Beautiful Jiangxi is my home.

A beat of bamboo board,

Listen to me, Jiangxi,

Beautiful scenery, Lushan Mountain,

Sanqingshan, Longhushan,

Jinggangshan, the holy land of revolution.

A beat of bamboo board,

Listen to me, Jiangxi,

Poyang Lake, the kingdom of migratory birds,

Such as Qin Lake and Fairy Lake,

Dotted with Zhelin Lake.

Beautiful mountains and waters are even more beautiful.

Beautiful Jiangxi is my home.

Jiangxi:

Jiangxi, referred to as "Jiangxi" for short, is the provincial administrative region of China people, an important part of the Yangtze River Economic Belt, and the "land of plenty" in the south of the Yangtze River. In ancient times, it was called "Wutou Chuwei, Humin Pavilion in Guangdong", which was called Jiangxi for short because it was the largest river in the province.

Jiangxi is located in the southeast of China, bordering Zhejiang and Fujian provinces in the east, Guangdong province in the south, Hunan province in the west, Hubei and Anhui provinces in the north and the Yangtze River in the north. By the end of 20021,the province's area was166,900 square kilometers, with jurisdiction over1/districts and cities and 100 counties (cities, districts). There are 55 nationalities in this province.

Jiangxi natural environment:

Jiangxi is dominated by hills and mountains, and the basins and valleys are widely distributed, belonging to subtropical warm and humid monsoon climate. There are many rivers and lakes, with Poyang Lake as the center and a centripetal water system. It is also one of the provinces with a large distribution area of red soil in southern China. The vegetation is mainly evergreen broad-leaved forest, with typical subtropical forest plant community.

Geologically and geomorphologically, bounded by Jinjiang-Xinjiang line, the northern part belongs to Jiangnan uplift of Yangtze paraplatform and the southern part belongs to South China fold system. At the end of Silurian, they were merged by the late Caledonian movement, and then reformed by Indosinian movement, Yanshan movement and Himalayan movement for many times, forming a series of northeast-southwest structural belts.

A large number of granites invaded the basin in southern China, and red clastic rocks from Cretaceous to Paleogene were deposited, and gypsum and rock salt were deposited. A faulted basin centered on Poyang Lake has been formed in the northern region, and Quaternary laterite has accumulated in the piedmont area at the edge of the basin. This is the geological basis that causes the topography of the whole province to tilt to the north.

Geomorphologically, it belongs to the main part of Jiangnan hills. The province is surrounded by mountains in the east, west and south, with hills and valley plains in the middle and Poyang Lake and alluvial plains in the north. Poyang Lake Plain and Hubei Lake Plain are both subsidence areas in the middle and lower reaches of the Yangtze River, which are formed by siltation of the Yangtze River and five major rivers in the province. It is narrow in the north and wide in the south, covering an area of nearly 20,000 square kilometers.

The surface is mainly covered with laterite and river alluvium, and laterite has been cut and slightly undulating. Lake fields and lakes are also widely developed in the lakeside area. The water network is dense, the river bends are intertwined, and the lakes are dotted.