There has always been a mysterious and fascinating interest in the far side of the moon. What kind of terrifying truth is hidden on the far side of the moon that has never been illuminated by the sun?Is it the habitat of an unknown force in the universe, or the remnants of a mysterious civilization?Perhaps, what we are looking at is not only the longed-for silver earth and the cold wind, but a series of incredible discoveries. Recently, a mysterious record of scientists exploring the far side of the moon up close** has unveiled the veil of this mysterious world. Follow me on this mysterious journey to the far side of the moon and decipher the terrifying truths.
The Far Side of the Moon Revealed: Why Has It Been Neglected by Humans for So Long?
Why has the far side of the Moon been neglected by humans for so long?One important reason is observation limitations. The far side of the Moon always faces outer space, and people on Earth can't witness this scene directly. Since ancient times, humans have only been able to observe the front side of the moon through telescopes on Earth, so the knowledge of the back side has been quite limited. This limitation has led to a low level of attention paid to the far side of the moon by scientists and researchers, and little research has been carried out on it.
In addition, the terrain on the far side of the moon is complex and relatively steep, which brings great difficulties to the exploration mission. Compared to the front side of the Moon, the geomorphological features on the back side are more complex, with a large number of craters, mountains, and canyons. The presence of these geomorphological features makes it impossible for the lunar module to perform a soft landing on the back, and also affects the correct landing of the probe.
However, despite the long neglect of the far side of the Moon, it is not a barren land. After the successful implementation of the Chang'e-4 mission, our understanding of the far side of the moon has improved dramatically. Through the scientific instruments carried by the probe, humans have managed to acquire a large number of images and data from the back and discover a series of amazing discoveries.
The far side of the Moon is widely regarded as the oldest and most original side of the Moon, providing a stark contrast to the front side. The surface of the earth on the back side is covered with a thicker lunar crust, which is closer in geological time to the beginning of the moon. This provides scientists with a valuable opportunity to understand the history of the formation and evolution of the Moon.
There is also a mysterious huge impact basin on the far side of the moon, which scientists call the "South Pole-Aitoken Impact Basin". This impact basin covers almost half of the entire far side of the moon and is one of the largest and deepest impact basins known. The canyons and mountains it forms are thought to be traces of the early formation of the Moon, which are of great significance for the study of the structure and evolution of extraterrestrial planets.
It is also possible that the surface of the earth on the back side contains minerals and resources that are still unknown on the moon. The far side of the moon has not yet been explored and used by humans on a large scale, which provides a huge potential for future deep space exploration.
Geological features of the far side of the Moon: How is it different from the front side of the Moon?
The terrain on the far side of the Moon is more rugged than on the front side of the Moon. The front side of the Moon is mainly made up of large areas of high ground and shallow depressions, while the back side is a lowland full of potholes. This is due to the large number of large and small impacts that the Moon has suffered during its evolution, resulting in numerous craters and craters forming on the surface rocks. Due to the large undulation of the terrain on the back, it is more difficult for human exploration and landing missions.
The thickness of the Earth's crust on the far side of the Moon is relatively low. The earth's crust is the rock crust formed by the outer rocks, which plays an important role in the transfer of matter and the transformation of energy. The average thickness of the crust on the front side of the Moon is about 50 km, while the thickness of the crust on the far side is significantly reduced to about 30-35 km. This difference is mainly due to the shattering and enormous pressure exerted by the impact of the star. The thickness of the Earth's crust has an important impact on the Moon's geothermal activity, magnetic field, and rock composition.
The geological features of the far side of the moon also include more folded mountains and broken surfaces. The front side of the moon has relatively regular mountains and craters, which were formed mainly during early volcanic activity and impacts. On the backside, there are almost no regular mountains, but numerous folds and mountain faults. This is due to the fact that the far side of the Moon experienced a massive impact 500 million years ago, forming a huge basin and severely distorting and shattering its crust.
The composition of the Earth's crust on the far side of the Moon is also different from the front side of the Moon. The rocks on the front side of the moon are dominated by basalt, which is rich in iron and magnesium and forms a relatively flat surface. On the far side of the Moon, the crust is less basalt and is mainly composed of rocks rich in aluminum and silicon, showing a different geological feature from the front.
The mysterious black zone on the far side of the moon: what is so special about it?
We need to understand what the black zone on the far side of the moon is. Since the Moon's rotation period is the same as its orbital period, it always faces the Earth in the same way. The side we see is called the front side of the moon, and the back side is the side that we can't directly observe. The black zone on the far side of the Moon is a special area on the far side that is fainter than the rest of the moon and has no bright features.
This black zone has attracted a lot of attention from the scientific community because it is able to provide us with important information about the formation and evolution of the Moon. One explanation is that the black zone may be covered by a large amount of basalt, a type of rock formed by volcanic eruptions. Because the substance on the black area has a weaker ability to reflect light, it appears darker. In addition, the black zone may also be formed by the accumulation of dust and rock chips from some impact craters. These craters may have been impacted by large meteorites or created early in the formation of the Moon.
Although the black zone is darker than other areas, it can still be observed and studied with some advanced scientific equipment. For example, the recently launched Chang'e-4 probe successfully landed in the Von Kármán impact crater in the black zone on the far side of the moon. This is the first successful exploration mission to land on the far side of the moon in human history, bringing a wealth of scientific data to mankind. The data from the detector can be used to gain a deeper understanding of the composition and characteristics of the black zone.
In addition to providing information about the formation and evolution of the Moon, the Black Zone could also have important implications for the study of celestial bodies in the solar system. Since the far side of the Moon is shielded by the Earth, there is less radio interference from the Earth, and the black zone becomes an ideal location for astronomical observations. Many astronomers believe that the establishment of antennas and telescope equipment in the dark zone allows for clearer observation of signals from other galaxies and planets in the universe, which is essential for us to understand the mysteries of the universe more deeply.
The black zone also provides beneficial conditions for the development of space science and technology and the exploration of outer space. The establishment of exploration stations in the black area can better observe and study solar activity, cosmic rays and other celestial phenomena, and provide valuable experimental environment and data support for the development of space science and engineering. The geological characteristics of the black zone can also help us better understand the composition and evolution of planets, and provide an important reference for human exploration of outer space in the future.
The rugged surface of the far side of the Moon: revealing the reasons behind its formation!
The rugged surface on the far side of the Moon was caused by a meteorite impact event. There is no large-scale flooding and wind erosion on the far side of the Moon, so a large number of meteorite impact craters are preserved. Meteorite impacts are a ubiquitous phenomenon in the universe, and they come from celestial bodies such as comets, asteroids, or debris. When these celestial bodies hit the Moon, they produce a violent release of energy and eruptions that spray rocks and soil on the Moon's surface into the air, creating a series of impact craters and mountains. Over time, these impact craters gradually formed the rugged surface of the far side of the Moon.
The rugged surface on the far side of the Moon may be caused by the Moon's internal activity. While the Moon is widely considered to be a dead celestial body, the latest research suggests that the Moon's interior may still have some degree of heat and activity. Scientists have studied the geological structure of the moon and found that the altitude and geological structure of the moon are closely related to the rugged surface on the backside. This suggests that there may be crustal movements, volcanic activity, and other phenomena in the interior of the Moon, which led to the formation of the surface on the far side of the Moon.
The rugged surface of the far side of the moon may also be influenced by the sun. The surface of the far side of the Moon, because it is not exposed to the sun, retains impact craters and minerals more easily than the front side, creating a rugged terrain. On the other hand, the surface of the moon is eroded by solar radiation and solar wind, making the surface relatively flat. Therefore, the reason for the formation of the far and front sides of the moon is the difference in exposure to solar radiation.
Scientific exploration of the far side of the Moon: human exploration of it has never stopped!
Human exploration of the far side of the moon began in the fifties of the last century. At that time, the Soviet Union successfully sent the unmanned probe "Luna-3" to the moon for the first time in 1959 and successfully landed. It was the first successful lunar exploration mission in human history, laying the foundation for later backside exploration. However, due to limitations in technology and communication, humans have not been able to directly observe the far side of the moon.
Until 2019, China successfully launched the Chang'e-4 probe, which achieved the first soft landing and patrol of the far side of the moon by humans. The success of this mission marks a new phase in human exploration of the far side of the Moon. Chang'e-4 carries a variety of scientific instruments, including a topographic camera and an infrared imaging spectrometer, to study the topography and rock composition of the far side of the moon, as well as to understand the evolution history of the moon.
The far side of the Moon is somewhat different from its visible side. Its topography is more complex, with more geological features such as craters, mountains, and mining areas. However, because there is no protection from the atmosphere, the far side of the moon is also exposed to the influence of cosmic radiation, solar wind and other external environments, so its geological characteristics are also different from those that can be seen. Through the exploration of the far side of the moon, scientists hope to gain a deeper understanding of the internal structure and geological evolution process of the moon, so as to provide more clues for human beings to understand the formation and evolution of the solar system.
The far side of the Moon is highly pure and unpolluted by human activities, making it one of the best places for astronomical observations. Observations from the far side of the Moon are more accurate and unaffected by the Earth's atmosphere, allowing scientists to better study the properties and evolution of celestial bodies such as cosmic background radiation, stars, and galaxies.
It is worth mentioning that human exploration of the far side of the moon is not only limited to unmanned probes, but also includes the plan of human missions to the moon. NASA is planning to send astronauts to the moon around 2024 and establish a permanent base on the far side of the moon. This will be the first time in human history that a human base will be established on the far side of the moon, laying the foundation for further human exploration of space.
Perhaps, this mysterious truth is just a myriad of unknown corners of the universe, and we still have more amazing facts to discover. Let's figure out the secrets of the Moon, open the door to the vastness of the universe, and move towards a wider field of knowledge. What do you think about the truth about the moon?Is it panic?Excited?Or curious?Come and share your thoughts with us in the comments section!
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