Silica-rich magma is much more thick and viscous.
it is normally intermediate flow because of the silica content.
The three things that determine how thick or thin magma is temperature, silica content, and gas content.
The air affects magma. Once magma is released above ground, called lava, the air hardens it. While it is underground, the higher the temperature and pressure, the runnier the 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.
The higher the silica content of the magma, the more explosive the eruption. Magma enriched in silica has a higher viscosity (resistance to flow). Pressures are more likely to build up behind the thicker, high silica content magma and result in potentially more explosive eruptions.
The silica content in magma has the greatest effect on its characteristics. High silica content makes magma more viscous and results in explosive volcanic eruptions, while low silica content produces runny magma and less explosive eruptions.
Silica is something in the magma, so it is a pretty important part of magma because it pretty much a part that makes magma!
The magma of all volcanoes contains silica. The 1991 eruption of Mount Pinatubo involved dacite magma, which has a high silica composition.
The more silica, the slower the lava flows and the more viscous it is.
The silica can make the magma flow slower and also can make the magma's color lighter.
Silica is the most abundant component in magma and has the greatest effect on its characteristics. The amount of silica present determines the magma's viscosity, which in turn influences the explosiveness of volcanic eruptions.
Silica content makes the magma thicker which can cause a more explosive eruption, and also make it so more gases aer open to be trapped
low silica content (basaltic magma)
low silica content (basaltic magma)
No, magma with a silica content of 50 percent is more felsic, while magma with a silica content of 70 percent is more mafic. Silica content is inversely proportional to magma's mafic or felsic classification.
it is normally intermediate flow because of the silica content.
Loud Erupt: The magma is really thick It is cooler lava More silicia Quiet Erupt: Thin Hotter lava low silica