By Yeshe De Project, Yeshe De Project Staff
Octavo. colour illustrated wraps. xi, 371 pp, illustrations. close to tremendous.
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Additional info for Ancient Tibet: Research Materials from the Yeshe de Project
Average elevations are 17,00019,000 feet (5100-5700 meters). Mi-nyag-sgang: Mi-nyag-sgang is located between the lower rGyal-mo-dngul-chu (Dadu He) and the She-chu and lower Nyagchu (Yalong) at elevations of 16,000-18,000 feet (4800-5400 meters). Just thirty miles south of Dar-rtse-mdo is Mi-nyag-gangsdkar (Minya Konka), a famous snow-capped mountain rising 25,047 feet (7756 meters). gYar-mo-sgang: gYar-mo-sgang extends between the 'Bri-chu (Yangtze) and the lower Nyag-chu (Yalong) at elevations of 17,00019,000 feet (5100-5700 meters).
Magnetic studies and seismic data also suggest that molten materials lie below the surface. This geothermal region, corresponding to the collision zone between India and Tibet, is part of a belt that extends through the plateau, west into Iran, Turkey, Greece, and Italy, and east into Yunnan and Burma. The increased temperatures beneath the surface across this zone are apparently related to the plate movements that built the Himalayas, closed the Tethys Sea, and moved India and Africa north. Efforts to collect scientific data continue.
On the Himalayas, huge glaciers, some of them 24 miles (40 kilometers) across, grew down into the foothills. Most of the slopes of Gangs-ti-se were glaciated as fingers of ice 12-15 miles (20-30 kilometers) long reached down the mountains. hams were filled with extensive glaciers nearly 80 miles (130 kilometers)long, and Ancient Environment 47 IDang-la glaciers also increased. As ice came down the mountainsides, it pushed huge amounts of rock and gravel in front of it. When the climate warmed and the glaciers retreated, they left behind these new hills, called moraines.
Ancient Tibet: Research Materials from the Yeshe de Project by Yeshe De Project, Yeshe De Project Staff