Excuse me, who has a tour guide for Wuyuan, Sanqingshan, Jiangxi? The more detailed, the better! thank you

Wuyuan-the most beautiful village in China!

1 Wuyuan Huizhou architecture

Second place Wuyuan natural ecological scenery

3 rd Wuyuan folk custom

Note that at this time, the red leaves in Shicheng are also a highlight.

Wuyuan is very suitable for photographers to shoot, for teachers and students in art colleges or writers to sketch, and for the elderly to take a leisure vacation. Wuyuan is full of pollution-free villages with beautiful environment. )

Sanqingshan

The beauty of Sanqingshan lies in its "three wonders" in nature and scenery: "the goddess of spring", "the python comes out of the mountain" and the west coast. There are many ancient buildings on Sanqing Mountain, most of which were built in the Ming Dynasty. Up to now, more than 50 ancient buildings and more than 200 stone carvings have been preserved, most of which are precious cultural relics of the Ming Dynasty. Such as Sanqing Palace, Leifeng Tower, Nantianmen, Longhu Hall, Jiutian Yingyun Building, Feixian Platform, etc.

The ropeway from 50 yuan to 40 yuan takes 38 minutes. It takes about two hours to walk up the mountain. There are stone steps in the scenic spot, so be careful when walking at night. There are many shade trees on the hiking route, so it is not hard to walk in midsummer. Therefore, it is recommended to walk down the mountain.

Sanqingshan Mountain is located in Dexing City in the northeast of Jiangxi Province.

Yushan county junction. Its geographical position is north latitude.

28 54', east longitude118 03', near zhejiang-jiangxi railway.

Road trunk line. In ancient times, Rao, Xin and Qu met, but today is.

A pearl on the East China Travel Network is the countryside.

Key scenic spots.

Sanqingshan is in the east 144 km and south of Quzhou, Zhejiang.

Wuyishan City, Fujian Province, 1 15km, 78km west of Shangrao City.

It is 263 kilometers north of Huangshan City, Anhui Province. Panorama of scenic spot

Covering an area of 220 square kilometers, the central scenic spot is 7 1 square kilometer.

The highest main peak, Yujing Peak, is 18 16.9 meters above sea level. Sanqingshan

The car body is 12.2km long from north to south and 6.3km wide from east to west, with flat terrain.

The face is lotus leaf-shaped and inclines from southeast to northwest.

Sanqingshan Mountain is constantly rising due to frequent and intense orogeny, dense faults and developed joints.

After a long period of weathering and erosion and the disintegration of gravity, the spectacular mountain scenery of Qifeng Weird Valley has been formed. Sanqingshan east danger, west

Strange, the beauty of the north, the beauty of the south, the beauty of simplicity and nature, the wonder of both form and spirit, full of fairy tales, lifelike, inviting you to visit the ethereal realm, which makes people linger.

In the fog, it is a paradise of ancient Taoism. There are countless strange peaks and rocks on the mountain, and the clouds are lingering, which is amazing and rare in the world.

You see, Lingquan Waterfall is comparable to single crystal Yu Ye, and the caves in the valley are the places where the phoenix rises and the crouching tiger hides the dragon. Palace architecture in past dynasties and magnificent dangerous buildings

The natural landscape is seamless and colorful, and Zhong Ling has beautiful scenery, so it has the reputation of "the first fairy peak in the world and the blessed land of chinese odyssey".

The magical and magnificent landscape of Sanqingshan is inseparable from the suitable geological climate, which is a long-term change of crustal movement on geological function.

Products. Sanqingshan Mountain has experienced1400 million years of geological historical vicissitudes, with three transgressions and many geological tectonic movements.

The first seawater immersion occurred in Mesoproterozoic1400 million years ago. At that time, the crustal movement in Sanqingshan area was in the "geosyncline" subsidence.

At this stage, the seawater was submerged for 400 million years, and the Shuangqiao Mountain Group flysch marine clastic rocks with a thickness of several thousand meters were deposited, mixed with submarine volcanoes.

Break out. After the Jinning Movement, the history of geosyncline subsidence ended, and the crust began to gradually return to rise, and the land flowed out.

Qingshan area has entered a relatively stable "platform" stage. Since then, the crust has still fluctuated, but the settlement speed is moderate and the range is wide.

At the end of Sinian 600 million years ago, the second sea immersion occurred, which lasted for 65.438+0.6 billion years and continued until Ordovician.

At the end of the 20th century, shallow-sea sand shale and carbonate rocks with a thickness of more than 4,000 meters were deposited, including marine paleontology such as trilobites, graptolites and sponges.

Fossil. The above two trips into the sea turned Sanqingshan headquarters into the sea of Wang Yang. After the Ordovician, "Caledonian was the first"

Curtain "orogeny, Sanqingshan completely out of the seawater environment, no longer accept deposition.

In the early Silurian 440 million years ago, although there was a third sea immersion, the seawater only reached the edge of the southeast corner of Sanqing Mountain.

Part. Until1.800 million years ago, an unusually strong orogeny occurred in the Late Jurassic and Cretaceous and the Sanqingshan area, that is, the Yanshanian period.

Movement, accompanied by large-scale acid magma soaking activities, thus laid the geological foundation of Sanqingshan landscape.

In the years from 20 million to 30 million years ago, Himalayan orogeny, that is, neotectonic movement, occurred one after another, and the mountains were greatly raised.

Uplift, accompanied by strong undercutting of hydraulic erosion, makes the terrain height difference disparity. Because the geological environment of Sanqingshan is in orogeny.

In areas with frequent and intense movements, faults are dense and joints are developed, especially vertical faults and joints. Shanzibo

Fault uplift, long-term weathering and erosion, coupled with gravity disintegration, have formed a strange landform in which peaks and mountains are inserted into the sky and valleys sink into the abyss. Sanqingshan wind

The formation of scenic spots can be said to be a masterpiece of nature.