Key words: water explosion, water explosion, rock sedimentation, cracks
introduction
As shown in Figure 1, such a piece of gravel solidified solid was previously considered sedimentary rock formed by sedimentation, but I found that during the same period, why did some soil layers form hard rock, while others still form loose soil? The statement of sedimentation is not valid. After my long-term investigation, I found that it is water burst rock formed by water burst. The meaning of water explosion is that when water encounters a high-temperature object, it suddenly heats up and becomes water vapor. Due to the sudden expansion of its volume and the power of the explosion, it is called a water explosion. For example, when diluting concentrated sulfuric acid, if the mixing speed is too fast, the water will explode and the sulfuric acid will be sprayed out. We can see the water explosion every day. When frying vegetables, suddenly put vegetables in the hot oil pot. The water brought in by the vegetables instantly vaporizes and expands, and the oil is sprayed out by the airflow. The geysers seen in Yellowstone Park in the United States are still the phenomenon of water explosions in nature. It is because water flows into underground cracks, is heated by hot rocks to form water vapor, and then is surrounded by water vapor to erupt. This is the final stage of the water explosion, where the magma underground has solidified, so the intensity of the eruption is low. Between 200 million and 65 million years ago, there was frequent crustal movement, and when the cracks first cracked, there was a large reserve of magma. If the cracks passed through the bottom of the river, the water in the river suddenly flowed into the cracks, forming a huge water explosion. The huge water explosion force enveloped the magma deep underground and erupted to the surface. The magma mixed in the river water. Due to the high density of the magma, it sank at the bottom of the river, flowed close to the bottom of the river, and continuously penetrated into the soil, The soil is like pouring 502 glue, and it turns into hard rock. It used to be treated as sedimentary rock, believed to be formed by long-term sedimentation. This erroneous theory has misled the geological community for hundreds of years, and in the future, humans need to re understand sedimentary rocks as rocks. Today, humans only know that volcanic eruptions can push magma to the ground, and they do not yet know that water explosions can push magma out of the ground.
Case 1: Water Explosion Rock in Jinan Ancient City
Figure 1: On the bank near the Black Tiger Spring in the Jinan moat, there is a piece of breccia, which is a gravel reef formed by water explosion. The gravel is mixed with "iron meteorites".
Figure 1 shows the south moat of the ancient city of Jinan, located on the north bank near the Black Tiger Spring. A piece of solidified gravel is formed by a water explosion, and the soil is red, possibly from the Mesozoic era. The gravel is wrapped in some suspected iron meteorites (Figure 2). This place is located about 2 kilometers north of Qianfo Mountain, downstream of the ancient Liyang River. Long ago, cracks appeared in the Earth's crust, and the stream water flowed into the cracks, causing a water explosion. The magma mixed with debris flow flowed here, solidifying and covering a very large area. Here, just to illustrate, the Black Tiger Spring water flowed out of the cracks in this type of gravel reef, and these channels were once channels for water vapor eruption (as shown in Figures 2 and 4). The current scholars claim that it is a limestone cave passage, which is unfounded. The ancient city of Jinan has a gravel structure, so how could there be a cave? How do sedimentary rocks deposit voids when channels appear within the solidified gravel structure? How did the crystals inside the cave form? These structures do not occur during the sedimentation process.
Figure 2 shows the condensation of magma vapor inside the gravel reef cavities, which lead to underground magma chambers. If there is a high-pressure environment, how did the cavities form? Magma vapor condenses together. These magma vapors come from water explosions, and these gravels are located in the riverbed of the Yufu River in Jinan. The gravels have been exposed to the air and have never experienced tremendous pressure. The magma vapors solidify on the surface of the gravels like 502 glue. Is there a reason for this deposition? This is a river, not to mention the result of calcification, why is there no magma solidification on the surface of the surrounding gravel.
In Figure 3, a row of small gravel on the surface of a piece of gravel is poured together by magma, which is carried by water vapor through cracks.
There are many voids on the gravel reef near Black Tiger Spring in Figure 4. These caves are channels for magma eruption and are now channels for spring water. Baotu Spring emerges from this channel and is connected to the underground dry hot rock. The spring water that emerges is hot, and in winter, when the temperature drops below minus ten degrees Celsius, Baotu Spring will not freeze.
Figure 5 shows the snail shells wrapped inside the gravel reef, firmly sticking together. The shells are intact, indicating that they have not experienced a high-pressure environment. The gaps between the gravel are channels for steam eruption, washing away all the soil.
Figure 6 shows the yellow biological fibrous tissue wrapped in the gravel reef (uncertain). During the debris flow process, the organisms were boiled and crushed at high temperatures. Magma infiltrates into the interior of biological tissues, forming fossils. Just like the grid texture of crab roe solidified inside the crab shell.
Figure 7 shows the Jinan "iron meteorite" cemented together by magma and soil, sturdy like concrete, and the "iron meteorite" scattered on the surface of the soil several tens of meters apart,
Figure 8 shows a mixture of magma and soil on the surface of meteorites, insoluble in water,
Figure 9 Iron meteorite is tightly wrapped in water burst rock, and after opening, the molten shell is peeled off, exposing the meteorite
The meteorite melting shell peeled off from the iron meteorite in Figure 10 is black iron trioxide, not brown iron trioxide (rust), indicating that it had just experienced high temperature before burial and had not yet oxidized and rusted with water before solidification. It did not stay in water for too long, and the solidification time was very short, without the conditions for sedimentation. If there is no rust, it indicates that the time spent in water is very short. So, how did the smooth surface of the iron block form when it was not polished by running water? What other environment is there for melting through the atmosphere?
Figure 11 shows some fossils adhered to the surface of an iron meteorite. Because this meteorite fell on the surface of the magma, only a portion was submerged, so only a portion was enveloped by the magma. If it is sedimentary rock, then why did the soil in other parts not deposit into rock.
In Figure 12, it can be seen that the internal structure of this rock is different. The high-purity area inside the rock is formed by pure calcite magma, which was originally a magma vapor channel. The solidified calcite magma slowly fills the channel, and the surrounding opaque part is mixed with soil. The area where pure magma is formed has high transparency, while the area where soil is mixed in frequently has poor transparency. Magmatic steam can penetrate into the soil like water under high temperature and pressure. At high temperature, the water inside the soil evaporates, and magma steam will replace water to penetrate into the soil. Some steam channels will be blocked by magma crystals, forming high-purity rocks.
Figure 13 shows a calcite water burst rock weighing about 1 ton excavated during the construction of the Laohushan Tunnel in Jinan. The pits on the surface of the rock are formed by soil wrapped in magma, and only the flow of viscous magma produces this shape. Initially, viscous magma was ejected, and later, water vapor containing magma was ejected, which washed away the soil to form a mixed rock containing soil. Due to the mixing of soil into the rock, the transparency decreased. It is stuck in the cracks of the mountain and buried in the soil. It is formed by the crystallization of magma steam in the channel. As the steam flow washes away the soil, the crystallization process begins with soil mixing, resulting in opaque rocks. In the later stage, the soil is solidified, resulting in high purity and good transparency of the rock.
In Figure 14 and Figure 13, calcite is a water-burst rock with good transparency and the same composition as stalactite.
In Figure 15, after the soil infiltrates the magma, it becomes hard and insoluble in water. The black traces are suspected to be carbide from ancient biological remains.
Figure 16 shows the cross-section of a water burst rock, where a small piece of magma is ejected to the ground and cooled in muddy water, forming a mud colored rock shell with high-purity rock inside,
Figure 17 shows a larger section of water burst rock, with magma wrapped in soil and a layer of mud rock on the surface. During the rolling process, soil mixed into the interior.
Figure 18 shows the cross-section of a rock containing crystalline water, which is a type of water burst rock with good transparency and fine texture. It should be considered as a type of jade. It looks like paraffin, which is the same as Mount Taishan Jade Cause. The formation process of Mount Taishan jade is that the deep source magma intrudes along the structure, and the magnesium rich ultrabasic rock is metamorphosed by the high-temperature gas liquid action, which belongs to the metamorphic ultrabasic magmatic deposit. Jieshou Village, which produces Mount Taishan jade, is on the border with Jinan City. It is on the Jishui fault zone and connected by a magma chamber. There are many granites coming in and out of the mountain near Jishui in Jinan, such as Yaoshan, Fenghuang Mountain, Fangshang, etc. Mount Taishan is granite, and between Jinan and Mount Taishan is carbonate rock.
Figure 19 shows biotite crystals wrapped in a unique water burst rock in Jinan. This rock is called pegmatite and contains a variety of rocks, indicating that the fault zone in Jinan is crisscrossed, with many large magma chambers and a long eruption time.
Figure 20: Water burst rocks inside the Yufu River in Jinan, resembling concrete (already disappearing)
It is the gravel reef in the Yufu River in Jinan. The Yufu River is an ancient ground fissure that originates from the Huangchao Reservoir at the north foot of Mount Taishan Mountain and flows into the Yellow River at Wujiapu. Due to the lack of river water in recent years, it has dried up without flowing into the Yellow River for many years. The Yufu River has cracked countless times in history, with water explosions occurring every time it cracks. Water explosions solidify the gravel and prevent it from flowing downstream. The gravel from upstream continues to pile up, causing the river bottom to rise continuously until the river overflows and changes its course. Figure 22 and Figure 23 show a gravel reef profile with a thickness of 4-5 meters, which clearly shows the process of accumulation. From the thickness of the gravel, it can be inferred how many years a water explosion occurs, The area and intensity of the water explosion can be seen. These gravel reefs are as sturdy as cement concrete and have not been drained after countless floods. As shown in Figure 20, a gravel reef in the river is believed by many to be concrete. The area with the highest frequency of diversion is in Yuanzhuang. Why is the frequency of water explosions so high in Jinan? It suggests that there have been unusual crustal changes underground in Jinan, and the mountains in the Yufu River area have all collapsed. Is it the water explosion caused by the collapse of the mountains? Or did the water explosion cause the collapse? Studying the water burst rocks in Jinan is very meaningful, but in 2015, when the Yufu River was cleared in Jinan, many gravel reefs were removed, and my video is already the only evidence. This is a new science that is on the brink of extinction and hopes to attract everyone's attention.
Figure 21 shows that after being washed away by flowing water, the gravel with high magma content still adheres together, indicating that the infiltration of magma into the gravel is uneven. (already disappeared)
Figure 22 shows the bottom profile of the Yufu River, where the flowing sand suddenly solidifies during the flow process. The solidified area is only about 100 square meters, with a length of about 40 meters, a width of about 3 meters, and a thickness of about 50 millimeters along the river. There are branches at the bottom. This solidified river bottom was neither buried by loose gravel nor raised, indicating that the solidification occurred in the past few hundred years. Otherwise, either it was buried by sediment or the raised river bottom (loose sediment around it was washed away). These solidified sand is not metamorphic rock, called water burst rock. It is magma from the underground magma chamber at the bottom of the river that seeps into the sand particles, solidifying the sand. For detailed information, please refer to the article "Principles of Water Explosion". The amount of rock burst in the Yufu River decreases and decreases until it disappears, indicating that the underground magma chamber has dried up and the geothermal energy has disappeared. Even if there is surface water entering the magma chamber, it cannot be heated into steam and cannot form a phenomenon of water vapor rising, so rainfall cannot occur. The low temperature of geothermal energy has caused dry and hot winds, resulting in drought and less rainfall in the Yufu River basin.
Figure 23 shows the rock burst profile of the Yufu River in Jinan, with a solidified gravel thickness of over 5 meters. Experts believe it is sedimentary rock formed by sedimentation?
This is the riverbed of the Yufu River in Jinan City, where layers of gravel and soil are carried down by floods from upstream. Each layer represents a flood, with the initial flood being large and carrying gravel; Later, the flood was small and only soil was left behind. Now the Yufu River is basically cut off. In addition to the construction of Huangchao Reservoir and Wohushan Reservoir in the upper reaches, the annual precipitation in Jinan and Mount Taishan is getting less and less. Many heavy rain forecasts do not have rainfall, what is the reason for the decreasing precipitation in the Yufu River Basin? It is because the geothermal energy underground the Yufu River is decreasing.
Figure 24 shows the "mud core" excavated from the Yufu River in Jinan, which was formed by magma infiltration into the soil. Below each "mud core" is a magma channel connecting the deep underground, all of which extend into a magma chamber. Calcite crystallized in areas with high magma steam flow has high purity and good transparency. This type of "mud core" is distributed throughout the rivers and valleys in the southern mountainous areas of Jinan City.
Figure 24 shows the Bayinova Mountain in Tuosu Lake, Xinjiang, which is actually a magma eruption. Magma seeps into the soil and solidifies, forming a "sedimentary rock". The surrounding soil without magma infiltration is carried away by floods, so this area is raised and turned into a mountain.
Figure 25, Inside the Bayanova Cave in Tuosu Lake, the smoothness and smoothness of the cave are washed away by water vapor.
Figure 26, Inside the Bayinova Cave in Tuosu Lake, the 'Falling Water Cave' is actually a water vapor eruption. The walls of the cave penetrate into the magma, which has petrified. Because the underground magma chamber disappears or there is no surface water flowing in, there is no water vapor eruption.
Figure 27 shows that all silicified wood in the Zhunge'er Basin of Xinjiang is dumped in one direction. It was 144 million years ago that a high-temperature flood containing magma flowed through this area, causing magma vapor to seep into ancient trees and form silicified wood.
Figure 28 shows the fossilized riverbed of an ancient river near Baixing in the Baoquan Grand Canyon of Shanxi Province, where the ripples are still present. This indicates that the Taihang Mountains are also an area where water explosions erupt. The bottom of the water that can form these ripples can only be shallow water, and it is the sediment accumulation caused by water wave vibrations. This indicates that this is a river (stream), not the seabed. Since it is the bottom of the river and there is no accumulation on it, where is the sedimentary pressure coming from? The only layer of petrification is a thin layer on the surface, which is a high-temperature flood containing magma flowing through. The water evaporates, and the magma seeps into the soil, forming this petrified soil.
Figure 29, Overall view of the ancient river bed, with locals drying corn on it. The highest part of the Taihang Mountains also has water burst rocks
Figure 30: In Laoxudian Village, Shiping County, Yunnan Province, the rock known as Quanhua by locals is called water explosion rock. There are various fossils in the rock, and leaf textures have been discovered. The debris flow containing magma carried the leaves, and the leaves may have been petrified. Later, they fell off and were carried away by rainwater.
Figure 31 shows a large amount of condensed rock vapor quartzite inside the water burst rock channel in Laoxudian Village, Shiping County, which is evidence of magma vapor eruption,
Discussion and Results
The discovery of water burst rocks has solved many mysteries in the geological and paleontological realms. From then on, humans learned that sedimentary rocks do not exist, that dinosaurs died from water burst disasters, how mountains collapsed, the true reason for the disappearance of the Pangea, and the true reason for the formation of stalactites. Knowing that there are natural disasters such as water explosions in the world, water explosions are a natural phenomenon. Through this phenomenon, we have seen many reasons for water explosions and also know the serious consequences caused by water explosions. Therefore, the discovery of water explosions is of great significance.
Due to the fact that water explosion science has just begun and lacks funding and technology, it is currently in the research stage. In the context of economic development, it is very difficult to promote individual scientific research that cannot directly generate economic benefits. I hope that those who are interested in the concept of water explosions can invest in this scientific research, discover and search for more scientific research related to water explosions, and understand nature. Understanding the Earth is the responsibility of heaven to humanity. Dinosaurs back then were just as busy as humans today. They were engulfed by a sudden water explosion and turned into fossils to freeze there. The self intelligent humans are still following the path of dinosaurs today.
The spring water channel was the channel formed by the water explosion at the beginning, but with the absence of magma vapor. At that time, floods entered from higher fissures and erupted from lower fissures. Although the magma cooled later, the channel was still open. There is a hot spring in Tashkurgan, Taxian County, Xinjiang, with a temperature of 80 degrees Celsius and a daily output of 800 tons of water. However, there is no volcanic rock around it, and some people claim that it is the heat generated by the decay of radioactive elements. There is no scientific basis for this claim, and no radioactive elements have been found in the water. In fact, this is the state of the end of the water explosion, and the magma can no longer erupt. However, the residual temperature of the magma is still very high, and the original water explosion eruption channel is still there, It has become the current underground river
The ancient silver mine in Lishui City, Zhejiang Province was discovered in water burst rocks, which are now called tuff. It is incorrect to say that it was formed by volcanic ash condensation. Silver ore is the force of water burst, which erupts sulfide containing silver magma from deep underground to the surface. The quartz rock containing arsenic sulfide (commonly known as chicken blood stone) discovered in Qingtougou Town, Xunyang County, Shaanxi Province is also formed by water burst, indicating that water burst rocks are ubiquitous and numerous.
Jiyuan and Jinan are connected by the Jishui River, which is a fault zone generated by the same geological movement. Both were formed during the formation of the Jishui River, resulting in many water burst rocks. One pulse of Jishui, three hidden and three visible, but to the clear and distant turbid. "The mountains and waters of Jiyuan are good, and the old Yin has known them for a long time. He often listens to people's words, and the golden autumn enters my hands." This is the lament of Tang Dynasty poet Bai Juyi when he came to Jiyuan as an official in Henan. During the reign of Wang Mang in the Eastern Han Dynasty, the Jishui River experienced drought and congestion, while during the reign of Emperor Gaozong of the Tang Dynasty, it was once again open and dry again. The Yellow River has repeatedly changed its course and invaded the south, gradually rushing into the Jishui riverbed and into the sea. Jishui Anning, now known as Jining City, is the place that used to move north in the middle of Jishui. The lower reaches of the Yellow River, as well as the Daqing River (originally located from Dongping Lake to the mouth of the Yellow River) and the Xiaoqing River (a small section of the river from Dongping Lake in Donga Town to the Yellow River called Xiaoqing River), are the old waterways of the Yuanji River. Jiyang County and Jinan City, located on the banks of the Yellow River in Shandong Province, are the best examples The water flowing eastward is called Ji, flowing into the river and overflowing into Xing. It originates from the north of Taoqiu in the east, reaches Yuhe in the east, meets Wen in the northeast, and flows into the sea in the northeast. Ji originates from Taiyi Lake on Wangwu Mountain in Jiyuan City, Henan Province. The source water flows more than 70 miles eastward through an underground river, and flows out to the ground of Jidu and Longtan, forming two rivers, Zhudu and Longtan, flowing eastward. Without leaving Jiyuan City, it intersects into a river called Shuishui, which is named Jishui when it reaches the northwest of Wen County. After the second underground flow, passing through the Yellow River without being muddy, it miraculously surfaced again in Xingyang. When the Jishui River flowed through Yuanyang, the Nanji River ambushed three times to Dingtao in Shandong, and merged with the Beiji River to form Juyeze. The Jishui River was hidden and appeared three times, and after a hundred fold into the sea, the Yellow River collapsed multiple times. The Jijiang River in the south of Dongping City is silted up, and it flows around the east of Dongping City to the north downstream of Qigou; Meet at Majiakou in the south of the city and flow all the way to Qinghe Gate before entering the Daqing River. In the ninth year of the Yongle reign of the Ming Dynasty (1411 AD), the Huitong River was reopened, and the Wen River was diverted for transportation. A city dam was built north of Ningyang to contain the incoming flow; Build Daicun Dam south of Kanhekou to curb the road to the sea. In the fifth year of the Xianfeng reign of the Qing Dynasty (1855 AD), after the Yellow River was captured and emptied into the sea, the Wen River became the last major tributary of the lower Yellow River. Wenzhi entered Huangkou and moved northward to Yushan. After the founding of the People's Republic of China, Dawen River flowed into the county from the east of Zhangcheng to the ditch and embankment. After the completion of the Dongping Lake Reservoir in 1958, the Wenshui Dam overflowed the Daqing River and flowed into Dongping Lake, passing through the Chenshankou Lake Gate and entering the Yellow River.
Conclusion
Through on-site investigations in Jinan, it has been found that water explosions have indeed occurred, and they occur frequently. Water explosions occur in a wide range of places in China, with different rocks produced in different places. The magma emitted by water explosions flows into rivers, causing the river to boil and a large number of organisms in the water to die. Water explosion disasters have caused many terrestrial ancient organisms to suffocate and die, and many dinosaurs have died from water explosions. Water explosion has solved many unsolved mysteries, and stalactites are also water explosion rocks formed by water explosion. Many jade stones, such as chicken blood stone, turquoise, and Shoushan stone, are water explosion rocks formed by water explosion. Crystals are also water explosion rocks formed by water explosion, and agate is also a type of water explosion rock. It is known that water explosion rocks are erupted from underground cracks, and from the chemical composition of the rocks, it can be known what minerals are underground, The laws of water burst eruptions can help us understand why water bursts occur, which is helpful for understanding the evolution of the Earth. This is a major topic that requires in-depth research, with many and wide fields of penetration and significant significance. What do people do for money? Should we do something serious when we have money?
The explanation of sedimentary and metamorphic rocks in textbooks:
Figure 0 Sedimentary Rock Theory: Weathered rock particles, transported by the atmosphere, water flow, and glaciers, settle at a certain location and undergo high-pressure diagenesis, gradually forming rocks.
Metamorphic rock is a new type of rock produced by changes and transformations in rock structure caused by the internal forces of the Earth. These forces include changes in temperature, pressure, stress, and chemical composition. [3] Under the pressure and temperature inside the Earth, solid rocks undergo the migration and recrystallization of material components, forming new mineral combinations. Ordinary limestone transforms into marble due to recrystallization. Metamorphic rocks are naturally metamorphosed from one type of rock to another under the mixed action of high temperature, high pressure, and minerals. Qualitative changes may be recrystallization, texture changes, or color changes. Metamorphic rocks are the main components that make up the earth's crust. Generally, metamorphic rocks are generated at high temperatures (150 ℃ -180 ℃ to 800 ℃ -900 ℃) and high pressures deep underground, and later exposed to the surface due to crustal movement. In special circumstances, metamorphism may not necessarily be caused by factors within the Earth's interior, but can also occur on the surface, such as the violent impact of meteorites that can cause surface rock metamorphism; The basalt at the bottom of the ocean near the ocean ridge can also undergo metamorphism on the surface due to the influence of huge underground heat flow.
Which theory is the truth? Let future generations verify it, at least it indicates that not all Chinese people are blindly following others without their own opinions. China has its own culture, rich geological materials, and naturally has its own theory. We hope that future generations will remember and conduct in-depth research.
