Which city does Taihu Lake belong to?

There are five cities in Taihu Lake: Wuxi, Suzhou, Changzhou, Huzhou and Jiaxing. Taihu Lake is bounded by Wuxi to the north, Suzhou to the east, Jiaxing to the southeast, Huzhou to the south. Huzhou is named after Taihu Lake, and Changzhou is to the northwest. There are five major cities surrounding Taihu Lake, also known as the Taihu Lake Economic Belt. The entire Taihu Lake spans Jiangsu and Zhejiang provinces, but the waters belong to the Jiangsu plate, making Taihu Lake the largest freshwater lake in Jiangsu Province.

Taihu Lake is a large shallow lake in the plain water network area. The lake area is known to have 48 islands and 72 peaks. Wuxi landscapes, Suzhou gardens, Dongting Dongshan and Xishan in Wuxian County, and Yixing Dongtian World are all famous tourist attractions in the Taihu Lake area.

The Taihu Lake Basin has a mild climate and abundant specialties. It has been a famous land of fish and rice since ancient times. Taihu Lake is rich in aquatic products, rich in fish

Shrimp. There is a saying that "Taihu Lake is 800 miles away, and there are endless fish and shrimps to catch". In 1982, Taihu Lake was approved by the State Council to be included in the first batch of national scenic spots in the name of Jiangsu Taihu Scenic Area.

Through several years of sampling and identification and field geological surveys on Sanshan Island in Taihu Lake, the existence of volcanoes was discovered and confirmed: there are explosive breccias, primary secondary eruption tuff breccias and Weakly fused glassy tuff, etc. The north and west of Sanshan Island are covered with volcanic breccias and volcanic bombs, which have all been silicified into flint, chalcedony, agate, etc. A geological section of volcanic eruptions was found in Dongbo Hill, with an eruption age of 50 million years. the end of the Cretaceous period before. Volcanic activity is the result of magmatic activity within its depths.

Magma and volcanic activity reduced the underground thermal pressure and bulk density of Taihu Lake and its surroundings, generating negative pressure. As a result, the area experienced slow subsidence in the Cenozoic. Taihu Lake and its surrounding lakes were all formed by volcanic eruptions of the same origin and cause. formed a land subsidence lake.