Concept:
Rock cleavage is a set of closely spaced planar surfaces along which a rock tends to split, produced during deformation and metamorphism. The style of cleavage depends on how the minerals are arranged within the rock.
Step 1:
Consider an evenly distributed mineral fabric. When the platy minerals are uniformly spread throughout a very fine grained rock, the cleavage planes are extremely close and pervasive, giving continuous (or slaty) cleavage.
Step 2:
When the minerals are not evenly distributed, the rock separates into distinct mineral-rich bands (cleavage domains) alternating with bands of other minerals (microlithons). The cleavage planes are then discrete and separated by measurable spacing. This is called spaced cleavage.
Answer: Option (4) — Spaced cleavage.