 7 km (4.3 mi) north of the town of Kargil.[2] The Suru River is a left tributary of the Indus River.[5] It originates from the Panzella glacier near Pensi La, flows northwards and merges with the Indus River at Nurla in Pakistan-administered Gilgit-Baltistan, 5 km (3.1 mi) north of its confluence with the Dras River. It enters the Pakistani-Administered Kashmir at Post 43 of India or Post 44 of Pakistan.[6]

Habitation

The Dras River flows through the towns of Matayan, Pandrass, Troungjen, Dras, Bhimbat, Thasgam, Shimsha, Kharbu and Kakshar. The largest settlement on its banks is Dras, which is the second-coldest inhabited place in the world after Siberia.[7] The water flow of the river increases during the late summer, due to the heavy melting of glaciers.[8]

References

  1. ^ "Kargil the Suru valley". gaffarkashmir.com. Archived from the original on 19 April 2019. Retrieved 29 August 2012.
  2. ^ a b c d Omacanda Hāṇḍā (2001). Buddhist Western Himalaya: A politico-religious history. Indus Publishing, 2001. p. -67. ISBN 9788173871245. Retrieved 27 August 2012.
  3. ^ a b Harish Kapadia (1999). Across Peaks & Passes in Ladakh, Zanskar & East Karakoram. Indus Publishing, 1999. p. -226. ISBN 9788173871009. Retrieved 27 August 2012.
  4. ^ Kapadia, Harish (1999), Across Peaks & Passes in Ladakh, Zanskar & East Karakoram, Indus Publishing, pp. 226–, ISBN 978-81-7387-100-9
  5. ^ S. S. Negi (2002). Cold Deserts of India. Indus Publishing, 2002. p. -13. ISBN 9788173871276. Retrieved 27 August 2012.
  6. ^ "Rivers of Ladakh". ladakh.com. Archived from the original on 2 September 2012. Retrieved 29 August 2012.
  7. ^ M.S. Kohli (2004). Mountains of India: Tourism, Adventure, Pilgrimage. Indus Publishing, 2004. p. -124. ISBN 9788173871351. Retrieved 29 August 2012.
  8. ^ Sharad Singh Negi (1991). Himalayan Rivers, Lakes, and Glaciers Informative books on the himalayas-forestry-environment. Indus Publishing, 1991. p. -61. ISBN 9788185182612. Retrieved 27 August 2012.

Further reading

External links

This page was last edited on 7 July 2023, at 18:34
Basis of this page is in Wikipedia. Text is available under the CC BY-SA 3.0 Unported License. Non-text media are available under their specified licenses. Wikipedia® is a registered trademark of the Wikimedia Foundation, Inc. WIKI 2 is an independent company and has no affiliation with Wikimedia Foundation.