Jinhua has a long history of organizational system. It was an ancient place that crossed the land, and Qin entered Huiji County. Jinhua, known as Wuzhou in ancient times, was named because it was located in the land where Venus and martial women competed for China. Dongyang County has a history of 1800 years since it was established in the first year of Baoding in the Three Kingdoms.
1949, the eighth administrative region of Zhejiang Province was established; 10, renamed Jinhua area. 1968, changed to Jinhua area. 1985, Jinhua and Quzhou were upgraded to prefecture-level cities respectively.
There are Panda Mountain and Huiji Mountain in the east and northeast of Jinhua, Xianxialing Mountain in the south, Longmen Mountain and Ganligang Mountain in the north and northwest. Xianxialing Mountain Range extends from Wuyi Mountain at the junction of Fujian and Jiangxi to Wuyi County, southern Wucheng District and Yongkang City, and extends to the northeast as Panda Mountain and Tiantai Mountain Range. These mountains are mainly composed of volcanic rocks and granite.
Pan Da is the source and watershed of Qiantang River, Caoejiang River, Jiaojiang River and Oujiang River.
Huiji Mountain is a branch of Tiantai Mountain, with its main body extending to the northeast and southwest to the north of Dongyang and Yiwu. This mountain is mainly composed of volcanic lava and clastic rocks.
Dongbai Mountain, the main peak, is located at the junction of Dongyang, Zhuji and Shengzhou. Longmen Mountain is located between Fuchunjiang River and puyang river, distributed in Pujiang, Wucheng District, the northern part of Jindong District, Lanxi and the western edge of Yiwu. The mountain is mainly composed of Mesozoic volcanic lava and clastic rocks, with granite and limestone in some areas. The rest of the veins in Jin Huashan are massive mountains, and the wharf basin in the north is connected with Longmen Mountain.
Qianligang Mountain Range extends from Huaiyu Mountain Range in the northeast of Jiangxi to the junction of Lanxi and jiande city. The mountain is composed of sedimentary clastic rocks, with Ganligang sandstone in the middle.
The mountain system extending into China is controlled by Cathaysian structure, and most of them are northeast-southwest trending. At the same time, it is cut by the northeast-southwest and east-west fault zones, and many branches extending outward crisscross, with broken mountains and staggered peaks.