Reposted by Stuart Swales
🧪⚒️Tiny grains of coesite — quartz that forms only at pressures found about 100 km down — turned up in rocks of western Norway. On the new Geology Bites, Torgeir Andersen explains how buoyant continental crust got that deep, and how it came back.
geologybites.com/torgeir-andersen #geology