Generally referred to as micaceous minerals, biotite and muscovite are silicate minerals having perfect basal cleavage. They both contain most of the same elements, just in different quantities. However, biotite is soluble in sulfuric acid and has iron and magnesium in it, where muscovite does not. They can be found in all types of rock.
Chemical composition determines density. In this case, I think it's safe to implicate iron content.
Slate is mainly composed of the minerals quartz and muscovite or illite
Schist typically belongs to the metamorphic category of minerals and does not have a specific crystal system since it is a foliated rock composed mainly of micaceous minerals. However, the individual minerals within schist, such as muscovite and biotite, usually belong to the monoclinic or hexagonal crystal systems. The foliation in schist is a result of the alignment of these plate-like minerals under directed pressure and temperature conditions during metamorphism.
The majority of minerals associated with igneous rocks are silicates. It is the proportion of certain silicate minerals that affects the color of igneous rocks. Igneous rocks that are high in orthoclase feldspar, quartz, and muscovite mica will be lighter in color than igneous rocks that are higher in olivine, pyroxene, amphibole, and biotite mica.
Muscovite generally displays a micaceous crystal habit, of thin flexible sheets.
Biotite mica contains iron and/or magnesium, but muscovite mica does not.
Biotite and Muscovite.
Quartz, Feldspar, Muscovite, Biotite are among most common silicate minerals.
Platy minerals are micas(muscovite and biotite) and chlorite
Biotite is typically darker in color compared to muscovite, and it has higher iron and magnesium content, which gives it a higher specific gravity. Biotite also exhibits stronger pleochroism compared to muscovite, meaning it shows more noticeable color variations when viewed from different angles. Additionally, biotite has a higher tendency to cleave into thin, flexible sheets compared to muscovite.
Mica is a group of sheet silicate minerals (e.x of micas : Biotite, muscovite)
Iron is present in biotite mica but not in muscovite mica.
The soft silicate flakes found in many rocks are likely to be mica minerals, such as muscovite or biotite. These minerals have a layered structure that allows them to break into thin flakes or sheets easily. Mica minerals are common in igneous, metamorphic, and sedimentary rocks.
Muscovite (clear) and Biotite (black) are the commonest mica forms. Fuchsite (green) is an unusual mica containing chromium. Please see the related link below for a listing of the mica group of minerals.
Biotite is definitely a mineral. It's in the same family as muscovite, another mineral in the mica family.
Some minerals that have only one direction of cleavage include mica (like muscovite), halite (salt), and graphite. Cleavage is the tendency of minerals to break along preferred planes due to their atomic structure.
Mica or silicate