Both consist of molten rock and minerals
gassy magma has more silicon than not so gassy that's why there's loud and quiet explosions by: Rielly Krumbholz
Yes. The rock will get hot, of course, and some pieces of rock will become magma itself.
contact metamorphism
As magma cools, elements combine to form minerals.
The rate of cooling of the magma determines the type of mineral formed by the magma or lava..
Yes. Felsic magma is very viscous.
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.
Felsic is a term that means that a rock contains types of silica. Fesic magma is magma that is high in silica particles and low in iron particles.
Felsic rocks have a lower melting point than mafic rocks and felsic magma has a lower temperature. In other words, felsic magma is not hot enough to melt mafic rock while mafic magma is hot enough to melt felsic rock.
Felsic magma.
No. Water lowers the melting point of magma, both mafic and felsic.
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.
felsic lava
The two main types of magma are mafic and felsic.
Felsic magma
Felsic magma. This type of magma is viscous with high silica content, resulting in explosive eruptions and the formation of light-colored rocks.
When felsic magma mixes with basic magma, it can lead to the formation of intermediate magma. This mixture can have a different composition in terms of silica and mineral content compared to the original magmas. The interaction can also trigger new chemical reactions, potentially changing the physical properties and eruption behavior of the magma.