micia
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.
Mica is actually a term for a group of sheet silicate minerals as such if you describe something as a mica you are not defining (or identifying) exactly what it is, only the group that it belongs to.
On Moh's scale Mica group minerals ranges 2.5 to 3.0 in hardness.
A good example of a mineral with basal cleavage are those from the mica group such as muscovite and biotite
The name of a mineral that splits along flat surfaces is called mica. Mica's cleavage planes allow it to be easily split into thin sheets.
The Mica mineral can change to the mineral group known as amphiboles when Gneiss is formed. This transformation occurs due to the high pressure and temperature conditions during the metamorphic process.
The mineral that is flat with flaky cleavage is mica. Mica is a group of silicate minerals that can easily be split into thin sheets or flakes. These sheets have excellent cleavage, making them easily separable into thin layers.
Black mica is also known as biotite. It is a common phyllosilicate mineral that is part of the mica group. Biotite is typically black or dark brown in color and is composed of potassium, iron, magnesium, aluminum, silicon, and hydrogen.
Mica :)
Mica is a mineral with basal cleavage. The atomic structure of mica allows it to cleave easily parallel to its basal plane, resulting in thin, sheet-like layers. This property makes mica useful in various applications such as in electronics and cosmetics.
The mineral mica is not a gemstone. It is not considered a precious mineral or gem. It is a valuable mineral that has a number of applications, and it is likely you have some mica in your home now. Mica is used in the electronics industry as an insulator beneath semiconductor packages when they are mounted on heat sinks in consumer (and other) electronic equipment.
Oxygen and silicon form the mineral group known as silicates. This group is the most abundant in the Earth's crust and includes minerals such as quartz, feldspar, and mica.