their are many types of magma because when a volcano has soft magma that means it either exploded small or the magma was going really slow and fast magma and big exploding volcano's are hard magma.:)
Because there are different types of magma and different pathways for that magma to cool.
All types of rock can melt. Thus potentially ALL types of rocks can form a magma. Your question - asking for 3 types, is therefore meaningless.
the hot type
The three main types of magma are basaltic magma, andesitic magma, and rhyolitic magma. They are classified according to their mineral composition. Basaltic magma is composed of SiO2 45-55 wt%, high in Fe, Mg, Ca, low in K, Na. Andesitic magma is composed of SiO2 55-65 wt%, intermediate. in Fe, Mg, Ca, Na, K. Rhyolitic magma is composed of SiO2 65-75%, low in Fe, Mg, Ca, high in K, Na.
All igneous rock has been created from the cooling of magma or lava.
The two main types of magma are mafic and felsic.
Felsic, intermediate, mafic and ultra mafic are the four broad types of magma.
Because there are different types of magma and different pathways for that magma to cool.
basaltic,andesitic,rhyolitic
There are different types of magma found in volcanic eruptions because they have varying compositions of minerals and gases, which are influenced by factors like the depth of the magma source, temperature, and the presence of water and other substances. These variations lead to different types of volcanic eruptions with varying levels of explosiveness and lava flow.
All types of rock can melt. Thus potentially ALL types of rocks can form a magma. Your question - asking for 3 types, is therefore meaningless.
magma is a mixture of several different types of rock.
idfk
the hot type
Most viscous Felsic magma i.e. rhyolite Intermediate magma i.e. andersite Mafic magma i.e. Basalt Ultramafic magma i.e. Komatiite Least viscous
When magma is cooled and hardened, it is an igneous rock. That being said, there's only three left and those three are the three types of rocks. Igneous, metamorphic, and sedimentary.
Mafic intermediate and Felsic