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Regional metamorphism is metamorphism that occurs over broad areas of the crust. Most regionally metamorphosed rocks occur in areas that have undergone deformation during an orogenic event resulting in mountain belts that have since been eroded to expose the metamorphic rocks.
Three other types of metamorphism are important in certain tectonic environments. 2) Contact Metamorphism is the result of baking the surrounding country rocks by an igneous intrusion. The metamorphic aureole surrounding an igneous body may be only 2 centimeters wide adjacent to a small dike or it may be 2 kilometers wide at the contact with a large, slow-cooling granite pluton. Contact metamorphosed rocks may be bleached out looking and non-descript fine-grained. A common contact metamorphic rock is hornfels (German for hard rock).