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Mica has perfect basal cleavage.
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.
It is schist.
Hardness, specific gravity, cleavage, chemistry, crystallography, color.
In a hand sample/specimen you can the properties used to identify minerals are luster, diaphaneity, color, streak, luminescence, play of colors, crystal shape, tenacity, cleavage, hardness, specific gravity and density, magnetism, electrical properties, reaction to acid.
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