Metamorphic rocks created under directed pressure show foliation with aligned minerals. Examples include slate, phyllite, schist, and gneiss.
Metamorphic rocks that are produced under directed pressure exhibit foliation due to the minerals aligning in distinct bands. Examples of foliated metamorphic rocks formed under directed pressure include slate, phyllite, schist, and gneiss. On the other hand, metamorphic rocks like hornfels, marble, and quartzite are formed without strong directed pressure and do not exhibit foliation.
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