the Moon lost its magnetic field about a billion years ago
The planet's Magnetic field is a unique substance with the help of special electric charge creates a special zone protecting the planet from harmful cosmic radiation. As the portal , the Moon lost its magnetic field as a result of crystallization of the core of our satellite of approximately one billion years ago, and thus deprived of any protection from the solar wind. But what exactly caused the emergence of such a process and whether you can explain it through science?
A Group of scientists, led by Saeed Milani from the Massachusetts Institute of technology (MIT), for several years studying the magnetic field of the moon. It is believed that our natural satellite was formed some 4.5 billion years ago after a powerful collision of Earth with an object the size of Mars. The debris from this collision eventually was pulled together by gravity, eventually forming a sphere which we can see in the sky and in the present day. Was initially much closer to Earth than it is now. Over time, the satellite moved away, continuing to move away from our planet at a speed of several centimeters per year, and although initially, it had a strong magnetic field, it gradually disappeared completely.
In previous studies, scientists found that about four billion years ago the magnetic field was more powerful than the earth almost two times that were determined in the study samples of lunar rocks ejected during eruptions. When the stones had cooled and hardened, the tiny grains lining up along magnetic field lines, locking them direction. When three billion years ago, volcanic activity ceased completely, the consequences of such a cosmic upheaval is not long to wait, lowering the strength of the magnetic field of the satellite as low as possible.
Ancient volcanoes on the moon may be witnessing the loss of the companion's magnetic field that existed in ancient times
According to experts, due to their relatively small size, sooner or later would have lost its outer protection in any way. However, surprising in this situation is that the internal Dynamo of the earth at least 2 billion years — a good time for a lightweight object. So, although the planet Mars boasts about twice the diameter, it is widely believed that the Martian magnetic field died about four billion years ago. This conclusion may indicate the existence in the distant past of our satellite long-lived source of energy. Also, being at close distance from the Earth, the liquid core of the moon was exposed to constant gravitational forces on our planet, accelerating to speeds necessary to create high magnetic fields.
As the Moon moved farther from Earth, this effect gradually weakened, giving place to a process called crystallization nuclei. When the core of the satellite is fully crystallized, the inner Dynamo of the moon has stopped, and she turned into a light gray lifeless ball, blown from all sides by the solar wind.
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