The way a mineral break apart is the characteristic involves cleavage and fracture.
Cleavage is the movement of a mineral along with even levels to zones of ineffective bonding.
Crystals with no cleavage never show any cleavage again, resulting in fractured and rough separated surfaces.
Most important minerals contain internal defects within their atomic arrangements, a plane on which the link intensity is lower than the encircling bonds.
When a mineral is beaten with a hammer or otherwise divided, it will split along the plane of a pre-existing defect. This type of breakage is known as cleavage, and its status varies with the strength of the bonds.
Thus, we can conclude that option A is correct.
You can learn more about cleavage minerals here:
https://brainly.com/question/26188940
#SPJ2
