| Mount Titiraupenga | |
|---|---|
 Titiraupenga from Pureora summit | |
| Highest point | |
| Elevation | 1,042 m (3,419 ft)[1] |
| Coordinates | 38°30′36″S 175°41′31″E / 38.509927°S 175.691857°E[1] |
| Geography | |
  Mount Titiraupenga | |
 Map centered to show approximate basaltic andesite surface volcanic deposits around Mount Titiraupenga. Mount Pureora deposits are to the south west. Other surface deposits are as in fuller key while mixed erosive volcanic surface deposits are uncoloured.
Clicking on the map enlarges it, and enables panning and mouseover of volcano name/wikilink and ages before present. Key for the volcanics that are shown with panning is: basalt (shades of brown/orange), monogenetic basalts, undifferentiated basalts of the Tangihua Complex in Northland Allochthon, arc basalts, arc ring basalts, andesite (shades of red), basaltic andesite, and plutonic. White shading is selected caldera features. | |
| Geology | |
| Rock age | Pleistocene |
| Mountain type | Stratovolcano |
| Last eruption | 1.89 ± 0.02 Ma.[2] |
Titiraupenga (also known as Mount Titiraupenga) is an extinct 1,042 metres (3,419 ft)[1] high basaltic andesite stratovolcano[2] on whose southern slopes is located the geographical centre of the North Island of New Zealand. It is in the Pureora Forest Park between Lake Taupō and Te Kūiti on the North Island Volcanic Plateau in New Zealand. The area of the mountain is in a scenic reserve that is "recognised as one of the finest rain forests in the world".[3]
- ^ a b c "NZTopoMap:Titiraupenga".
- ^ a b Pittari, Adrian; Prentice, Marlena L.; McLeod, Oliver E.; Zadeh, Elham Yousef; Kamp, Peter J. J.; Danišík, Martin; Vincent, Kirsty A. (2021). "Inception of the modern North Island (New Zealand) volcanic setting: spatio-temporal patterns of volcanism between 3.0 and 0.9 Ma" (PDF). New Zealand Journal of Geology and Geophysics. 64 (2–3): 250–272. doi:10.1080/00288306.2021.1915343.
- ^ "Walks in the Pureora Forest". Visit Ruapehu. Retrieved 23 November 2022.