Kermadec Islands

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map of the Kermadec Islands
Raoul Island from space

The Kermadec Islands /kərˈmædɛk/ 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, 33 km2 (12.7 sq mi) in total area and nowadays uninhabited, except for the permanently manned Raoul Island Station, the northernmost outpost of New Zealand.

History[edit]

Polynesian people settled the Kermadec Islands in around the 14th century (and perhaps previously in the 10th century), but the first Europeans to reach the area—the Lady Penrhyn in May 1788—found no inhabitants. The islands were named for the Breton captain Jean-Michel Huon de Kermadec, who visited the islands as part of the d'Entrecasteaux expedition in the 1790s. European settlers, initially the Bell family, lived on the islands from the early nineteenth century until 1937, as did whalers. One of the Bell daughters, Elsie K. Morton, recounted the family's experience there in her memoir, Crusoes of Sunday Island.

Raoul Island Station[edit]

The Station comprises a government meteorological and radio station, and a hostel for Department of Conservation officers and volunteers, that has been maintained since 1937. It lies on the northern terraces of Raoul Island, at an elevation of about 50 m (160 ft), above the cliffs of Fleetwood Bluff. It is the northernmost inhabited outpost of New Zealand.

Geography[edit]

The islands lie within 29° to 31.5° south latitude and 178° to 179° west longitude, 800–1,000 km (500–620 mi) northeast of New Zealand's North Island, and a similar distance southwest of Tonga. The centre of the Kermadec Islands group is located at approximately 29°16′37″S 177°55′24″W / 29.27694°S 177.92333°W / -29.27694; -177.92333Coordinates: 29°16′37″S 177°55′24″W / 29.27694°S 177.92333°W / -29.27694; -177.92333. The total area of the islands is 33.08 km2 (12.77 sq mi).

Climate[edit]

The climate of the islands is subtropical, with a mean monthly temperature of 22.4 °C (72.3 °F) in February and 16.0 °C (60.8 °F) in August. Rainfall is approximately 1,500 mm (60 in) annually, with lower rainfall from October through January.

The islands[edit]

The group includes four main islands (three of them might be considered island groups, because the respective main islands have smaller islands close by) and some isolated rocks, which are, from north to south:

Seamounts north and south of the Kermadec Islands are an extension of the ridge running from Tonga to New Zealand (see Geology).

  • Star of Bengal Bank, 103 km (64 mi) south-southwest of L'Esperance Rock, with a least depth of 48 metres (157 ft)

Geology[edit]

Bathymetry of the Kermadec volcanic island arc and surrounding areas
The Kermadec scalyfin - part of the rich marine biota of the Kermadecs

The islands are a volcanic island arc, formed at the convergent boundary where the Pacific Plate subducts under the Indo-Australian Plate. The subducting Pacific Plate created the Kermadec Trench, an 8 km deep submarine trench, to the east of the islands. The islands lie along the undersea Kermadec Ridge, which runs southwest from the islands towards the North Island of New Zealand and northeast towards Tonga (Kermadec-Tonga Arc).

The four main islands are the peaks of volcanoes that rise high enough from the seabed to project above sea level. There are several other volcanoes in the chain that do not reach sea level, but form seamounts with between 65 and 1500 m of water above their peaks. Monowai Seamount, with a depth of 120 m over its peak, is midway between Raoul Island and Tonga. 100 km south of L'Esperance Rock is the little-explored Star of Bengal Bank, probably with submarine volcanoes.

Further south are the South Kermadec Ridge Seamounts, the southernmost of which, Rumble IV Seamount, is just 150 km North of the North Island of New Zealand. The ridge eventually connects to White Island in New Zealand's Bay of Plenty, at the northern end of the Taupo Volcanic Zone. The islands experience many earthquakes from plate movement and volcanism.

Raoul and Curtis are both active volcanoes. The volcanoes on the other islands are currently inactive, and the smaller islands are the eroded remnants of extinct volcanoes.

On 6 July 2011 (2pm CDT, GMT-5), a large earthquake provisionally measuring 7.6 on the Richter Scale was reported, centered near the Kermadec Islands, 211 km east of Raoul Island.[2]

On 20 October 2011 a 7.3 earthquake on the Richter Scale was reported, centered near the Kermadec Islands, 112 miles east of Raoul Island. No immediate tsunami threat was reported.[3][4]

On 21 October 2011 a 7.4 earthquake on the Richter Scale was reported near the Kermadec Islands, 169 km (105 miles) E of Raoul Island at 17:57:16 UTC at epicenter.[5]

From 18 to 21 July 2012, Havre Seamount (near Havre Rock) erupted, breaching the ocean surface from a depth of more than 1100 m and producing a large raft of pumice floating northwest of the volcano. The eruption was not directly observed, but it was located using earthquake and remote sensing data after the pumice raft was spotted by aircraft and encountered by the HMNZS Canterbury.[6]

Environment[edit]

Flora[edit]

The islands are recognized by ecologists as a distinct ecoregion, the Kermadec Islands subtropical moist forests. They are a tropical and subtropical moist broadleaf forests ecoregion, part of the Oceania ecozone. The forests are dominated by the red-flowering Kermadec Pōhutukawa, related to the Pōhutukawa of New Zealand. The islands are home to 113 native species of vascular plants, of which 23 are endemic, along with mosses (52 native species), lichens and fungi (89 native species). Most of the plant species are derived from New Zealand, with others from the tropical Pacific. 152 non-native species of plants introduced by humans have become established on the islands.

Dense subtropical forests cover most of Raoul, and formerly covered Macauley. Metrosideros kermadecensis is the dominant forest tree, forming a 10 – 15 meter high canopy. A native Nikau Palm (Rhopalostylis baueri) is another important canopy tree. The forests had a rich understory of smaller trees, shrubs, ferns, and herbs, including Myrsine kermadecensis; Lobelia anceps, Poa polyphylla, Coprosma acutifolia, and Coriaria arborea. Two endemic tree ferns, Cyathea milnei and the rare and endangered Cyathea kermadecensis, are also found in the forests.

Areas near the seashore and exposed to salt spray are covered by a distinct community of shrubs and ferns, notably Myoporum obscurum, Coprosma petiolata, Asplenium obtusatum, Cyperus ustulatus, Disphyma australe, and Ficinia nodosa.

Fauna[edit]

The islands have no native land mammals. An endemic bird subspecies is the Kermadec Red-crowned Parakeet. The group has been identified as an Important Bird Area (IBA) by BirdLife International because of its significance as a breeding site for several species of seabirds, including White-necked and Black-winged Petrels, Wedge-tailed and Little Shearwaters, Sooty Terns and Blue Noddies.[7]

Conservation[edit]

The introduction of cats, rats, and goats devastated the forests and seabirds.[8][9] Overgrazing by goats eliminated the forests of Macauley Island, leaving open grasslands, and altered the understory of Raoul Island. Predation by rats and cats reduced the seabird colonies on the main islands from millions of birds to tens of thousands. The New Zealand government has been working for the last few decades to restore the islands. New Zealand declared the islands a nature reserve in 1937, and the sea around them a marine reserve in 1990. Goats were removed from Macauley in 1970 and from Raoul in 1984, and the forests have begun to recover. The islands are still known for their bird life, and seabird colonies presently inhabit offshore islets, which are safe from introduced rats and cats. Efforts are currently underway to remove the rats and cats from the islands, as well as some of the invasive exotic plants.

Visits to the islands are restricted by the Department of Conservation. The Department allows visits to Raoul by volunteers assisting in environmental restoration or monitoring projects, and other visitors engaged in nature study. Visits to the other islands are generally restricted to those engaged in scientific study of the islands.

References[edit]

  1. ^ Chart NZ 2225, Hydrographic Office, Royal New Zealand Navy, 1994. Accessed 2007-05-07.
  2. ^ http://ptwc.weather.gov/ptwc/text.php?id=hawaii.2011.07.06.191349
  3. ^ http://www.newsroomamerica.com/story/184229/7.3_earthquake_off_coast_of_new_zealand.html
  4. ^ http://www.staradvertiser.com/news/breaking/132331228.html
  5. ^ http://earthquake.usgs.gov/earthquakes/recenteqsww/Quakes/usb0006b6p.php
  6. ^ "NASA Satellites Pinpoint Volcanic Eruption". NASA Earth Observatory. NASA. 14 August 2012. Retrieved 14 August 2012. 
  7. ^ BirdLife International. (2012). Important Bird Areas factsheet: Kermadec Islands. Downloaded from http://www.birdlife.org on 2012-02-03.
  8. ^ Courchamp, F.; Chapuis, J. L.; Pascal, M. (2003). "Mammal invaders on islands: Impact, control and control impact". Biological Reviews 78 (3): 347–383. doi:10.1017/S1464793102006061. PMID 14558589.  edit
  9. ^ Towns, D. R.; Broome, K. G. (2003). "From small Maria to massive Campbell: Forty years of rat eradications from New Zealand islands". New Zealand Journal of Zoology 30 (4): 377. doi:10.1080/03014223.2003.9518348.  edit

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