A new study from Brown University shows the moon might be flowing with more water than we thought, thanks to ancient volcanic deposits. NPR reports: Using satellite data, scientists from Brown University studied layers of rock on the moon that likely formed from large volcanic eruptions, called lunar pyroclastic deposits. The magma created by these eruptions has been carried to the moon’s surface from very deep within its interior, the study showed. What’s interesting about this new study, though, is that it shows the water is far more than just ice hiding in shadowy areas of the moon. In fact, there are likely pools of water in the moon’s mantle, as well. If there’s water in the moon’s mantle, that suggests that the water was delivered to the moon very early in its formation, before it fully solidified, the study’s lead author, Ralph Milliken told Space.com. Because the magma originally comes from deep within the lunar interior, Milliken explains, “the deep interior of the moon must also contain water.”
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