[QUOTE]Io's calderas (craters) are remarkably hot. "Our temperature measurements indicate hotter temperatures than any active volcanism on Earth," McEwen says. "It implies that the magma is magnesium-rich -- comparable to the mantle composition of the Earth. This is what happened on Earth during the Archean era, 2.5 billion years ago, when the Earth was hotter. That's interesting, because it suggests that we might learn something about ancient volcanoes on Earth by studying Io today."[QUOTE]
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The earth in general was hotter.