Is Bengbu south or north?

South refers to the area south of Huaihe River in Qinling Mountains and east of Qinghai-Tibet Plateau, and often refers to the area south of specific or implied azimuth points. In China, "southern region" generally refers to the vast area south of the Qinling-Huaihe line.

Penang, referred to as Bengbu, is also called Pearl City. It is a prefecture-level city in Anhui Province, the first prefecture-level city in Anhui Province (1947). There are four municipal districts, namely bengshan district, Yuhui District, Huaishang District and Longzihu District, which govern Huaiyuan County, Guzhen County and Wuhe County. During the Republic of China, it was the residence of Anhui military government and Fengyang county government; With a total area of 5,952 square kilometers and a total population of 38 1.25 million in 20 17, the territory is connected by mountains and rivers and has four distinct seasons. It has a long history and splendid culture. According to historical records, Bengbu is "the place where pearls were picked in ancient times", so it is called "Pearl City".

Bengbu is located at the intersection of beijing-shanghai railway and Huainan railways, and the intersection of Beijing-Shanghai high-speed railway and Beijing-Fuzhou high-speed railway. It is a national civilized city, a national regional central city, a national comprehensive transportation hub city, a central city in Huaihe River Basin, a central city in northern Anhui and a tourist center city in Anhui Province. Huaishang is known as the land of princes and the pearl.

20 17 years Bengbu's regional GDP 155066 billion yuan.

Extended data:

Bengbu City is located in the north of Anhui Province, with latitude 32 43 ′ to 33 30 ′ north latitude and longitude116 45 ′ to18 04 ′ east longitude, bordering Suzhou City, Suixi County, Lingbi County in the north.

The longest distance from east to west is 32.3 kilometers, and the longest span from north to south is 23.5 kilometers. The Jin-Pu Railway runs through the north and south from the middle of the border region, and the Huaihe River transits from west to east and south. Most of the jurisdiction is located at the southern end of Huaibei Plain.

Bengbu City is a transitional zone between the Huang-Huai-Hai Plain and the Jianghuai hilly area, at the end of the Jianghuai watershed. The territory is dominated by plains, with hills scattered in the south; The northwest of the ground tends to the southeast, and the natural slope drops to about one in ten thousand. Most of the urban areas are located on the south bank of Huaihe River. In addition to the isolated one in the city center, there are more than 20 mountains in the east, south and west of the city. In the urban area of 445.4 square kilometers, there are 50 square kilometers of hills and mountains, and the water surface 15.3 square kilometers.

Landforms are mainly divided into three types: plains, hills and terraces. China's plains are dominated by the flood plains of the Yellow River, and there are also shallow lowlands between rivers, low terraces with hills in rivers and flood plains beside rivers. The platform is mainly distributed in the wavy area south of the river, and consists of loess of Qizui Formation, which is divided into flat hills and inclined hills. Bengbu hills are mainly distributed in the suburbs south of Huaihe River, which is the northern edge of Jianghuai hills.

Most of the bedrock in the hills is exposed by weathering and denudation, with occasional residual slope deposits, which are basically undeveloped and have thick bones. According to the ground height, it can be divided into high hills and low hills.

The surface water in Bengbu is mainly Huaihe River, with other small water systems in the north, Tianhe in the southwest, Baligou in the west and Zi Long and Baojiagou in the east. Small water systems, except the North Feihe River, are all combined with rivers and lakes, with short rivers and small water, which are often cut off in dry years. The groundwater in Bengbu basically belongs to the pervaporation type, and the lateral recharge generated by the surrounding terrain is very small, and the static reserve of groundwater is about 320 million cubic meters.

The south bank of Huaihe River belongs to poor water area, and the north bank belongs to rich water area. Groundwater occurrence types can be divided into Quaternary Holocene pore water and bedrock fissure water.

Bengbu city is relatively poor in mineral resources, and the main mineral resources are coal mine, iron mine, gold mine and limestone mine for cement. There are 276 mineral deposits in the city, and there are 23 kinds of minerals (including subspecies), including energy minerals (coal) 1 species, metal minerals (iron, rock gold, placer gold, copper, lead, zinc and silver) 7 kinds, non-metal minerals 13 kinds and water-gas minerals (groundwater and mineral water) 2 kinds.

The scale of the deposit shows that there are many small mines and few large ones. There are 4 large-scale deposits (3 coal mines, underground water source 1), 8 medium-sized deposits (including mineral water) and 62 small-scale deposits, and the mineral area below the small-scale deposits accounts for 73. 19% of the discovered mineral area. Non-metallic mineral areas account for 9 1.64% of the total mineral area. Clay minerals for brick and tile 179, accounting for 65.09% of the total mineral area; There are 26 limestone mines for building stones, accounting for 9.45% of the total deposits.

References:

Baidu encyclopedia-Bengbu