Post-perovskite is hypothesized to exist in this area, whose upper region features a large quantity of olivine.
Post-perovskite is hypothesized to exist in this area, whose upper region features a large quantity of olivine. The lowest two hundred meters of it is known as "D double prime," after which the Gutenberg discontinuity is found, and the Mohorovicic (mo-ho-RO-vitch-itch) discontinuity lies above this area. Including the (*) asthenosphere and consisting of highly plastic, mostly solid rock, name this layer of the Earth, found between the outer core and the crust.
Post-perovskite is hypothesized to exist in this area, whose upper region features a large quantity of olivine.
{Mantle}