Correct. The lower the silica content, the more mafic the magma is.
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.
Ultra mafic rocks have the least amount of silica.
A low silica magma is called a "mafic" magma.
== == Felsic lava has a higher silica content than mafic lava. Felsic lava is slower moving (high viscosity) than the less viscous mafic lava. Mafic lava is higher in dark minerals and higher in the elements iron and magnesium.
It varies. The term lapilli is applied to pyroclastic material between 2 and 64 mm in size, which does not necessarily indicate anything about composition. It can range anywhere from mafic to felsic, with silica content ranging from 45% to over 70% silica.
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.
No, we call something mafic if it has a relative low silica content. As quartz is 100% silica, it's not mafic, but felsic.
Ultra mafic rocks have the least amount of silica.
They are descriptive terms as to the relative silica content of igneous rocks. Igneous rock which is high in silica is referred to as felsic. Igneous rock which is relatively low in silica is referred to as mafic.
A low silica magma is called a "mafic" magma.
== == Felsic lava has a higher silica content than mafic lava. Felsic lava is slower moving (high viscosity) than the less viscous mafic lava. Mafic lava is higher in dark minerals and higher in the elements iron and magnesium.
basalt
It varies. The term lapilli is applied to pyroclastic material between 2 and 64 mm in size, which does not necessarily indicate anything about composition. It can range anywhere from mafic to felsic, with silica content ranging from 45% to over 70% silica.
Nealy all magma on Earth is originally low-silica, mafic magma. Most magma originates from the upper mantle, which is ultramafic, meaning it has a very low silica content. This rock may partially melt under certain conditions, forming mafic magma, which has a somewhat higher silica content than the mantle rock.
Mafic lava
Silica content determines viscosity. The higher the silica content the more viscous (slower moving). Ultramafic <45% silica Least viscous Mafic 45-52% Silica Intermediate 53-65% Silica Felsic >65% Silica Highly viscous
low silica content, thin and fluid, forms dark-colored rock.