Peridotite and dunite are examples of ultramafic igneous rocks primarily composed of the mineral olivine. Peridotite typically contains a mix of olivine, pyroxenes, and possibly other minerals, while dunite is almost entirely made up of olivine. These rocks are commonly found in the Earth's mantle and are significant in understanding tectonic processes and the composition of the Earth's interior. Their formation is associated with high-temperature and high-pressure conditions beneath the Earth's surface.
Peridotite is a dense, coarse-grained igneous rock.
A peridotite is a dense, coarse-grained igneous rock
Gabbro, obsidian, and peridotite are examples of igneous rocks. Chert is a sedimentary rock formed from the accumulation of silica-rich microorganisms or chemical precipitation, not from the cooling and solidification of molten magma like igneous rocks.
Garnet peridotite is a type of rock that forms in the Earth's mantle and contains a high proportion of both garnet and peridotite minerals. It is commonly found in subduction zones where oceanic plates are forced beneath continental plates. Garnet peridotite is important in understanding the processes that occur in the Earth's mantle.
peridotite
Peridotite, andesite, pumice, rhyolite, obsidian, granite, and basalt.
Peridotite is a dense, coarse-grained igneous rock.
A peridotite is a dense, coarse-grained igneous rock
Peridotite is mainly composed of olivine, along with pyroxenes and minor amounts of other minerals like spinel and garnet. These minerals give peridotite its characteristic green color.
peridotite
Gabbro, obsidian, and peridotite are examples of igneous rocks. Chert is a sedimentary rock formed from the accumulation of silica-rich microorganisms or chemical precipitation, not from the cooling and solidification of molten magma like igneous rocks.
The mineral olivine is present in much greater quantities in peridotite compared to gabbro. Olivine is a common mineral in peridotite and gives it its characteristic green color, while gabbro contains less olivine and more plagioclase feldspar.
Garnet peridotite is a type of rock that forms in the Earth's mantle and contains a high proportion of both garnet and peridotite minerals. It is commonly found in subduction zones where oceanic plates are forced beneath continental plates. Garnet peridotite is important in understanding the processes that occur in the Earth's mantle.
The layer composed of peridotite is the mantle, which is located between the Earth's crust and core. Peridotite is the main rock type found in the upper mantle and is rich in minerals such as olivine and pyroxene.
There are many rock forming minerals but some examples are peridotite,gabbro,basalt etc.Olivine is used in jewellery and a rock forming mineral.
peridotite
peridotite