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.
Low silica magma tends to form shield volcanoes such as Mauna Loa.
High silica magma is more viscous (sticky) than low silica magma, so low silica magma lows easier.
A low silica magma is called a "mafic" magma.
yes
Basaltic magma is low in silica compared to andesitic or granitic 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)
High silica magma is more viscous (sticky) than low silica magma, so low silica magma lows easier.
A low silica magma is called a "mafic" magma.
yes
Basaltic magma is low in silica compared to andesitic or granitic magma.
Low viscosity mafic 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.
A high silica content of the magma will form tall, steep-sided, or cone-shaped mountains. A low silica content produces shield shaped or broad volcanoes.
Silica.
It depends on how much silica is in the magma. If there is low-silica in the magma then the volcano will erupt quietly. If there is high-silica in the magma then the volcano will erupt explosively.
magma that is low in silica and flows easily