青藏高原和喜马拉雅地区分布着数以千计的冰川，是除了两极之外冰雪储量最为丰富的地区。
With thousands of glaciers scattered across the Plateau and the Himalayas, the region has the most snow and ice outside of the polar regions.
科学界普遍认为，青藏高原和喜马拉雅山是6500万年前向北漂移的印度板块与欧亚板块相撞而形成的。
Scientists believe that 65 million years ago, the Indian Plate moving north collided with the Eurasian Plate, and the upheaval saw the emergence of the Qinghai-Tibet Plateau as well as the Himalayas.
青藏高原南缘前陆盆地中的磨拉石主要沉积在小喜马拉雅带和次喜马拉雅带中，次之出现在冲积平原带。
Cenozoic molasse at the south edge of Qinghai-Tibetan Plateau was mostly deposited in the zones of Lesser-Himalaya and Sub-Himalaya, others in Alluvial Plain zone.
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