Xinfeng County, Ganzhou City, Jiangxi Province

Xinfeng County is a county under the jurisdiction of Ganzhou City, Jiangxi Province. It is located in the middle of Ganzhou, Jiangxi Province, in the middle reaches of Taojiang River, a tributary of Jugong water, covering an area of 2878 square kilometers. It has jurisdiction over 16 townships and a provincial high-tech industrial park. At the end of 2018, 779 thousand and 371 registered residence population.

Xinfeng County has coal, limestone, Maifanshi, rare earth, tungsten and other mineral resources; 470000 mu of arable land, including 388000 mu of paddy field; 3.02 million mu of mountainous area, mainly producing grain, tobacco, fruit, mushroom, melon, vegetable, sweet corn, tea and pigs, cattle, poultry, etc. Xinfeng County is a national commodity grain base county, which has been listed as more than 10 national agricultural bases, known as "China's navel orange town", "China's orange town" The hometown of straw mushroom. Xinfeng County was established in the first year of Yongchun (682) of the Tang Dynasty. It is a famous historical and cultural city in Jiangxi Province. It is one of the 21 red counties in the former Central Soviet area. It is the location of the first blockade of the Red Army in the long march. It is the core area of the three-year guerrilla war in the south. There is a national key cultural relic protection unit - "the first song Pagoda in Jiangnan" - Dasheng Temple Pagoda. In March 2019, it will be listed in the first batch of counties for the protection and utilization of revolutionary cultural relics.

In 2019, the GDP of Xinfeng County will reach 23.491 billion yuan, an increase of 8.3% over the previous year.

Historical evolution

The spring and Autumn period belongs to Wu.

During the Warring States period, it belonged to Chu.

In the Qin Dynasty, it belonged to Jiujiang county.

In the Han Dynasty, it belonged to Yuzhang Prefecture

The Western Jin Dynasty belongs to Nankang county.

In the Sui Dynasty, it belonged to Qianzhou.

In the Tang Dynasty, the first year of Yongchun (682) was divided into Nankang county and Nanan county. In the first year of Tianbao (724), because of the same name as Nan'an County, Quanzhou, Fujian Province, it was renamed Xinfeng, which means "renxinwufeng" and belongs to Nankang county.

Song Dynasty, Kaibao eight years (975) belong to Qianzhou. The first year of Shaoxing (1131) belongs to Ganzhou.

In the Yuan Dynasty, it belonged to Ganzhou road.

The Ming and Qing Dynasties belonged to Ganzhou Prefecture.

The fourth year of the Republic of China (1915) belongs to Ganzhou road.

In 1926, it directly belonged to the province.

In 1932, it belonged to 12 administrative regions.

In 1935, it was the fourth administrative region.

It was liberated on August 16, 1949 and belonged to Ganzhou special region (later southwest Jiangxi Administrative Region).

In 1954, it belonged to Gannan administrative region.

In 1964, it belonged to Ganzhou special region.

In 1968, it belonged to Ganzhou area.

In 1999, it was a prefecture level Ganzhou City.

Ganzhou Songcheng ancient charm

administrative division

On April 5, 1987, Jifu Township, Tieshi Township and Daqiao Township were abolished and TieShiKou town and Daqiao town were set up instead. Five administrative villages in Tongyi Township, including Shuidong, Changsheng, Huayuan, Tongyi and Shuibei, were transferred to Jiading town (reply No. 165 of Gan Fu Ting Zi).

On December 10, 1988, Xiaojiang Township, Xintian Township, Gupi Township, Dahe Township, Datangbu Township and Anxi Township were abolished, and Xiaojiang Town, Xintian Town, Gupi Town, Dahe Town, Datangbu town and Anxi town were established (GaN min Han No. 138 reply).

On November 23, 1989, Youshan township was abolished and Youshan town was established (reply No. 149 of ganmin Zi).

On August 18, 1994, Xiaohe township was abolished and Xiaohe Town was established (GaN min Zi No. 130 reply).

On May 9, 2001, Tongyi Township and longshe Township were abolished and assigned to Jiading town; Pingshi township was abolished and assigned to Datangbu town; xiaojinpenshan township was assigned to Gupi town; Huangni Township, Xingcun Township and Xiniu Township were abolished and merged to form Xiniu town; Jiudu Township and Zhengping Township were abolished and merged to form Zhengping town (GaN min Zi No. 201 reply).

At the end of 2004, Xinfeng County had jurisdiction over 13 towns and 3 townships: Jiading town, Datangbu Town, Gupi Town, Daqiao Town, Xintian Town, Anxi Town, Xiaojiang Town, TieShiKou Town, DAA Town, Youshan Town, Xiaohe Town, Xiniu Town, Zhengping Town, Hushan Town, Chongxian town and Wanlong town. There are 28 neighborhood committees and 260 village committees. An industrial park management committee.

geographical environment

Location and territory

Xinfeng County is located in the middle of Ganzhou, Jiangxi Province, in the middle reaches of Taojiang River, a tributary of Jugong water, covering an area of 2878 square kilometers. It is adjacent to Anyuan County in the East, Longnan City, Dingnan county and QUANNAN County in the south, Nanxiong City in Guangdong Province in the West, Dayu County in the northwest, Nankang district and Ganxian District in the north.

geology

The geology in Xinfeng is complicated due to a series of crustal tectonic movements. In the structural position, it is located at the confluence of the East-West structure and the depression belt of the Xinhua Xia system, and it is located in the two wings of the Shanzi type forward extension in southern Jiangxi and the west side of the horseshoe type geology. Based on the analysis of the structural features and their relationship, it can be roughly divided into the East-West Huaxia system, the Xinhua Xia system, the northwest and North-South structural systems or belts, among which the NE, NNE and NW faults are the most developed, followed by the East-West faults. From the strength and density of folds and faults, they are strong in the South and weak in the north, strong in the East and weak in the West. For these reasons, the formation of polymorphic geological characteristics.

Except Ordovician, Silurian, Lower Devonian and Tertiary strata in Xinfeng County, other strata from Paleozoic to Cenozoic are exposed. The Sinian, Cambrian and middle upper Devonian strata are mainly exposed around the red bed basin, forming a low mountain and hilly terrain; the Carboniferous and Permian strata are exposed at the edge of the red bed basin, island like and banded sporadically; the Triassic and Jurassic strata are exposed in TieShiKou, Gaoqiao, Xintian and Jinji, respectively; the Cretaceous strata have the largest distribution area, forming low hills Quaternary system is developed in Taojiang River and its main tributaries and valley basins.

There are more than 10 intrusive rocks in Xinfeng County, which are mainly late Caledonian and early Yanshanian intrusive rocks. The former is exposed in Niujing and Zhengping to TieShiKou, and its lithology is mainly medium fine grained hornblende quartz monzonite and medium fine grained monzonitic granite; the latter is widely distributed, and it is exposed in Anxi, jinpenshan and Hushan, and sporadically in other places, and its lithology is mainly granite (medium grained porphyritic biotite granite, fine grained granite, medium grained biotite granite and granite porphyry granite) They are mainly composed of granite, medium and fine grained mica granite. In addition, there are some basic acidic extrusive rocks in the area.

terrain

The terrain in Xinfeng is inclined from south to north, high around and low in the middle. The highest is at the east of Hushan mountain, with an altitude of 1015.7 meters; the lowest is at Wuyang village, Xiniu Town, with an altitude of 135 meters; generally, the altitude is between 200 and 400 meters. The edge of the county is rugged and rugged. Taojiang river runs through the north and South in the central part, with tributaries converging, and the water level is gentle. In the central part of the territory, there are about 600 square kilometers of low hilly ports, gentle slopes, wide valleys and fields.

The general topographical structure is as follows: the East, South and northwest are medium and low mountains, the southwest and North are low mountains and hills, and the central region is mostly low hills and plains, thus forming a South to North sloping terrain.

The topography of Xinfeng County can be divided into two categories: Hilly Basin and high hilly area.

1、 Topography of Hilly Basin

climate

Xinfeng is located in the East Asian monsoon region, with mild climate, sufficient light, abundant heat and abundant rainfall. It belongs to the humid monsoon climate of the middle subtropical zone, with four distinct seasons, short spring and autumn, long summer and winter, short ice and snow period, long frost free period, less summer, hot summer and less severe winter. At the turn of winter and spring, it is mostly affected by Siberian dry and cold air, with changeable climate and continuous rain; in midsummer, it is mostly controlled by the Pacific subtropical high, with hot climate and little rain, and occasionally affected by typhoons; in autumn, due to the weakening of the Pacific subtropical high, it is crisp in autumn, often dry, with large temperature difference between day and night; in winter, the temperature gradually drops, with dry and cold climate and sometimes frost The frost appeared.

Seasonal changes

The terrain of Xinfeng County is complex, with heavy mountains around and low hills in the middle. Due to the complexity and diversity of topography and the redistribution of light, heat and water resources, the stereoscopic climate is obvious.

Spring is mild and rainy. According to the observation of the county meteorological observation station (county station for short), the average temperature in March is 14.0 ℃, 20.1 ℃ in April and 24.0 ℃ in May; while jinpanshan and Hushan Xiaozhai (310 meters above sea level) are located in mountainous areas. Spring comes later, with the average temperature in March being 13.9 ℃, 18.7 ℃ in April and 22.4 ℃ in May. From March to April, affected by the cold air, Xinfeng County has always had "cold spring". From March every year, it rains continuously and enters the rainy season. The average precipitation measured by the county station is 187.6 mm in March, 201.6 mm in April and 215.2 mm in May. In some years, there are torrential rains, and the water level of rivers and streams rises sharply, causing floods and waterlogging.

In summer, there is high temperature and thunderstorm. The average temperature in June is 26.9 ℃, 28.9 ℃ in July and 28.3 ℃ in August, which is high in white weather. The extreme maximum temperature over the years is 40 ℃, which is the hot season of the year. The average temperature of jinpenshan and hushanxiaozhai in remote mountainous areas is 24-26 ℃ from June to August, which is relatively cool. The average precipitation of Xinfeng station in June is 221.6 mm, 133.3 mm in July and 152.8 mm in August. Generally, the average precipitation in mountain area is more than that in valley plain area. The end of flood season in Xinfeng County is usually in early July, and the earliest year is advanced to the end of May. If there is rainstorm before the end of flood season, it is easy to form flood.

Autumn is warm and cool, and precipitation is scarce. The average temperature in September is 25.4 ℃, 21.1 ℃ in October and 15.9 ℃ in November. The average temperature of hushanxiaozhai is 23.3 ℃ in September, 19.0 ℃ in October and 14.0 ℃ in November. The first year is September 26, the average date is October 12, and the latest year is November 3. The precipitation in autumn is rare, and there are often autumn droughts. In some years, there are summer droughts and even autumn droughts. The average precipitation of the county station in September is 92.9mm, and that in October is 48mm

Chinese PinYin : Jiang Xi Sheng Gan Zhou Shi Xin Feng Xian