The results, published on August 7 in the Journal of Geophysical Research: Planets, reveal hidden structures and billions of years of previously concealed lunar history.
A Journey into the Lunar Depths
Since landing in 2018, Chang’e-4 has been capturing stunning panoramas of impact craters and sampling minerals from the moon’s mantle. A rover named Yutu-2, equipped with Lunar Penetrating Radar (LPR), has been instrumental in this mission. The LPR sends radio signals deep into the moon’s surface, and the echoes are used to create a map of the lunar subsurface.
In 2020, scientists used Yutu-2’s LPR to map the upper 130 feet (40 meters) of the moon’s surface. The new data, however, goes much deeper, revealing multiple layers of dust, soil, broken rocks, and hidden craters.
The Crater Daedalus on the lunar farside as seen from the Apollo 11 spacecraft in lunar orbit (Image credit: NASA).
Discovering Hidden Structures
The scientists discovered five distinct layers of lunar lava that flowed across the landscape billions of years ago. They also found evidence of a crater formed by a large object’s impact, surrounded by ejecta—debris from the collision. These findings provide valuable insights into the moon’s geological history, including its volcanic activity, which is thought to have petered out about 1 billion years ago.
The layers of volcanic rock were found to grow thinner closer to the moon’s surface, suggesting that less lava flowed in later eruptions compared to earlier ones. Lead study author Jianqing Feng described the moon as “slowly cooling down and running out of steam in its later volcanic stage.”
Continued Exploration and Future Insights
Chang’e-4’s work on the moon is far from over. The craft continues to explore, and scientists hope it will provide further insights into unexpected geological formations. The detailed mapping of hidden structures beneath the lunar surface represents a significant advancement in our understanding of the moon’s complex history.
