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Taihu (Chinese:太湖), also known asLake Tai orLake Taihu, is a lake in theYangtze Delta and the third largestfreshwaterlake[1] inChina. The lake is inJiangsu province and a significant part of its southern shore forms its border withZhejiang. With an area of 2,250 square kilometers (869 sq mi) and an average depth of 2 meters (6.6 ft),[2] it is thethird-largest freshwater lake entirely in China, afterPoyang andDongting.[a] The lake contains about 90 islands, ranging in size from a few square meters to several square kilometers.
Lake Tai is linked to theGrand Canal and is the origin of a number of rivers, including theSuzhou Creek. The major cities around Taihu Lake includeSuzhou,Wuxi,Changzhou andHuzhou. These urban areas form the core of the lake's cultural and economic region.[3] University-led hydrological and ecological studies note that these four cities are the primary urban centers surrounding the lake.[3]
Taihu Lake is officially designated as a national key scenic area under China's Major National Historical and Cultural Sites programme.[4]
View of Taihu Lake from the top of Baojie Mountain, overlooking Sanshan Island in Wuxi
Taihu Lake features 48 islands and 72 surrounding peaks, forming a distinctive landscape of "mountains beyond mountains, lakes within lakes."[5]
The area includes famous scenic locales such asYuantouzhu, Sanshan (Three Hills),Dongshan,Xishan, and Majishan.[5]
Bordering cities—Wuxi, theClassical Gardens of Suzhou, ancient sites of Wu culture, and the grottoes ofYixing—collectively form the internationally recognized Taihu Scenic Area.[6]
At a normal Wusong elevation of 3.00 m, the lake averages 1.9 m and reaches a maximum of about 2.6 m in depth, holding roughly 4.66 × 109 m3 of water. With an approximate inflow of 7.66 × 109 m3 annually, its waters renew several times a year.[9]
Scientific studies suggest that Lake Tai's circular structure is the result of ameteor impact, which resulted inshatter cones,shock-metamorphosedquartz,microtektites, and shock-metamorphic unloading fractures.[10] The prospectiveimpact crater has been dated to be greater than 70 million years old and possibly from the lateDevonian Period.[11] Research in 2012 suggested that present evidence shows no impact crater structure or shock-mineral at Lake Tai.[12] A more comprehensive study of soils in the lake in 2021 supported the hypothesis that the crater was instead formed by ameteor air burst high up, explaining the lake's shallowness.[13] Fossils indicate that Lake Tai was dry land until the ingression of theEast China Sea during theHolocene epoch. The growingdeltas of theYangtze andQiantang rivers eventually sealed off Lake Tai from the sea, and the influx of fresh water from rivers and rains turned it into a freshwater lake.
Three of the lake's islands are preserved as anational geological park under the nameSanshan. They are famed as a former haunt of local bandits.[citation needed]Mei Yuan is also located in Lake Tai, along withYuantouzhu. Yuantouzhu received its name ("Turtle Head Isle") from the shape of its outline.
The "Star of Lake Tai" is a giant, 115-meter (377 ft)ferris wheel on the shore of the lake.[14] Completed in 2008, it takes 18 minutes to complete one revolution. Passengers can enjoy the scenery of Lake Tai and the city center. At night, lighting effects are switched on around the wheel.
Yuantouzhu (Turtle Head Isle) is a prominent tourism site in Binhu District, Wuxi, situated between Taihu and Lake Li. Named for its turtle-head shape, it is referred to as “Taihu’s finest spot, indeed at Yuantouzhu.” The park was established in 1917, and wealthy locals built private gardens and villas nearby—including Hengyun Villa, Guangfu Temple, Taohu Villa, and Chen Garden. After 1949, these gardens were integrated into Yuantouzhu Park. In the 1980s, the park underwent master planning and expansion, adding over ten scenic spots—such as Chongshan’s Hidden Beauty, Deer Peak Sunrise, Spring Waves, and the Cherry Blossom Friendship Grove—spanning more than 500 ha, making it one of Jiangnan’s largest landscape gardens.[15]
Liyuan Garden is located on the shores of Lake Li (part of Taihu). The garden features Taihu-style rockeries, a thousand-step lakeside corridor with 89 carved windows, and lakeside embankments. Named after the historical figure Fan Li, the site commemorates the story of Fan Li and Xi Shi boating on Li Lake.[16]
Other famous scenic sites in Wuxi’s Taihu area include Sanshan Park, Plum Garden (Meiyuan), Xihui Park, the “Second Spring under Heaven,” and Jichang Garden.
Dongshan (East Hill of Dongting Lake) is a peninsula on Taihu surrounded on three sides by water. Its main summit, Mali Peak (293.5 m), is the second highest among Taihu’s peaks. The zone includes 11 islands such as Sanshan, Zeshan, and Jueshan. The town features preserved pavilions, Xi family gardens, and Ming-style nanmu halls, with other attractions like Zijin Temple and historic villages dotted throughout.[17]
Located in Zhenhu Subdistrict, Huqiu District, Suzhou,Taihu National Wetland Park spans 4.6 km² (2.3 km² open in phase I). It conserves lakeside wetlands with zones for fishing, ecological display, habitat protection, education, and recreation. The park contains over 50 bridges and opened to the public in 2010.[18]
The lake is known for its productive fishing industry and is often covered by fleets of small private fishing boats.[19] Since the late 1970s, harvesting food products such as fish and crabs has been invaluable to people living along the lake and has contributed significantly to the economy of the surrounding area.
The lake is home to an extensive ceramic industry, including theYixing pottery factory, which producesYixing clay teapots.
The Wujiang Water Regulation Stele records 29 major flood events in Taihu Lake from 1194 to 1954. The 1991 flood ranked second in farmland impact after the 1954 flood.[20]
Taihu's flood-control warning water level is 3.8 m, and the alert level at Wuxi's Grand Canal is 3.90 m. The regulated reservoir level is set at 4.65 m. The highest recorded average water level was 4.79 m on July 14, 1991, corresponding to a storage volume of 8.72 × 109 m3[20]
The Taihu Basin Authority oversees flood regulation through 59 sluice gates on surrounding outlets—including the Taipu sluice on the Taipu River (which discharges approximately 60% of floodwater), Yangwan Gate, Guajing Gate, Xin Kai River Gate, among others—extending into Yangtze and Huangpu systems.
The lowest inflow year on modern record was 1978, with an annual lake inflow of just 0.24 × 108 m3, approximately 0.46% of the average annual inflow.
Modern hydrological studies confirm that 1954 and 1991 rank as the two highest average annual lake levels over a 45-year continuous gauge record, correlating with regional precipitation and anthropogenic changes.[20]
Flood control in the basin is guided by long-term water level records and contemporary hydrological analysis performed by the Hydrology Bureau of the Taihu Basin Authority.[20]
Pollution of the lake has been ongoing for decades despite efforts to reduce pollution that were not sustained and thus proved ineffective. In the 1980s and 1990s, the number of industries in the lake region tripled, and the population also increased significantly. One billion tons of wastewater, 450,000 tons of garbage, and 880,000 tons of animal waste were dumped into the shallow lake in 1993 alone. The central government intervened and initiated a campaign to clean up the lake, setting a deadline to comply with pollution standards. When the deadline was not met, 128 factories were closed on New Year's Eve in 1999. Compliance improved somewhat afterward, but the pollution problem remained severe.[21]
In May 2007, the lake was overtaken by a majoralgae bloom and by major pollution withcyanobacteria.[22] The Chinese government called the lake a majornatural disaster despite the anthropogenic origin of this environmental catastrophe. With the average price of bottled water rising to six times the normal rate, the government banned all regional water providers from implementing price hikes.[23] (The lake provides water to 30 million residents, including about one million in Wuxi.[24]) By October 2007, it was reported that the Chinese government had shut down or given notice to over 1,300 factories around the lake. Nonetheless,Wu Lihong, one of the leading environmentalists who had been publicizing pollution of the lake, was sentenced to three years in prison for alleged extortion of one of the polluters,[22] but, undeterred, alleged in 2010 that not a single factory was closed.[25]
Jiangsu province planned to clean the lake;[26] chaired by then prime ministerWen Jiabao, the State Council set a target to complete the task by 2012.[27] However, in 2010The Economist reported that pollution had broken out again and that Wu Lihong, released from prison that April, was claiming that the government was trying to suppress news of the outbreak while switching to other supplies in place of lake water.[28]
^太湖 [Lake Tai].The Suzhou Science Window苏州科普之窗 (in Chinese). Science and Technology Association of Suzhou City [苏州市科学技术协会]. Archived fromthe original on June 11, 2007.
^Wang Erkang; Wan Yuqiu; Xu Shijin (May 2002). "Discovery and implication of shock metamorphic unloading microfractures in Devonian bedrock of Taihu Lake".Science in China Series D: Earth Sciences.45 (5): 459.doi:10.1360/02yd9048.S2CID195300513.
^Wang, K.; Geldsetzer, H. H. J. (1992). "A late Devonian impact event and its association with a possible extinction event on Eastern Gondwana".Lunar and Planetary Inst., International Conference on Large Meteorite Impacts and Planetary Evolution: 77.Bibcode:1992lmip.conf...77W.
^Dong; et al. (2012). "The Deformation Features of Quartz grains In the Sandstone of Taihu Area: Taihu Impact Origin Controversy".Geological Journal of China Universities.