Travel strategy of two days and one night in Changsha, Hunan Province

Two-day and one-night travel guide route in Changsha, Hunan: Orange Island in Changsha-Taiping Old Street-Fire Palace-Huangxing Pedestrian Street-Yuelu Mountain-Hunan University.

Changsha, also known as Xingcheng, is a prefecture-level city, provincial capital and megacity under the jurisdiction of Hunan Province. It is an important central city in the middle reaches of the Yangtze River approved by the State Council and a member city of Changsha-Zhuzhou-Xiangtan metropolitan area. It is also a national experimental zone for comprehensive reform of two-oriented society, an important grain production base in China, an important node city in the middle reaches of the Yangtze River and the Yangtze River Economic Belt, an integrated transportation hub and a national logistics hub. By the end of 2022, Changsha has 6 municipal districts, with 65438+.

Changsha is one of the first national historical and cultural cities. Three thousand years later, its name and location remain unchanged. Known as the hometown of Qujia, the famous city of Chu and Han, and the hometown of Xiaoxiang bamboo silk. There are Mawangdui Han Tomb, Siyang Fangzun, Three Kingdoms Wu Bamboo Slips, Yuelu Academy, Tongguan Kiln and other historical sites. , condensed the practical and eclectic Huxiang culture.

geologic feature

The geological characteristics of Changsha are: the strata are completely exposed, the granite bodies are widely distributed and the geological structure is complex. Various geological and historical strata are exposed in Changsha, and the oldest stratum was formed about 1 100 million years ago. About 600 million years ago, Changsha was still a sea of Wang Yang, but the sea was not deep.

After that, the sea gradually withdrew from east to west, and most areas of Liuyang, Changsha and Wangcheng surfaced, becoming the northwest edge of Jiangnan ancient land. About/kloc-0.40 billion years ago, the seawater immersion in Changsha area ended and rose to land. Due to the influence of crustal movement and geological structure, a long-strip intermountain depression basin-Chang (Sha) Ping (Jiang) basin has been formed. Since Cenozoic, the whole Changping basin has risen to land. About 3.5 million years ago, the third ice age occurred on the earth, and Liuyang preserved the remains of glacial landforms.

Reference to the above content: Baidu Encyclopedia-Changsha