With data from China’s Chang’e-4 rover, scientists were able to visualize the upper 1,000 feet of the moon’s surface for the first time. Their results reveal billions of years of previously hidden lunar history.

The farside of the moon, as photographed by Apollo 13, hangs upside-down over the blackness of space. (Image credit: NASA)

Since it first landed in 2019, China’s Chang’e-4 — the first spacecraft to ever land on the far side of the moon — has been taking stunning panoramas of impact craters and sampling minerals from the moon’s mantle. Now, the spacecraft has enabled scientists to visualize the layer cake of structures that comprise the upper 1,000 feet (300 meters) of the moon’s surface in finer detail than ever before.

Their results, which were published Aug. 7 in the Journal of Geophysical Research: Planets, reveal billions of years of previously hidden lunar history.

A rover that traveled aboard Chang’e-4, named Yutu-2, is equipped with a technology called Lunar Penetrating Radar (LPR). This device enables the rover to send radio signals deep into the moon’s surface, said lead study author Jianqing Feng, an astrogeological researcher at the Planetary Science Institute in Tucson, Arizona.

“Then, it listens to the echoes dancing back,” Feng told Live Science. Scientists can use those “echoes,” or radio waves that bounce off of underground structures, to create a map of the lunar subsurface. In 2020, scientists used Yutu-2’s LPR to map the upper 130 feet (40 m) of the moon’s surface — but hadn’t gone deeper until now.

These new data suggest the top 130 feet of the lunar surface are made up of multiple layers of dust, soil, and broken rocks, Feng said.  Hidden within these materials was a crater, formed when a large object slammed into the moon. Feng and his colleagues hypothesized that the rubble surrounding this formation was ejecta — debris from the impact. Farther down, the scientists discovered five distinct layers of lunar lava that seeped across the landscape billions of years ago.

The Crater Daedalus on the lunar farside as seen from the Apollo 11 spacecraft in lunar orbit (Image credit: NASA)

Scientists think our moon formed 4.51 billion years ago, not long after the solar system itself, when a Mars-size object slammed into Earth and broke off a chunk of our planet The moon then continued to be bombarded by objects from space for roughly 200 million years. Some impacts cracked the moon’s surface. Like Earth, the moon’s mantle at that time contained pockets of molten material called magma, which seeped out through the newly formed cracks in a series of volcanic eruptions, Feng said.

The new data from Chang’e-4 shows that process slowing down over time: Feng and his colleagues found that the layers of volcanic rock grew thinner the closer they were to the moon’s surface. This suggests that less lava flowed in later eruptions compared with earlier ones. “[The moon] was slowly cooling down and running out of steam in its later volcanic stage,” Feng said. “Its energy became weak over time.”

Volcanic activity on the moon is thought to have petered out about 1 billion years ago (though scientists have discovered some evidence of younger volcanic activity as recently as 100 million years ago). For this reason, the moon is often considered “geologically dead.” However, there could still be magma deep underneath the lunar surface, Feng said.

Chang’e-4 isn’t done with its work on the moon yet. Feng hopes that in the future, the craft will give us insight into different, unexpected geological formations.