Most micas contain potassium (K), aluminum (Al), silicon (Si), oxygen (O), and hydrogen (H). Depending on the actual mineral species, other elements may also be present. Below is a list of some common mica minerals (though some are not actually approved mineral species):
Phlogopite: KMg3(AlSi3O10)(OH)2
Biotite: K(Mg,Fe)3(AlSi3O10)(OH)2
Annite: KFe3(AlSi3O10)(OH)2
Muscovite: KAl2(AlSi3O10)(OH)2
Lepidolite: K(Li,Al)2-3(AlSi3O10)(OH,O,F)2
The mica group of sheet silicate (phyllosilicate) minerals includes several closely related materials having highly perfect basal cleavage. All are monoclinic with a tendency towards pseudo-hexagonal crystals and are similar in chemical composition. The highly perfect cleavage, which is the most prominent characteristic of mica, is explained by the hexagonal sheet-like arrangement of its atoms.
The word "mica" is derived from the Latin word mica, meaning "a crumb", and probably influenced by micare, "to glitter".\
Name
Mica
Chemistry
KAl2(AlSi3O10)(F,OH)2, Potassium aluminum silicate hydroxide fluoride.
Uses
It is used as heat and electrical insulators for industrial purposes.
Color
White, yellow, green, brown and silver,
Hardness
2-2.5
Specific gravity
2.8
Determination of Range of Alpha particle in Mica Window?
-Properties of Alpha
-Range of Alpha
-Usage
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Mica is dark colored. It also has high dielectric strength
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Both are platy, silicate, mica group minerals with perfect cleavage in one direction.
As Mica splits perfectly parallel to its base, it is considered to have perfect basal cleavage. No other cleavage planes are present in Mica so the flaking occurs readily along this single plane. A good analogy would be a stack of A4 paper. The layers are easily peelable in one direction [parallel to the base] as opposed to the other axis [refer to the miller indices].
Muscovite mica has perfect cleavage in one direction. It splits into thin sheets.
the arrangement of the atoms in mica
The physical properties are hardness, cleavage, color, and luster.Halite does not have any chemical properties.
weak bonds between flat layers
Cleavage refers to the tendency of a mineral to break along flat surfaces. Graphite and mica have the same type of cleavage, which is a perfect basal cleavage.
Mica has perfect basal cleavage.
Both are platy, silicate, mica group minerals with perfect cleavage in one direction.
cleavage
Mica.
No, it does not have perfect cleavage and it is not hydrous.
The cleavage of mica is perfect. Sometimes it has parallel parting. The cleavage laminae is flexible and elastic. The thin translucent sheets allow geologists to view the metamorphosis.
Biotite (black mica) and muscovite (white mica) are both minerals that have perfect basal cleavage--one direction. It cleaves into thin sheets. Feldspars (albite, oligoclase, andesine, labradorite, bytownite, anorthite) have good cleavage in two directions at nearly right angles, poor in a third direction.
A good example of a mineral with basal cleavage are those from the mica group such as muscovite and biotite
As Mica splits perfectly parallel to its base, it is considered to have perfect basal cleavage. No other cleavage planes are present in Mica so the flaking occurs readily along this single plane. A good analogy would be a stack of A4 paper. The layers are easily peelable in one direction [parallel to the base] as opposed to the other axis [refer to the miller indices].
mica and something else