The silica-rich magma, also called felsic magma, is more viscous than iron-rich or mafic magma. This means resists flow more (just as syrup is more viscous than water). The high viscosity means that the felsic magma can trap more gasses, leading to explosive eruptions, rather than effusive ones.
High silica magma is more viscous (sticky) than low silica magma, so low silica magma lows easier.
The silica content. A higher silica content results in a more viscous magma.
High levels of silica cause magma to be more viscous
magma that has more silica is more viscous
magma that has more silica is more viscous
Correct. The lower the silica content, the more mafic the magma is.
no, it's silica
A magma containing not much silica (= SiO2). For example: a basaltic magma. These magma's have a low viscosity since the lower the SiO2-content, the lower the viscosity; and hence flow easily (↔ a felsic magma).
rhyolitic magma has a lot of silica and water vapors... thanks for asking answers.com ;)
Silica is silicon dioxide. Is is perhaps the most common compound on earth. In magma the amount of silica is key in determining the viscosity. More silica leads to a more viscous magma.
Peridotite, a type of ultramafic rock composed largely of the mineral olivine, has the least silica.Read more: Which_igneous_rock_out_of_granite_basalt_andesite_and_peridotite_has_the_lowest_silica_SiO2_content
Not usually. Explosive eruptions are more often to magma with high or moderate silica levels.