Taupō Rift

The recent volcanism of the Taupō Volcanic Zone has been divided into three segments, with a central rhyolitic segment, dominated by explosive caldera associated with more typical Island Arc type andesite-dacite stratovolcanoes in either surrounding segment. In the hundreds of faults and their segments, some have associations with volcanism, but most fault activity is tectonic.[2]

The rift is in that part of the continental Australian Plate associated with the largely underwater Zealandia continental tectonic plate region. The rate of spread of the rift varies from effectively zero, at its southern inland end where the South Wanganui Basin is forming an initial back-arc basin, and volcanic activity has not yet begun,[5] to in the Bay of Plenty as much as 19 mm (0.75 in)/yr.[2][6] To the north east it is related tectonically to the Havre Trough off the continental shelf which is also an active rift structure.[7] The spread of the rift is associated with the basement graywacke rocks subsiding between the rift walls, so creating grabens infilled with volcanic deposits, sometimes from much higher volcanic mountains than the rift walls. The majority of the fault activity is normal faulting.[6] While continental intraarc rifts such as this, and those associated with Mount Aso in Japan, and the Trans-Mexican Volcanic Belt result from a different tectonic process from the more studied intracontinental (intraplate) rifts it has been shown that the Taupō Rift displays all of the three modes of evolution. These are narrowing, lateral migration, and along-strike propagation, as found with intracontinental rifts.[1] The Taupo Rift is widening much faster that other continental intraarc rifts, which might drive this evolution during a relatively short geological timeframe.[1]

In the Bay of Plenty region the current active faults of the old Taupō Rift can align with those of the modern Taupō Rift. This was illustrated by the Edgecumbe Fault and the off sea White Island Fault in the Whakatāne Graben of the rift.[8] The parallel Tauranga Fault Zone to the north represents a now mainly inactive old Taupō Rift margin.[9] Further south, where more of the old Taupō Rift faults appear to be inactive, the active and very complex Taupō Fault Belt is orientated north-north-east. This is trending with the modern Taupō Rift alignment, which is not always quite parallel with the old rift alignment.[1] Beyond Lake Taupō to the south, there is a relatively narrow rifting segment in the Tongariro graben which considerably widens at the Ruapehu graben. South of Ruapehu the rift, and its normal faulting, terminates with east to west faulting in the Taupō Rift termination faults. At the scale of the tectonic plate boundary, the rift trends NE-SW (41 ± 2°) but within New Zealand this trend is presently at 30° south of Lake Taupō and is 55° at the Bay of Plenty coast.[2] A significant change in the mean fault strike occurs just south of the Ōkataina Caldera.[2] The normal fault trends range from N20°E in the south to N45°E in the central and northern sectors.[1] There is good evidence that the orientation of intra-arc strike and extension processes has been maintained for 4 million years in this region of New Zealand.[2]

The modern active rift ranges in width from 15 kilometres (9.3 mi) in the northern Bay of Plenty sector, to 40 kilometres (25 mi) beyond Lake Taupō. Significant faults may be separated by as little as 100 metres (330 ft) in the north but in the south increase to up to 10 kilometres (6.2 mi) separation. There are breaks in the intra-rift fault systems in the recently active central rhyolitic caldera segments at the Taupō Volcano and Ōkataina Caldera. In the later case, the strike of the basaltic dyke of the 1886 eruption of Mount Tarawera follows that of faults to the south and north, confirming other hints that orientation of volcanism is preserved.[2]

The modern Taupō Volcanic Zone starting forming 61,000 years ago but the modern Taupō Rift appears to only have intra-rift fault activity after the immensely disruptive Oruanui eruption.[10]