Suraj Tal
Suraj Tal, also called Tso Kamtsi or Surya Tal, is a 800 m long lake that lies just below the 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. 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 . The other major tributary of the Chandrabhaga, the Chandra originates and flows south-east of the Bara-lacha La. Access. Suraj Tal is from Keylong, the district headquarters of the Lahaul Spiti district. It is approachable by National Highway NH 21, also known as the Leh-Manali Highway. The road skirts Suraj Tal which is just short of the Bara-lacha-la pass. It remains inaccessible during the winter months of November to April since the pass becomes totally snowbound during this period. Physical description. Terrain. The lake is fed from the glaciers and nullahs (streams) originating from the Bara -lacha-la pass. 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. 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. 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 all round the year. Rainfall precipitation is rare in the region. Snow precipitation from snow storms is reported to be less than of snow in nearly 50% of the storms, even though one observatory in the region has reported of snow fall. The precipitation starts melting from May. Snow on slopes is generally slackly bonded, with wind redistributing it. The average total snowfall recorded in a year is reported to be with highest temperature , mean highest temperature , mean minimum temperature and lowest temperature . The ground in the zone is covered with scree and boulders . Geology. The Lake's geology is similar to the nearby Bara-lacha-la Pass, which is reported to be an early rifting event on the northern Indian passive margin and that the Basalts which are emplaced along the trans–tensional faults indicate that. Bhaga Valley. The Bhaga River originates in Bara-lacha La and flows north-west through Suraj Tal to Tandi, the confluence point with Chandra River. The Bhaga Valley (Tod or Stod Valley) is long. The valley, which is a narrow gorge, is devoid of any vegetation up to Darcha and thereafter it widens up to its confluence  with Chandra River at Tandi with terraces between Darcha and Tandi which are under cultivation in the lower slopes, with the middle slopes having grasslands. Plantation of trees and shrubs to meet fuel wood and fodder requirements have been done on the hill slopes. Tourism. Lahaul Spiti valley is a common destination for Indian and foreign tourists for road trips, trekking and motorcycling. The NH 21 route from Manali to Leh covers the Suraj Tal Lake and the Bara-lacha-la pass. Trekking. Trekking tours are common. One trek route is the Zingzingbar–Suraj Tal–Bara-lacha-la. This involves  trekking along the Bhaga River for , crossing a bridge to the North bank, then a further climb of from the bridge followed by a steep foot trail up to Suraj Tal.