Auckland volcanic field - wikipedia Auckland volcanic field Map of the field drawn by Hochstetter in 1859 and published in English in 1864 The Auckland volcanic field is an area of monogenetic volcanoes covered by much of the metropolitan area of Auckland, New Zealand 's largest city, located in the North Island. The approximately 48 volcanoes in the field have produced a diverse array of maars ( explosion craters ), tuff rings, scoria cones, and lava flows. Aside from Rangitoto, which erupted repeatedly, no volcano has erupted twice, but eruptions lasted for various periods ranging from a few weeks to several years. The field is fuelled entirely by basaltic magma, unlike the explosive subduction - driven volcanism in the central North Island, such as at Mount Ruapehu and Lake Taupo. The field is currently dormant, but could become active again. Contents 1 Features 2 Human context 2.1 Usage 2.2 Dangers 3 List of volcanoes 4 See also 5 References 5.1 Further reading 6 External links Features The field ranges from Lake Pupuke and Rangitoto Island in the north to Matukutururu ( Wiri Mountain ) in the south, and from Mount Albert in the west to Pigeon Mountain in the east. The first vent erupted at Onepoto 248,000 ± 28,000 years ago. The most recent eruption ( about 600 years ago and within historical memory of the local Māori iwi ) was of Rangitoto, an island shield volcano just east of the city, erupting 2.3 cubic kilometres of lava. The eruptions have tended to become bigger over time, with Rangitoto making up almost 60 per cent of the field 's entire volume of erupted material. The field 's volcanoes are relatively small, with most less than 150 metres ( 490 ft ) in height. Lake Pupuke, on the North Shore near Takapuna, is a volcanic explosion crater. A few similar craters such as Orakei Basin are open to the sea. The field has produced voluminous lava flows that cover much of the Auckland isthmus. One of the longest runs from Mt Saint John northward, almost crossing the Waitematā Harbour to form Meola Reef. More than 50 lava tubes and other lava caves have been discovered, including the 290 - metre ( 950 ft ) - long Wiri Lava Cave. The second - longest individual cave in the Auckland field, some 270 metres ( 890 ft ) in total length, is the Cave of a Thousand Press - ups to the east of Maungakiekie / One Tree Hill. Two impressive depressions caused by lava cave collapses are the Puka Street Grotto and the nearby Hochstetter Pond, also known as Grotto Street Pond, in Onehunga. For most of the 250,000 years that the field has been erupting, the planet has been in glacial periods ( ice ages ) where sea levels were much lower due to water being locked up as ice, and the Waitemata and Manukau Harbours were dry land. All the volcanoes probably erupted on land except for Rangitoto, which erupted during the current interglacial ( warmer ) period. Human context Terraces carved by Māori into the slopes of One Tree Hill Usage Many of the volcanic cones were occupied by substantial Māori pā before European settlement, and many terraces and other archeological remnants are still visible. Many of the cones have been levelled or strongly altered -- in small part due to the historical Māori use, but mostly through relatively recent quarrying of construction materials ( especially scoria ). However several of the remaining volcanoes are now preserved as landmarks and parks. The cones are also protected by a 1915 law, the Reserves and Other Lands Disposal and Public Bodies Empowering Act 1915, which was passed due to early concern that the distinctive landscape was being eroded, especially by quarrying. While often ignored until the late 20th century, it has amongst other things minimised severe changes to Mount Roskill proposed by Transit New Zealand for the Southwestern Motorway. In March 2007, New Zealand submitted the volcanic field, with several specifically named features, as a World Heritage Site candidate based on its unique combination of natural and cultural features. At that time, only 2 per cent of more than 800 World Heritage Sites worldwide were in this `` mixed '' category. Dangers Since the field is not extinct, new volcanic events may occur at any time, though the usual period between events is, on average, somewhere between hundreds to thousands of years. However, the effects of such an event -- especially a full - scale eruption -- would be substantial, ranging from pyroclastic surges to earthquakes, lava bombs, ash falls, and the venting volcanic gas, as well as lava flows. These effects might continue for several months, potentially causing substantial destruction and disruption, ranging from the burial of substantial tracts of residential or commercial property, to the mid-to - long - term closures of major parts of the country 's infrastructure such as the Port of Auckland, the State Highway network, or the Auckland Airport. It is possible that several volcanoes could erupt simultaneously. There is strong evidence that five erupted within a span of 50 years or less, approximately 32,000 years ago. Various operative structures, plans and systems have been set up to prepare responses to volcanic activity within the urban areas, mainly coordinated in the ' Auckland Volcanic Field Contingency Plan ' of the Auckland Regional Council, which provides a framework for interaction of civil defence and emergency services during an eruption. Auckland also has a seismic monitoring network comprising six seismometers -- including one 250 metres ( 820 ft ) deep at Riverhead -- and three repeaters within the region that will detect the small tremors likely to precede any volcanic activity. This is likely to give between a few hours and several days ' warning of an impending eruption, and its approximate location. Auckland War Memorial Museum, itself built on the crater rim of Pukekawa, has an exhibition on the field, including the `` Puia Street multi-sensory visitor experience '', which simulates a grandstand view of an eruption in Auckland. In 2013, scientists said new studies showed Rangitoto had been much more active in the past than previously thought, suggesting it had been active on and off for around 1000 years before the final eruptions around 550 years ago. Civil Defence officials said the discovery did not make living in Auckland any more dangerous, but did change their view of how an evacuation might proceed. List of volcanoes The volcanoes within the field are : Volcanoes Age Height ( m ) Refs Images Albert Park Volcano Ash Hill 32,000 years old 30 Auckland Domain / Pukekawa Boggust Park Crater 5 Cemetery Crater Crater Hill 32,000 years old Grafton Volcano Greenmount 78 Hampton Park 35 Kohuora 32,000 years old Lake Pupuke ~ 200,000 years old − 57 Little Rangitoto 75 Mangere Lagoon Mangere Mountain 106 Matukutureia / McLaughlin Mountain 73 Maungataketake / Elletts Mountain 76 McLennan Hills ~ 40,000 years old Browns Island 68 Mount Albert / Owairaka 135 Mount Cambria Maungawhau / Mount Eden 28,000 years old 196 crater of Maungawhau / Mount Eden Mount Hobson 143 Mount Richmond 32,000 years old 50 Mount Robertson / Sturges Park 78 Mount Roskill 110 Mount Saint John 126 Mount Smart Mount Victoria 87 Maungarei / Mount Wellington 10,000 years old 135 North Head 50 One Tree Hill / Maungakiekie 182 One Tree Hill and its obelisk Onepoto Basin ~ 250,000 years old Orakei Basin ~ 85,000 years old Otara Hill / Smales Hill Otuataua Panmure Basin Pigeon Mountain 55 Puhinui Craters 22 Pukaki Lagoon ~ 65,000 years old Pukeiti 30 Puketutu Island 32,000 years old 65 Pukewairiki / Highbrook Park 30 Purchas Hill 10,000 years old Rangitoto Island 600 years old 260 Rangitoto Island on the horizon Saint Heliers / Glover Park -- see Achilles Point Styaks Swamp Tank Farm, also known as Tuff Crater Taylors Hill 32,000 years old 56 Te Hopua a Rangi / Gloucester Park Te Pou Hawaiki Te Tatua - a-Riukiuta 28,500 years old 133 Waitomokia / Mt Gabriel Wiri Mountain / Matukutururu 32,000 years old See also List of volcanoes in New Zealand Volcanism in New Zealand References ^ Jump up to : McClure, Margaret ( 26 February 2018 ). `` Auckland Volcanoes ''. Auckland Places ( Auckland Places ) : 19. Retrieved 26 February 2018 -- via Te Ara - the Encyclopedia of New Zealand. Check date values in : year =, year = / date = mismatch ( help ) ^ Jump up to : Hayward, Bruce W. ; Murdoch, Graeme ; Maitland, Gordon ( 2011 ). Volcanoes of Auckland : The Essential Guide. Auckland University Press. ISBN 978 - 1 - 86940 - 479 - 6. Jump up ^ Ian E.M. Smith and Sharon R. Allen. Auckland volcanic field geology. Volcanic Hazards Working Group, Civil Defence Scientific Advisory Committee. Retrieved 30 March 2013. Also published in print as Volcanic hazards at the Auckland volcanic field. 1993. ^ Jump up to : Beca Carter Hollings & Ferner ( 2002 ). Contingency Plan for the Auckland Volcanic Field, Auckland Regional Council Technical Publication 165. Accessed 12 May 2008. Jump up ^ M.O. McWilliams research, 2002, associated with Shane P, Sandiford A ( 2003 ) Paleovegetation of marine isotope stages 4 and 3 in northern New Zealand and the age of the widespread Rotoehu Tephra. Quaternary Research 59 : 420 -- 429 ^ Jump up to : Auckland Volcanic Fields submission ( from the UNESCO World Heritage Centre, 30 March 2007. Accessed 2007 - 05 - 04 ) Jump up ^ Hayward, Murdoch, Maitland ( 2011 ). pp. 134 -- 135. Jump up ^ David Lomas ( Winter 2006 ). `` Cave new world ''. Heritage New Zealand. Accessed 4 May 2007. Jump up ^ Kermode, Les ( March 1994 ). `` New Zealand lava caves worth preserving for their geologic and geomorphic features '' ( PDF ). Geoscience Reports of Shizuoka University. 20 : 15 -- 24. Retrieved 6 December 2011. Jump up ^ Hayward, Murdoch, Maitland ( 2011 ). pp. 17 -- 18. Jump up ^ `` Geology ''. The Onehunga Grotto. Retrieved 25 April 2013. Jump up ^ Hayward, Murdoch, Maitland ( 2011 ). pp. 2 -- 3. Jump up ^ `` The volcanic hills are being destroyed... '' -- City of Fire, insert magazine in The New Zealand Herald, 15 February 2008 ^ Jump up to : `` When the earth starts to shake ''. City of Fire, insert magazine in The New Zealand Herald, 15 February 2008. Jump up ^ New recorder boosts earthquake, volcano warnings, The New Zealand Herald, NZPA, 11 May 2008. Accessed 2008 - 05 - 12. Jump up ^ `` Volcanoes ''. Auckland War Memorial Museum. Retrieved 28 September 2017. Jump up ^ `` Rangitoto more active than thought -- study ''. 3 News NZ. 11 April 2013. Jump up ^ `` Officials downplay volcano danger ''. 3 News NZ. 12 April 2013. Jump up ^ Lindsay, J.M. ; Leonard, G.S. ; Smid, E.R. ; Hayward, B.W. ( December 2011 ). `` Age of the Auckland Volcanic Field : a review of existing data ''. New Zealand Journal of Geology and Geophysics. 54 ( 4 ) : 379 -- 401. doi : 10.1080 / 00288306.2011. 595805. Further reading Lava and Strata : A guide to the volcanoes and rock formations of Auckland. Homer, Lloyd ; Moore, Phil & Kermode, Les ; Landscape Publications and the Institute of Geological and Nuclear Sciences, 2000. ISBN 0 - 908800 - 02 - 9. `` Probabilistic assessment of future vent locations and eruption styles for the Auckland Volcanic Field, New Zealand ''. Magill, Christina R ; McAneney, K.J. ; Proceedings of the International Association for Mathematical Geology 2003, Portsmouth, UK, 7 -- 12 September 2003. Volcanic risk ranking for Auckland, New Zealand. I : Methodology and hazard investigation. Magill, Christina R. ; Blong, Russell ; Bulletin of Volcanology, Volume 67, Issue 4, April 2005, Pages 331 -- 339, DOI 10.1007 / s00445 - 004 - 0374 - 6, accessed 2006 - 07 - 14. City of Volcanoes : A geology of Auckland. Searle, Ernest J. ; revised by Mayhill, R.D. ; Longman Paul, 1981. First published 1964. ISBN 0 - 582 - 71784 - 1. `` Facies analysis of pyroclastic deposits within basaltic tuff - rings of the Auckland volcanic field, New Zealand ( abstract ) ''. Sharon R. Allen, Vivienne F. Bryner, Ian E.M. Smith, Peter F. Ballance, New Zealand Journal of Geology and Geophysics, 1996, Vol. 39 : 309 -- 327. External links Wikimedia Commons has media related to Auckland volcanic field. Volcanic hazards, Auckland Council `` Auckland field ''. Global Volcanism Program. Smithsonian Institution. `` Volcanoes ''. Auckland War Memorial Museum. Retrieved 28 September 2017. Geology : Rocks and minerals, School of Geography, Geology and Environmental Science, University of Auckland ( with interactive maps, requiring Apple QuickTime ). Auckland volcanic field Central Auckland Pukekawa / Auckland Domain Grafton Volcano Albert Park Volcano Te Pou Hawaiki Maungawhau / Mt. Eden Ohinerangi / Mt. Hobson Te Kopuke / Mt. St John Maungakiekie / One Tree Hill Te Tatua a Riukiuta / Three Kings Puketapapa / Mt. Roskill Te Ahi ka roa a Raka / Mt Albert / Owairaka Te Hopua a Rangi / Gloucester Park Rarotonga / Mt Smart Orakei Basin Maungarahiri / Little Rangitoto East Auckland Maungarei / Mt. Wellington Te Tauoma / Purchas Hill Whakamuhu / Glover Park Taurere / Taylors Hill Te Kopua Kai a Hiku / Panmure Basin Ō Huiarangi / Pigeon Mountain Hampton Park Te Puke o Taramainuku / Ōtara Hill Matanginui / Green Hill Styaks Swamp Pukewairiki / Highbrook Park Te Apunga o Tainui / McLennan Hills Ōtāhuhu / Mt. Richmond Mt. Robertson / Sturges Park South Auckland Te Pane a Mataaho / Mangere Mountain Māngere Lagoon Te Motu a Hiaroa / Puketutu Moerangi / Waitomokia / Mt. Gabriel Puketapapakanga a Hape / Pukeiti Ōtuataua Maungataketake / Ellett 's Mount Te Pukaki Tapu o Poutukeka / Pukaki Lagoon Crater Hill Kohuora Matukutūruru / Te Manurewa o Tamapahore / Wiri Mountain Ash Hill Matukutūreia / McLaughlins Mountain Waitematā Harbour and North Shore Rangitoto Motukorea / Browns Island Pupuke Moana / Pupuke Volcano Te Kopua o Matakamokamo / Tank Farm Te Kopua o Matakerepo / Onepoto Basin Maungauika / North Head Takarunga / Mt. Victoria Takararo / Mt. Cambria Retrieved from `` https://en.wikipedia.org/w/index.php?title=Auckland_volcanic_field&oldid=827651347 '' Categories : Auckland volcanic field Potentially active volcanoes Monogenetic volcanic fields Geography of Auckland Landforms of the Auckland Region Mountains of the Auckland Region Hidden categories : CS1 errors : dates Use dmy dates from September 2017 Talk Contents About Wikipedia Čeština Deutsch Magyar Русский Slovenčina Edit links This page was last edited on 25 February 2018, at 23 : 18. 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Question: when did the last volcano erupt in auckland
Answer: around 550 years ago