Authors: Jeffrey Joseph Wolynski
In Earth’s earlier history when it had an extremely thick atmosphere, on par with atmospheres thicker than Jupiter’s, the central core was very, very pressurized and essentially liquid. This means it was extremely comparatively smooth to Earth as it currently is with mountains and ocean trenches. A short explanation for how the transition to its varying surface from being at an initial smooth state is provided.
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[v1] 2017-07-18 07:39:53
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