Suraj Tal

Coordinates: 32°45′46″N 77°23′52″E / 32.76278°N 77.39778°E / 32.76278; 77.39778
Source: Wikipedia, the free encyclopedia.

Suraj Tal
Surya Tal
Primary inflows
Glacier and Snow melt
Primary outflowsBhaga River
Basin countriesIndia
Shore length14 km (2.5 mi)
Surface elevation4,883 m (16,020.3 ft)
FrozenDuring winter
1 Shore length is not a well-defined measure.

Suraj Tal, also called Tso Kamtsi or Surya Tal, is an 800 m (2,600 ft) long lake that lies just below the 4,890 m (16,040 ft) high

Jammu region of Jammu and Kashmir.[2] The other major tributary of the Chandrabhaga, the Chandra, originates and flows south-east of the Bara-lacha La.[3]

Access

Suraj Tal is 65 km (40 mi) from

Bara-lacha-la pass.[4] It remains inaccessible during the winter months of November to April since the pass becomes totally snowbound during this period.[5][6][7]

Physical description

Terrain

View of Suraj Tal towards Bara-lacha La
View of Suraj Tal down the Bhaga valley

The glaciers and nullahs (streams) that from the Bara-lacha-la pass feed the lake. The pass is 8 km long and is also called the "Pass with Crossroads on Summit" since roads from Zanskar, Ladakh, Spiti, and Lahaul meet at this pass.[4] In addition to the Bhaga River that originates from it and flows through Suraj Tal, Bara-lacha-la Pass is also the source of the Chandra and Yunan Rivers in the southeast and north, respectively.[4]

The lake is situated in the Upper Himalayan Zone, or High Latitudinal Zone part of the

precipitation from snow storms is reported to be less than 200 mm (7.9 in) of snow in nearly 50% of the storms, even though one observatory in the region has reported 800 mm (31 in) of snowfall. The precipitation starts melting in May. Snow on slopes is generally slackly bonded, with the wind redistributing it. The average total snowfall recorded in a year is reported to be 12–15 m (39–49 ft), with the highest temperature at 13 °C (55 °F), the mean highest temperature at 0.5 °C (32.9 °F), the mean minimum temperature at −11.7 °C (10.9 °F), and the lowest temperature at −27 °C (−17 °F). The ground in the zone is covered with scree and boulders.[4]

Geology

The lake's geology is similar to thet of the nearby Bara-lacha-la Pass, which is reported to be an early rifting event on the northern Indian passive margin, and the Basalts which are emplaced along the trans–tensional faults indicate that.[8]

Bhaga Valley

The Bhaga River originates in Bara-Lacha La and flows north-west through Suraj Tal to Tandi, the confluence point with the Chandra River. The Bhaga Valley (Tod or Stod Valley) is 72 km (45 mi) long.[3] The valley, which is a narrow gorge, is devoid of any vegetation up to Darcha, and thereafter it widens up to its confluence with the Chandra River at Tandi. There are terraces between Darcha and Tandi which are under cultivation in the lower slopes, with the middle slopes having grasslands. Plantations of trees and shrubs to meet fuel wood and fodder requirements have been done on the hill slopes.[9]

Tourism

National Highway skirting the lake on the left

Lahaul-Spiti Valley is a common destination for Indian and foreign tourists on road trips, trekking, and motorcycling. The NH 21 route from Manali to Leh covers the Suraj Tal Lake and the Bara-lacha-la pass.[10]

Trekking

Trekking tours are common. One trek route is the Zingzingbar–Suraj Tal–Bara-lacha-la. This involves trekking along the Bhaga River for 3 km (1.9 mi), crossing a bridge to the north bank, then a further climb of 2.5 km (1.6 mi) from the bridge, followed by a steep foot trail up to Suraj Tal.[11]

References

  1. ^ The Highest Lake in the World
  2. ^ a b Lakes
  3. ^ a b Harcourt, A.F.P. (1871). The Himalayan Districts of Kooloo, Lahoul and Spiti. London: W.H. Allen & Sons. pp. 16–23.
  4. ^ a b c d Sharad V. Oberoi & P. Mathur, "Training Report on Feasibility Study of Existing Manali-Darcha Highway and Proposed Darcha-Padam Road Using Remote Sensing and GIS Techniques", SASE, Chandigarh, India, (pages 11-13), 22 Jun 2004 Archived 22 September 2007 at the Wayback Machine
  5. ISBN 81-7387-113-2
    .
  6. ^ Lahaul and Spiti District Archived 13 June 2010 at the Wayback Machine
  7. ^ "Lahaul & Spiti District, Himachal Pradesh, India". Archived from the original on 13 July 2006. Retrieved 13 November 2008.
  8. ^ "The Carboniferous Baralacha la basaltic dykes (Upper Lahul, Ladakh): remnants of an early rifting event along the Indian northern plate". Archived from the original on 8 October 2006. Retrieved 13 November 2008. They derive from the partial melting of an enriched OIB mantle source, characterized by a HIMU component, and contaminated by the lower continental crust.
  9. ^ Indian Himalayas, Lahaul and Spiti
  10. ^ Suraj Tal
  11. ^ Darcha Baralacha Pass Trek Lahaul

External links

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