By Yeshe De Project, Yeshe De Project Staff
Eightvo. colour illustrated wraps. xi, 371 pp, illustrations. close to effective.
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Eightvo. colour illustrated wraps. xi, 371 pp, illustrations. close to nice.
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Extra info for Ancient Tibet: Research Materials from the Yeshe de Project
The climate became even warmer and more humid than it is now; vegetation was more lush, and glaciers were no greater in extent than they are at present. New lakes formed from melting glaciers, and older lakes became fresher and deeper. Forests of pine and birch grew around many lakes, even in the Himalayas. The far north was still quite cold and not so moist as the south and east, which were more humid and more heavily forested than today. Many lakes and swamps dotted the landscape, and the climate was tropical enough around Chab-mdo for ferns and brake to grow.
C. , the environment grew more favorable; the variety of plants and animals Ancient Environment 49 increased, and the glaciers retreated. The plateau may now have been well over 15,500 feet (4700 meters) in height, and the Himalayas near 20,000 feet (6000 meters). C. C. the climate became even warmer and more humid than it is now; vegetation was more lush, and glaciers were no greater in extent than they are at present. New lakes formed from melting glaciers, and older lakes became fresher and deeper.
42 The Land In some regions primitive fish had emerged by this time as well. By about 400-300 million years ago, fishlike ancestors had given rise to amphibians that could inhabit dry land as well as the seas. But no evidence of ancient fish or amphibians has as yet been found in Tibet. There are abundant fossils of marine plants, however, which differ from region to region. Many researchers interpret the variations as evidence that cold water covered southem Tibet, while warm-water seas existed over the land destined to become northern Tibet.
Ancient Tibet: Research Materials from the Yeshe de Project by Yeshe De Project, Yeshe De Project Staff