|Location||Taupo District, Waikato Region, North Island|
|Type||crater lake, oligotrophic|
|Primary inflows||Waitahanui River, Tongariro River, Tauranga Taupo River|
|Primary outflows||Waikato River|
|Catchment area||3,487 km2 (1,346 sq mi)|
|Basin countries||New Zealand|
|Max. length||46 km (29 mi)|
|Max. width||33 km (21 mi)|
|Surface area||616 km2 (238 sq mi)|
|Average depth||110 m (360 ft)|
|Max. depth||186 m (610 ft)|
|Water volume||59 km3 (14 cu mi)|
|Residence time||10.5 years|
|Shore length1||193 km (120 mi)|
|Surface elevation||356 m (1,168 ft)|
|Islands||Motutaiko Island (11 ha)|
|1 Shore length is not a well-defined measure.|
Lake Taupo is a lake situated in the North Island of New Zealand. With a surface area of 616 square kilometres (238 sq mi), it is the largest lake by surface area in New Zealand, and the second largest freshwater lake by surface area in geopolitical Oceania after Lake Murray (Papua New Guinea).
Lake Taupo has a perimeter of approximately 193 kilometres, a deepest point of 186 metres. It is drained by the Waikato River (New Zealand's longest river), while its main tributaries are the Waitahanui River, the Tongariro River, and the Tauranga Taupo River. It is a noted trout fishery with stocks of introduced brown trout and rainbow trout.
Lake formation and volcanism
Lake Taupo lies in a caldera created by a supervolcanic eruption which occurred approximately 26,500 years ago. According to geological records, the volcano has erupted 28 times in the last 27,000 years. It has ejected mostly rhyolitic lava, although Mount Tauhara formed from dacitic lava.
The initial event 26,500 years ago is the largest eruption and is known as the Oruanui eruption. It ejected an estimated 1170 cubic kilometres of material and caused several hundred square kilometres of surrounding land to collapse and form the caldera. The caldera later filled with water, eventually overflowing to cause a huge outwash flood. It is possible that the Lake Taupo event contributed to starting the Last Glacial Maximum.
Several later eruptions occurred over the millennia before the most recent major eruption, which is traditionally dated as about 180 CE from Greenland ice-core records. Tree ring data from two studies suggests a later date of 232 CE ± 5. Known as the Hatepe eruption, it is believed to have ejected 100 cubic kilometres of material, of which 30 cubic kilometres was ejected in the space of a few minutes. This was one of the most violent eruptions in the last 5000 years (alongside the Tianchi eruption of Baekdu at around 1000 and the 1815 eruption of Tambora), with a Volcanic Explosivity Index rating of 7; and there appears to be a correlation, to within a few years, of a year in which the sky was red over Rome and China. The eruption devastated much of the North Island and further expanded the lake. The area was uninhabited by humans at the time of the eruption, since New Zealand was not settled by the Māori until about 1280. Possible climatic effects of the eruption would have been concentrated on the southern hemisphere due to the southerly position of Lake Taupo. Taupo's last known eruption occurred around 30 years later, with lava dome extrusion forming the Horomatangi Reefs, but that eruption was much smaller than the 180 CE eruption.
Underwater hydrothermal activity continues near the Horomatangi vent, and nearby geothermal fields with associated hot springs are found north and south of the lake, for example at Rotokawa and Turangi. These springs are the site of occurrence of certain extremophile micro-organisms, that are capable of surviving in extremely hot environments.
The volcano is currently considered to be dormant rather than extinct.
Much of the watershed of Lake Taupo is a beech and podocarp forest with associate understory ferns being Blechnum filiforme, Asplenium flaccidum, Doodia media, Hymenophyllum demissum, Microsorum pustulatum and Microsorum scandens, and some prominent associate shrubs being Olearia ranii nd Alseuosmia quercifolia.
Native faunal species in the lake include northern koura or crayfish (Paranephrops planifrons) and kokopu or whitebait (Galaxias species). The lake is noted for stocks of brown trout (Salmo trutta) and rainbow trout (Oncorhynchus mykiss), introduced from Europe and California respectively in the late nineteenth century. There has also been a subsequent introduction of smelt (Retropinnidae species) as a food for the trout.
A community of sponges and associated invertebrates live around the underwater geothermal vents.
Tourism is a major component of Taupo's commercial sector, and the city attracts over 1.2 million visitors per year. The busiest time for the industry is the high summer season around Christmas and New Year.
The lake area has a temperate climate. Daily maximum temperatures recorded for Taupo range from an average of 23.3°C in January and February to 11.2°C in July, while the nighttime minimum temperatures range from 11.6°C in February down to 2.2°C in July. Rain falls in all seasons but is greatest in winter and spring, from June to December.
Taupo hosts the Lake Taupo Cycle Challenge, a cycling tour around the lake which can take anywhere between four and ten hours. Hundreds of volunteers from the Taupo township are involved in the event. Skydiving is a popular local sport and tourist attraction.
Māori rock carving
On the north west side of Lake Taupo on the cliffs of Mine Bay, there are Māori rock carvings created in the late 1970s by Matahi Whakataka-Brightwell and John Randall. Carved in likeness of Ngatoroirangi, a navigator who guided the Tuwharetoa and Te Arawa tribes to the Taupo area over a thousand years ago according to Māori legend. The 10-metre-high carving is intended to protect Lake Taupo from volcanic activities underneath. The cliff has become a popular tourist destination with hundreds of boats and yachts visiting the spot daily.
The two major tribes of Lake Taupo are Tuwharetoa from the Te Arawa waka and Ngati Maniapoto from the Tainui waka. Ngati Maniapoto also descend through Te Arawa waka as the mother of Maniapoto was Turongoihi, who married Raukawa (Maniapoto's father). Turongoihi was a direct descendant of Tia for which the name "Tauponui a- Tia" comes from. Ngati Rora( a hapu from Ngati Maniapoto) also descend from the Te Arawa waka through ancestors Ngatoroirangi, Tohoto-ariki, Ngaruahaoa, Tuwharetoa, Tamatekapua,Rangitihi, Pikiao, Hei, Tuparahaki.
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- Hogg A, Lowe DJ, Palmer J, Boswijk G, Ramsey CB (2011). "Revised calendar date for the Taupo eruption derived by 14C wiggle-matching using a New Zealand kauri 14C calibration data set". The Holocene. doi:10.1177/0959683611425551.
- Climate, History and the Modern World, Lamb,H. (1995), Routledge
- C. E. J. de Ronde, P. Stoffers, D. Garbe-Schönberg, B. W. Christenson, B. Jones, R. Manconi, P. R. L. Browne, K. Hissmann, R. Botz, B. W. Davy, M. Schmitt and C. N. Battershill (2002). "Discovery of active hydrothermal venting in Lake Taupo, New Zealand". Journal of Volcanology and Geothermal Research 115 (3-4): 257–275. Bibcode:2002JVGR..115..257D. doi:10.1016/S0377-0273(01)00332-8.
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- C. Michael Hogan. 2009. Crown Fern: Blechnum discolor, Globaltwitcher.com, ed. N. Stromberg
- "Mean Daily Maximum Temperatures". NIWA. Retrieved 1 September 2011.
- "Mean Daily Minimum Temperatures". NIWA. Retrieved 1 September 2011.
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- "Moari Rock Varvings Taupo, New Zealand". Retrieved 8 November 2011.
- Ben G. Mason; David M. Pyle, and Clive Oppenheimer (2004). "The size and frequency of the largest explosive eruptions on Earth". Bulletin of Volcanology 66 (8): 735–748. Bibcode:2004BVol...66..735M. doi:10.1007/s00445-004-0355-9.
- "Taupo". Global Volcanism Program, Smithsonian Institution. http://www.volcano.si.edu/world/volcano.cfm?vnum=0401-07%3D. Retrieved 2009-01-01.
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