Peridotite rocks are coarse-grained, dark-colored igneous rocks. They are the main source of all chromium ore and naturally occurring diamonds. Their magnesium content helps mitigate global warming.
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∙ 9y agoThey are the only two ignous rocks that are ultramafic.
There are three intrusive igneous rocks that are composed of at least 50% olivine. These rocks are peridotite, kimberlite and dunite.
At transform boundaries, two plates grind past each other with no loss of material from the lithosphere. Rocks found at these boundaries are peridotite and gabbro.
Olivine is a mafic mineral. It is most abundant in ultramafic rocks.
A use for peridotite Is to absorb carbon dioxide from the air
They are the only two ignous rocks that are ultramafic.
The four I know of are: gabbro, basalt, peridotite, and dolerite.
The four I know of are: gabbro, basalt, peridotite, and dolerite.
Peridotite, andesite, pumice, rhyolite, obsidian, granite, and basalt.
There are three intrusive igneous rocks that are composed of at least 50% olivine. These rocks are peridotite, kimberlite and dunite.
At transform boundaries, two plates grind past each other with no loss of material from the lithosphere. Rocks found at these boundaries are peridotite and gabbro.
Rocks of the mantle are peridotite, dunite, and eclogite. In deeper regions, the olivine may be replaced by more stable minerals.
Peridotite originates from the upper mantle.
Even in the most generalized classification, more than two igneous rocks have phaneritic textures. In that generalized classification, they are granite, diorite, gabbro, and peridotite.
Olivine is a mafic mineral. It is most abundant in ultramafic rocks.
The mantle, or interior of the Earth is made up of mostly of rocks that have high amounts of silicon and aluminum. There is also an abundance of nickel and iron in the mantle.
A use for peridotite Is to absorb carbon dioxide from the air