Chinese rover Yutu-2 has been found A hidden network of volcanic passages and structures on the far side of the Moon, opening up new possibilities for lunar research.
Yutu-2 and the discovery of underground passages
In a recently published study, the Yutu-2 spacecraft, which landed on the moon in 2018, discovered a series of passages under the lunar surface. Using LPR equipment, the rover sent radio signals to explore the subterranean structure of the moon.
This is the first time that scientists have used LPR to penetrate the upper 40 meters of the lunar surface, revealing an intricate network of passages and rock formations.
Author Jian Qingfeng, an astrogeology researcher, explained the process, which is similar to bat echolocation, allowing for a detailed analysis of the lunar geology.
Lunar lava: an unexpected discovery
The data collected by Yutu-2 also revealed five layers of lunar lava hidden among the fractured rocks. It is possible that these layers were formed as a result of collisions with large structures such as asteroids.
This discovery supports the theory that the Moon may have been part of the Earth 4.51 billion years ago, before it broke apart due to a massive impact. The resulting cracks can lead to volcanic eruptions and craters.
These discoveries provide unique insight into the moon’s geological and volcanic history, and may lead to new investigations into its formation and origin.
Is there still magma on the moon?
Although volcanic activity on the moon is believed to have ended about a billion years ago, researcher Feng notes that it is possible that some magma may still be present. This statement could open new horizons for the study of geothermal activity on the Moon.
Understanding the presence of magma and its possible residual activity can provide insights into the geological evolution of the Moon and contribute to the study of other celestial bodies.
The research conducted by the Yutu-2 spacecraft remains an essential contribution to understanding the solar system and space exploration.
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