What are the attractions in Mount Tai? What are the cultural landscapes in Mount Tai?

Mount Tai, also known as Daishan, Daizong, Daiyue, Dongyue and Taiyue, is located in the central part of Shandong Province and is affiliated with Tai'an City. It stretches between Tai'an, Jinan and Zibo, with a total area of ??24,200 hectares. . The main peak, Yuhuangding, is 1,545 meters above sea level. It is majestic and majestic. It is known as the "first of the five mountains", "the longest of the five mountains", the respect of the five mountains and "the first mountain in the world". It is a world natural and cultural heritage, a world geological park, a national AAAAA tourist attraction, a national scenic spot, a national key cultural relic protection unit, and a national civilized scenic tourist area. ?

Mount Tai was regarded by the ancients as a paradise that "directly leads to the throne of the emperor". It became a sacred mountain worshiped by the people and a sacred mountain for emperors to offer sacrifices. There is a saying that "if Mount Tai is safe, all the world will be safe". From the beginning of Qin Shihuang to the Qing Dynasty, 13 generations of emperors visited Mount Tai to worship or offer sacrifices in person, and 24 generations of emperors sent officials to offer sacrifices 72 times. ?

More than 20 ancient building groups and more than 2,200 steles and stone carvings have been left on the majestic mountain of Mount Tai. Taoism and Buddhism regard Mount Tai as the "Fairy Mountain Buddha Country", deify Mount Tai, and build a large number of palaces and temples on Mount Tai. ?

The six major scenic areas of Mount Tai:

The Mount Tai Scenic Tourist Area includes six major scenic areas: You District, Kuang District, Ao District, Miao District, Xiu District and Li District.

The Four Wonders of Mount Tai;

The best time to visit Mount Tai is from May to November every year. Visit Mount Tai to see four wonders: sunrise on Mount Tai, jade plate in the sea of ??clouds, sunset glow, and golden belt of the Yellow River.

Yin and Yang Realm

On the stone flat south of the Changshou Bridge in Mount Tai, at the top of the East Baizhang Cliff, there is a light white rock belt spanning the vertical river valleys on both sides, like a white stripe embroidery On the edge of the cliff, due to the erosion of water for many years, the surface is as smooth as a mirror, with bright colors and very eye-catching. If you are not careful when crossing it, you will lose your footing and fall down the cliff, falling into the valley and dying, so it is called the "Yin and Yang Realm".

The stone flat under the bridge is made of medium-grained gneissic monzogranite from Mount Aolai. It is hard in texture and has strong resistance to weathering and erosion. After long-term weathering and erosion and erosion by streams, it has formed such a wide and smooth stone flat. Dashiping. The so-called "Yin Yang Boundary" is actually a granite vein composed of feldspar and quartz. The surface is gray-white and the vein width is 1 to 1.2 meters. It extends along the southeast 130° direction and is nearly upright in the monzogranite. In the middle, the boundary with the surrounding rocks is very clear. The occurrence is stable, linearly spread, and the colors are bright. It is also located on the edge of the cliff of Dongbaizhang Cliff, and the terrain is very steep. The ancients regarded this rock vein as the dividing line between the Yang world and the underworld. ?

Taohuayu

Taohuayu is located in the northwest of Daiding. There is a cable car that leads directly to Daiding. The rocks exposed around the cableway station are mainly medium-grained gneissic monzogranite from Mount Aolai. The northwest-trending Longjiaoshan fault passes through it on its east side, and associated faults that are basically parallel to it develop on both sides of the fault. One of the associated faults cuts through a mountain top, creating a joint-intensive zone about 5 meters wide. The joint surfaces are nearly upright, cutting the monzogranite into many thin plate-shaped rock blocks. Under the action of gravity, the rock blocks continue to collapse along the upright joint surfaces. In the end, a large crack several meters wide was formed where the two peaks faced each other. This is the famous Taohuayu Yixiantian.

Caishixi is not only an important source of strange rocks in Mount Tai. According to the investigation of Taishan staff, it is believed that there is a set of basic amphibolite (basic volcanic rock) in Caishixi. The epicrust rock system belongs to the Taishan Rock Group. The original rock is acidic volcanic rock and acidic volcanic tuff, forming a bimodal structure. Due to strong deformation, the basic volcanic rock has been pulled into structural patches, and its structural deformation has been cut off by later stages, and later veins have been cut off. In addition, there is the phenomenon of mylonitization, and the geological phenomena such as structure and stratigraphy are very rich. ?

Aolai Peak

To the west of Fanzi Cliff is Aolai Peak. Because of its majestic protrusion, it has the potential to compete with the main peak of Mount Tai. There is an ancient folk proverb: "Aolai is high, Aolai is high." "Lai Gao is on par with Dai when viewed from afar, and is on the mountainside when viewed from a distance." The junction of Aolai Peak and Fanzi Cliff is the mountain pass. Behind the mountain pass is Qingtong Stream, which is unpredictable. To the north of the stream is Huping Cliff, a dangerous cliff thousands of feet high. Standing at the mountain pass, looking at Fanzi Cliff to the east, it looks like half a ruined wall, crumbling, which makes people dizzy. Looking to Aolai Peak to the west, it seems to be connected to the heaven. Looking to Huping Cliff to the north, the cliff reaches into the clouds. The rocks exposed in Fanzi Cliff and Aolai Peak are all medium-grained gneissic monzogranite in Aolai Mountain.

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