Dr. Claire Marie Guimond is a planetary scientist and exogeoscientist at ETH Zurich and a Brownlee Junior Research Fellow at the University of Oxford, where she uses mantle convection models to study exoplanet geology, lava worlds, and rocky planet evolution.
Well, it comes down to the fact that rocks behave the same anywhere in the universe, and this is actually the, this principle of geology that you're taught as an undergraduate geology students, where the whole reason why we can study Earth and the past is because we know that rocks are behaving the same way four billion years ago as they are today.
What's happening at the terminator between the two zones?
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