Peridotite, a type of ultramafic rock composed largely of the mineral olivine, has the least silica.
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Basaltic magma has low silica levels. It has high levels of iron and magnesium, and is therefore has the lowest viscosity.
ultramafic
When it cools and crystallizes into rock, the rock will be described as felsic igneous rock. Examples of felsic igneous rocks are granite, rhyolite, and pumice.
Correct. The lower the silica content, the more mafic the magma is.
silica
The silica content. A higher silica content results in a more viscous magma.
There are three types of magma that contains silica. Basaltic Magma has 50 percent silica, Andesitic Magma has 60 percent silica, and Granitic Magma has 70 percent silica.
low silica content (basaltic magma)
low silica content (basaltic magma)
Igneous rocks that are dense and dark-colored are called basaltic rocks. They are formed from magma that is rich in iron and magnesium and poor in silica content.
The silica content. A higher silica content results in a more viscous magma.
When it cools and crystallizes into rock, the rock will be described as felsic igneous rock. Examples of felsic igneous rocks are granite, rhyolite, and pumice.
basalt
Higher silica contents will be in the igneous rocks that form with lower temps. Ones that form earlier in the series like olivine have lower percentages of silica.
Correct. The lower the silica content, the more mafic the magma is.
it is normally intermediate flow because of the silica content.
Silica in molten material tends to crystallise as quartz, which is white or mostly pale in colour. So felsic rocks (from silica-rich magma) tend to be pale, while mafic rocks (from silica-poor magma) tend to be dark in colour.
silica
The silica can make the magma flow slower and also can make the magma's color lighter.