Sharing some interesting readings:
2) The Deep Cycle of Water: Every schoolkid is taught about the hydrologic cycle wherein water moves between the atmosphere and shallow surface reservoirs. But water is present much deeper inside the earth, in fact it is present thousands of kilometers deep. It occurs not as free flowing H2O, but is incorporated inside the atomic structure of minerals as OH anions. It can escape this prison when minerals dehydrate during metamorphic reactions. The released water then rises and is expelled at the surface via volcanoes. In an alternate pathway, carried by sinking pieces of tectonic plates, water can reach even deeper in the earth, affecting the properties of the lower mantle and even the core. A short summary in Nature Geoscience on the state of our knowledge about this topic.
3) Plate Tectonics on Europa. The earth's outer silicate shell is broken up into tectonic plates which move around and jostle driving geologic activity and transforming the surface through geologic time. Scientists are looking to Jupiter's moon Europa and finding that its icy shell shows features indicative of intermittent plate motions, although the driving mechanisms will be different. In Phys.Org, by Morgan Rehnburg.
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