Option A
the way a mineral breaks apart is characteristic involves cleavage and fracture
Step-by-step explanation:
Cleavage is the drift of a mineral to cut along even levels alike to zones of ineffective bonding. Crystals with not cleavage nevermore manifest some cleavage, thus separated surfaces are fractured and rough. Most utmost minerals comprise internal defects inside their atomic arrangements, a plane on which the link intensity is below the encircling bonds.
When beaten with a hammer or differently divided, a mineral will lead to splitting onward that plane of a pre-existing defect. This sort of breakage is called cleavage, and the status of the cleavage alters with the intensity of the bonds.