175.90778 38.80694 motutaiko tuwharetoa taupo turangi ngati arawa supervolcanoes niwa waikato tongariro 14c tianchi whenua botz s00445 vei tauranga baekdu planifrons koura extremophile boswijk stoffers fumarole galaxias mykiss discolor brightwell
is lake taupo the largest lake in the world
Lake Taupo - Wikipedia Lake Taupo Jump to : navigation , search <Th_colspan="2"> Lake Taupo <Td_colspan="2"> Location Taupo District , Waikato Region , North Island Coordinates 38 ° 48 ′ 25 '' S 175 ° 54 ′ 28 '' E ﻿ / ﻿ 38.80694 ° S 175.90778 ° E ﻿ / - 38.80694 ; 175.90778 Coordinates : 38 ° 48 ′ 25 '' S 175 ° 54 ′ 28 '' E ﻿ / ﻿ 38.80694 ° S 175.90778 ° E ﻿ / - 38.80694 ; 175.90778 Type Crater lake , oligotrophic Primary inflows Waitahanui River , Tongariro River , Tauranga Taupo River Primary outflows Waikato River Catchment area 3,487 km ( 1,346 sq mi ) Basin countries New Zealand <Th_colspan="2"> Max. length 46 km ( 29 mi ) Max . width 33 km ( 21 mi ) Surface area 616 km ( 238 sq mi ) Average depth 110 m ( 360 ft ) Max . depth 186 m ( 610 ft ) Water volume 59 km ( 14 cu mi ) Residence time 10.5 years Shore length 193 km ( 120 mi ) Surface elevation 356 m ( 1,168 ft ) <Th_colspan="2"> Islands Motutaiko Island ( 11 ha ) <Td_colspan="2"> Shore length is not a well - defined measure . Lake Taupo Lake Taupo is in the Waikato Region of the North Island . Lake Taupo is a lake in the North Island of New Zealand . It is in the caldera of the Taupo Volcano . 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 ) . Motutaiko Island lies in the south east area of the lake . Lake Taupo has a perimeter of approximately 193 kilometres and a deepest point of 186 metres . It is drained by the Waikato River ( New Zealand 's longest river ) , and 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 and rainbow trout . Contents ( hide ) 1 Lake formation and volcanism 2 Biota 3 Tourism 3.1 Māori rock carving 3.2 Māori tribes 4 See also 5 References 6 Further reading 7 External links Lake formation and Volcanism ( edit ) Main article : Taupo Volcano Lake Taupo is 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 known as the Oruanui eruption . It was the world 's largest known eruption over the past 70,000 years , ejecting 1170 cubic kilometres of material and causing 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 a few minutes . This was one of the most violent eruptions in the last 5000 years ( alongside the Minoan eruption in the 2nd millennium BCE , the Tianchi eruption of Baekdu around 1000 CE 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 because of moderate fumarole activity and hot springs along the shores of the lake . Biota ( edit ) Lake Taupo 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 and 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 ( edit ) NASA satellite photo of Lake Taupo Tourism is a major component of Taupo 's commercial sector , and the city attracts over 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 . Taupo also hosts the Kellogg 's Ironman event . Māori rock carving ( edit ) Māori rock carvings at Mine Bay on Lake Taupo are over 10 metres high and accessible only by boat or kayak . 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 yearly . Māori tribes ( edit ) Lake Taupo is a taonga ( treasure or something special to the person ) of Ngati Tuwharetoa from the Te Arawa waka . Ngati Tuwharetoa still own the bed of the lake and its tributaries . They grant the public free access for recreational use . See also ( edit ) Lists of Supervolcanoes : VEI - 8 volcanoes and VEI - 7 volcanoes List of lakes in New Zealand List of volcanoes in New Zealand Taupo Volcanic Zone References ( edit ) Jump up ^ `` Motutaiko Island : Current Nga Whenua Rahui and Matauranga Kura Taiao projects '' . Department of Conservation . Archived from the original on 4 March 2014 . Jump up ^ Cussen , Laurence ( 1887 ) . `` Notes on the Physiography and Geology of the King Country '' . Transactions of the Royal Society of New Zealand . 20 : 317 -- 332 . See Lake Taupo , pp 328 -- 331 Jump up ^ Manville , Vern & Wilson , Colin J.N. ( 2004 ) . `` The 26.5 ka Oruanui eruption , New Zealand : a review of the roles of volcanism and climate in the post-eruptive sedimentary response '' . New Zealand Journal of Geology & Geophysics. 47 ( 3 ) : 525 -- 547 . doi : 10.1080 / 00288306.2004. 9515074 . Archived from the original on 8 September 2008 . CS1 maint : Multiple names : authors list ( link ) Jump up ^ 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 . Jump up ^ Climate , History and the Modern World , Lamb , H. ( 1995 ) , Routledge ^ Jump up to : 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 . CS1 maint : Multiple names : authors list ( link ) Jump up ^ C. Michael Hogan . 2010 . Extremophile . eds . E. Monosson and C. Cleveland . Encyclopedia of Earth . National Council for Science and the Environment , Washington DC Jump up ^ C. Michael Hogan . 2009 . Crown Fern : Blechnum discolor , Globaltwitcher.com , ed . N. Stromberg Archived 13 February 2012 at the Wayback Machine . Jump up ^ `` Mean Daily Maximum Temperatures '' . NIWA . Archived from the original on 19 January 2012 . Retrieved 1 September 2011 . Jump up ^ `` Mean Daily Minimum Temperatures '' . NIWA . Archived from the original on 19 January 2012 . Retrieved 1 September 2011 . Jump up ^ `` Mean Monthly Rainfall '' . NIWA . Archived from the original on 19 January 2012 . Retrieved 1 September 2011 . Jump up ^ `` Maori Rock Carvings Lake Taupo '' . Retrieved 8 November 2011 . Jump up ^ `` New deed of settlement for Lake Taupo '' ( Press release ) . Further reading ( edit ) Ben G. Mason ; David M. Pyle ; 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 . Retrieved 2009 - 01 - 01 . External links ( edit ) Wikimedia Commons has media related to Lake Taupo . Great Lake Taupo Official Visitor Information Website Turangi and Lake Taupo Website Lake Taupo Webcam Lake Taupo at the Waikato Regional Council Lake Taupo area at the Department of Conservation Retrieved from `` https://en.wikipedia.org/w/index.php?title=Lake_Taupo&oldid=830777451 '' Categories : Taupo Volcanic Zone Calderas of New Zealand Taupo District VEI - 8 volcanoes Supervolcanoes Crater lakes Lakes of Waikato Hidden categories : CS1 maint : Multiple names : authors list Webarchive template wayback links Use dmy dates from April 2013 Use New Zealand English from April 2013 All Wikipedia articles written in New Zealand English Coordinates on Wikidata All articles with unsourced statements Articles with unsourced statements from May 2011 Articles with unsourced statements from February 2014 Articles using GVP links in vnum format Talk Contents About Wikipedia Ænglisc Azərbaycanca Беларуская Беларуская ( тарашкевіца ) ‎ Български Català Чӑвашла Čeština Deutsch Eesti Ελληνικά Español Esperanto فارسی Français Galego 한국어 हिन्दी Hrvatski Bahasa Indonesia Italiano עברית ქართული Latviešu Lietuvių Magyar Македонски മലയാളം Nederlands 日本 語 Norsk Norsk nynorsk Polski Português Runa Simi Русский Српски / srpski Srpskohrvatski / српскохрватски Suomi Svenska Türkçe Українська اردو Tiếng Việt 中文 37 more Edit links This page was last edited on 16 March 2018 , at 21 : 48 . 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