Shaanxi xi 'an Address

Xi 'an, located in the central part of China, is the capital city of Shaanxi Province.

Xi is a famous historical and cultural city in China, located in the middle of China. It is the capital city of Shaanxi Province, and the capital of one of the thirteen dynasties in ancient China, such as Western Zhou Dynasty, Qin Dynasty, Western Han Dynasty, Xinxing, Western Jin Dynasty, Pre-Qin Dynasty, Later Qin Dynasty, Western Wei Dynasty, Northern Zhou Dynasty, Sui Dynasty, Tang Dynasty, Later Shu Dynasty and Ming Dynasty. It was once one of the starting points of the Silk Road.

Xi 'an enjoys an excellent geographical position and unique natural conditions. It borders the Yellow River in the east, the Qinling Mountains in the south, Inner Mongolia in the north and the Loess Plateau in northern Shaanxi in the west. The terrain is high in the east and low in the west, and the natural scenery is very beautiful. Xi belongs to the temperate semi-humid monsoon climate and is a city with four distinct seasons in China. Its climate characteristics are: cold and dry in winter, hot and humid in summer, pleasant in spring and autumn, suitable for tourism.

Xi The average temperature in Miko Wu is 13.5 degrees Celsius, and the annual rainfall is 530mm, mainly from July to September, with an annual average relative humidity of 60%. Fog, haze and sandstorm are the main meteorological disasters in Xi, so we must pay attention to the weather when traveling.

topography

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 Neogene about 3 million years ago, the neotectonic movement in the Qinling geosyncline fold belt south of the great fault has been extremely active, and the mountains have fallen sharply from north to south, creating 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. Weihe plain is 400-700 meters above sea level, of which the lowest point of Weihe river bed in the northeast is 345 meters above sea level. The urban area of Xi is built on the second terrace of Weihe Plain.

Baidu encyclopedia -Xi' an