The Chinese automatic probe “Chang’e-5” detected a microscopic particle of magnetite within lunar soil samples. This mineral, which requires oxidizing conditions and water for its formation, casts doubt on the notion of the Moon as a geologically “inert” body.
The discovery of magnetite with its unique microstructure suggests that volcanic activity might have existed on the Moon in the distant past. Gas emissions (fumaroles) could have established a temporary oxidizing environment where such minerals and potentially mineral deposits formed.
This finding holds strategic importance for the future exploration of the Moon. Confirmation of local resources, shaped by the satellite’s own geological activity, will be crucial for establishing sustainable lunar bases, lessening reliance on costly shipments from Earth. The research portrays the Moon as a more dynamic and possibly “useful” celestial object.
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