Like most cinder cones Paricutin was fed by mafic magma.
Paricutin volcano in Mexico predominantly erupted mafic lava, which is rich in magnesium and iron and has a low silica content. This type of lava tends to flow more easily compared to felsic lava.
They can. Composite volcanoes vary in what they erupt. Many composite volcanoes are composed of a mixture of mafic, felsic, and intermediate rock. However, in most cases intermediated or felsic rock predominates.
Quartz monzonite ranges from intermediate to felsic.
Composite volcanoes can erupt both mafic and felsic material, but intermediate material is the most common.
No. The terms mafic and felsic apply to igneous rocks. Limestone is a sedimentary/biochemical rock and so cannot be said to be mafic, felsic, or intermediate.
Paricutin volcano in Mexico predominantly erupted mafic lava, which is rich in magnesium and iron and has a low silica content. This type of lava tends to flow more easily compared to felsic lava.
They can. Composite volcanoes vary in what they erupt. Many composite volcanoes are composed of a mixture of mafic, felsic, and intermediate rock. However, in most cases intermediated or felsic rock predominates.
Quartz monzonite ranges from intermediate to felsic.
Composite volcanoes can erupt both mafic and felsic material, but intermediate material is the most common.
No. The terms mafic and felsic apply to igneous rocks. Limestone is a sedimentary/biochemical rock and so cannot be said to be mafic, felsic, or intermediate.
The 1980 eruption of Mount St. Helens produced dacite, which has an intermediate-felsic composition.
Monzonite is an intermediate rock.
Mafic intermediate and Felsic
are a mixture of both mafic and felsic rocks
felsic, intermediate, mafic, and ultramafic.
Neither. The terms mafic and felsic refer to the composition of igneous rocks, which are dominated by silicate minerals. Marble is a metamorphic rock composed of carbonate minerals. The terms mafic and felsic do no apply to it.
Felsic, intermediate, mafic and ultra mafic are the four broad types of magma.