Which city does Binxian belong to?

Binzhou, also known as Binxian. It belongs to Xianyang City, Shaanxi Province, located in the west of Weibei Plateau, in the middle and lower reaches of Jinghe River, bordering Xunyi County and Chunhua County in the east, Changwu County and Lingtai County in Gansu Province in the west, Yongshou County and linyou county in the south and Zhengning County in Gansu Province in the north.

Binxian is 20 km away from Xianyang1in the south, Xi 'an 150km away from the provincial capital in the north and Pingliang 160km away from Gansu. The total area of Binxian County is 1 185km2, which governs 8 towns, 1 sub-district offices and 1 administrative villages. In 20 17, the registered population was 366,800.

On July 20 13, Binxian County (Binzhou City) won the title of "National Greening Model County". 2065438+In June 2008, the county was withdrawn to set up a city.

Extended data:

The geographical environment of Bin County:

1, landform

Binzhou is a hilly and gully region of Longdong Loess Plateau. The terrain is high in the southwest and low in the northeast. Jinghe River obliquely crosses the central part from northwest to southeast, dividing Binzhou into two platforms, northeast and southwest, and both platforms are inclined to the lower reaches of Jinghe River. The platform is broken and the ravines are densely covered. There are 4089 gullies, including main gullies 12 gullies, with an area of 639.59 square kilometers, accounting for 54. 1% of Binzhou's total area.

2. Characteristics of soil

There are 5 soil types, 9 subtypes, 17 soil genera and 37 soil species in Binzhou city. There are mainly black loessial soil, loessial soil, red soil, silt and fluvo-aquic soil. With the change of topography, soil has zonal, regional and regular distribution.

3. Climate characteristics

Binzhou city belongs to warm temperate semi-arid continental monsoon climate. It has the characteristics of rain and heat in the same season, extremely cold and midsummer, and four distinct seasons. Winter is mainly affected by Mongolian high pressure, with scarce precipitation and long cold and dry days. In spring, the Mongolian high pressure gradually decreased, the tropical heating mass gradually moved northward, the temperature rose rapidly and the precipitation increased. Due to frequent cold air activities and changeable weather, it is prone to "late spring cold", strong wind and frost.

Baidu Encyclopedia-Binzhou