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Revision as of 13:08, 24 December 2024 by ChaseKiwi (talk | contribs) (Create- notable due to being southern most volcanic area in Taupo Rift and its lake cores contributing to historic temperature studies)(diff) ← Previous revision | Latest revision (diff) | Newer revision → (diff) Lake in the central North Island of New Zealand| Rangatauanui | |
|---|---|
| Rangataua Crater Lake | |
| Rangatauanui and Rangatauaiti maar lakes. Known active east - west Taupō Rift termination fault surface traces are in red. Click on the map to enable mouse over that can show feature names. | |
| Location | North Island |
| Coordinates | 39°26′02″S 175°22′44″E / 39.434°S 175.379°E / -39.434; 175.379 |
| Surface area | 2.5 ha (6.2 acres) |
| Average depth | 7 m (23 ft) |
| Surface elevation | 580 m (1,900 ft) |
| References | |
Rangatauanui is a maar lake south of Ohakune in the North Island of New Zealand. It is in the area of the southernmost volcanic activity in the Taupō Rift. Its undisturbed lake sediments have proved useful in reconstructing recent climate proxy records for New Zealand.
Geography
It is 3 km (1.9 mi) south of Ohakune in the Ngā Roto-o-Rangataua Scenic Reserve, which before 2019 was known as the Ohakune Lakes Scenic Reserve. This has an area of about the about 58 ha (140 acres). Historically it has been called Rangataua Crater Lake. Adjacent is another smaller maar lake, Rangatauaiti, and the area that has been called the Rangataua craters in the geological literature.
Geology
Along with Rangatauaiti it is a maar lake, believed to have been formed about 30,000 years ago. The nearest other volcanoes are to the north, being the Ohakune volcanic complex and it is unclear if the maar lakes are similar potential Ruapehu parasites, representing the southernmost vents of the Taupō Volcanic Zone which is defined as terminating at Mount Ruapehu. The structure of the southern Ruapehu magma system is unknown and evidence exists in the case of the Ohakune volcanic complex for an approximately 16–18 km (9.9–11.2 mi) depth for the originating magma reservoir, fair magma ascent rates and that the magma conduit may be independent of the main feeder system of Mount Ruapehu. Either way these volcanoes may be the present propagating tip of the arc system that extends from the Taupō Rift through the South Kermadec Ridge Seamounts and Kermadec Islands to beyond Tonga.
Because the lake has no major inflows or outflows sediment cores have been undisturbed, and provide a useful dated tephra record of nearby eruptions.
Climate studies
Consistent with Tasmanian and Chilean studies there is a peak in summer temperatures at about 16,000 years ago similar to the later Holocene. Summer temperatures then cooled from 14.5 to 12.9 cal ka BP, before peaking at 11.7 cal ka BP. Forest developed after 11.5 cal ka BP, similar to today's and the climate record here is consistent with other New Zealand Holocene studies.
Ecology
Currently the lake is surrounded by wetland for 50 m (160 ft) dominated by New Zealand flax and also containing raupō, mānuka, and cabbage trees. Within surrounding reserve associated with the two lakes is regenerating native forest containing the trees kahikatea, kāmahi, and rewarewa, as well as the epiphyte northern rātā.
Notes
- The volcanoes are technically either one of the most southern in the Taupō Rift or the Taupō Volcanic Zone depending upon which definition is used of the later. Unresolved are the issues of whether they are parasitic volcanoes to Mount Ruapehu, volcanoes with separate magma sources or a single volcano with a single magma source being part of the Ohakune volcanic complex.
References
- New Zealand Active Fault database
- ^ Rees et al. 2021, 2. Study site.
- "Notice of New and Altered Geographic and Crown Protected Area Names for Ngāti Rangi Claims Settlement Act 2019". NZ gazette. 2019. Retrieved 24 December 2024.
- Lilley, Ian (1909). "Lantern Slide: "Rangataua Crater Lake"". Christchurch, New Zealand: Canterbury Museum. Retrieved 24 December 2024.
- ^ Houghton & Hackett 1984.
- Kósik et al. 2016, 2. Regional setting.
- Gamble, Wright & Baker 1993.
- Kósik et al. 2016, 9.3. Volcanic hazard assessment.
- Booden et al. 2010.
- Moebis 2010.
- ^ Rees et al. 2021, 5.1. Is there evidence for Holocene-like temperatures during the early deglacial?.
- Rees et al. 2021, 5.2. Expression of late-glacial climate reversal at Lake Rangatauanui.
- Rees et al. 2021, 5.3. Were early Holocene summers cool?.
Sources
- Houghton, B.F.; Hackett, W.R. (1984). "Strombolian and phreatomagmatic deposits of Ohakune Craters, Ruapehu, New Zealand: a complex interaction between external water and rising basaltic magma". Journal of Volcanology and Geothermal Research. 21 (3–4): 207–231. Bibcode:1984JVGR...21..207H. doi:10.1016/0377-0273(84)90023-4.
- Rees, A.B.; Holt, K.A.; Hinojosa, J.L.; Newnham, R.M.; Eaves, S.; Vandergoes, M.J.; Sessions, A.L.; Wilmshurst, J.M. (2021). "Duelling narratives of chironomids and pollen explain climate enigmas during The Last Glacial-Interglacial transition in North Island New Zealand". Quaternary Science Reviews. 263. 106997. Bibcode:2021QSRv..26306997R. doi:10.1016/j.quascirev.2021.106997.
- Kósik, S.; Németh, K.; Kereszturi, G.; Procter, J.N.; Zellmer, G.F.; Geshi, N. (2016). "Phreatomagmatic and water-influenced Strombolian eruptions of a small-volume parasitic cone complex on the southern ringplain of Mt. Ruapehu, New Zealand: facies architecture and eruption mechanisms of the Ohakune Volcanic Complex controlled by an unstable fissure eruption". Journal of Volcanology and Geothermal Research. 327: 99–115. doi:10.1016/j.jvolgeores.2016.07.005.
- Gamble, J. A.; Wright, I. C.; Baker, J. A. (1993). "Seafloor geology and petrology in the oceanic to continental transition zone of the Kermadec-Havre-Taupo Volcanic Zone arc system, New Zealand". New Zealand Journal of Geology and Geophysics. 36 (4): 417–435. doi:10.1080/00288306.1993.9514588. Archived from the original on 2008-11-22.
- Booden, M.A.; Smith, I.E.; Mauk, J.L.; Black, P.M. (2010). "Evolving volcanism at the tip of a propagating arc: The earliest high-Mg andesites in northern New Zealand". Journal of Volcanology and Geothermal Research. 195 (2–4): 83–96. doi:10.1016/j.jvolgeores.2010.06.013.
- Moebis, A. (2010). Understanding the Holocene explosive eruption record of the Tongariro Volcanic Centre, New Zealand: a thesis presented in partial fulfilment of the requirements for the degree of Doctor of Philosophy in Earth Science at Massey University, Palmerston North, New Zealand (Doctoral dissertation) (PDF) (Thesis). Massey University.