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, but did you know that if you turn a telescope to our planet's neighboring satellite, you will also see bright patches blemishing the surface?
But researchers at Stanford and WUSL now dispute that hypothesis. They argue that some other force has 'magnetized' the lunar swirls, deflecting the solar wind particles. Using a model of these magma cooling rates, Krawczynski and his colleagues have examined how a titanium-iron oxide mineral called ilmenite – abundant on the Moon and commonly found in volcanic rock – could produce a magnetizing effect.
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