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The basin later underwent fore-arc and intra-arc basin development, due to the subduction of the Pacific Plate under the Australian Plate at the Hikurangi Subduction System. While it underwent block faulting throughout the Late Cretaceous to the Eocene, it has been stable since. This section of the basin contains between and m of sediment, dating from the Late Cretaceous to present. The Western Platform is separated from the Eastern Mobile Belt on the East by the Cape Egmont fault zone, a northwest trending fault zone consisting of multiple subparallel reverse and normal faults.
Most visitors venture to Taranaki to climb the enormous cone-shaped mountain. But there's a lot more to Taranaki than first meets the eye. Egmont National Park , which includes Mount Taranaki, offers fascinating outdoor adventures.