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Where Mianyang plays at night.
Mianyang can go to Tieniu Square to watch the night scene, cruise in Sanjiang Square and stroll in People's Park at night.

The light show on both sides of Fujiang River can reflect the night when Mianyang does not belong to Victoria Harbour. From a distance, you can see Wang Yue Tower next to Dongfanghong Bridge, Fule Pavilion opposite the Third Bridge, and Nanshan coming from the east. You can also overlook the night view of the whole city from the roof of the city, such as the lounge on the top floor of downtown Han Wei.

Food has nothing to do with Fucheng District. In the evening, you can have a cold cup in Majiaxiang, Tongan Lane, Shunhe Qian Jie, Jian 'an Street and many other small food streets, and you can also have a big meal in Laoshushu, Dong Tian 1, 1958 and other places. Of course, there are Kaide Food City, wanda plaza and so on. Entertainment, KTV, high, middle and low grades, bar performances and so on. Mainly distributed in Lin Yuan Kou, Jinzhuyuan and other places, major shopping malls also have cinemas.

Mianyang geographical environment

Mianyang City is located in the northwest of Sichuan Basin, in the middle and upper reaches of Fujiang River, bordering Qingchuan County and Jiange County of Guangyuan City in the east and nanbu county County and Xichong County of Nanchong City in the east. It is connected to Shehong City and Daying County in Suining City in the south. It is adjacent to Luojiang District, Zhongjiang County and Mianzhu City of Deyang City in the west. The northwest borders Jiuzhaigou County, Songpan County, Maoxian County and Wenxian County, Longnan City, Gansu Province, Aba Tibetan and Qiang Autonomous Prefecture.

Mianyang city has developed strata, complex rock structure and great changes in lithology and lithofacies. Multi-period and multi-period structural inheritance and interference superposition, and the structural form is extremely complex. Late magmatism and regional metamorphism are weak, sedimentary mineralization is strong, and endogenous mineralization is weak. It is bounded by Jiangyou fault and spans two first-class structural units.

Reference to the above content: Baidu Encyclopedia-Mianyang