This is the tendency of a mineral to break in a definite preferred direction to give a smooth flat cleavage plane. These are parallel to plane of weakness in the chemical structure of the mineral. VERY DIAGNOSTIC!
Is referred to as being, perfect, good, fair or poor, depending on how easy it is for a mineral to break along its cleavage planes.
It can occur in 1, 2 or 3 directions.
For example, GALENA has 3 perfect cleavages at 90 degrees.
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