Mantle rocks shallower than about 410 km depth consist mostly of olivine, pyroxenes, spinel-structure minerals, and garnet.
These mionerals make up rocks called peridotite, dunite (olivine-rich peridotite), and eclogite. We know these from xenoliths brought up with magmas.
Between 410 km and 650 km, olivine is no longer stable and is replaced by its polymorphs wadsleyite and ringwoodite.
Below about 650 km, all of the minerals of the upper mantle begin to become unstable due to the extreme pressure and elevated temperatures. It is difficult for us to know which minerals will be stable in these conditions but we believe silicate perovskites and ferropericlase will prediminate (and diamond).
No, Geologist do.
The crust is made of solid rocks and minerals. Beneath the crust is the mantle, which is also mostly solid rocks and minerals, but punctuated by malleable areas of semi-solid magma. At the center of the Earth is a hot, dense metal core.
Many minerals occur naturally on the earths surface in rock form
Minerals make up the rocks of earth, so minerals are found wherever there are rocks at the surface. Water too is a mineral so this includes the oceans.
Silicon
The Earths mantle is filled with ferromagnesian rocks with minerals such as Olivine and Pyroxene.
The Earths mantle is filled with ferromagnesian rocks with minerals such as Olivine and Pyroxene.
iron and magnesium
They both have minerals and rocks
heat and pressure
No, Geologist do.
The crust is made of solid rocks and minerals. Beneath the crust is the mantle, which is also mostly solid rocks and minerals, but punctuated by malleable areas of semi-solid magma. At the center of the Earth is a hot, dense metal core.
the mantle and crust
dirt and rigid rocks
geologists
Many minerals occur naturally on the earths surface in rock form
The crust.