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Large igneous province and subsurface plateau in the Pacific Ocean
The Hikurangi Plateau is an oceanic plateau in the South Pacific Ocean east of the North Island of New Zealand. It is part of a large igneous province
Hikurangi_Plateau
Oceanic trench off the east coast of New Zealand
The Hikurangi Trough (previously known as the Hikurangi Trench) is a sea floor feature of the Pacific Ocean off the north-east South Island and the east
Hikurangi_Trough
Plateau in the southwest Pacific Ocean
volcanic event around 90 Ma. Two other southwestern Pacific plateaus, Manihiki and Hikurangi, now separated from the OJP by Cretaceous oceanic basins, are
Ontong_Java_Plateau
Large igneous province and subsurface plateau in the Pacific Ocean
million years ago the Manihiki Plateau formed part of the giant Ontong Java-Manihiki-Hikurangi plateau. The Manihiki Plateau extends from 3°S to 6°S and
Manihiki_Plateau
Linear ocean trench in the South Pacific
(620 mi) from the Louisville Seamount Chain in the north (26°S) to the Hikurangi Plateau in the south (37°S), north-east of New Zealand's North Island. Together
Kermadec_Trench
Deep oceanic basin in the southwestern Pacific Ocean
Java-Manihiki-Hikurangi large igneous province (LIP), as it has been shown to be the spreading centre that lead to the separation of the Manihiki Plateau to its
Osbourn_Trough
Subduction zone off the east coast of New Zealand's North Island
The Hikurangi Margin (also known as the Hikurangi Subduction Zone) is New Zealand's largest subduction zone and fault. The Hikurangi Subduction Zone is
Hikurangi_Margin
Topics referred to by the same term
North Island of New Zealand Hikurangi Plateau, an oceanic plateau off the East Coast of the North Island of New Zealand Hikurangi, the traditional Te Kawerau
Hikurangi_(disambiguation)
Ridge in the Pacific Ocean
Caratori-Tontini, F.; Gamble, J. A. (2014). "Subduction of the oceanic Hikurangi Plateau and its impact on the Kermadec arc" (PDF). Nature Communications.
Tonga–Kermadec_Ridge
Mostly submerged continental crust area in Oceania
separated by the Alpine Fault and Kermadec Trench and by the wedge-shaped Hikurangi Plateau, and they are moving separately from each other. The case for Zealandia
Zealandia
Plateau (Indian) Hikurangi Plateau (Southwest Pacific) Kerguelen Plateau (Indian) Manihiki Plateau (Southwest Pacific) Marquesas Plateau (Southwest Pacific)
List of submarine topographical features
List_of_submarine_topographical_features
Relatively flat submarine region that rises well above the level of the ambient seabed
Plateau (Caribbean) Exmouth Plateau (Indian) Hikurangi Plateau (Southwest Pacific) Iceland Plateau (North Atlantic) Kerguelen Plateau (Indian) Magellan Rise
Oceanic_plateau
Area of ocean floor to the east of New Zealand
Zealand coast, and further from the coast the Rise borders on the Hikurangi Plateau. To the south, similar depths are achieved in the Bounty Trough. Past
Chatham_Rise
Feature of the Pacific Ocean floor
Wishbone scarp Tonga Trench Osbourn Trough Kermadec Trench Hikurangi Plateau Chatham Rise The Wishbone scarp is a Pacific Ocean floor feature in
Wishbone_scarp
Huge regional accumulation of igneous rocks
Kerguelen Plateau (Indian Ocean) Iceland Plateau (Atlantic Ocean) Ontong Java Plateau, Manihiki Plateau and Hikurangi Plateau (southwest Pacific Ocean) Jameson
Large_igneous_province
Brian (31 January 2006). "The single largest oceanic plateau: Ontong Java-Manihiki-Hikurangi" (PDF). Earth and Planetary Science Letters. 241 (3–4)
List of largest volcanic eruptions
List_of_largest_volcanic_eruptions
Large oceanic plateau south of New Zealand
The Campbell Plateau is a large oceanic plateau south of New Zealand and the Chatham Rise. It originated in the Gondwanan breakup and is part of Zealandia
Campbell_Plateau
Fault zone of the east coast of New Zealand's North Island
Wairarapa shore this decreases to perhaps 2 cm/year (0.79 in/year). The Hikurangi Plateau, a remnant of a large igneous province is being subducted under the
North_Island_Fault_System
Submarine plateau west of New Zealand
The Challenger Plateau is a large submarine plateau west of New Zealand and south of the Lord Howe Rise. It has an approximate diameter of 500 km (310 mi)
Challenger_Plateau
Oceanic rift valley in the south-west Pacific Ocean to the north of New Zealand
to 35°S. South of the Rapuhia Scarp at 35°S it is thought that the Hikurangi Plateau volcanics which are up to 15 km (9.3 mi) thick are subducting and
Havre_Trough
Supervolcano in New Zealand
present high rate of rift spreading and the recent subduction of the Hikurangi Plateau this area is very productive in its surface volcanism. If the magma
Taupō_Volcano
Geology of continental crust containing New Zealand and New Caledonia
separated by the Alpine Fault and Kermadec Trench and by the wedge-shaped Hikurangi Plateau, and they are moving separately from each other. The case for Zealandia
Geology_of_Zealandia
Deep cleft in the floor of the south Tasman Sea south of New Zealand's South Island
Dampier Ridge Fairway Ridge Hikurangi Plateau Kenn Plateau Lord Howe Rise Loyalty Ridge Mellish Rise Norfolk Ridge Northland Plateau Puysegur Ridge Resolution
Puysegur_Trench
Oil and gas field offshore of north Taranaki in New Zealand
Dampier Ridge Fairway Ridge Hikurangi Plateau Kenn Plateau Lord Howe Rise Loyalty Ridge Mellish Rise Norfolk Ridge Northland Plateau Puysegur Ridge Resolution
Pohokura_field
Deep sea plateau, west of New Zealand
The Lord Howe Rise is a deep sea plateau which extends from south west of New Caledonia to the Challenger Plateau, west of New Zealand in the south west
Lord_Howe_Rise
Hydrocarbon field in New Zealand
Dampier Ridge Fairway Ridge Hikurangi Plateau Kenn Plateau Lord Howe Rise Loyalty Ridge Mellish Rise Norfolk Ridge Northland Plateau Puysegur Ridge Resolution
Maui_gas_field
Submarine canyon near New Zealand
(930 mi) long Hikurangi Channel, which supplies turbidites to the Hikurangi Trough, as well as to low parts of the oceanic Hikurangi Plateau, and to the
Kaikōura_Canyon
Volcano that has erupted with a volcanic explosivity index of 8
Java Plateau has an area of about 2,000,000 km2 (770,000 sq mi), and the province was at least 50% larger before the Manihiki and Hikurangi Plateaus broke
Supervolcano
Tectonic plate in the south Pacific Ocean
Dampier Ridge Fairway Ridge Hikurangi Plateau Kenn Plateau Lord Howe Rise Loyalty Ridge Mellish Rise Norfolk Ridge Northland Plateau Puysegur Ridge Resolution
Kermadec_plate
Area of mainly sea to the south of the South Island of New Zealand
Dampier Ridge Fairway Ridge Hikurangi Plateau Kenn Plateau Lord Howe Rise Loyalty Ridge Mellish Rise Norfolk Ridge Northland Plateau Puysegur Ridge Resolution
Great_South_Basin
unknown Honshū Unknown 070 70 Noi Rhyolite 8 Ontong-Java-Manihiki-Hikurangi Plateau Southwestern Pacific Ocean, north of the Solomon Islands Unknown 121
List of large volcanic eruptions
List_of_large_volcanic_eruptions
Caratori-Tontini, F.; Gamble, J. A. (2014). "Subduction of the oceanic Hikurangi Plateau and its impact on the Kermadec arc" (PDF). Nature Communications.
Geology_of_New_Zealand
Oilfield off the coast of South Taranaki, New Zealand
Dampier Ridge Fairway Ridge Hikurangi Plateau Kenn Plateau Lord Howe Rise Loyalty Ridge Mellish Rise Norfolk Ridge Northland Plateau Puysegur Ridge Resolution
Maari_oil_field
Oilfield off the coast west of Taranaki, New Zealand
Dampier Ridge Fairway Ridge Hikurangi Plateau Kenn Plateau Lord Howe Rise Loyalty Ridge Mellish Rise Norfolk Ridge Northland Plateau Puysegur Ridge Resolution
Tui_oil_field
The Kenn Plateau is a large piece of submerged continental crust off northeastern Australia that rifted from northeastern Australia about 63-52 mya, along
Kenn_Plateau
Large region of volcanic rock in Russia
swarm) Matachewan Mistassini North Atlantic Ongeluk Ontong Java-Manihiki-Hikurangi Panjal Paraná and Etendeka Shatsky Siberian Skagerrak Ungava Winagami
Siberian_Traps
Submarine volcanic field off New Zealand
Dampier Ridge Fairway Ridge Hikurangi Plateau Kenn Plateau Lord Howe Rise Loyalty Ridge Mellish Rise Norfolk Ridge Northland Plateau Puysegur Ridge Resolution
Maahunui_volcanic_field
Depression in the submerged eastern part of Zealandia
is located to the South of the Chatham Rise, and North of the Campbell Plateau. It runs East-West for a distance of some 800 kilometres (497 mi) to the
Bounty_Trough
Tectonic process
the sinking slab is characterized by the Hikurangi plateau in the south. The thickness of this oceanic plateau ranges from 15 km to 10 km along the oceanic
Oblique_subduction
English-born New Zealand geologist
1144/gsjgs.149.6.0967. Nick Mortimer, Dave Parkinson (January 1996). "Hikurangi Plateau: a Cretaceous large igneous province in the southwest Pacific Ocean"
Nick_Mortimer
Volcanic activity of New Zealand
years ago and so likely come from a large singe event. The Hikurangi Plateau is an oceanic plateau on the Pacific Plate that attached to the Chatham Ridge
Volcanism_of_New_Zealand
Terrane found in New Zealand
emplaced, deformed and metamorphosed during collision of the LIP Hikurangi Plateau with Zealandia". Gondwana Research. 27 (3): 1255–1269. Bibcode:2015GondR
Torlesse_composite_terrane
Oceanic ridge in the south-west Pacific Ocean between Fiji and New Zealand
Dampier Ridge Fairway Ridge Hikurangi Plateau Kenn Plateau Lord Howe Rise Loyalty Ridge Mellish Rise Norfolk Ridge Northland Plateau Puysegur Ridge Resolution
Lau–Colville_Ridge
Continental flood basalts and oceanic plateaus
Plateau and Hikurangi Plateau were then part of the same large igneous province, forming the world's largest oceanic plateau. The Ontong Java Plateau
List of flood basalt provinces
List_of_flood_basalt_provinces
Seamount chain in the southwest Pacific Ocean
Wishbone scarp Tonga Trench Osbourn Trough Kermadec Trench Hikurangi Plateau Chatham Rise The oldest volcanic rocks of the chain come from Osbourn
Louisville_Ridge
Guyot, or flat-topped underwater volcano, in the Coral Sea
Dampier Ridge Fairway Ridge Hikurangi Plateau Kenn Plateau Lord Howe Rise Loyalty Ridge Mellish Rise Norfolk Ridge Northland Plateau Puysegur Ridge Resolution
Banc_Capel
Oceanic trough between New Caledonia and New Zealand
Norfolk Ridge Three Kings Ridge Taranaki Basin Aotea Basin Challenger Plateau New Zealand The New Caledonia Trough is an ocean floor feature that
New_Caledonia_Trough
Onshore-offshore Cretaceous rift basin on the West Coast of New Zealand
the subduction of the Pacific Plate under the Australian Plate at the Hikurangi Subduction System. The basin covers approximately 100,000 km2 of which
Taranaki_Basin
Deep sea plateau, north of New Zealand
North Island, and its extension under the Tasman Sea of the Northland Plateau. However, there is a distinct age difference between the 25 million years
Three_Kings_Ridge
Volcanic seamount north of New Zealand
Dampier Ridge Fairway Ridge Hikurangi Plateau Kenn Plateau Lord Howe Rise Loyalty Ridge Mellish Rise Norfolk Ridge Northland Plateau Puysegur Ridge Resolution
Monowai_(seamount)
Lateral-moving transform fault south of New Zealand
Macquarie Island and to its east towards the southern tip of the Campbell Plateau there has been some historic earthquake activity outside the zone. In the
Macquarie_fault_zone
Volcanic seamount in the Kermadec Islands group
Dampier Ridge Fairway Ridge Hikurangi Plateau Kenn Plateau Lord Howe Rise Loyalty Ridge Mellish Rise Norfolk Ridge Northland Plateau Puysegur Ridge Resolution
Havre_Seamount
Submarine volcano in New Zealand's Kermadec Islands
Dampier Ridge Fairway Ridge Hikurangi Plateau Kenn Plateau Lord Howe Rise Loyalty Ridge Mellish Rise Norfolk Ridge Northland Plateau Puysegur Ridge Resolution
James_Healy_Seamount
Geological area of the North Island of New Zealand
Rangitikei Rivers before terminating at the foot of the North Island Volcanic Plateau. The southern half of the basin extends into the South Taranaki Bight.
Wanganui_Basin
Submarine ridge between New Caledonia and New Zealand
Dampier Ridge Fairway Ridge Hikurangi Plateau Kenn Plateau Lord Howe Rise Loyalty Ridge Mellish Rise Norfolk Ridge Northland Plateau Puysegur Ridge Resolution
Norfolk_Ridge
Series of 28 small underwater volcanoes on the Chatham Rise, east of New Zealand
cover about 140 km2 (54 mi2) and stand out from the surrounding oceanic plateau that measures several hundred kilometers. They are named after various
Graveyard_Seamounts
Metamorphic unit in New Zealand
emplaced, deformed and metamorphosed during collision of the LIP Hikurangi Plateau with Zealandia". Gondwana Research. 27 (3): 1255–1269. Bibcode:2015GondR
Haast_Schist
Geology and geomorphology of a national park in New Zealand
ended c. 105 – c. 100 Ma possibly as a result of the thick basaltic Hikurangi Plateau moving into the Gondwana-Zealandia subduction zone and effectively
Geology and geomorphology of Kahurangi National Park
Geology_and_geomorphology_of_Kahurangi_National_Park
Geology in New Zealand
emplaced, deformed and metamorphosed during collision of the LIP Hikurangi Plateau with Zealandia". Gondwana Research. 27 (3): 1255–1269. doi:10.1016/j
Geology of the West Coast Region
Geology_of_the_West_Coast_Region
Oceanic basin in the south-west Pacific Ocean between New Caledonia and New Zealand
abyssal plain North Fiji Basin North Norfolk plateau North Norfolk Basin Nepean saddle Bates plateau Reinga Ridge Kermadec Trench Lau– Colville
Norfolk_Basin_(Oceania)
Deepest oceanic trench in the southwestern Pacific Ocean
Tonga Trench Kermadec Trench Osbourn Trough Louisville Seamount Chain Hikurangi Trough New Zealand The Tonga Trench is an oceanic trench located in the
Tonga_Trench
First epoch of the Cretaceous Period
Java–Manihiki–Hikurangi large igneous province, emplaced in the South Pacific at c. 120 Ma, is by far the largest LIP in Earth's history. The Ontong Java Plateau today
Early_Cretaceous
Waka, one of the great voyaging canoes of Māori tradition
found at Kirikino in Tūranganui. Along the way, they visited Tama-ki-hikurangi at Kakahoroa and discovered that the people of New Zealand had no kūmara
Mātaatua
Hierarchical outline list of articles related to oceanography
Kermadec Islands Hikurangi Margin – Subduction zone off the east coast of New Zealand's North Island Hikurangi Plateau – An oceanic plateau in the South Pacific
Outline_of_oceanography
Oceanic plateau in the north-west Pacific Ocean
(LIPs) together with Hess Rise, Magellan Rise, and Ontong Java-Manihiki-Hikurangi. It was named for Nikolay Shatsky (1895-1960), a Soviet geologist, expert
Shatsky_Rise
Species of shark
Reinga Ridge, the West Norfolk Ridge, the Hikurangi Trough and the Chatham Rise as well as on the Campbell Plateau. The overall colouration of this species
Bulldog_catshark
system 156–120 Ma. Following the formation and break-up of the Ontong Java–Hikurangi–Manihiki large igneous province 120 Ma, however, the Phoenix plate broke
Geology_of_the_Pacific_Ocean
Tectonic belt of earthquakes and volcanoes
Yap Trench Philippine Trench Sunda Trench Tonga Trench Kermadec Trench Hikurangi Trough Subduction zones around the Pacific Ocean do not form a complete
Ring_of_Fire
Volcano in New Zealand
the southern end of the Taupō Volcanic Zone and North Island volcanic plateau in New Zealand. It is 23 km (14 mi) northeast of Ohakune and 23 km (14 mi)
Mount_Ruapehu
Oceanic basin in the south-west Pacific Ocean between Fiji and New Zealand
However the current best fit model is one of west-dipping Tonga–Kermadec–Hikurangi subduction zone rolling back clockwise, and an approximately east-dipping
South_Fiji_Basin
Active volcanic zone in New Zealand
associated with oblique Australian and Pacific Plate convergence in the Hikurangi subduction zone. At Taupō the rift volcanic zone is widening east–west
Taupō_Volcanic_Zone
Species of fish
Challenger Plateau, Chatham Slope and its rise, Hikurangi Trough, Campbell Plateau, and Bounty Plateau. Chimaera carophila differs from C. fulva, C. macrospina
Chimaera_carophila
crop out at Kamo, near Whangārei, and Oligocene limestone crops out at Hikurangi, near Whangārei. A subduction zone is believed to have existed to the
Geology of the Northland Region
Geology_of_the_Northland_Region
Island country in the Pacific Ocean
plate under the other, producing the Puysegur Trench to the south, the Hikurangi Trough east of the North Island, and the Kermadec and Tonga Trenches further
New_Zealand
Species of flowering plant
east. In the North Island it is found south of the Volcanic Plateau and Mount Hikurangi, in tussock and fellfields, and in snow tussock in the Tararua
Celmisia_spectabilis
Lallemand, S. (2001). "The giant Ruatoria debris avalanche on the northern Hikurangi margin, New Zealand: Result of oblique seamount subduction". Journal of
List_of_landslides
Species of evergreen tree
and geography. The upper tree line reaches 1,430 m (4,690 ft) on Mount Hikurangi, 1,200–1,280 m (3,940–4,200 ft) in the Tararua Ranges and Nelson, and
Nothofagus_menziesii
Leader of the Waikato tribes and second Māori King (c. 1822–1894)
many of them armed, rode into Pirongia from the Tainui settlement at Hikurangi, modern-day Taumarunui. A pacifist, Tāwhiao had finally elected to sue
Tāwhiao
Extinct volcano in Waikato district of New Zealand
basaltic eruption 2.03 ± 0.03 Ma 2.25 to 2.13 Ma Hiwikiwi 2.30 ± 0.005 Ma Hikurangi 2.35 ± 0.2 Ma Ruapane 2.396 ± 0.005 Ma Mahaukura Mahaukura edifice . Central
Mount_Pirongia
Long and narrow depressions of the sea floor
such as the arrival of buoyant lithosphere (a continent, arc, ridge, or plateau), a change in the subduction dynamics, or a change in the plate kinematics
Oceanic_trench
Strait between the North and South Islands of New Zealand
with steep walls descending eastwards into the bathyal depths of the Hikurangi Trough. To the north-west lies the Narrows Basin, where water is 300 and
Cook_Strait
Early Māori explorer
who had settled in the Far North. Tahu-whakatiki's sons Te Whara and Hikurangi took Īhenga in a canoe past Taranga and Hauturu to Moehau in the Coromandel
Īhenga
Species of flowering plant in the plantain family
Zealand in 1961. The holotype was collected by Donald Petrie in 1897 on Hikurangi, North Island, New Zealand and is housed at the herbarium of the Museum
Plantago_novae-zelandiae
Times. Retrieved 25 April 2015. McKinnon, Malcolm (25 May 2015). "Volcanic Plateau places – Rotorua city". Te Ara: The Encyclopedia of New Zealand. Retrieved
List of former local authorities in New Zealand
List_of_former_local_authorities_in_New_Zealand
Species of plant
North, it is found from Mount Hikurangi south to Tararua Range, including Taranaki, the mountains of the Central Plateau, and Ruahine Ranges. South Island
Agrostis_dyeri
back-arc basin, which lies behind the Kermadec-Tonga subduction zone (Hikurangi Trough – Kermadec Trench – Tonga Trench). Some lakes in the area: Taupo
List of Quaternary volcanic eruptions
List_of_Quaternary_volcanic_eruptions
New Zealand radio network
Taupō is a radio station based in Taupō, broadcasting across the Central Plateau. The More FM brand replaced the previous local branded 93.5 KIS FM. More
More_FM
Harbour estuary in New Zealand
Dargaville is the principal centre in the Kaipara area. Its population plateaued in the 1960s. It is the country's main kūmara (sweet potato) producer
Kaipara_Harbour
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