New Zealand outlying islands

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Map of the New Zealand outlying islands in relation to the main New Zealand archipelago New Zealand outlying islands.png
Map of the New Zealand outlying islands in relation to the main New Zealand archipelago

The New Zealand outlying islands are nine offshore island groups that are part of New Zealand, with all but Solander Islands lying beyond the 12nm limit of the mainland's territorial waters. Although considered integral parts of New Zealand, seven of the nine island groups are not part of any administrative region or district, but are instead each designated as an Area Outside Territorial Authority. The two exceptions are the Chatham Islands, which are covered by their own special territorial authority, and the Solander Islands, which are part of the Southland Region and Southland District.

Contents

Eight island groups sit on the New Zealand continental shelf, which forms a part of Zealandia. The Kermadec Islands, northeast of mainland New Zealand, are on a ridge, whose location as part or not part of Zealandia is not yet proven by geologists. [1] [2] Both sources show a map drawn of Zealandia, marking the location of islands north and south of New Zealand.

The term is also used sometimes to further encompass the Balleny Islands, a group of sub-Antarctic islands technically considered a part of the Ross Dependency and covered by the Antarctic Treaty.[ citation needed ]

The five island groups of the New Zealand Subantarctic Islands, including their territorial seas, are a World Heritage Site. [3]

Island groups

The nine island groups classed as part of New Zealand's outlying islands are:

MapIsland group
(other names)
LocationCoordinatesAreaHighest peak
Altitude
Notes
Topographical map of the Antipodes Islands in English.svg Antipodes Islands [4]
(Moutere Mahue)
New Zealand Subantarctic Islands, 860 kilometres (530 mi) east-southeast of Stewart Island / Rakiura 49°41′S178°48′E / 49.683°S 178.800°E / -49.683; 178.800 (Antipodes Islands) 21 square kilometres (8.1 sq mi) Mount Galloway
366 m (1,201 ft)
Part of the New Zealand Subantarctic Islands World Heritage Site
Auckland Islands New Zealand geographic map en.svg Auckland Islands [5]
(Motu Maha, Maungahuka)
New Zealand Subantarctic Islands, 360 kilometres (220 mi) of Stewart Island / Rakiura 50°42′S166°05′E / 50.700°S 166.083°E / -50.700; 166.083 (Auckland Islands) 625.64 square kilometres (241.56 sq mi) Mount Dick
705 m (2,313 ft)
Part of the New Zealand Subantarctic Islands World Heritage Site
Bounty Islands New Zealand geographic map en.svg Bounty Islands [6]
(Moutere Hauriri)
New Zealand Subantarctic Islands, roughly 670 km (416 mi) east-south-east of New Zealand's South Island and 530 km (329 mi) south-west of the Chatham Islands 47°46′S179°02′E / 47.767°S 179.033°E / -47.767; 179.033 (Bounty Islands) 1.35 square kilometres (0.52 sq mi)Unnamed point on Funnel Island
73 m (240 ft)
Part of the New Zealand Subantarctic Islands World Heritage Site
Campbell Island New Zealand geographic map en.svg Campbell Islands [7]
(Motu Ihupuku)
New Zealand Subantarctic Islands, 360 kilometres (220 mi) of Stewart Island / Rakiura 52°32′S169°09′E / 52.533°S 169.150°E / -52.533; 169.150 (Campbell Islands) 113.31 square kilometres (43.75 sq mi) Mount Honey
558 m (1,831 ft)
Part of the New Zealand Subantarctic Islands World Heritage Site
Chatham-Islands map topo en.svg Chatham Islands [8]
(Rēkohu, Wharekauri)
South Pacific Ocean, roughly 800 kilometres (500 mi) east of New Zealand's South Island 43°54′S176°32′W / 43.900°S 176.533°W / -43.900; -176.533 (Chatham Islands) 966 square kilometres (373 sq mi)Unnamed point on Chatham Island
299 m (981 ft)
Largest outlying island group, and the only one with a permanent population (800 as of June 2022 [9] ).
Karta NZ Kermadec isl.PNG Kermadec Islands [10]
(Rangitāhua)
South Pacific Ocean, roughly 800–1,000 kilometres (500–620 mi) north of New Zealand's North Island 29°16′S177°55′W / 29.267°S 177.917°W / -29.267; -177.917 (Kermadec Islands) 33.6 square kilometres (13.0 sq mi) Moumoukai Peak
516 m (1,693 ft)
Northernmost outlying island group, consisting of a range of volcanic islands which are part of the wider Tonga-Kermadec Ridge. Despite having no permanent population, a meteorological station on Raoul Island is permanently staffed.
Three Kings Islands New Zealand geographic map en.svg Manawatāwhi / Three Kings Islands [11]
(Ngā Motu Karaka)
Convergence of the Tasman Sea and the South Pacific Ocean, roughly 55 kilometres (34 mi) northwest of Cape Reinga / Te Rerenga Wairua 34°09′S172°08′E / 34.150°S 172.133°E / -34.150; 172.133 (Three Kings Islands) 6.85 square kilometres (2.64 sq mi)Unnamed point on Manawatāwhi / Great Island
295 m (968 ft)
Northernmost outlying island group, consisting of a range of volcanic islands which are part of the wider Tonga-Kermadec Ridge.
Snares Islands New Zealand geographic map en.svg Snares Islands / Tini Heke [12]
(Te Taniwha)
New Zealand Subantarctic Islands, 200 kilometres (120 mi) south of New Zealand's South Island 48°01′S166°32′E / 48.017°S 166.533°E / -48.017; 166.533 (The Snares) 3.5 square kilometres (1.4 sq mi)Unnamed point on North East Island
130 m (430 ft)
Part of the New Zealand Subantarctic Islands World Heritage Site. Given a dual name with the Ngāi Tahu Claims Settlement Act 1998.
Solander Islands New Zealand geographic map en.svg Solander Islands / Hautere [13] West of the Foveaux Strait, roughly 50 kilometres (31 mi) south of Fiordland on New Zealand's South Island 46°34′S166°53′E / 46.567°S 166.883°E / -46.567; 166.883 (Solander Islands) 1.2 square kilometres (0.46 sq mi)Unnamed point on Solander Island / Hautere
330 m (1,080 ft)
Only outlying island group to fall within the authority of a regional council, in this case Environment Southland. Given a dual name with the Ngāi Tahu Claims Settlement Act 1998.

Population

The islands are all uninhabited except the Chatham Islands.

There is a staffed meteorological station on Raoul Island of the Kermadec Islands. The meteorological station on Campbell Island has been unstaffed and automated since 1995. There was a meteorological station on the Auckland Islands from 1942 to 1945. The Three Kings Islands and the Auckland Islands were formerly inhabited. There have been failed settlement attempts on Raoul Island, the Antipodes Islands and the Auckland Islands. The Solander Islands have never been inhabited except by shipwrecked sailors or marooned stowaways (for the longest period, from 1808 to 1813 by five European stowaways).

See also

Related Research Articles

<span class="mw-page-title-main">Auckland Islands</span> Volcanic archipelago of New Zealands subantarctic islands

The Auckland Islands are an archipelago of New Zealand, lying 465 kilometres (290 mi) south of the South Island. The main Auckland Island, occupying 510 km2 (200 sq mi), is surrounded by smaller Adams Island, Enderby Island, Disappointment Island, Ewing Island, Rose Island, Dundas Island, and Green Island, with a combined area of 626 km2 (240 sq mi). The islands have no permanent human inhabitants.

<span class="mw-page-title-main">Manawatāwhi / Three Kings Islands</span> Island group near Cape Reinga, New Zealand

The Manawatāwhi / Three Kings Islands are a group of 13 uninhabited islands about 55 kilometres (34 mi) northwest of Cape Reinga / Te Rerenga Wairua, New Zealand, where the South Pacific Ocean and Tasman Sea converge. They measure 6.85 km2 (2.64 sq mi) in area. The islands are on a submarine plateau, the Three Kings Bank, and are separated from the New Zealand mainland by an 8 km wide, 200 to 300 m deep submarine trough. Therefore, despite relative proximity to the mainland, the islands are listed with the New Zealand Outlying Islands. The islands are an immediate part of New Zealand, but not part of any region or district, but instead Area Outside Territorial Authority, like all the other outlying islands except the Solander Islands.

<span class="mw-page-title-main">Kermadec Islands</span> Subtropical island arc in the South Pacific Ocean

The Kermadec Islands are a subtropical island arc in the South Pacific Ocean 800–1,000 km (500–620 mi) northeast of New Zealand's North Island, and a similar distance southwest of Tonga. The islands are part of New Zealand. They are 33.6 km2 (13.0 sq mi) in total area and uninhabited, except for the permanently staffed Raoul Island Station, the northernmost outpost of New Zealand.

<span class="mw-page-title-main">Bounty Islands</span> 13 islets and rocks in the subantarctic South Pacific administered by New Zealand

The Bounty Islands are a small group of 13 uninhabited granite islets and numerous rocks, with a combined area of circa 50 ha in the South Pacific Ocean. Territorially part of New Zealand, they lie about 670 km (416 mi) east-south-east of New Zealand's South Island, 530 km (329 mi) south-west of the Chatham Islands, and 215 km (134 mi) north of the Antipodes Islands. The group is a World Heritage Site.

<span class="mw-page-title-main">Campbell Island, New Zealand</span> Island in New Zealand

Campbell Island / Motu Ihupuku is an uninhabited subantarctic island of New Zealand, and the main island of the Campbell Island group. It covers 112.68 square kilometres (43.51 sq mi) of the group's 113.31 km2 (43.75 sq mi), and is surrounded by numerous stacks, rocks and islets like Dent Island, Folly Island, Isle de Jeanette-Marie, and Jacquemart Island, the latter being the southernmost extremity of New Zealand. The island is mountainous, rising to over 500 metres (1,640 ft) in the south. A long fiord, Perseverance Harbour, nearly bisects it, opening out to sea on the east coast.

<span class="mw-page-title-main">Snares Islands / Tini Heke</span> Small group of islands of New Zealand

The Snares Islands / Tini Heke, known colloquially as The Snares, is a group of uninhabited islands lying about 200 km south of New Zealand's South Island and to the south-southwest of Stewart Island / Rakiura. The Snares consist of the main North East Island and the smaller Broughton Island and Alert Stack, as well as the Western Chain Islands some 5 km (3.1 mi) to the west-southwest. Collectively, the Snares have a total land area of 3.5 km2 (1.4 sq mi).

<span class="mw-page-title-main">Antipodes Islands</span> Subantarctic archipelago of New Zealand

The Antipodes Islands are inhospitable and uninhabited volcanic islands in subantarctic waters to the south of – and territorially part of – New Zealand. The 21 km2 archipelago lies 860 km to the southeast of Stewart Island/Rakiura, and 730 km to the northeast of Campbell Island. They are very close to being the antipodal point to Normandy in France, meaning that the city farthest away is Cherbourg-en-Cotentin, France.

<span class="mw-page-title-main">New Zealand Subantarctic Islands</span> Southernmost parts of the South Pacific country

The New Zealand Subantarctic Islands comprise the five southernmost groups of the New Zealand outlying islands. They are collectively designated as a UNESCO World Heritage Site.

<span class="mw-page-title-main">Marine reserves of New Zealand</span>

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<span class="mw-page-title-main">Horoirangi Marine Reserve</span> Marine reserve near Nelson, New Zealand

The Horoirangi Marine Reserve, sometimes referred to as the Glenduan Marine Reserve, is situated to the north east of Nelson in New Zealand. It stretches along the coast from the northern end of Boulder Bank to just south of Cable Bay.

<span class="mw-page-title-main">Campbell Islands</span> Group of subantarctic South Pacific islands, administered by New Zealand

The Campbell Islands are a group of subantarctic islands, belonging to New Zealand. They lie about 600 km south of Stewart Island. The islands have a total area of 113.31 km2 (43.75 sq mi), consisting of one big island, Campbell Island, and several small islets, notably Dent Island, Isle de Jeanette Marie, Folly Island, Jacquemart Island, and Monowai Island. Ecologically, they are part of the Antipodes Subantarctic Islands tundra ecoregion. The islands are one of five subantarctic island groups collectively designated as a World Heritage Site by UNESCO.

<span class="mw-page-title-main">Solander Islands</span> Three islets off the South Island of New Zealand

The Solander Islands / Hautere are three uninhabited volcanic islets toward the western end of the Foveaux Strait just beyond New Zealand's South Island. The Māori name Hautere translates into English as "flying wind". The islands lie 38 km (24 mi) south of Prices Point, near where Lake Hakapoua drains through Big River to the ocean due west of Te Waewae Bay, and 64 km (40 mi) northwest of the Putatara (Rugged) Point in the northwest of Stewart Island / Rakiura, or 56 km (35 mi) from Codfish Island / Whenua Hou. The islands measure 1.2 km2 (0.46 sq mi). Administratively, the islands form part of Southland District, making them the only uninhabited outlying island group of New Zealand to be part of a local authority.

Cuvier Island is a small uninhabited island off the east coast of the North Island of New Zealand. It lies on the seaward end of the Colville Channel, 15 km (9.3 mi) north of the Mercury Islands and approximately 23 km (14 mi) south-east of Great Barrier Island. The 195 ha island is a wildlife sanctuary, managed by the Department of Conservation and is the subject of an ongoing island restoration project to eliminate non-native mammals and restore the original ecosystem. It is also the location of the Cuvier Island Lighthouse which was constructed in 1889 and the wreck of the old HMNZS Philomel which was scuttled near the island on 6 August 1949 after decommissioning and being stripped of useful equipment.

<span class="mw-page-title-main">Zealandia</span> Mostly submerged mass of continental crust containing New Zealand and New Caledonia

Zealandia, also known as Te Riu-a-Māui (Māori) or Tasmantis, is an almost entirely submerged mass of continental crust in Oceania that subsided after breaking away from Gondwanaland 83–79 million years ago. It has been described variously as a submerged continent, continental fragment, and microcontinent. The name and concept for Zealandia was proposed by Bruce Luyendyk in 1995, and satellite imagery shows it to be almost the size of Australia. A 2021 study suggests Zealandia is 1 billion years old, about twice as old as geologists previously thought.

<span class="mw-page-title-main">Blumine Island</span>

Blumine Island / Ōruawairua is an island in the outer reaches of Queen Charlotte Sound / Tōtaranui, in the Marlborough Sounds at the northern end of New Zealand's South Island.

Kapiti Marine Reserve is a protected area on two sides of Kapiti Island, off the southern west coast of the North Island of New Zealand. It was created in 1992.

<span class="mw-page-title-main">Motu Manawa (Pollen Island) Marine Reserve</span>

Motu Manawa-Pollen Island Marine Reserve is a 501 hectares (1.93 sq mi) protected area in the Waitemata Harbour in Auckland, New Zealand, established in 1996. It includes the entire area between Rosebank Peninsula and Waterview, and surrounds Motumānawa / Pollen Island and Traherne Island. Its northeastern boundary runs roughly parallel to Rosebank Peninsula, from the mouth of the Oakley Creek estuary. Its northernmost boundary is north of Pollen Island, at the same latitude as the tip of Point Chevalier. Its westernmost point is in the mouth of the Whau River, between the tip of Rosebank Peninsula and Te Atatū. It is bisected by the Northwestern Motorway.

The Whangarei Harbour Marine Reserve is a protected area in the North Island of New Zealand. It was established in 2006 and measures 236.5 ha over two sites. The students and faculty of the nearby Kamo High School played an important role in establishing this reserve.

<span class="mw-page-title-main">Chetwode Islands</span>

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References

  1. Daly, Michael (17 February 2017). "New Zealand actually sits on a continent called Zealandia, it's just that most of it is under water". Stuff.co. Wellington, New Zealand. Retrieved 18 March 2022.
  2. Mortimer, Nick; Campbell, Hamish J.; Tulloch, Andy J.; King, Peter R.; Stagpoole, Vaughan M.; Wood, Ray A.; Rattenbury, Mark S.; Sutherland, Rupert; Adams, Chris J.; Collot, Julien; Seton, Maria (March–April 2017). "Zealandia: Earth's Hidden Continent". GSA Today. 27 (3): 27–35. doi:10.1130/GSATG321A.1 . Retrieved 18 March 2022. Several elevated bathymetric features north of Zealandia are possible candidates for Zealandia prolongations or separate microcontinents (Fig. 2). These include the Three Kings, Lau-Colville, and Tonga-Kermadec ridges and Fiji, which are known Cenozoic volcanic arcs (Graham, 2015), and the Mellish Rise and Louisiade and West Torres plateaus. However, no continental basement rocks have yet been sampled from any of these features, so their continental nature remains unproven.
  3. "New Zealand Sub-Antarctic Islands". UNESCO World Heritage Centre. Retrieved 8 November 2022.
  4. "Data Table – Protected Areas – LINZ Data Service (recorded area 2100 ha)". Land Information New Zealand. Retrieved 27 August 2019.
  5. "Data Table – Protected Areas – LINZ Data Service (recorded area 62564 ha)". Land Information New Zealand. Retrieved 27 August 2019.
  6. "Data Table – Protected Areas – LINZ Data Service (recorded area 135 ha)". Land Information New Zealand. Retrieved 27 August 2019.
  7. "Data Table – Protected Areas – LINZ Data Service (recorded area 11331 ha)". Land Information New Zealand. Retrieved 27 August 2019.
  8. "Data Table – Protected Areas – LINZ Data Service (recorded area 11331 ha)". Land Information New Zealand. Retrieved 27 August 2019.
  9. "Population estimate tables - NZ.Stat". Statistics New Zealand . Retrieved 25 October 2022.
  10. "Data Table – Protected Areas – LINZ Data Service (recorded area 3359.9864 ha)". Land Information New Zealand . Retrieved 27 August 2019.
  11. "Data Table – Protected Areas – LINZ Data Service (recorded area 684.7281 ha)". Land Information New Zealand. Retrieved 27 August 2019.
  12. "Data Table – Protected Areas – LINZ Data Service (recorded area 120 ha)". Land Information New Zealand. Retrieved 27 August 2019.
  13. "Data Table – Protected Areas – LINZ Data Service (recorded area 350 ha)". Land Information New Zealand. Retrieved 27 August 2019.