Andesitic magma has intermediate silica content. Rhyolite has the highest(>68%) and Basaltic the least.
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.
High levels of silica cause magma to be more viscous
Magma with high silica content is formally referred to as "rhyolitic" magma. It typically has a high viscosity due to the increased silica, which can lead to explosive volcanic eruptions. Another term used for high-silica magma is "felsic" magma, encompassing a range of compositions that include high amounts of quartz and feldspar minerals.
yes
Magma that is high in silica tends to be more viscous and traps gas bubbles, leading to explosive eruptions. The high silica content increases the magma's explosivity and can result in ash clouds and pyroclastic flows during eruptions. These types of eruptions are characteristic of stratovolcanoes, such as Mount St. Helens.
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.
High levels of silica cause magma to be more viscous
If a volcano's magma is high in silica, the volcano will probably erupt explosively. If the magma is not high in silica, the volcano will probably erupt quietly.
Magma with high silica content is formally referred to as "rhyolitic" magma. It typically has a high viscosity due to the increased silica, which can lead to explosive volcanic eruptions. Another term used for high-silica magma is "felsic" magma, encompassing a range of compositions that include high amounts of quartz and feldspar minerals.
yes
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.
it is normally intermediate flow because of the silica content.
Magma that is high in silica tends to be more viscous and traps gas bubbles, leading to explosive eruptions. The high silica content increases the magma's explosivity and can result in ash clouds and pyroclastic flows during eruptions. These types of eruptions are characteristic of stratovolcanoes, such as Mount St. Helens.
True. High-silica magma, such as that found in rhyolitic compositions, has a high viscosity due to the increased bonding between silica molecules. This results in a thicker, more resistant flow compared to low-silica magma, which is more fluid and has lower viscosity.
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.
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 ;)