The Taupō Rift is the seismically active rift valley containing the Taupō Volcanic Zone, central North Island of New Zealand.
Intra-arc continental rifts North Island, New Zealand. Red approximately delineates the active modern Taupō Rift, yellow the inactive old Taupō Rift, and purple the still active Hauraki Rift. The rifts intersect in an area where volcanic deposits over 2 million years have buried non active fault systems. There is very complex active normal faulting in the Taupō Rift aligned mainly (apart from at the inland termination of the rift) with the rift alignment.
The Paeroa Fault is a seismically active area in the Taupō District, Waikato Region of the central North Island of New Zealand.
The Paeroa Fault (left in red) is associated with the splay Ngapouri-Rotomahana Fault (right in red) in the Taupō Rift, North Island, New Zealand