Tongling epidemic prevention department phone

Tongling epidemic prevention department phone is 0562-2834659.

Epidemic in some parts of the country from time to time, to support and do a good job in the prevention and control of the new coronavirus infections everyone has a responsibility to prevent and control the epidemic of all people to participate in the fight against pneumonia everyone has a responsibility to do.

On the issue of epidemic prevention and control, I collected the online public outbreak prevention and control center hotline, you can consult the relevant departments, Tongling Tongguan District CDC, Tongling Tongguan District Health Commission.

Tongling

Tongling City, alias: Tongdu, is located in the south-central part of Anhui Province, the lower reaches of the Yangtze River, north of Hefei, south of Chizhou, east of Wuhu, west of Anqing, is a city under the jurisdiction of Anhui Province, as of the end of 2020, the total area of Tongling is 3008 square kilometers, as of February 21, 2022, Tongling under the jurisdiction of 3 districts and 1 county.

During the Xia and Shang dynasties, the Tongling area belonged to Yangzhou. After the Qin Dynasty unified China, Tongling belonged to Place County. During the Ming Dynasty, Tongling County belonged to the Chizhou Prefecture, which was directly under Nanjing. In the first year of the Republic of China (1912), the government was abolished in January, Tongling County is directly under the Anhui Province. 1914 June to 1928 August belongs to the Anhui Province Wuhu Road. 1932 after October belongs to the second special zone. 1938 August 6, changed to belong to the Eighth Special Zone until the liberation of Tongling. 1971 changed the special zone of Tongling for the city of Tongling, is the province directly under the jurisdiction.

Tongling's geotectonic position is in the Lower Yangzi Plateau of the Yangzi Quasi-Tectonic Plateau, or the eastern flank of the front arc of the Huaiyinshan Zigzag Tectonics. The strata exposed in the territory range from the Ordovician Upper Series to the Quaternary Series, with the development of folds and fracture structures, strong magmatic activity, and metamorphic rocks scattered around the intrusive rock body.