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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 metamorphic rocks in this area were produced by a collision of two tectonic plates: an ancient oceanic plate subducting beneath the North American continent. Such a process produced many types of metamorphic rocks, depending on the type of parent rock as well as the varying degrees of temperature and pressure. One unusual rock that was found at Ring Mountain was the blueschist.