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Foliation forms when pressure squeezes the flat or elongate minerals within a rock so they become aligned. These rocks develop a platy or sheet-like structure that reflects the direction that pressure was applied in. Slate, schist, and gneiss (pro...
The layering within metamorphic rocks is called foliation (derived from the Latin word folia, meaning leaves), and it occurs when a rock is being shortened along one axis during recrystallization.