The moon’s ancient magnetic field has long puzzled scientists. A buried rock could offer new clues

Scientists are investigating a hidden structure located on the far side of the Moon that may fundamentally rewrite the known magnetic history of the satellite. According to coverage from CNN and ETH Zürich, this buried rock structure is offering new clues regarding an ancient magnetic field that has long puzzled the scientific community. The discovery is linked to the analysis of lunar samples brought back by the Chang'e-6 mission, which phys.org reports contains what scientists are describing as a 'magnetic fossil.' This finding suggests that the Moon once possessed a magnetic field similar to that of Earth, a development that challenges previous understanding of lunar evolution. Multiple outlets are tracking the implications of this discovery, with Discover Magazine emphasizing that the hidden structure is a lunar volcano. The research utilizes data from several key missions to build its case.

Specifically, dongascience.com reports that the GRAIL and Lunar Prospector missions have been instrumental in revealing a lunar magnetic field that dates back 4.2 billion years. The intersection of orbital data from these missions and the physical samples from Chang'e-6 has allowed researchers to pinpoint the existence of these magnetic anomalies on the lunar far side. This discovery is significant because the Moon currently lacks a global magnetic field, making the existence of an ancient, Earth-like field a major point of scientific contention. The context provided by ETH Zürich and other sources indicates that the far side of the Moon is uniquely positioned to provide these clues. By analyzing the 'magnetic fossil' found in the Chang'e-6 samples, scientists can better understand the internal processes that once occurred within the lunar core, potentially explaining why the Moon's magnetic activity ceased while Earth's persisted.

Future attention will likely focus on the continued analysis of the Chang'e-6 samples to verify the properties of the magnetic fossil. According to the coverage, the primary goal is to determine how the buried volcanic structure relates to the 4.2-billion-year-old field identified by GRAIL and Lunar Prospector. Researchers will look to see if further evidence of hidden structures exists on the far side that could explain the transition from an active magnetic state to the current dormant state of the Moon.