三清山英文介绍.docVIP

Description Sanqing Mountain lies in the northeast of Jiangxi Province, with Yujingfei as its highest peak (altitude 1 816.9m). Sanqingshan has an area of 22 950 hm2, among which core tone covers 7 690 hm2, natural reserve zone 15 260 hm2. Besides, buffer zone surrounding it covers 14 000 hm2. Sanqing Mountain is located at the conjunction between the Yangtze Plate and the Huaxia plate, north to it is the Jiangxi Northeast suture cincture deep fault. Ever since the Indochina movement, Sanqing has entered continent margin violent changes and Pro-Pacific Ocean structure development stage. At late Yanshan movement period, a large scale of acid magma intrude activities took place under the integrative effect of three faults in Northeast-East, North-Northeast and North-West. Sanqing were uplifted during (at) late Himalayan period. The sediment of Carbonate which deposited during the Carnbrian and Ordovician even late C, P and early Triassic was eroded more easily than the harder granite. The granite rocks were exposed as a result the granite mountains further developed their characteristic shape through erosion and dissection. Sanqing continues to be uplifted till now. Unique geologic structure and suitable geographic environment makes Sanqing Mountain famous with its granite hill forest physiognomy. And it is a natural museum for the evolvement process of granite hill forest which is composed of with ridges and peak, apex wall, apex woods, apex pillar and stone sprout, etc. The various shapes of hills also have high aesthetic and tourism development value. Sanqing Mountain is the product of geological history of the Earth and biological evolvement, which includes all types of Chinas Mid-and Sub-tropical zone vegetation and they are in stale condition. With the increase of altitude, there are 6 vegetation cinctures by sequence, namely: indeciduous latifoliate forest, indeciduous-defoliation latifoliate forest, taiga-latifoliate forest, warm taiga, mountainous region moss