Pumice is more related to a textural feature, rather than a compositional attribute. For example, pumice originates when there are enough dissolved gases in the magma, such that when it is ejected from the volcano, the depressurization of the dissolved gases causes a rapid expansion as the gases exsolve (just like when you open a pop - the gases are initially under pressure, and you release that pressure by opening the can or bottle). The rapid change in temperature, from hundreds to thousands of degrees to the temperature of of the surrounding environment, causes a rapid cooling effect, whereby the expanding gases are frozen in place. These two factors are what give pumice its distinctive texture and ability to float when placed in water, as opposed to other volcanic rocks (such as scoria).
Whether or not the pumice is felsic (light in color) or mafic (dark in color) depends on its chemical composition and therefore, pumice can be both felsic or mafic depending on its parental magma.
General classification as to whether a rock is felsic or mafic is with regards to the silicate content of the rock as follows:
felsic < 69% SiO2
Intermediate Felsic 63 - 69% SiO2
Intermediate 52- 63% SiO2
Mafic < 52% SiO2
Ultra Mafic < SiO2
This said, felsic pumice (white or light tan brown colors) are more common to find than mafic pumice.
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.
No, rhyolite has a more felsic composition than basalt. Rhyolite is rich in silica, which makes it a felsic rock, while basalt is more mafic due to its lower silica content.
Olivine is a mafic mineral. It is rich in iron and magnesium, which are characteristic components of mafic rocks like basalt and gabbro.
Monzonite is an intermediate rock.
No, granite is not considered mafic. It is an igneous rock that is classified as felsic due to its high silica content and lower concentration of iron and magnesium minerals compared to mafic rocks like basalt.
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.
Is mineral amphibolite a felsic, mafic or intermidiate in term of color
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.
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.
No, rhyolite has a more felsic composition than basalt. Rhyolite is rich in silica, which makes it a felsic rock, while basalt is more mafic due to its lower silica content.
Felsic minerals are Silicon-rich; whereas Mafic ones are low in Silicon, but contain Iron and Magnesium.
Mafic lava is hotter than felsic lava and therefore flows faster.
Quartz monzonite ranges from intermediate to felsic.
Olivine is a mafic mineral. It is rich in iron and magnesium, which are characteristic components of mafic rocks like basalt and gabbro.
Mafic and felsic.
The mantle is ultramafic.