The Paeroa Fault is a seismically active area in the Taupà  District, Waikato Region of the central North Island of New Zealand.
North of Lake Taupà Â, volcanic ignimbrite at least thick, and called the Paeroa Ignimbrite (dated to 339 ñ 5 ) is exposed along the very steep fault scarp of the Paeroa Fault that defines the western flank of the high Paeroa Range. The Paeroa Ignimbrite appears to have been erupted from a linear vent alignment parallel to the current Paeroa Range and fault. This fault area of the Taupà  Rift is displacing at a rate of /year. At the north eastern end of the fault is the geothermally active Maungaongaonga volcano that with the fault defines the far south western border of the . The Ngapouri-Rotomahana Fault too extends to the à Âkataina Caldera and is a splay from the Paeroa Fault.
The southern portion of the fault is associated with the raised Paeroa Fault block immediately to its east which is the largest ground surface fault block within the Taupà  Volcanic Zone. The raised block further to the east goes into the down lands associated with the Reporoa Caldera that extend to form the Taupo-Reporoa Basin. To the west is the adjacent Te Weta Fault block in what has been called the Paeroa Garben, a rift valley that extends to the presently much less tectonically active Horohoro Fault.
This intra-rift fault has been estimated to have single event earthquakes in its northern portion about 6.4 Mw and for the whole fault, rupture intensity of about 6.8 Mw with up to upward displacement. Almost half of rupture events in the last 16,000 years have been associated with nearby volcanic eruptions so it is not only the direct earthquake impact that may be important. The Mamaku eruption of about 8000 years ago and Rotoma eruption of about 9500 years ago of the à Âkataina Caldera are associated in time with deposits indicating the earthquake fault rupture events took place either just before or during the eruption sequence.