Answer: D
Correct answer: The alignment of mineral crystals under directed pressure
Foliation arises when metamorphism occurs under pressure that is greater in one direction than another. Platy minerals such as mica recrystallise with their flat faces perpendicular to the maximum stress, so the rock develops parallel layers and splits easily along them. It produces a recognisable sequence of increasing metamorphic grade: shale becomes slate, then phyllite, then schist, then gneiss, the crystals growing coarser and the banding more pronounced at each step. Slate’s ability to split into thin sheets - its cleavage - is what makes it a roofing material. Rocks metamorphosed under uniform pressure, or made of minerals with no platy habit, come out non-foliated instead: limestone becomes marble and sandstone becomes quartzite, both massive rather than banded. The layers of a sedimentary rock look similar but are bedding, formed by deposition, and they record the surface on which the sediment settled rather than the direction of later stress.