The direction of the maximum differential stress placed on the rock is Along a direction from the top to the bottom.
A foliated texture is known to be a kind of texture that is caused as a result of pressure. Mineral grains that are found form pre-existing rocks are known to be in an oriented that is parallel to each other.
They are often seen or organized into a kind of distinctive bands in the the metamorphosis stage. The Examples of foliated textures includes de slaty, phyllitic, and others.
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