In Mianyang at night, you can go to Tieniu Square to see the night view, take a Sanjiang cruise in Youth Square, and take a stroll in People's Park.

The light shows on both sides of the Fujiang River can reflect the night view of Mianyang that does not belong to the Victoria Harbor. From a distance, you can see the Yuewang Tower next to the Dongfanghong Bridge, the Fule Pavilion opposite the Third Bridge, and the Nanshan Mountain where the purple energy comes from the east. You can also overlook the night view of the entire city from the rooftop of the city, such as the rooftop lounge of Hanwei City Center.

Fucheng District has a lot of delicious food. In the evening, you can have a cold cup in many food streets such as Majia Lane, Tong'an Lane, Shunheqian Street, Jian'an Street, etc. You can also have a big meal at Lao Tea Tree, Dongtian No. 1, 1958 and other places. Of course, there are also CapitaLand Food City, Wanda Plaza, etc. For entertainment, there are KTV, high school and low-end, as well as bar performances and so on. Mainly located in Linyuankou, Jinzhuyuan and other places, there are also theaters in major shopping malls.

Mianyang Geographic Environment

Mianyang City is located in the northwest of the Sichuan Basin, in the middle and upper reaches of the Fujiang River. It borders Qingchuan County and Jiange County of Guangyuan City to the east and the southern counties of Nanchong City and Xichong County. It borders Shehong City and Daying County of Suining City in the south. It borders Luojiang District, Zhongjiang County and Mianzhu City of Deyang City to the west. To the northwest, it borders Jiuzhaigou County, Songpan County, and Mao County in the Aba Tibetan and Qiang Autonomous Prefecture, and Wen County in Longnan City, Gansu Province.

Mianyang City has relatively complete stratigraphic development, complex rock formations, and large changes in lithology and lithofacies. Multiple structures are inherited, interfered with, and superimposed in multiple phases, making the structure extremely complex. Late magmatic activity and regional metamorphism are weak, sedimentary mineralization is strong, and endogenous mineralization is weak. Bounded by the Jiangyou fault, it spans two primary structural units.

Reference for the above content: Baidu Encyclopedia—Mianyang