granitic
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.
Continental rift magmas typically form in regions where tectonic plates are pulling apart, leading to decompression melting of the mantle, which often results in basaltic to andesitic compositions. In contrast, continental arc magmas are generated at convergent plate boundaries where an oceanic plate subducts beneath a continental plate, leading to the melting of both the subducted slab and the overlying mantle wedge, producing more silicic and diverse magma compositions, including andesite and rhyolite. Thus, the primary difference lies in their tectonic settings and resulting mineral compositions.
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.:)
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.
Granite igneous rocks are lighter in color than basaltic rocks primarily due to their mineral composition. Granite is rich in light-colored minerals such as quartz and feldspar, which contribute to its lighter hues. In contrast, basaltic rocks contain a higher proportion of dark-colored minerals like pyroxene and olivine, resulting in their darker appearance. This difference in mineralogy reflects the varying magma compositions from which these rocks are formed.
andesitic rock
Andesite and diorite are two common igneous rocks that have a mineral composition intermediate between granitic and basaltic rocks. Andesite is fine-grained and contains plagioclase feldspar and pyroxene minerals, while diorite is coarse-grained and composed of plagioclase feldspar, amphibole, and other minerals.
The three kinds of Earth Igneous Rocks are: basaltic (mafic), granitic (felsic), and intermediate (andesitic). These rock types vary in their mineral composition, color, density, and overall characteristics based on the amount of silica and other elements present. Each type forms from different magma compositions and processes within the Earth's crust.
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.
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.
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.:)
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.
Olivine
The three families of igneous rocks are basaltic (mafic), andesitic (intermediate), and granitic (felsic). These families are classified based on their silica content and mineral composition, which in turn influence their color, density, and overall characteristics.
felsic and something else i do not remember the second one.
Granite igneous rocks are lighter in color than basaltic rocks primarily due to their mineral composition. Granite is rich in light-colored minerals such as quartz and feldspar, which contribute to its lighter hues. In contrast, basaltic rocks contain a higher proportion of dark-colored minerals like pyroxene and olivine, resulting in their darker appearance. This difference in mineralogy reflects the varying magma compositions from which these rocks are formed.
Granite has feldspar, quartz, biotite.