Yes. Felsic magma is very viscous.
Felsic magma tends to be thick and viscous, while mafic magma tends to be fluid.
felsic
Felsic magmas that are high in silica content and are highly viscous produce explosive eruptions.
Well, lava and magma can be very very dangerous! Lava is something that you can die in. And magma is still lava. They both can be very dangerous! So I would say it is 90% dangerous.
Felsic and mafic (basic) magam mix to form intermediate 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.
Most viscous Felsic magma i.e. rhyolite Intermediate magma i.e. andersite Mafic magma i.e. Basalt Ultramafic magma i.e. Komatiite Least viscous
Felsic magma tends to be thick and viscous, while mafic magma tends to be fluid.
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.
Felsic magma is very viscous, so if often gets "stuck" in plutons rather than erupting.
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.
felsic
Felsic magmas that are high in silica content and are highly viscous produce explosive eruptions.
Well, lava and magma can be very very dangerous! Lava is something that you can die in. And magma is still lava. They both can be very dangerous! So I would say it is 90% dangerous.
Highly viscous felsic magma causes the most violent volcanic eruptions.
Felsic and mafic (basic) magam mix to form intermediate magma.
High-silicate magma, also known as "felsic magma", is molten rock below the Earth's surface (or that of any other planet, I suppose) that is made up 70% or more silica (silicon dioxide). Compared with other compositions of magma (andesitic, mafic, ultramafic) felsic is often cooler and more viscous, and so is associated with violent and explosive volcanism. Rocks formed from felsic magma include granite and rhyolite, their porphyritic relatives, granite pegmatite, rhyoltic tuff, pumice, and obsidian.