Zhang Chi said, waved his hand to the house of the village and the house in the house. After the house just shake slightly, a large pit appeared on the ground in the room ...
The sky is not like the mountains, the scenery is picturesque. Here is an unexpected beauty. It is said that this is a banned place. As long as you enter the mountains, no one will believe it ...
After Zhang Chi left the Rolling Stone Village, he directly entered the Tiantian Mountain in the Top Ten Banners, because when he wanted to come, the three ancestors must enter the Sky Sama Mountain, otherwise there would be no clues ...
The ancient road is Yi Qingyu, the green pillow is green.
Water sounds and mountains lock fog, the past is thoughtful.
Yunyu is still twilight, fireworks spring and autumn.
Why should we cry?
There are poems again:
Last night, the sound of the apes was long.
Peach blossoms fly green water, go to Qutang in March.
The rainy wind blows away, and the south walks to the country.
Gaoqiu Wang Erzhou, visit Gu Yizhan.
Tianban Mountain is also called the place where heaven is banned. It is located in the northeast of the Tianhan Empire and the region is vast. Some of them have penetrated into the territory of the sky. From the Tianhan Empire, enter the Shanshu Mountain.
Deep in the mountains ...
The clouds are lingering all year round, the clouds are deep and dense, and the mountain high road dangerous pit is deep.
According to the historical records of the mainland, in the ancient times, the Tianshan Mountain was part of the huge sink belt or the sea tank, and it accumulated a very thick mud matter and base volcanic substances.
Later, after the crustal movement, the fold bulge became a huge mountain system. At the same time, a series of fractures, magma activities and deterioration effects occurred, forming a Tianjin Mountain Miscellaneous Rock composed of various deterioration miscellaneous rocks and magma rocks.
The ancient Tianbaba Mountain standing on the sea level, after a long period of weathering and erosion, the terrain of Zhejiang became gentle.
In the early days of the ancient generations, the vast areas of the vast area of the northeast of the Heavenly and Han Empires declined sharply in the vast area bordering the northwest of the sky.
On the base of the ancient metamorphic miscellaneous rocks, a set of Cambrian, which is nearly two kilometers thick, the limestone of the Cambrian of nearly two kilometers.
At the end of the Chinese Olympic Tao, under the influence of the continuous movement of the crust, this area rose to the land as a whole, and experienced a long -term sedimentary interruption.
By the beginning of Zhongshi Charcoal, a short -term lifting alternation occurred. The Tianfu Mountain area was in the environment of time and sea. On the erosion surface of the Chinese Olympic Tao, it was deposited.
Later, the area of Tianfu Mountain continued to rise and entered the stage of development in the mainland.
During the middle of the middle generation, a break was generated in the southern foot of Yu Shan. The original ancient sky was abandoned in the northern Panpan.
By the new generation, the Tianshi Mountain continued to rise sharply. At the height of the mountain, all the sedimentation layers covered with ancient metamorphic miscellaneous rocks were eroded.
The metamorphic miscellaneous rocks formed more than 2 billion years ago were reappeared on the surface. Until the middle of the new generation, about 30 million years ago, the overall wheel of the mountains today was basically formed.
Later, under the continuous erosion, cutting and weathering of various external force geological effects, it gradually shaped into the magnificent and magnificent scenery of the Tianjin Mountains today.
The fracture of the southern foot of the Mesozoic Mountain in the Mesozoic generation tended to the south, with an inclination of more than 800 degrees. The north plate is the ancient mountains and rocks of the Tai ancient Tianshan Mountain.
The form of the fault.
Ten tens of meters to hundreds of meters from the fault, consisting of multiple faults and multiple fractures, and extending to more than thousands of kilometers. It has the characteristics of large gaps, extension, and complicated mechanics and multi -phase activities.
Since the formation of the Jurassic world, its activities have continued to modern times, causing the Tianshan Mountains in the North Pan to continue to rise and suffer, and the basin of the south plate has continued to decline and accept it.
It directly controls the formation and evolution of the Tianshan and Basin. It is the natural dividing line of the two, which plays a decisive role in the formation of the formation of the mountains.
As a relatively young blocking mountain system, Tianshan Mountain is the result of the continuous lifting and new structure movement of the Thai front break northern disk.
Under the influence of the new structural movement, the erosion and cutting effect of Tianban Mountain is very strong, and it has developed different types of erosion landforms.
Because the rise in the south slope of the Tianfu Mountain is far greater than that of the north slope, the erosion strength of the south slope is relatively strong, and the erosion landforms are relatively developing.
The corrosion structure is concentrated in Zhongshan around the main peak of Tianjun Mountain and the old platform, Huangshiya and Huangya Mountain, with an altitude of about 1,500 meters.
The rock properties that make up the mountains are mainly changing rocks and granite. It is the highest potential in the region, the largest increase in the area, and the strongest erosion and cutting.
Here the peaks are deep, the terrain is steep, and the maximum depth of cutting is 800 meters.
The corrosion structure is distributed in the sky forbidden peaks, the middle and Tianmen and the spicing mountain area. The altitude is between 700 meters and a relatively high height of more than 200 meters.
The erosion and cutting strength is slightly weaker than the main peak area. However, the terrain is still very steep, deep groove gorge, spire mountain head, sawtooth -shaped ridge, clueless peak, visible.
The lymous and erosion structure is mostly distributed in the cockle Guanshan to the Qingshan area of the northeast of the main peak. The altitude is generally 700 meters, and the relatively high height is more than 200 meters.
The erosion and cutting strength is medium, and the mountains are stretched. If the top is covered with thick layers of limestone, it often forms the "Fangshan" or "table -shaped mountain" with steep tops on the top of the four walls. It is called "Shang" locally.
The hills in the area around the Montech of Zhangxia, sometimes due to the erosion effect of limestone, can form a cave and "transparent mountain" solubility landform.
The solubility and erosion and erosion hills are mostly distributed in the Cambrian limestone area on the edge of the northern edge of the Tianshan Mountain. The altitude is between 500 meters.
The relative height difference is less than two hundred meters, the degree of erosion and cutting is relatively weak, the terrain is low and smooth, and the groove valley is not developed. It forms a "pig back mountain" with a dome spine. It is more common.
The tin erosion hills are mainly distributed on the edge of the low mountain south of the mountains. The large river to Hu Mountain and Huangqian are about 200 meters. The base rocks are mostly metamorphic rocks and granite. The erosion intensity is very weak.
, Multi -formation of Guqiu Ringling.
Under the influence of the new structure movement, Tianban Mountain not only develops various types of erosion landforms, but also formed many small or miniature landform landscapes.
Such as Dazhigou, Digou Lane, Kilnzigou, Sanchagou Gorge Land, Baizhang Cliff, Cliff Landfrogs of Fanzi Cliff.
And the dangerous and strange landform landscapes such as Tanaka Gutuka, in addition, Tianfu Mountain has many three -level micro -landforms. They are strong evidence of new constructive motion intermittent raising.
The first level of 分 第一: It is distributed on the southern foot of Tianfu Mountain, the Red Gate, Jinshan and Huangshan Highway. The altitude is 200 meters, forming a ripple -shaped hill, which is equivalent to the level of the plane of the urban period in North China.
The second level of the flat plane is distributed on the gentle ridge of the Fanziya and the Moto Ridge, with an altitude of 800 meters, which is equivalent to the pyramid plane in Tangxian County, Beibei.
The third level of the plane is distributed on the top of the top and its surrounding mountains. The altitude is 1,500 meters, which constitutes a cap surface that is tilted north to the north, which is equivalent to the middle of the north and Lu in the middle of China.
Three turns occurred in the valley of the canyon on both sides of the north and south of the Dingding. For example, a canyon in the north of Shanbei is about 200 meters above it.
More than two hundred meters down, Gu Po is almost upright, up to about 20 meters. According to the 30 % off of the valley valley.
The canyon development process can be roughly divided into three periods of the upper section of the canyon, the lower section of the canyon and the formation of the Gulfu.
In addition, the phenomenon of turning in the stream lines on the vertical section of some gaps. For example, from the Black Dragon Pond on the West Road, the slope of the valley has gradually increased.
ten.
There are twelve degrees between the Huangxi River and the Yunbuqiao, and the slope of the bottom slope from the Yunbuqiao to the south Tianmen Valley has quickly changed to sixty degrees. This situation can also explain the phase of the new structure movement and its landform development of the Wushan.
Xiaolouyu in the northern part of Tianshan Mountain is revealed that the thick layer of limestone of the Zhangxia group in the Cambrian department is more significant in the dissolution in the stone rocks. There are many large and small caves develop.
They are distributed at different heights between 510 and 560 meters above sea level. The phenomenon of grading is very obvious.
The first -class cave is located between more than 510 meters above sea level. The second -level cave is between 550 meters above sea level. The third -level cave is located at a high place of 560 meters above sea level.
The peculiar landscape of the place is also the indirect and phased ideal example of the new structure movement of the Skytanic Mountains.
The third -level land of the river around the mountains is developed. Among them, the first and second -level land preservation is better, and the third -level land is mostly eroded and destroyed in the front of the mountain.
There are a lot of waterfalls in the Temple of Tianshan Tuling, which creates the beautiful scenery of the flowing mountains and waterfalls, such as the waterfalls of Heilongtan and Yunbaqiao.
Due to the intermittentity of the new structure movement, the multi -level nature of the waterfall is formed. Below Baizhang Cliff in Heilongtan, there are two small ponds at 30 meters and fifty meters, which together form a three -linked waterfall.
In Doutian's Shandong side ditch, Santan Lian Waterfall, which consists of three small drops of water, is about three meters per level. The pond waterfall is quite distinctive. It is known as "Tianchi Xiaoyue".
On this day, a sound of breaking through the sky passed, and then I saw a figure rushing into the mountains of the mountains ...
The shadow flashed quickly in the mountains, and the flying forward was not half a low -key in the mountains of the heavenly Han Empire ...
The consciousness is completely let go, looking for any clues that the three ancestors may have left. This is his last effort, otherwise he cannot explain why the three ancestors disappeared under the mountains ...
But just when Zhang Chi had just flew through two peaks, the world was suddenly dark, and then Zhang Chi's body fell to the earth instantly ...