The Emperor's Life of a Wretched Man

"It's a pity that a young man like a fairy, Solo, don't blame me, you forced all of this, and at the same time, I didn't expect you to be so arrogant that you agreed to these three conditions.

Don't talk about the three conditions, even one of them, I think you are in a situation where you are dead but not alive, Ten Witches!The tribe is incompetent, so they can only use tricks..."

In the forbidden area in the center of the Great Wilderness of the Witch Clan, the Prophet's Palace at the foot of the Holy Mountain is decorated with lights and festoons to welcome Solo and his party. Now this garden-style palace building has become the residence of Solo and others.

Not long after Solo and others moved in, the twelve high priests of the Wu clan were officially announced by the prophet to be used under Wu Nier's account, and Solo also released the four elders of the Wu clan.

During this period, the Prophet of the Holy Mountain of the Wu Clan issued an announcement to the whole clan, announcing to the witches in the wilderness of hundreds of thousands of miles, that some high-ranking people came to the Wu Clan to redeem Wu Qingcheng, a pariah, and complete three miracles. If... so...

The policy of ignoring the people has made the whole Wu clan boil, and now a master named Solo has come, who wants to complete three tasks, swim on the East China Sea, remove the reverse scale of the dragon; climb to the top of Wushan, fight against the immortals; break the void with martial arts.

Nima, is this something that humans can accomplish?The East Water Conservancy Wu Clan's Great Wilderness, the East Sea, where the Jiaolong makes waves every year. If the dragon's reverse scale can be removed, the Jiaolong will become Yilong and be a blessing to the Wu Clan.

And ascending to the top of the witch clan, fighting against immortals is something that you can't even think about...

There are poems:

The ancient temple rests on Qingzhang, and the palace is surrounded by blue streams.

The sound of water and the color of the mountains lock the makeup building, thinking about the past.

**The morning returns to the evening, and the fireworks spring and autumn.

Why should a crowing ape approach a lone boat?Pedestrians worry about themselves.

There are poems again:

Last night at the foot of Wushan Mountain, the sound of apes was in the dream.

Peach blossoms fly into the green water, and go to Qutang in March.

The rain is blown away by the wind, and the king of Chu travels south.

Gao Qiu is pregnant with Song Yu, and visits Gu Yizhan.

Wushan is located in the southwest of the Great Wilderness, surrounded by clouds and mists all year round, with deep clouds and dense forests, high mountains, dangerous roads and deep pits.

In the Archaean period, Wushan was once a part of the huge subsidence zone or trough of the Great Wilderness, where thick muddy sandy and basic volcanic materials were accumulated.

Later, after the Wushan movement, the folds and uplifts became a huge mountain system, and a series of faults, magmatic activities and metamorphism occurred at the same time.The Wushan complex composed of various metamorphic complexes and igneous rocks was formed.

The ancient Wushan towering above the sea level, after long-term weathering and denudation, the terrain has become flat.

At the beginning of the Paleozoic Era, the vast area of ​​the Great Wilderness declined significantly, and the ancient Wushan Mountain also sank below sea level. On the denuded surface of the basement of the ancient metamorphic complex, a set of nearly 2000-meter-thick Cambrian-Ordovician limestone was deposited.

At the end of the Middle Ordovician, under the influence of the Caledonian movement, the North China region as a whole rose to land, and experienced a long-term sedimentary hiatus.

At the beginning of the Middle Carboniferous, there was a short-term alternation of ups and downs, and the Wushan area was in the environment of land and sea. On the denudation surface of the Middle Ordovician, the coal-rock series of the middle and late Carboniferous was deposited.

After that, the Wushan area continued to rise and entered the stage of mainland development.

During the Mesozoic Era, a fault occurred at the southern foot of Yushan Mountain, and the original ancient Wushan Mountain on the north side of the fault was continuously uplifted and suffered from weathering and denudation.

In the Cenozoic Era, Wushan continued to tilt and uplift substantially, and at the height of the mountain, all the sedimentary caprocks that originally covered the ancient metamorphic complex were eroded away.

The metamorphic complex formed more than 20 billion years ago was re-exposed on the surface.It was not until the middle of the Cenozoic Era, that is, about 3000 million years ago, that the overall shape of Wushan today was basically formed.

Later, under the continuous erosion, cutting and weathering erosion of various external geological forces, it was gradually shaped into today's majestic Wushan landform landscape.

The fault formed at the southern foot of Wushan Mountain formed in the Mesozoic Era, tends to the southeast, with a dip angle of more than 800 degrees. The north wall is the Archaean Wushan complex, and the south wall is the Cambrian limestone and shale, which is in the form of a normal fault.

The fault width is tens of meters to hundreds of meters. It is composed of multiple faults and fragments, and the strike extends for more than [-] kilometers. It has the characteristics of large drop, long extension, complex mechanical properties and multi-phase activities.

Since the formation of the Late Jurassic, its activities have continued to modern times, causing Wushan in the north to be continuously uplifted and subjected to weathering and denudation, and Tailai Basin in the south to continue to sink and receive deposition.

It directly controls the formation and evolution of Wushan and Tailai Basin, is the natural boundary between the two, and plays a decisive role in controlling the formation of Wushan.

As a young fault-block mountain system, Wushan is the result of the continuous uplift and neotectonic movement of the northern wall of the Taiqian fault.

Under the influence of neotectonic movement, the erosion and cutting effect of Wushan is very strong, and different types of erosion landforms are widely developed.

Since the rise of the southern slope of Wushan Mountain is much larger than that of the northern slope, the erosion intensity of the southern slope is relatively strong, and the eroded landform is relatively developed.

Erosion structure Zhongshan is concentrated around Taihuangding, the main peak of Wushan Mountain, as well as Laotai, Huangshiya and Huangyashan, with an altitude of about 500 meters.

The lithology that composes the mountain is mainly metamorphic rock and granite, and it is the mountain with the highest terrain, the largest uplift, and the strongest erosion and cutting in the region.

Here, the peaks are high and the valleys are deep, the terrain is steep, the maximum cutting depth is 800 meters, the valley slope is steep, there are many falls, and the effect of gravity collapse is significant.

The low mountains of erosion structure are distributed in Dahuangfeng, Zhongyaomen and Jianding Mountains, with an altitude of 700 meters and a relative height of more than 200 meters. The lithology of the mountains is mainly metamorphic rock, granite and diorite.

The erosion cutting intensity is slightly weaker than that around the main peak.But the terrain is still very steep, with deep valleys, pointed hills, jagged ridges, and steep cliffs, all of which can be seen everywhere.

The low mountains of dissolution and erosion structure are mostly distributed in the area from Jiguan Mountain to Qingshan Mountain in the northeast of the main peak. The altitude is generally 700 meters, and the relative height is above 200 meters. The mountains are mainly composed of metamorphic rocks and Paleozoic Cambrian limestone.

The erosion and cutting intensity is moderate, and the mountains are continuous. For example, the top is covered with thick limestone, often forming a "square mountain" or "table mountain" with steep walls and a gentle top, which is called "Shang" locally.

For example, the hilltops in the area of ​​Zhangxia Monk Mountain can sometimes form caves and "transparent mountains" due to the dissolution of limestone.

Dissolution and erosion hills are mostly distributed in the Cambrian limestone area on the northern edge of Wushan Mountain, with an altitude of 500 meters.

The relative height difference is less than 200 meters, the degree of erosion and cutting is relatively weak, the terrain is low and flat, and the valleys are not developed, forming a kind of "pig's back mountain" with gentle domes and ridges. Solvent ditches and caves are relatively common.

Tin-eroded hills are mainly distributed on the edge of low mountains in the south of the mountain, from Dahe to Hushan and Huangqian, with an altitude of about 200 meters. The bedrock is mostly metamorphic rock and granite, and the erosion intensity is very weak. It is dominated by denudation and weathering. Many hills and gentle ridges are formed.

Under the influence of neotectonic movement, Wushan not only developed various types of eroded landforms, but also formed many small or miniature landforms.

Such as the canyon landforms of Dazhigou, Dagouxiang, Yaozigou and Sanchagou, and the cliff landforms of Baizhang Cliff and Fanziya.The strange gorge landforms of Longjiao Mountain, Waitou Mountain and Aolai Peak.

As well as the precipitous and peculiar landforms such as the valley in the valley of Huyao Pavilion, in addition, there are many three-level micro-landforms developed in Wushan, which are strong evidence for the intermittent uplift of neotectonic movement.

The first-level flattening plane: distributed around the Humen, Hongmen, Jinshan and Huangshan highways at the southern foot of Wushan Mountain.The altitude is 200 meters, forming undulating hills, which is equivalent to the flattening plane in the Lincheng period of North China.

The second-level flattening plane is distributed on the gentle ridges around Fanziya and Motianling, with an altitude of 800 meters, which is equivalent to the flattening plane of Tang County in North China.

The third-level flattening plane is distributed on Daiding and its surrounding broad mountain tops, with an altitude of 500 meters, forming a capping surface slightly inclined to the north, which is equivalent to the flattening plane in the middle of Shandong in North China.

On the north and south sides of Daiding, it is often seen that the valley slope of the canyon has three turns. For example, a canyon in the north of the mountain is about 200 meters deep in its upper section, and the valley slope suddenly becomes steeper.

Going down for more than 20 meters, the valley slope is almost upright, with a height of about [-] meters.According to the three-fold change of the valley slope of the canyon.

The development process of the canyon can be roughly divided into three periods: the upper section of the canyon, the lower section of the canyon and the formation of the valley.

In addition, in the longitudinal section of some valleys, it can also be seen that the stream line has turned. For example, from Heilongtan on the West Road upwards, the slope of the valley bottom gradually increases, and the slope of the valley bottom between Heilongtan and Huangxi River is nearly nine. ten.

The slope from Huangxi River to Yunbu Bridge is twelve degrees, and from Yunbu Bridge to the bottom of Nantianmen Valley, the slope quickly changes to sixty degrees.This situation can also explain the stages of Wushan neotectonic movement and its landform development.

In Xiaolouyu in the north of Wushan Mountain, thick-bedded limestone of the Cambrian Zhangxia Formation is exposed. The dissolution is relatively significant in the limestone, and there are many large and small caves.

They are distributed at different heights between 510 meters and 560 meters above sea level.The classification phenomenon is very obvious.

The first-level caves are located at an altitude of more than 510 meters, the second-level caves are located at an altitude of 550 meters, and the third-level caves are located at an altitude of 560 meters.The natural arrangement of the three-level karst caves constitutes a peculiar landscape here, and it is also an ideal example of the indirect and staged neotectonic movement in Wushan.

The three-level terraces of the rivers around Wushan are developed, among which the first and second-level terraces are well preserved, and the third-level terraces are mostly damaged by later denudation and often remain in the piedmont.

For example, in the Xiaosha River near Qingyang Village, the first terrace is about six meters above the river bed, the second terrace is 20 meters above the river bed, and the third terrace is 30 meters above the river bed. difference in rise. ?

There are many waterfalls in Wushan Valley, which create the beautiful scenery of Wushan waterfalls, such as the waterfalls of Heilongtan and Yunbu Bridge.

Due to the intermittent nature of neotectonic movement, the multi-level nature of the waterfall is formed.Below the Baizhang Cliff of Heilongtan, there are two small pools at 30 meters and 50 meters respectively, which together form a triple-style waterfall.

In the ditch on the east side of Doutian Palace, there are three pools and overlapping waterfalls composed of three small falls, each with a drop of about three meters.

But on this day, a piercing sound passed in the sky, and then a figure was seen rushing into the dense fog of the mountains...