Traditional Culture Encyclopedia - Tourist attractions - Why on Zhihu, most netizens have a low evaluation of Xi 'an, which is consistent with the reality?
Why on Zhihu, most netizens have a low evaluation of Xi 'an, which is consistent with the reality?
Xi 'an is located in the middle of Guanzhong Plain, with Weihe River in the north, Qinling Mountain in the south and Bashui running to Chang 'an. It is a "world historic city" designated by UNESCO 198 1, one of the important birthplaces of Chinese civilization and the Chinese nation, and the starting point of the Silk Road.
More than ten dynasties established their capitals here in history. Fenghao Capital, Qin Epang Palace, Terracotta Warriors, Han Weiyang Palace, Changle Palace, Sui Daxing City, Tang Daming Palace and Xingqing Palace outlined the "Chang 'an Complex".
Terrain:
The geological structure of Xi 'an is divided into two units: Qinling geosyncline fold belt and North China platform. The great fault at the northern foot of Qinling Mountains occurred during the Yanshan Movement 654.38+300 million years ago. Since the Late Tertiary about 3 million years ago, the neotectonic movement in the Qinling geosyncline fold belt south of the great fault has been extremely active.
The mountain rises sharply from north to south, forming the Qinling Mountains. At the same time, the Weihe fault depression, which belongs to the North China platform to the north of the great fault, continued to subside, and the Weihe plain was formed under the joint action of aeolian loess cover and Weihe alluvial.
The altitude difference in Xi 'an ranks first among the cities in China. The Qinling Mountains, with its steep and beautiful peaks, and the wide and flat Weihe Plain have clear boundaries, which constitute the main landforms of Xi 'an. The main peak of Qinling Mountain is 2000-2800 meters above sea level, of which the main peak of Taibai Mountain in the southwest is 3867 meters above sea level, which is the highest peak in the central part of the mainland.
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