The location of the park was a passive continental margin during the Precambrian and early Paleozoic. Sediment was derived from continental sources and was deposited in shallow water. These rocks became deformed and metamorphosed.
The location of the park was a passive continental margin during the Precambrian and early Paleozoic Sediment was derived from continental sources and was deposited in shallow water. T.hese rocks became deformed and metamorphosed.