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The Discovery and Conquering of the Worlds
From Sea to Roof of the World
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alpine climate alpine zone ancient Himalaya Sea ancient sea Asiatic black bears bar-headed geese broad-leaved forest broad-leaved trees Cenozoic Central Rongbuk Glacier Chinese geologists Chinese mountaineers climate cold crops crustal movement direct solar radiation evergreen broad-leaved face of Qomolangma flag cloud fossils Gangdise Range glacier terminal glacier valley Glossopteris Gondwana grass grassland grow height limit high altitudes high mountains highland barley Himalayas humidity ice and snow ice pinnacles intense solar radiation kilometres lakes langma area lichen lower melting metres above sea million years ago monsoon Mount Qomolangma mountain massif needle forest needle-leaved forest neve basin noctuid north face plates Proterozoic Qomo Qomolangma area rainfall rainy season rhododendrons river valleys Rongbuk Glacier Rongbuk Lamasery screes sea level sediments snow alga snow-line solar radiation south face South Tibet southern slopes species Springtails summer summit sunshine temperature terraces thrive Tibet Plateau Tibetan peasants ture weather wind yaks Yarlung Zangbo River