Detailed road map and scenic spots of Mount Tai

The road map and scenic spots of Mount Tai are detailed as follows:

I. Route

1, half-day tour

It is suitable for arriving at Mount Tai scenic spot in the morning, shooting the sunrise in Nantianmen, then visiting Wuyue Hall on foot or by cable car, and finally descending from Hong Men.

2. One-day tour

Morning: The tour guide leads the tourists to climb the mountain, go to Nantianmen to enjoy the beautiful scenery such as sunrise and sea of clouds, and then take the cable car to Yuhuangding to visit Wuyue Hall, Tianjie and Huang Yu Temple.

Afternoon: Visitors can have free activities, enjoy the mountain scenery and experience local specialties.

Step 3 travel on weekends

It is recommended to choose a two-day tour for the weekend tour. Arrive at Taishan scenic spot on the first morning, complete the half-day tour or one-day tour route, and stay near Taishan scenic spot at night. The next morning, continue to visit other scenic spots in Mount Tai, such as Jiuhua Mountain and Dai Temple.

Second, the details of scenic spots

Nantianmen 1

Nantianmen is located at the southern foot of Mount Tai, which is the only way to climb the mountain. Here, visitors can enjoy the magnificent scenery of Mount Tai, especially the sunrise and the sea of clouds. The scenery is even more shocking and it is an excellent place to take beautiful photos.

2. Wuyue Hall

Wuyue Hall is located in Jade Emperor Peak, the main peak of Mount Tai. It is an ancient architectural complex with triple halls, which is mainly used to worship the five gods. The statues, murals and other buildings in the temple are exquisite and have a long history, which is worth seeing.

3. Yuhuangding

Yuhuangding is the main peak of Mount Tai and the highest peak in China, with an altitude of1545m. It is a great honor to climb the top of Mount Tai. Looking down from the top of the mountain, the scenery is very shocking and refreshing.

Geological characteristics of Mount Tai

The geological structure of Mount Tai is very complex, mainly faults, and its structural feature is the inclined uplift of fault blocks. There are structures formed in Precambrian, Mesozoic and Cenozoic.

The Precambrian geological structure of Mount Tai is characterized by multi-stage folds, faults and ductile shear zones. They are superimposed and transformed with each other, forming extremely complex structural features, and the study of their genetic mechanism is one of the important contents of Precambrian geological research. In addition, the rare "tubular structure" of Mesoproterozoic diabase porphyrite at home and abroad has high scientific value.

From the perspective of regional structure, the strong subduction of the Pacific plate to the Eurasian plate in the near east-west direction made the Taishan area tilt strongly to the front fault in the near north-south direction, and Taishan rose sharply, which made the neotectonic movement of Taishan very common and intense, and they played a leading role in controlling the formation and geomorphological pattern of Taishan. The gravity sliding structure formed on the unconformity surface of lower Paleozoic and Precambrian crystalline basement around Mount Tai is also closely related to neotectonic movement.

Reference to the above content: Baidu Encyclopedia-Mount Tai