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Situated at the western edge of the Tibetan plateau, Ladakh is bound by the mighty Karokaram mountain range in the north and the Great Himalayas in the South. Landscape of Ladakh has been modified and sculpted into the spectacular shape by the wind and the erosion over the centuries. Its altitude ranges from 9000 to 25000 feet. And is traversed by other mountain chains, the Ladakh range and Zanaskar range. It is rightly called “the broken moonland” and “land of endless discovery”.
Today a high-altitude desert, shelter ed from the rain-bearing clouds of the Indian monsoon by the barrier of the Great Himalaya, Ladakh was once covered by an extensive lake system, the vestiges of which still exist on its south-east plateaux of Rupshu and Chushul, in the drainage basins or lakes of Tso-moriri, Tso-kar and Pangong-tso. But the main source of water is winter snowfall.
Dras, Zanskar and the Suru Valley on the Himalaya's northern flanks receive heavy snow in winter, this feeds the glaciers from which melt water, carried down by streams, irrigates the fields in summer. For the rest of the region, the snow on the peaks is virtually the only source of water. As the crops grow, the villagers pray not for rain, but for sun to melt the glaciers and liberate their water.
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