Upper Waikato Stream Fault
The Upper Waikato Stream Fault is an eastern Taupō rift-bounding north–south striking normal fault in the Ruapehu Graben, a seismically active area of the central North Island of New Zealand to the west of Mount Ruapehu. While its own whole fault rupture potential is, such a rupture could be part of a multi-fault rupture.
Geography
It is located near the eastern side of the Tongariro National Park, and its surface traces commence to the east of State Highway 1 where it is known as "the Desert Road" and extend to the north east for crossing the top of the Tongariro River and for a short distance into the foothills of the Kaimanawa Mountains.Geology
The Upper Waikato Stream Fault is one of the eastern wall faults of the Ruapehu Graben and it is immediately to the north of the longer Rangipo Fault. Its alignment has it as a potential continuation from the west of the Wahianoa Fault. This intersection of the three faults could result in a 7.1 MW event if all three faults had a total rupture. The fault is normal with a NE strike, and about a 75°W dip. From past to present the slip-rate has changed from /year between 45 and 36.1 ka BP to /year for an active period between 36.1 and 23.65 ka BP and after the Taupō Volcano Oruanui eruption it has reduced to /year. It is believed to have been activated by this eruption.| Fault event Number | date of last marker before event | Max Displacement | Note |
| 12 | 3,520 years BP | possible match to a Rangipo Fault rupture | |
| 11 | 11,000 years BP | possible match to a Rangipo Fault rupture Is about times of Pahoka–Mangamate eruption sequence. | |
| 10 | 11,770 years BP | probable match to a Rangipo Fault rupture | |
| 9 | 25,400 years BP | before 17,700 years BP | |
| 8 | 25,400 years BP | At time of Oruanui eruption | |
| 7 | 27,000 years BP | ||
| 6 | 27,000 years BP | ||
| 5 | 28,200 years BP | ||
| 4 | 36,100 years BP to 28,200 years BP | ||
| 3 | 36,100 years BP to 28,200 years BP | ||
| 2 | 36,100 years BP | ||
| 1 | 45,500 years BP or more |