Flood facts. Part 11

2024 Author: Seth Attwood | [email protected]. Last modified: 2023-12-16 15:55

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Another collection of information that directly or indirectly relates to this topic.

If you recall the information from the previous parts that during catastrophic mountain building, faults, huge volumes of water, mud, steam, etc. could escape from the depths of the Earth, look at these videos, where pipes are squeezed out on the drilling rigs:

An example of pipe extrusion and the release of water with mud in our territory

A selection of accidents at drilling sites. Pay attention to the gas pressure in some of the examples, which ejects water vapor and sand. After watching the video, you understand that, in truth, the courageous work of specialists, called fountains …

An example when drilling to a very shallow depth:

And there are natural, natural fountains:

It turns out that such cases are not isolated. Continuation of the theme of natural fountains:

Aisky fountain (geyser)

Here, most likely, it is simple to explain: the aquifer descends at an angle to the river and in this place it found a way out.

A gushing artesian source of pure spring water, which is an interesting place and one of the natural attractions located on the banks of the Ai River in the Republic of Bashkortostan. The jets of the Aisky fountain reach a height of 5 meters. Artesian water is crystal clear, laboratory tests of the samples taken did not reveal any harmful impurities. The temperature of the jet leaving the Aisky fountain is 7 degrees Celsius. In winter, the Aisky fountain, like the similar fountain Zyuratkul, does not freeze completely. Opinions about the origin of the Aisky fountain differ. According to one of the versions, geological exploration work was carried out at this place in the 1960s, as a result of which, instead of minerals, groundwater was discovered. According to another version, the well was drilled initially to the aquifer in order to divert groundwater from the Mezhevoy Log mine. An iron pipe was installed at the site of the groundwater outlet.

Fountain Zyuratkul

The fountain is semi-natural - semi-artificial. It arose in 1976, when geologists drilled an exploration well here. No minerals were found, but they ended up in an artesian basin, and a stream of water gushed out of the well. And for more than forty years, a fountain has been beating from the ground in this place. Geologists hammered the plug, but the pressure of the water was so strong that soon the plug was knocked out. The height of the artesian fountain is about 7-10 meters. Such a jet is formed as a result of high pressure in the aquifer due to groundwater flowing down from the slopes of the mountains.

Sudogodskiy geyser

"Fountain" or as it is also called "Sudogodskiy geyser". It is located in the bed of the Peredel River, on the Vladimir-Murom highway, 4 kilometers from Sudogda. The fountain is a natural spring gushing from an underground lake, raising its jets to a height of two meters. Old-timers say that 10 years ago, the height of the geyser reached 5 meters.

Natural Fountain near Zhulanovo

The fountain is semi-natural - semi-artificial. It arose when geologists drilled an exploration well here. At the same time, they fell into an artesian basin, and a stream of water gushed out of the well. Such a jet is formed as a result of high pressure in the aquifer. There used to be a plug on the pipe, but then it was torn off.

Located on the banks of the Talitsa river. Initially, the well was drilled on the shore, but during the existence of the fountain, the space around it was severely eroded.

Natural fountains in the village of Megletsy (Novgorod region)

Everyone knows about geysers in Ieluston, Kamchatka and Iceland. There it is explained by geothermal activity, which is also not excluded with movements of the earth's crust.

Those. all these examples show what pressure and such volumes of water are not even at great depths. There was information about underground oceans in previous articles. Indeed, if the integrity of the earth's crust was violated, these volumes could come to the surface, flood the territories not only with clean water, but with clay and sand, as well as create mud flows.

Scientific information about underground oceans:

Earth's underwater ocean

British and American geophysicists have discovered a conserved ocean of water in the deep bowels of the Earth. The study is published in Proceedings of the National Academy of Sciences and reported by Florida State University. Vast volumes of water are located at a depth of 400-600 kilometers from the surface of the planet and are conserved in hydrated minerals, in particular, brucite. It was the research of scientists that made it possible to show that this mineral at high pressures is thermodynamically stable and includes water. Geochemists from Russia, as well as France and Germany have discovered at a depth of 410-660 kilometers under the surface of the Earth an ocean of the Archean period (2, 7 billion years old), the volume of which is several times larger than the size of the World Ocean. Research scientists published in the journal Nature. A huge reservoir is located under the earth's crust and was formed in ancient times under conditions of high pressures and temperatures (1530 degrees Celsius). The water in it is enclosed in the crystalline structure of minerals. Scientists came to their conclusions by analyzing solidified samples of lava flows. A source

Hot ocean under Western Siberia

Geothermal water. When in the fifties oil prospectors received hot water from drilled wells, this water did not cause joy to anyone. They needed oil, oil and only oil. Somehow, the shores of the West Siberian underground geothermal sea were not immediately outlined. And when its area was approximately measured, it turned out to be … three million square kilometers! The area of the Mediterranean Sea is almost half the size. And in terms of water supplies - hot water! - the underground sea is larger. This sea has absorbed no less than a trillion cubic meters of water. Two Mediterranean seas of boiling water! The depths of the hot dungeon are still poorly measured. In any case, the underground basin is not shallow - its average depth is three thousand meters. Upon further study, it may turn out that its volume is five times larger than the Mediterranean, and maybe twenty-five! In this sea, water does not splash, it occupies the voids of sedimentary rocks. The sea is a sponge, and the sponge is not simple, but flaky, like a pie. The upper layer of the underground sea is cold. It feeds deep wells with clear water, and when you taste it, you can feel your teeth dropping. Under fresh water, a layer of warm solution with significant doses of iodine, bromine and other elements. The underground ocean has an approximate area of approximately 3 million square meters. km. This territory could freely accommodate the Barents, Caspian and three Black Seas. According to the calculations of scientists, the underground ocean holds over 65 thousand cubic meters. km of water. Another feature: unlike the usual, so to speak, terrestrial oceans, the water in this "underground" ocean is fresh. The underground ocean has a depth relative to the earth's surface from several tens of meters in the south and up to two or even three kilometers in the north. As you know, the further into the depths of the earth, the warmer, therefore there is one more, the most important feature of this underground "miracle": if on the "southern coast" of the underground ocean - somewhere near Biysk, Semipalatinsk or Kostanay - the water temperature reaches only +5 - +10 degrees Celsius, then further north, at the latitude of Pavlodar, Petropavlovsk, Tomsk, where the depth is already 500-600 m, the thermometer in the borehole shows +25 degrees Celsius. Even hotter water (+75 degrees Celsius) was found at a depth of 1.5 km near the city of Tyumen. And where it is necessary to drill boreholes to a depth of 2.5–3 km, from time to time fountains of real boiling water burst out to a height of up to 50 m. The temperature of one of these artificial geysers (in Kolpashevo) reaches +125 degrees Celsius! True, this water does not boil, as it is under high pressure. Scientists believe that in the north, this extraordinary underground ocean goes under the bottom of the Kara Sea. The water reserves of the underground ocean are practically inexhaustible. Scientists have calculated: even when we take 2.5 million cubic meters every day. m of water, then over 100 years it would be only 1% of the water that is in the ocean. There are many more underground water basins on the globe, but the West Siberian underground ocean is by far the largest. A source

I find notes about this almost every three months. In the cycle of posts "Facts about the Flood" I indicated this information. It was this water that washed to the surface all the sand of the deserts during a cataclysm, where even they did not need to be (Chara sands, for example, in Yakutia), all the lime. It is possible that later the lime was collected in the hills (Bashkir shikhans, the hills of Bohol Island, etc.)

If we accept the version of the release of water from the depths, from the underground oceans, then where could so much water come from? Well, okay, there is hydrogen degassing of the Earth. And where does oxygen come from for the formation of H2O? We read the news: Russian and German physicists and geologists, experimenting with a laser "anvil" press at the German synchrotron center DESY, discovered a previously unknown layer in the Earth's mantle, which contains a huge amount of liquid oxygen. "According to our estimates, this layer contains about 8-10 times more oxygen than in the Earth's atmosphere. It was a big surprise for us, and we do not yet know what is happening with these" oxygen rivers "in the bowels of the planet," - said Elena Bykova from the University of Bayreuth (Germany). The fate of this oxygen remains unknown - these oxygen "rivers" can equally interact with the surrounding rocks and oxidize them, and rise to higher layers of the mantle and even higher. In any case, the presence of oxygen, as noted by Maxim Bykov, one of the other authors of the article, suggests that complex and most active chemical processes can occur in the depths of the Earth, the existence of which we do not yet know, and which can affect not only geochemistry, but also on the climate and the state of the planet's atmosphere. A source

Clay yars

Lena river banks

Formed either by a huge flood, or by streams of mud and mudflow masses. See how much higher the layers of sand are than the water level. But it is possible that first a mudflow passed through the territory, and then the river made its way. A source

The left bank of Krasnoyarsk is located on similar yars. And this fact is present in the name of the city: Krasny Yar.

Coquina layers in the Caucasus Mountains. Maybe the former bottom of the sea, or maybe it was thrown by a wave …

Kataiskoye lake

A good documentary film about the melting of the permafrost of the New Siberian Islands

***

"These animals in Alaska died so suddenly that they immediately froze to death, not having time to decompose - and this is confirmed by the fact that locals often thawed carcasses and ate meat." “The same story happened in Siberia - and here, too, many animals were found buried in the permafrost, most of which were typical of temperate regions. And here the corpses of animals were among the trunks of trees and other vegetation uprooted and bore signs of death from an unexpected and sudden catastrophe … Mammoths died suddenly, and in large numbers, in severe frost. Death came so quickly that they did not have time to digest the food they had swallowed … "(A. Elford," Gods of the New Millennium ") *** expressed an interesting thought: Why is it generally accepted by everyone that streams of water flowed ??? But this is not at all necessary, streams of acid or caustic alkali can flow, they eat up all organic matter and very quickly dissolve rocks, therefore, mushroom formations are formed, acids and alkalis will eventually turn into salts that will settle in the seas and minerals. But in Siberia and Canada, streams of LIQUID NITROGEN most likely poured, a comet consisting of liquid nitrogen crashed and flooded a quarter of the northern hemisphere, otherwise it is simply impossible to explain the permafrost and instant freezing of living creatures (mammoths, etc.), and this happened quite recently (mammoths still fresh, you can eat), 200 years ago.: As version. Why not? If there are deposits of sulfur in the depths, then, theoretically, sulfuric acid can form and, in a geotectonic catastrophe, come to the surface. Then both salts and minerals can be formed very quickly. And somewhere the acid will react or dissolve the rock. Liquid nitrogen from a comet. Also an interesting thought. About permafrost in the north, there is a version of rapid freezing during the decomposition of methane hydrites. There are many of them at the bottom of the oceans, even at the bottom of Lake Baikal. They decompose by absorbing heat. And it is for this reason that permafrost is hundreds of meters thick. It is impossible to freeze such layers from above. *** And in conclusion, one more interesting thought from the reader: "Any loose rocks have their own, strictly defined angles of repose. They depend both on the properties of rocks and on the force of gravity: the less the force of gravity, the less conditions will be steeper slope. In ancient sedimentary rocks can be found clear traces of "fossilized" angles of inclination of loose formations (wind ripples in the sand, ancient dunes, river sediments). So: measuring the slopes of ancient loose formations, candidate of geological and mineralogical sciences L. S. Smirnov discovered that in the past, steeper slopes were formed than now! Does this mean that previously the physicochemical properties of loose rocks were different? It is extremely doubtful. It means that the force of gravity was less! " Source In addition, the Earth annually moves away from the Sun by 15 cm. This can be caused by an increase in the centrifugal force of the Earth, if its mass is constantly growing.