Mantle
A peridotite is a dense, coarse-grained igneous rock, consisting mostly of the minerals olivine and pyroxene. Peridotite is ultramafic, as the rock contains less than 45% silica.
There are three intrusive igneous rocks that are composed of at least 50% olivine. These rocks are peridotite, kimberlite and dunite.
False. The upper mantle is believed to be composed primarily of peridotite.
A use for peridotite Is to absorb carbon dioxide from the air
Mantle
A peridotite is a dense, coarse-grained igneous rock, consisting mostly of the minerals olivine and pyroxene. Peridotite is ultramafic, as the rock contains less than 45% silica.
Peridotite, a type of ultramafic rock composed largely of the mineral olivine, has the least silica.
yes it is made up of olivine and various pyroxenes
Basalt, welcome
There are three intrusive igneous rocks that are composed of at least 50% olivine. These rocks are peridotite, kimberlite and dunite.
The mantle is 82% of Earth's volume. It is composed of ultramafic rock called peridotite, which is hot enough to flow.
The mantle is 82% of Earth's volume. It is composed of ultramafic rock called peridotite, which is hot enough to flow.
False. The upper mantle is believed to be composed primarily of peridotite.
Peridotite originates from the upper mantle.
A use for peridotite Is to absorb carbon dioxide from the air
ultramaficur welcome 🥴