Oxygen.
it is normally intermediate flow because of the silica content.
rhyolitic magma has a lot of silica and water vapors... thanks for asking answers.com ;)
Low silica magma typically flows easier than high silica magma because low silica magma has lower viscosity, meaning it is less resistant to flow. High silica magma is more viscous due to the presence of more silica tetrahedra in its composition, making it thicker and more difficult to flow.
Basaltic magma is low in silica compared to andesitic or granitic magma.
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.
The mineral that affects magma thickness is silica. Magma with high silica content tends to be more viscous, resulting in thicker magma. Conversely, magma with low silica content is less viscous and flows more easily.
low silica content (basaltic magma)
low silica content (basaltic magma)
No, intermediate magma typically contains a moderate amount of silica compared to other magma types. Basaltic magma has the lowest silica content, while rhyolitic magma has the highest silica content.
yes
Oxygen.
The silica can make the magma flow slower and also can make the magma's color lighter.