Yes. Felsic magma is very viscous.
Felsic magma tends to be thick and viscous, while mafic magma tends to be fluid.
highly viscous; cools quickly
fewer silicate chains in the magma
Eruptions are explosive if the magma is viscous and has a high gas content.
Most viscous Felsic magma i.e. rhyolite Intermediate magma i.e. andersite Mafic magma i.e. Basalt Ultramafic magma i.e. Komatiite Least viscous
Yes. Felsic magma is very viscous.
Felsic magma tends to be thick and viscous, while mafic magma tends to be fluid.
The three types of magma, named for the rock they form are basaltic, rhyolitic and andesitic. Rhyolitic magma is rich in silica and water vapor.
highly viscous; cools quickly
fewer silicate chains in the magma
Not usually. Because it is so viscous, felsic magma does not erupt as easily as mafic magma. While eruptions of felsic magma do occur, most felsic rocks are intrusive, meaning they solidify underground.
I'm not sure... but the two different types of lava are: Viscous - sticky and slow moving, resulting in tall volcanoes Non Viscous - runny and fast moving, resulting in short and very spread out volcanoes (shield volcanoes)
Eruptions are explosive if the magma is viscous and has a high gas content.
If the magma is more viscous, the eruption is stronger.
The more viscous or "stiff" types of magma usually contain more trapped gasses. When the magma reaches lower pressure near the surface, the gasses expand explosively, blasting ash and pumice into the air.
Silica-rich magma is much more thick and viscous.