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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.
The Acadian Orogeny was one of three major orogenic phases in the creation of the Appalachian mountain chain. The first of these phases is called the Taconic orogeny and occurred during the middle to late Ordovician period.This phase is generally attributed to the subduction of North America under an island arc.The second is the Acadian and briefly it is associated with the collision of North America with the Avalonia terrane. The third was the Allegheny orogeny and deformation due to it is most visible in the central Appalachians.his phase is generally attributed to the subduction of North America under an island arc. The second is the Acadian and briefly it is associated with the collision of North America with the Avalonia terrane. The third was the Allegheny orogeny and deformation due to it is most visible in the central Appalachians.