Mount Tauhara is a dormant lava dome volcano in New Zealand's North Island, reaching above sea level. It is situated in the area of caldera rim overlap of the Whakamaru Caldera and Taupà  Volcano towards the centre of the Taupà  Volcanic Zone, which stretches from Whakaari / White Island in the north to Mount Ruapehu in the south. It is east of the town of Taupà Â, next to the northeastern shore of Lake Taupà Â.
Formed about 65,000 years ago, Mount Tauhara was not a violently explosive vent, instead slowly oozing a viscous dacitic lava. It is the largest mass of dacite within the Taupà  volcano, whose material is 98% rhyolitic. Little evidence of its volcanic past remains today; the peak is covered in dense native bush.
There is a steep walking track to the top of Mount Tauhara, starting at Mountain Road. On a clear day, the summit offers views over the Volcanic Plateau, encompassing the entirety of Lake Taupà  in the southwest. The hike is relatively strenuous and takes about an hour and a half each way. The track is not well groomed; being slightly overgrown in some places. There is a spring near the top.
In MÃÂori tradition, Tauhara was among the mountains in the central North Island which fought for the female Pihanga. After a battle won by Tongariro, the other mountains decided to flee: Taranaki moved to his present location to the west, while Pà «tauaki and Tauhara travelled north. However, due to Tauhara's sadness he moved slowly and by dawn had only reached the shore of Lake Taupà Â.
Tauhara is the point to which NgÃÂtoroirangi, the high priest of Te Arawa canoe, and ariki-ancestor of Tà «wharetoa, climbed when he first came to the region seeking lands for his followers.
"Tauhara" is MÃÂori for "alone, or isolated".