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Nubra River

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Geography

The Siachen Glacier terminates in a snout located at around 3,570 m (11,700 ft) and two pro-glacial melt-water streams originate out of two ice caves in the region. They merge about one kilometer downstream and becomes the Nubra river. Numerous other glaciers of the Karakoram descend into the Nubra. It then flows between the Karakoram range and the Saltoro Mountains in a general southeasterly direction for about 90 kilometres (56 mi) before its confluence with the Shyok River near Diskit, forming the Nubra Valley.

The side valleys of the Nubra Valley contain some 33 glaciers of varying proportions, and the heavy sediment load carried by the river from the melt-water is responsible for many glacio-fluvial deposits including braided channels, outwash plains and alluvial fans. The valley has been formed by ancient glaciers, now long receded, and has an average elevation of 4,000 m (13,000 ft) above sea level. The area has a very arid climate, and the lack of precipitation and the high elevation means that the upper reaches of the valley are nearly devoid of vegetation. At its junction with the Shyok, the sandy flats support patches of Tamarix and Myricaria. There are small villages at the foot of ravines, where poplars and willow trees grow. Small pasture fields have been enclosed on the un-denuded fans and fruit trees are grown.

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