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 Bara-lacha-la pass in Lahaul and Spiti district of the Indian state of Himachal Pradesh. It is the third-highest lake in India and the 21st-highest in the world.[1][2] Suraj Tal Lake is just below the source of the Bhaga River that joins the Chandra River downstream at Tandi to form the Chandrabhaga River in Himachal Pradesh. The Chandrabhaga River is known as the Chenab as it enters the 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]
Suraj Tal is 65 km (40 mi) from Keylong, the district headquarters of the Lahaul Spiti district. It is accessible by National Highway NH 21, also known as the Leh-Manali Highway. The road skirts Suraj Tal, which is just 3 km (1.9 mi) short of the 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 descriptionedit
Terrainedit
View of Suraj Tal towards Bara-lacha LaView 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 Himalayas which has very sparse population with climatic conditions akin to polar conditions. Snowfall in this zone, though scanty, is reported to be spread throughout the year. Rainfall is rare in the region. Snowprecipitation 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]
Geologyedit
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 Valleyedit
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]
Tourismedit
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]
Trekkingedit
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]
^ abHarcourt, A.F.P. (1871). The Himalayan Districts of Kooloo, Lahoul and Spiti. London: W.H. Allen & Sons. pp. 16–23.
^ abcdSharad 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 22 September 2007 at the Wayback Machine
^Bajpai, S.C. (2002). Lahaul-Spiti: A Forbidden Land in the Himalayas. Indus Publishing. p. 130. ISBN81-7387-113-2.
^. Archived from the original on 13 July 2006. Retrieved 13 November 2008.
^. 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.
suraj, also, called, kamtsi, surya, long, lake, that, lies, just, below, high, bara, lacha, pass, lahaul, spiti, district, indian, state, himachal, pradesh, third, highest, lake, india, 21st, highest, world, lake, just, below, source, bhaga, river, that, joins. 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 Bara lacha la pass in Lahaul and Spiti district of the Indian state of Himachal Pradesh It is the third highest lake in India and the 21st highest in the world 1 2 Suraj Tal Lake is just below the source of the Bhaga River that joins the Chandra River downstream at Tandi to form the Chandrabhaga River in Himachal Pradesh The Chandrabhaga River is known as the Chenab as it enters the 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 Suraj TalSurya TalSuraj TalSurya TalLocationCB Range Lahaul Valley HimachalCoordinates32 45 46 N 77 23 52 E 32 76278 N 77 39778 E 32 76278 77 39778TypeHigh altitude LakePrimary inflowsGlacier and Snow meltPrimary outflowsBhaga RiverBasin countriesIndiaShore length14 km 2 5 mi Surface elevation4 883 m 16 020 3 ft FrozenDuring winter1 Shore length is not a well defined measure Contents 1 Access 2 Physical description 2 1 Terrain 2 2 Geology 2 3 Bhaga Valley 3 Tourism 3 1 Trekking 4 References 5 External linksAccess editSuraj Tal is 65 km 40 mi from Keylong the district headquarters of the Lahaul Spiti district It is accessible by National Highway NH 21 also known as the Leh Manali Highway The road skirts Suraj Tal which is just 3 km 1 9 mi short of the 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 editTerrain edit nbsp View of Suraj Tal towards Bara lacha La nbsp 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 Himalayas which has very sparse population with climatic conditions akin to polar conditions Snowfall in this zone though scanty is reported to be spread throughout the year Rainfall is rare in the region Snow 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 edit 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 edit 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 edit nbsp 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 edit 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 edit The Highest Lake in the World a b Lakes a b Harcourt A F P 1871 The Himalayan Districts of Kooloo Lahoul and Spiti London W H Allen amp Sons pp 16 23 a b c d Sharad V Oberoi amp 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 Bajpai S C 2002 Lahaul Spiti A Forbidden Land in the Himalayas Indus Publishing p 130 ISBN 81 7387 113 2 Lahaul and Spiti District Archived 13 June 2010 at the Wayback Machine Lahaul amp Spiti District Himachal Pradesh India Archived from the original on 13 July 2006 Retrieved 13 November 2008 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 Indian Himalayas Lahaul and Spiti Suraj Tal Darcha Baralacha Pass Trek LahaulExternal links edit nbsp Wikimedia Commons has media related to Suraj Tal Suraj Tal Lake Surya Taal photos on Trek Earth Road and trekking map Lahaul and Spiti Bara lacha la Pass Retrieved from https en wikipedia org w index php title Suraj Tal amp oldid 1188528543, wikipedia, wiki, book, books, library,
