Mafic rocks, such as those found in the oceanic crust, are more dense than the felsic rocks found in the continental crust.
Mafic magma and rock are higher in density that felsic magma and rock.
Silica content increases from mafic to felsic, and Mg and Fe content decreases. These differences affect things such as viscosity, density and colour. Felsic magmas are the most viscous and least dense, and felsic rocks are the lightest in colour.
Felsic rocks have 0-15% mafic crystals, while mafic rocks have 46-85% mafic crystals.
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
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.
Rhyolite is not a mafic rock, but a felsic rock, high in silicates, and similar to granite in composition.
Olivine is a mafic mineral. It is most abundant in ultramafic rocks.
Is mineral amphibolite a felsic, mafic or intermidiate in term of color
NO it is felsic
Oceanic crust is mafic.
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.