Kakaramea-Tihia Massif
Geology
Eruptions from the Kakaramea-Tihia Massif commenced at 229,000 ± 1,000 years ago. A more recent dated eruption was from Tihia, at 198,000 ± 23,000 years ago, with even more recent activity possible to Tihia's south-west. The older formations are from vents aligned north-west to south-east, but the more recent eruptions are consistent with the north-north-east to south-south-west alignment of the present southern Taupō Volcanic Zone rifting. The Kakaramea-Tihia Massif is adjacent to the Waihi Fault Zone which lies almost directly under Kakaramea. Eruptives from it define part of the shore line of Lake Taupō so would have defined part of the shore line of Lake Huka that preceded Lake Taupō given that the mountain first formed before Lake Huka.
Biology
It is one of the habitats where Dactylanthus taylorii a very rare endangered fully parasitic flowering plant is found. This is pollinated by the endangered New Zealand lesser short-tailed bat.
The Keepers of the Wai
In Māori custom, the area became the responsibility of the Matapuna people (a mix of Tuwharetoa, Tama Kopiri/Upper Whanganui whanau/Tu Hope - Descendants of Te Rere Ao, the First of Tuwharetoa) of the Tuwharetoa people, who have traditionally been the keepers of the wai (Keepers of the Water) and Maunga Kaitiaki (Protectors of the Mountain).
See also
References
- ^ Topping, Wayne William (1974). "Some Aspects of Quaternary History of Tongariro Volcanic Centre".
- ^ PeakVisor: Kakaramea
- ^ PeakVisor: Tihia
- ^ Pure, Leo (2020). The volcanic and magmatic evolution of Tongariro volcano, New Zealand (PDF) (Thesis). Te Herenga Waka-Victoria University of Wellington. Retrieved 6 December 2023.
- ^ "Dactylanthus".
- ^ Kahui Maunga Vol. 1 Page 125, Page 126 A history of the Tuwharetoa People
External links
- United Nations Environment Programme: Parks and Protected Areas: World Heritage Sites: Tongariro National Park
- Best, Elsdon. The Maori - Volume I, V Myth and Folk Lore. p205.
- Mt Tihia Tramp