Lunar rocks collected by Apollo astronauts decades ago are offering a renewed understanding of the moon’s magnetic behavior, according to research published Wednesday in England. Scientists from the University of Oxford found that the moon’s magnetic field was mostly weak throughout history but experienced brief periods of intense activity between 3 billion and 4 billion years ago. These short bursts, described as intermittent, sometimes exceeded Earth’s magnetic strength. Magnetic fields can shield planetary surfaces from harmful radiation, making such discoveries important for understanding planetary environments.

The research team analyzed earlier measurements and observed that magnetic strength appeared to fluctuate alongside titanium-rich rock formations. These results correspond with samples collected during the Apollo missions, particularly Apollo 11 and Apollo 17, where titanium levels were high. Scientists believe volcanic activity may have pushed these materials to the surface, influencing magnetic conditions. Future missions under NASA’s Artemis program are expected to explore different lunar regions, especially the south pole, to gather new samples. These upcoming studies may provide additional evidence and help clarify how the moon’s magnetic field evolved over time, offering deeper insight into planetary development and environmental protection beyond Earth.