Video of ancient immigrants in Shizuishan

The area to the north of the territory of the Western Zhou and Zhou Dynasties, including Hetao in Inner Mongolia, Ningxia, Shaanxi and northwestern Shanxi, is called Shuofang.

During the Spring and Autumn Period, today Guyuan area was inhabited by warrior Rong, and today this area is the sphere of influence of Yan centered on Yanchi.

During the Warring States Period, King Huiwen of Qin seized Wu Rong's land and established Wushi County (now the north bank of Nanjingshui in Guyuan County) to govern today's Guyuan area. Later, in Yanchi County, Kanyan County was established to manage today's Yin Nan area.

After the thirty-fifth year of Qin Dynasty and the reign of Zhao Xiangwang (272 BC), the two counties were placed under the jurisdiction of Beijun County, which was the beginning of the administrative system in Ningxia. During the Qin Dynasty, Ningxia was a northern county, and the county governed Ning County in Gansu Province. Qin Changcheng and Qinqu were built here to divert water from the Yellow River to irrigate farmland.

The Han Dynasty belongs to the Shuofang History Department.

In the Western Han Dynasty, Beidi County was under the jurisdiction of Huan County, Gansu Province. Guyuan is located in Anding County; Ningxia belongs to Beidi County and Anding County.

In the Eastern Han Dynasty, Anding County moved to zhenyuan county, Gansu, and Beijun moved to the southwest of Litong District, Wuzhong City.

Sixteen countries, the territory of Daxia country built by Helian Bobo, the leader of Xiongnu Iron Buddha Department.

During the Northern Wei and Zhou Dynasties, immigrants continued to promote the development of villages, and the villages were effectively developed again. Ningxia was originally named "South of the Saibei River".

In the Tang Dynasty, Ningxia belonged to Guannei Road, including Yuanzhou, Lingzhou, Xi Hui, Anle, Xiongzhou and Policeman. In the 14th year of Tianbao (755), the "Anshi Rebellion" broke out in the Tang Dynasty, and Prince Hengli became Tang Suzong in Lingwu, Ningxia.

In the Northern Song Dynasty, Ningxia belonged to Qingfeng Road, and the northern part of Ningxia was occupied by Li and Dangxiang. The Northern Song Dynasty only controlled the southern part of Ningxia, and the southern part of Ningxia was changed to Jingyuan Road.

In the Yuan Dynasty, Xixia Zhongxing was established at the site of Xixia National Memorial. In the 24th year of Zhiyuan (1287), Ningxia government road was established, hence the name Ningxia.

Ningxia Prefecture was established in the early Ming Dynasty, and later changed to Wei. Ningxia Zuo Tunwei, Zhong Tunwei and avant-garde, central defender and defender were added. Later, Ningxia Town and Guyuan Town were set up, and nine defense zones were set up along the Great Wall, called Nine Towns, which was the second important border town in the Ming Dynasty.

In the fifth year of Shunzhi in the Qing Dynasty (1648), the Qing Dynasty set up a governor in Ningxia, which was the chief secretary of Shaanxi Province and affiliated to Jiankangyuan, and Ningxia was the subject province. Retreat, change the Ningxia government, set up a county, and belong to Gansu, but promote the Ningxia company commander as the prefect and add the Ningxia general government, without losing the provincial pattern.

In the year of the Republic of China (19 12), the government was changed to Taoism in June. Because Shuo Fang is on the right, it is changed to Shuo Fang Road.

Extended data:

The elevation of Ningxia Hui Autonomous Region is1100-1200m, and the terrain gradually inclines from southwest to northeast. The Yellow River enters from Zhongwei, obliquely crosses the plain to the northeast, and exits through Shizuishan along the terrain. On the plain, the soil layer is deep, the terrain is flat and the slope is suitable, which is convenient for water diversion and irrigation.

Ningxia has complex landforms, many mountainous areas and scattered basins, which can be roughly divided into three sections: Loess Plateau, Ordos Platform, Alluvial Plain and Liupanshan Mountain, Luoshan Mountain and Helan Mountain. The average altitude is above 1000 meters. According to the surface characteristics, it can also be divided into southern warm plain, mid-temperate semi-desert area and northern desert area.

From south to north, the whole area is characterized by the transition from flowing water landform to wind erosion landform. Ningxia is located in the transition zone between the Loess Plateau and Inner Mongolia Plateau, with high terrain in the south and low terrain in the north. In terms of landform types, the loess landform eroded by flowing water is dominant in the south, and drought erosion and wind erosion are dominant in the middle and north, which is a part of the Inner Mongolia Plateau.

There are steep mountains and widely distributed hills, alluvial plains formed by stratum subsidence and Yellow River alluvial, platforms and sand dunes. The surface morphology is complex and diverse. ?

Baidu Encyclopedia-Ningxia