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Norfolk Island

Norfolk Island

Norfolk Island is a small inhabited island in the Pacific Ocean located between Australia, New Zealand and New Caledonia, and along with two neighbouring islands forms one of Australia's external territories. The Norfolk Island pine, a symbol of the island pictured in its flag, is a very striking evergreen tree endemic to the island and is quite popular in Australia, where two related species grow.

History

Discovery and settlement decision

Norfolk Island was first settled by East Polynesian seafarers, probably from the Kermadec Islands north of New Zealand. They arrived in the 14th or 15th century, and survived for several generations before disappearing. Their main village site has been excavated at Emily Bay, and they also left behind stone tools, rats, and banana trees as evidence of their sojourn. The final fate of these early settlers remains a mystery. The first European known to have sighted the island was Captain James Cook, in 1774, on his second voyage to the South Pacific on HMS Resolution. He named it after the wife of the premier peer of Britain, Edward Howard, 9th Duke of Norfolk (1685-1777). Cook went ashore on Tuesday 11 October 1774, and was impressed with the tall straight trees and flax-like plants. He took samples back to England and reported on their potential uses for the Royal Navy. At the time, Britain was heavily dependent on flax (for sails) and hemp (for ropes) from the shores of the Baltic Sea ports. Any threat to their supply endangered Britain's sea power. She also relied on timbers from New England for mainmasts, and these were not supplied after the American War of Independence. The alternative source of Norfolk Island for these supplies is argued by some historians, notably Geoffrey Blainey in The Tyranny of Distance, as being a major reason for the founding of the convict settlement of New South Wales by the First Fleet in 1788.

First penal settlement

Before the First Fleet sailed to found a convict settlement in New South Wales, Governor Arthur Phillip's final instructions, received less than three weeks before sailing, included the requirement to colonize Norfolk Island to prevent it falling into the hands of France, whose naval leaders were also showing interest in the Pacific. When the fleet arrived at Port Jackson in January 1788, Phillip ordered Lieutenant Philip Gidley King to lead a party of fifteen convicts and seven free men to take control of the island and prepare for its commercial development. They arrived on 6 March 1788. It was soon found that the flax was difficult to prepare for manufacturing and no one had the necessary skills. An attempt was made to bring two Maori men to teach the skills of dressing and weaving flax, but this failed when it was discovered that weaving was women's work and the two men had little knowledge of it. The pine timber was found to be not resilient enough for masts and this industry was also abandoned. More convicts were sent, and the island was seen as a farm, supplying Sydney with grain and vegetables during its early years of near-starvation. However, crops often failed due to the salty wind, rats and caterpillars. The lack of a natural safe harbour hindered communication and the transport of supplies and produce. Manning Clark observed that "at first the convicts behaved well, but as more arrived from Sydney Cove, they renewed their wicked practices". These included an attempted overthrow of King in January 1789 by convicts described by Margaret Hazzard as "incorrigible rogues who took his 'goodwill' for weakness". While some convicts responded well to the opportunities offered to become respectable, most remained "idle and miserable wretches" according to Clark, despite the climate and their isolation from previous haunts of crime. The impending starvation at Sydney led to a great transplantation of convicts and marines to Norfolk Island in March 1790 on HMS Sirius. This attempt to relieve the pressure on Sydney turned to disaster when Sirius was wrecked and, although there was no loss of life, some stores were destroyed, and the ship's crew was marooned for ten months. This news was met in Sydney with “unspeakable consternation.” Norfolk Island was now further cut off from Sydney which, with the arrival of the Second Fleet with its shameful cargo of sick and abused convicts, had more pressing problems to contend with. In spite of this the settlement grew slowly as more convicts were sent from Sydney. Relationships were established and children were born here. Many convicts chose to remain as settlers on the expiry of their sentence, and the population grew to over 1000 by 1792. Norfolk Island was governed by a succession of short-term commandants for the next 11 years, starting with King's replacement, Robert Ross 1789-1790. When Joseph Foveaux arrived as Lieutenant Governor in 1800, he found the settlement in a most disorderly state of things, little maintenance having been carried out in the previous four years, and he set about building it up, particularly through public works and attempts to improve education. As early as 1794 King suggested its closure as a penal settlement as it was too remote and difficult for shipping, and too costly to maintain. By 1803 the Secretary of State, Lord Hobart, called for the removal of part of the Norfolk Island military establishment, settlers and convicts to Van Diemen's Land, due to its great expense and the difficulties of communication between Norfolk Island and Sydney. This was achieved more slowly than anticipated, due to reluctance of settlers to uproot themselves from the land they had struggled to tame, and compensation claims for loss of stock. It was also delayed by King's insistence on its value for providing refreshment to the whalers. The first group of 159 left in February 1805 and comprised mainly convicts and their families and military personnel, only four settlers departing. Between November 1807 and September 1808, five groups of 554 people departed. Only about 200 remained, forming a small settlement until the remnants were removed in 1813. A small party remained to slaughter stock and destroy all buildings so that there would be no inducement for anyone, especially from another European power, to visit that place. Norfolk Island lay abandoned, to return to its primeval state, leaving behind only the physical and mental scars of a quarter of a century of human penal occupation. Between 15 February 1814 and 6 June 1825 the island lay abandoned. Lieutenant governors of the first settlement:
- 6 March 1788–24 March 1790: Lieutenant Philip Gidley King (1758–1808)
- 24 March 1790–Nov 1791: Major Robert Ross (c.1740–1794)
- 4 November 1791–Oct 1796: Lieutenant Philip Gidley King
- October 1796–Nov 1799: Captain John Townson (1760–1835)
- November 1799–Jul 1800: Captain Thomas Rowley (c.1748–1806)
- 26 June 1800–9 September 1804: Major Joseph Foveaux (1765–1846)
- 9 September 1804–January 1810: Lieutenant John Piper (1773–1851)
- January 1810–15 February 1813: Lieutenant Thomas Crane (caretaker)
- 15 February 1813–15 February 1814: Superintendent William Hutchinson

Second penal settlement

In 1824 the British government instructed the Governor of New South Wales Thomas Brisbane to occupy Norfolk Island as a place to send “the worst description of convicts”. Its remoteness, seen previously as a disadvantage, was now viewed as an asset for the detention of the “twice-convicted” men, those who had committed further crimes since arriving in New South Wales. Brisbane assured his masters that “the felon who is sent there is forever excluded from all hope of return.” He saw Norfolk Island as “the ne plus ultra of Convict degradation”. His successor, Governor Ralph Darling, was even more severe than Brisbane, wishing that “every man should be worked in irons that the example may deter others from the commission of crime” and “to hold out [Norfolk Island] as a place of the extremest punishment short of death”. Governor George Arthur, in Van Diemen's Land, likewise believed that “when prisoners are sent to Norfolk Island, they should on no account be permitted to return. Transportation thither should be considered as the ultimate limit and a punishment short only of death.” Clearly, reformation of the convicts, a supposed goal of the system of transportation as much as punishment, was not seen as an objective of the Norfolk Island penal settlement. The evidence that has passed down through the years points to the creation of a "Hell in Paradise". The most widespread and popular notion of the harshness of the penal settlements, including Norfolk Island, has come from the novel For the Term of His Natural Life by Marcus Clarke, which appears to be based on the writings and recollections of witnesses and from the fictional writings of Price Warung. Following a convict mutiny in 1834, Father William Ullathorne, Vicar general of Sydney, visited Norfolk Island to comfort the mutineers due for execution. He found it “the most heartrending scene that I ever witnessed.” Having the duty of informing the prisoners as to who was reprieved and who was to die, he was shocked to record as “a literal fact that each man who heard his reprieve wept bitterly, and that each man who heard of his condemnation to death went down on his knees with dry eyes, and thanked God.” The 1846 report of magistrate Robert Pringle Stuart exposed the scarcity and poor quality of food, inadequacy of housing, horrors of torture and incessant flogging, insubordination of convicts, and corruption of overseers. Bishop Robert Willson visited Norfolk Island from Van Diemen's Land on three occasions. Following his first visit in 1846 he reported to the House of Lords who, for the first time, came to realise the enormity of atrocities perpetrated under the British flag and attempted to remedy the evils. Willson returned in 1849 and found that many of the reforms had been implemented. However, rumours of resumed atrocities brought him back in 1852, and this visit resulted in a damning report, listing atrocities and blaming the system, which invested one man at this remote place with absolute power over so many people. Only a handful of convicts left any written record and their descriptions (as quoted by Hazzard and Hughes) of living and working conditions, food and housing, and, in particular, the punishments given for seemingly trivial offences, are unremittingly horrifying, describing a settlement devoid of all human decency, under the iron rule of the tyrannical autocratic commandants. The actions of some of the commandants, such as Morisset and particularly Price appear to be excessively harsh. All but one were military officers, brought up in a system where discipline was inhumanely severe throughout the period of transportation. In addition, the commandants relied on a large number of military guards, civil overseers, ex-convict constables, and convict informers to provide them with intelligence and carry out their orders. Of the Commandants, only Alexander Maconochie appeared to realise that brutality would breed defiance, as demonstrated by the mutinies of 1826, 1834 and 1846, and he attempted to apply his theories of penal reform, providing incentives as well as punishment. His methods were criticised as being too lenient and he was replaced, a move that returned the settlement to its harsh rule. The second penal settlement began to be wound down by the British Government after 1847 and the last convicts were removed to Tasmania in May 1855. It was abandoned because transportation to Van Diemen's Land had ceased in 1853 and was replaced by penal servitude in Britain. Commandants of the second settlement:
- 6 June 1825–March 1826: Captain Richard Turton
- March 1826–August 1827: Captain Vance Young Donaldson (1791–?)
- August 1827–November 1828: Captain Thomas Edward Wright
- November 1828–February 1829: Captain Robert Hunt
- February 1829–29 June 1829: Captain Joseph Wakefield
- 29 June 1829–1834: Lieutenant-Colonel James Thomas Morisset (1782–1852)
- 1834: Captain Foster Fyans (1790–1870) (Acting)
- 1834–April 1839: Major Joseph Anderson (1790–1877)
- April - July 1839: Major Thomas Bunbury (b. c1791)
- July 1839 - March 1840: Major Thomas Ryan (b.c1790) (Acting)
- 17 March 1840–1844: Captain Alexander Maconochie (1787–1860)
- 8 February 1844–5 August 1846: Major Joseph Childs
- 6 August 1846–18 January 1853: John Giles Price (1808–1857)
- January 1853–September 1853: Captain Rupert Deering
- September 1853–5 May 1855: Captain H. Day
- 5 May 1855–8 June 1856: T.S. Stewart (Caretaker)

References to the penal settlements of Norfolk Island


- Clark, Manning, A History of Australia, Vols. I–III, Melbourne, MUP, 1962, 1968, 1973.
- Hazzard, Margaret, Punishment Short of Death: a history of the penal settlement at Norfolk Island, Melbourne, Hyland, 1984. (ISBN 0-908090-64-1)
- Hughes, Robert, The Fatal Shore, London, Pan, 1988. (ISBN 0-330-29892-5)
- Wright, R., The Forgotten Generation of Norfolk Island and Van Diemen's Land, Sydney, Library of Australian History, 1986.
- Clarke, Marcus, For the Term of his Natural Life (novel)

Third settlement: Pitcairn Islanders

On 6 June 1856, another group of exiles arrived at Norfolk Island. These were the descendants of Tahitians and the HMAV Bounty mutineers, resettled from the Pitcairn Islands which had become too small for their growing population. The British government had permitted the transfer of the Pitcairners to Norfolk, which was thus established as a colony separate from New South Wales but under the administration of that colony's governor. The Pitcairn people occupied many of the buildings remaining from the penal settlements, and gradually established their traditional farming and whaling industries on the island. Although some families decided to return to Pitcairn in 1858 and 1863, the island's population continued to slowly grow as the island accepted settlers, often arriving with whaling fleets. In 1867, the headquarters of the Melanesian Mission of the Church of England were established on the island, and in 1882 a church of St. Barnabas was erected to the memory of the Mission's head Bishop John Coleridge Patteson, with windows designed by Burne-Jones and executed by William Morris. In 1920 the Mission was relocated from the island to the Solomon Islands to be closer to its target population. After the creation of the Commonwealth of Australia in 1901, Norfolk Island was placed under the authority of the new Commonwealth government to be administered as an external territory. During World War II, the island was used as a key airbase and refuelling location between Australia and New Zealand. In 1979, Norfolk was granted self-government by Australia, under which the island elects a government which runs most of the island's affairs.

Geography

Norfolk Island is located in the South Pacific Ocean, east of Australia. Norfolk Island is the main island of the island group the territory encompasses amd is located at . It has an area of 34.6 km², with no large-scale internal bodies of water but 32 km of coastline. The island's highest point is Mt. Bates (319 m above sea level), located in the northwest quadrant of the island. The majority of the terrain is suitable for farming and other agricultural uses. Philip Island, the second largest island of the territory, is located at , several kilometres south of the main island. The coastline of Norfolk Island consists, to varying degrees, of cliff faces. A downward slope exists towards Sydney Bay and Emily Bay, the site of the original colonial settlement of Kingston. There are no safe harbour facilities on Norfolk Island, with loading jetties existing at Kingston and Cascade Bay. All goods not domestically produced are brought in by ship, usually to Cascade Bay. Emily Bay, protected from the Pacific Ocean by a small coral reef, is the only safe area for recreational swimming, although surfing is sometimes done at Ball Bay. Norfolk Island claims an exclusive fishing zone extending 200 nautical miles (370 km) and territorial sea claims to three nautical miles (6 km) from the island. The climate is subtropical and mild, with little seasonal differentiation. The island is a volcanic formation with mostly rolling plains. volcanic The only major natural resource of Norfolk Island is fish. There are no major arable lands or permanent farmlands, though about 25% of the island is a permanent pasture. There is no irrigated land. The area surrounding the highest point of the island, Mt. Bates, is preserved as the Norfolk Island National Park. The park, covering around 10% of the land of the island, contains remnants of the forests which originally covered the island, including stands of subtropical rainforest. The park also includes the two smaller islands to the south of Norfolk Island, Nepean Island and Philip Island. The vegetation of Philip Island was devastated due to the introduction during the penal era of pest animals such as pigs and rabbits, giving it a red-brown colour as viewed from Norfolk; however, pest control and remediation work by park staff has recently brought some improvement to the Philip Island environment. The major settlement on the Island is Burnt Pine, located predominantly along Taylor's Road, where the shopping centre, post office, liquor store, telephone exchange and community hall are located. Settlement also exists over much of the island, consisting largely of widely-separated homesteads. Government House, the official residence of the Administrator, is located on Quality Row in what was the penal settlement of Kingston. Other government buildings, including the court, Legislative Assembly and Administration, are also located there. Kingston's role is largely a ceremonial one, however, with most of the economic impetus coming from Burnt Pine.

Politics

Norfolk Island is the only non-mainland Australian territory to have achieved self-governance. The Norfolk Island Act, passed by the Parliament of Australia in 1979, is the Act under which the island is governed. The Australian Government maintains authority on the island through an Administrator (currently Grant Tambling) that is appointed by the Governor-General of Australia. A Legislative Assembly is elected by popular vote for a term of not more than three years, although legislation passed by the Australian Parliament can extend its laws to the territory at will. The Assembly consists of nine seats, with electors casting nine equal votes, of which no more than four can be given to any individual candidate. It is a method of voting called a "weighted first past the post system". Four of the members of the Assembly form the Executive Council, which devises policy and acts as an advisory body to the Administrator. The current Chief Minister of Norfolk Island is Geoffrey Robert Gardner. All seats are held by independent candidates as Norfolk Island does not have political parties. The island's official capital is Kingston; however, Kingston functions mainly as a government centre and not as a settlement. The most important national holiday is Bounty Day, celebrated on June 8, in memory of the arrival of the Pitcairn Islanders in 1856. Local ordinances and acts apply on the island, where most laws are based on the Australian legal system. Australian common law applies when not covered by either Australian or Norfolk Island law. Suffrage is universal at age eighteen. As a territory of Australia, Norfolk Island does not have diplomatic representation abroad, or within the territory, and is also not a participant in any international organizations, other than sporting organizations. The flag is three vertical bands of green (hoist side), white, and green with a large green Norfolk Island pine tree centered in the slightly wider white band.

Constitutional Status

Controversy exists as to the exact status of Norfolk Island. Despite the island's status as a self-governing territory of Australia, some Islanders claim that it was actually granted independence at the time Queen Victoria granted permission to Pitcairn Islanders to re-settle on the island. Residents of Norfolk Island do not pay Australian taxes (creating a tax haven for locals and visitor alike) and the island is subject to separate immigration controls from the remainder of the nation. These views have been repeatedly rejected by the Australian parliament's joint committee on territories, most recently in 2004, and were also rejected by the High Court of Australia in Berwick Limited v R R Gray Deputy Commissioner of Taxation. The Australian parliament has plenary power to make laws for the island, including the power to override any laws made by the Norfolk Island Legislative Assemby. Australian citizens and residents from other parts of the nation do not have automatic right of residence on the island. Australian citizens must carry either a passport or a Document of Identity to travel to Norfolk Island. Citizens of all other nations must carry a passport to travel to Norfolk Island even if arriving from other parts of Australia. Non-Australians without a multiple entry visa to Australia (or authority to enter without a visa) will be refused entry if they try to return to mainland Australia from Norfolk Island. Residency on Norfolk Island is normally granted in a manner similar to most sovereign nations today – sponsorship must be made by an existing resident of Norfolk Island or a business operating on the island. Temporary residency may also be granted to skilled workers necessary for the island's services – examples are medical, government and teaching staff. Permanent residents of Norfolk Island may apply for Australian citizenship after meeting normal residence requirements. Children born on Norfolk Island are Australian citizens if at least one parent is an Australian citizen or permanent resident at the time of birth (or the person was born before 20 August 1986). See Australian nationality law Medicare does not cover Norfolk Island. All visitors to Norfolk Island, including Australians, are recommended to purchase travel insurance. Serious medical conditions are not treated on the island; rather, the patient is flown back to mainland Australia, if necessary by the Royal Australian Air Force.

Crime

Though usually peaceful, Norfolk Island has been the site of two murders in the 2000s so far. The Deputy Chief Minister of the island, Ivens Buffett, was found shot dead in 2004, two years after the body of Janelle Patton was found. The murders are not related. Other than these two events, crime is low on the island.

Economy

Tourism, the primary economic activity, has steadily increased over the years. As Norfolk Island prohibits the importation of fresh fruit and vegetables, a vast majority of produce is grown locally. Beef is both produced locally and imported. The island uses the Australian dollar as its currency.

Demographics

currency The population of Norfolk Island was estimated in July 2003 to be 1,853, with an annual population growth rate of 0.01%. In July 2003, 20.2% of the population were 14 years and under, 63.9% were 15 to 64 years and 15.9% were 65 years and over. Emigration is growing as many Islanders take advantage of the close ties between Norfolk and Australia and New Zealand. The sole school on the island provides education to Australian Year 12; therefore, any student seeking to complete tertiary study must travel overseas. Additionally, the small economy of the island causes many skilled workers to emigrate as well. Literacy is not recorded officially, but it can be assumed to be roughly at a par with Australia's literacy rate of 100%. Most Islanders are of Caucasian ancestry, being descendants of the Bounty mutineers as well as more recent arrivals from Australia and New Zealand. The Bounty descendants have some Polynesian stock; however, only a minority consider themselves ethnically Polynesian. The majority of Islanders are Protestant Christians. In 1996, 37.4% identified as Anglican, 14.5% as Uniting Church, 11.5% as Roman Catholic and 3.1% as Seventh-day Adventist. Islanders speak both English and a creole language known as Norfuk, a blend of 1700s-English and Tahitian. The Norfuk language is decreasing in popularity as more tourists travel to the island and more young people leave for work and study reasons; however, there are efforts to keep it alive via dictionaries and the renaming of some tourist attractions to their Norfuk equivalents. In April 2005, it was declared a co-official language of the island.

Transport and communications

There are no railways, waterways, ports or harbours on the island. Loading jetties are located at Kingston and Cascade, but ships cannot get close to either of them. When a supply ship arrives, it is emptied by whaleboats towed by launches, five tonnes at a time. Which jetty is used depends on the prevailing weather on the day. The jetty on the leeward side of the island is used. If the wind changes significantly during unloading/loading, the ship will move round to the other side. Visitors often gather to watch the activity when a supply ship arrives. There is one airport, Norfolk Island Airport. There are 80 km of roads on the island. As of 2004, 2532 telephone main lines are in use, a mix of analog (2500) and digital (32) circuits. Norfolk Island's country code is 672. Undersea coaxial cables link the island with Australia, New Zealand and Canada. Satellite service is planned. There is one local TV programming station and two repeaters that bring in Australian programs by satellite. The Internet country code top-level domain (ccTLD) is .nf.

Culture

One of the island's residents is the novelist Colleen McCullough, whose works include The Thorn Birds and the Masters of Rome series as well as Morgan's Run, set, in large part, on Norfolk Island. Helen Reddy also moved to the island for a period but was denied a long term entry permit and has since moved on.

External links


- [http://www.norfolk.gov.nf/ Norfolk Island], official homepage
- [http://www.customs.gov.nf/ Norfolk Island Customs]
- [http://www.norfolkisland.nf/ Norfolk Island Tourism]
- [http://www.school.edu.nf/ Norfolk Island Central School]
- [http://www.historyofnations.net/oceania/norfolkisland.html History of Norfolk Island]
- [http://www.world-atlas.net/Norfolk_Island Norfolk Island History, geographic and economic information]
- [http://67.1911encyclopedia.org/N/NO/NORFOLK_ISLAND.htm Norfolk Island]
- [http://nlkisland.blogspot.com Norfolk Island Pictures]
- [http://www.worldwildlife.org/wildworld/profiles/terrestrial/aa/aa0114_full.html Norfolk Island subtropical forests (WWF)]
- [http://www.dotars.gov.au/terr/norfolk/government.aspx Australian Department of Transport and Regional Services]
- [http://www.austlii.edu.au/au/cases/cth/high_ct/133clr603.html Berwick Limited v R R Gray Deputy Commissioner of Taxation] Category:Australian states and territories Category:Ecoregions Category:Islands Category:Islands of Australia
- zh-min-nan:Norfolk-tó ja:ノーフォーク島

Pacific Ocean

:For other meanings of Pacific, see Pacific (disambiguation). The Pacific Ocean (from the Latin name Mare Pacificum, "peaceful sea", bestowed upon it by the Portuguese explorer Ferdinand Magellan) is the world's largest body of water. It encompasses a third of the Earth's surface, having an area of 179.7 million km² (69.4 million sq miles). Extending approximately 15,500 km (9,600 miles) from the Bering Sea in the Arctic to the icy margins of Antarctica's Ross Sea in the south (although the Antarctic regions of the Pacific are sometimes described as part of the circumpolar Southern Ocean)the Pacific reaches its greatest east-west width at about 5°N latitude, where it stretches approximately 19,800 km (12,300 miles) from Indonesia to the coast of Colombia. The western limit of the ocean is often placed at the Strait of Malacca. The lowest point on earth—the Mariana Trench—lies some 10,911 m (35,797 ft) below sea level. The Pacific contains about 25,000 islands (more than the total number in the rest of the world's oceans combined), the majority of which are found south of the equator. (See: Pacific Islands.) Along the Pacific Ocean's irregular western margins lie many seas, the largest of which are the Celebes Sea, Coral Sea, East China Sea, Sea of Japan, South China Sea, Sulu Sea, Tasman Sea, and Yellow Sea. The Straits of Malacca joins the Pacific and the Indian Oceans on the west, and the Straits of Magellan links the Pacific with the Atlantic Ocean on the east. As the Pacific straddles the ±180° longitude where East becomes West, the Asian side of the ocean (where latitudes are E) is correctly referred to as East Pacific and the opposite side (eastwards) where latitudes are W is the West Pacific. To retain the popular "left is western" and "right is eastern" means of reference, the Western Pacific is thus the East Pacific and the Eastern Pacific the West Pacific. The International Date Line follows the ±180° longitude to the greater part of its North-South demarcation but veers far eastwards around Kiribati (Caroline Island, which, not coincidentally, was renamed Millennium Island) and westwards round the Aleutian Islands as can be seen on the map at International Date Line. For most of Ferdinand Magellan's voyage from the Straits of Magellan to the Philippines, the Portuguese explorer indeed found the ocean peaceful. However, the Pacific is not always peaceful. Many typhoons and hurricanes batter the islands of the Pacific and the lands around the Pacific rim are full of volcanoes and often rocked by earthquakes. Tsunamis, caused by underwater earthquakes, have devastated many islands and wiped out whole towns. Tsunami

Ocean bottom

The ocean floor of the central Pacific basin is relatively uniform, an abyssal plain with a mean depth of about 4270 m (14,000 ft). The major irregularities in the basin are the extremely steep-sided, flat-topped submarine peaks known as seamounts. The western part of the floor consists of mountain arcs that rise above the sea as island groups, such as the Solomon Islands and New Zealand, and deep oceanic trenches, such as the Mariana Trench, the Philippine Trench, and the Tonga Trench. Most of the trenches lie adjacent to the outer margins of the wide western Pacific continental shelf. Along the eastern margin of the Pacific Basin is the East Pacific Rise, which is a part of the worldwide mid-oceanic ridge. About 3000 km (1800 miles) across, the rise stands about 3 km (2 miles) above the adjacent ocean floor. Because a relatively small land area drains into the Pacific, and because of the ocean's immense size, most sediments are authigenic or pelagic in origin. Authigenic sediments include montmorillonite and phillipsite. Pelagic sediments derived from seawater include pelagic red clays and the skeletal remains of sea life. Terrigenous sediments eroded from land masses are confined to narrow marginal bands close to land.

Elevation extremes


- lowest point: -10,924 m (-35,840 ft). at the bottom of the Mariana Trench
- highest point: 0 m (0 ft), sea level.

Water characteristics

Water temperatures in the Pacific vary from freezing in the poleward areas to about 29°C (84°F) near the equator. Salinity also varies latitudinally. Water near the equator is less salty than that found in the mid-latitudes because of abundant equatorial precipitation throughout the year. Poleward of the temperate latitudes salinity is also low, because little evaporation of seawater takes place in these frigid areas. The surface circulation of Pacific waters is generally clockwise in the Northern Hemisphere (the North Pacific Gyre) and anti-clockwise in the Southern Hemisphere. The North Equatorial Current, driven westward along latitude 15°N by the trade winds, turns north near the Philippines to become the warm Japan or Kuroshio Current. Turning eastward at about 45°N, the Kuroshio forks and some waters move northward as the Aleutian Current, while the rest turn southward to rejoin the North Equatorial Current. The Aleutian Current branches as it approaches North America and forms the base of an anti-clockwise circulation in the Bering Sea. Its southern arm becomes the chilled slow, south-flowing California Current. The South Equatorial Current, flowing west along the equator, swings southward east of New Guinea, turns east at about 50°S, and joins the main westerly circulation of the Southern Pacific, which includes the Earth-circling Antarctic Circumpolar Current. As it approaches the Chilean coast, the South Equatorial Current divides; one branch flows around Cape Horn and the other turns north to form the Peru or Humboldt Current.

Climate

Only the interiors of the large land masses of Australia, New Guinea, and New Zealand escape the pervasive climatic influence of the Pacific. Within the area of the Pacific, five distinctively different climatic regions exist: the mid-latitude westerlies, the trades, the monsoon region, the typhoon region, and the doldrums. Mid-latitude westerly air streams occur in both northerly and southerly latitudes, bringing marked seasonal differences in temperature. Closer to the equator, where most of the islands lie, steadily blowing trade winds allow for relatively constant temperatures throughout the year of 21-27°C (70-81°F). The monsoon region lies in the far western Pacific between Japan and Australia. Characteristic of this climatic region are winds that blow from the continental interior to the ocean in winter and in the opposite direction in summer. Consequently, a marked seasonality of cloudiness and rainfall occurs. Typhoons often cause extensive damage in the west and southwest Pacific. The greatest typhoon frequency exists within the triangle from southern Japan to the central Philippines to eastern Micronesia. Although more poorly defined than the other climatic regions, two major doldrum areas lie within the ocean, one located off the western shores of Central America and the other within the equatorial waters of the western Pacific. Both areas are noted for their high humidity, considerable cloudiness, light fluctuating winds, and frequent calms.

Geology

The Andesite Line is the most significant regional distinction in the Pacific. It separates the deeper, basic igneous rock of the Central Pacific Basin from the partially submerged continental areas of acidic igneous rock on its margins. The Andesite Line follows the western edge of the islands off California and passes south of the Aleutian arc, along the eastern edge of the Kamchatka Peninsula, the Kuril Islands, Japan, the Mariana Islands, the Solomon Islands, and New Zealand. The dissimilarity continues northeastward along the western edge of the Albatross Cordillera along South America to Mexico, returning then to the islands off California. Indonesia, the Philippines, Japan, New Guinea, and New Zealand—all eastward extensions of the continental blocks of Australia and Asia—lie outside the Andesite Line. Within the closed loop of the Andesite Line are most of the deep troughs, submerged volcanic mountains, and oceanic volcanic islands that characterize the Central Pacific Basin. It is here that basaltic lavas gently flow out of rifts to build huge dome-shaped volcanic mountains whose eroded summits form island arcs, chains, and clusters. Outside the Andesite Line, volcanism is of the explosive type, and the Pacific Ring of Fire is the world's foremost belt of explosive volcanism.

Landmasses

The largest landmass entirely within the Pacific Ocean is the island of New Guinea— the second largest in the world. Almost all of the smaller islands of the Pacific lie between 30°N and 30°S, extending from South-east Asia to Easter Island; the rest of the Pacific Basin is almost entirely submerged. The great triangle of Polynesia, connecting Hawaii, Easter Island, and New Zealand, encompasses the island arcs and clusters of the Cook, Marquesas, Samoa, Society, Tokelau, Tonga, and Tuamotu islands. North of the equator and west of the international date line are the numerous small islands of Micronesia, including the Caroline Islands, the Marshall Islands, and the Mariana Islands. In the southwestern corner of the Pacific lie the islands of Melanesia, dominated by New Guinea. Other important island groups of Melanesia include the Bismarck Archipelago, Fiji, New Caledonia, the Solomon Islands, and Vanuatu. Islands in the Pacific Ocean are of four basic types: continental islands, high islands, coral reefs, and uplifted coral platforms. Continental islands lie outside the Andesite Line and include New Guinea, the islands of New Zealand, and the Philippines. These islands are structurally associated with the nearby continents. High islands are of volcanic origin, and many contain active volcanoes. Among these are Bougainville, Hawaii, and the Solomon Islands. The third and fourth types of islands are both the result of coralline island building. Coral reefs are low-lying structures that have built up on basaltic lava flows under the ocean's surface. One of the most dramatic is the Great Barrier Reef off northeastern Australia. A second island type formed of coral is the uplifted coral platform, which is usually slightly larger than the low coral islands. Examples include Banaba (formerly Ocean Island) and Makatea in the Tuamotu group of French Polynesia.

History and economy

See the Oceania article for information on one set of the Pacific Island states listed below here. Important human migrations occurred in the Pacific in prehistoric times, most notably those of Polynesians from Tahiti to Hawaii and New Zealand. The ocean was sighted by Europeans early in the 16th century, first by Vasco Núñez de Balboa (1513) and then by Ferdinand Magellan, who crossed the Pacific during his circumnavigation (1519-1522). In 1564 conquistadors crossed the ocean from Mexico led by Miguel López de Legazpi who sailed to the Philippines and Mariana Islands. For the remainder of the 16th century Spanish influence was paramount, with ships sailing from Spain to the Philippines, New Guinea, and the Solomons. The Manila Galleons linked Manila and Acapulco. During the 17th century the Dutch, sailing around southern Africa, dominated discovery and trade; Abel Janszoon Tasman discovered (1642) Tasmania and New Zealand. The 18th century marked a burst of exploration by the Russians in Alaska and the Aleutian Islands, the French in Polynesia, and the British in the three voyages of James Cook (to the South Pacific and Australia, Hawaii, and the North American Pacific Northwest). Growing imperialism during the 19th century resulted in the occupation of much of Oceania by Great Britain and France, followed by the United States. Significant contributions to oceanographic knowledge were made by the voyages of the HMS Beagle in the 1830s, with Charles Darwin aboard; the HMS Challenger during the 1870s; the U.S.S. Tuscarora (1873-76); and the German Gazelle (1874-1876). Although the United States took the Philippines in 1898, Japan controlled the western Pacific by 1914, and occupied many other islands during World War II. By the end of that war the U.S. Pacific Fleet was the virtual master of the ocean. Seventeen independent states are located in the Pacific: Australia, Fiji, Japan, Kiribati, Marshall Islands, Micronesia, Nauru, New Zealand, Palau, Papua New Guinea, the Philippines, Samoa, Solomon Islands, Republic of China (Taiwan), Tonga, Tuvalu, and Vanuatu. Eleven of these nations have achieved full independence since 1960. The Northern Mariana Islands are self-governing with external affairs handled by the United States, and Cook Islands and Niue are in similar relationships with New Zealand. Also within the Pacific are the U.S. state of Hawaii and several island territories and possessions of Australia, Chile, Ecuador, France, Japan, New Zealand, the United Kingdom, and the United States. The exploitation of the Pacific's mineral wealth is hampered by the ocean's great depths. In shallow waters of the continental shelves off the coasts of Australia and New Zealand, petroleum and natural gas are extracted, and pearls are harvested along the coasts of Australia, Japan, Papua New Guinea, Nicaragua, Panama, and the Philippines, although in sharply declining volume. The Pacific's greatest asset is its fish. The shoreline waters of the continents and the more temperate islands yield herring, salmon, sardines, snapper, swordfish, and tuna, as well as shellfish. In 1986, the member nations of the South Pacific Forum declared the area a nuclear-free zone in an effort to halt nuclear testing and prevent the dumping of nuclear waste there.

Ports and harbours


- Acapulco (Mexico)
- Anchorage (United States)
- Auckland (New Zealand)
- Brisbane (Australia)
- Callao (Peru)
- Hong Kong (Hong Kong (China (PRC)))
- Honolulu (United States)
- Kobe (Japan)
- Long Beach (United States)
- Los Angeles (United States)
- Panama City (Panama)
- Portland (Oregon) (United States)
- Prince Rupert (Canada)
- San Diego (United States)
- San Francisco (United States)
- Sapporo (Japan)
- Seattle (United States)
- Shanghai (China (PRC))
- Sydney (Australia)
- Taipei (China (ROC))
- Vancouver (Canada)
- Victoria (Canada)
- Vladivostok (Russia)
- Yokohama (Japan)

Bibliography


- Barkley, R.A., Oceanographic Atlas of the Pacific Ocean (1969)
- Cameron, I., Lost Paradise (1987)
- Couper, A., Development in the Pacific Islands (1988)
- Crump, D.J., ed., Blue Horizons (1980)
- Gilbert, John, Charting the Vast Pacific (1971)
- Lower, J. Arthur, Ocean of Destiny: A Concise History of the North Pacific, 1500-1978 (1978)
- Oliver, D.L., The Pacific Islands, 3nd ed. (1989)
- Ridgell, R., Pacific Nations and Territories, 2nd ed. (1988)
- Soule, Gardner, The Greatest Depths (1970)
- Spate, O.H., Paradise Found and Lost (1988)
- Terrell, J.E., Prehistory in the Pacific Islands (1986). :Based on public domain text from US Naval Oceanographer

External links


- [http://www.epic.noaa.gov/epic/ewb/ EPIC Pacific Ocean Data Collection] Viewable on-line collection of observational data
- [http://dapper.pmel.noaa.gov/dchart/ NOAA In-situ Ocean Data Viewer] Plot and download ocean observations
- [http://www.mapsouthpacific.com/ Map South Pacific]
- [http://www.oscar.noaa.gov/datadisplay/ NOAA Ocean Surface Current Analyses - Realtime (OSCAR)] Near-realtime Pacific Ocean Surface Currents derived from satellite altimeter and scatterometer data
- [http://floats.pmel.noaa.gov/floats/ NOAA PMEL Argo profiling floats] Realtime Pacific Ocean data
- [http://www.pmel.noaa.gov/tao/jsdisplay/ NOAA TAO El Nino data] Realtime Pacific Ocean El NIno buoy data
- [http://www.southpacific.org/ South Pacific Organizer] Category:Oceans
- zh-min-nan:Thài-pêng-iûⁿ ko:태평양 ja:太平洋 simple:Pacific Ocean th:มหาสมุทรแปซิฟิก

New Zealand

New Zealand or Aotearoa, the Land of the Long White Cloud, is a country of two large islands and many smaller islands in the south-western Pacific Ocean. New Zealand is notable for its isolation, being separated from Australia on the northwest by the Tasman Sea, some 2,000 km wide. The closest neighbours to the north are New Caledonia, Fiji and Tonga. The population of New Zealand is mostly of European descent, with the indigenous Māori as the largest minority. Non-Māori Polynesian and Asian peoples are also significant minorities, especially in the cities. Officially, Elizabeth II is the Queen of New Zealand and is represented in the country by a non-political Governor-General; though the Queen has no real political influence. Political power is held by the Prime Minister who is leader of the Government in the democratically elected Parliament of New Zealand. The monarch's Realm of New Zealand also includes the Cook Islands and Niue, which are entirely self-governing; Tokelau, which is moving towards self-government, and New Zealand's claim in Antarctica.

History

New Zealand is one of the most recently settled major land masses. Polynesian settlers arrived in their waka some time between 800 and 600 years ago to establish the indigenous Māori culture. Settlement of the Chatham Islands to the south-east of New Zealand produced the Moriori people but it is disputed whether they moved there from New Zealand or elsewhere in Polynesia. Most of New Zealand was divided into tribal territories called rohe, resources within which were controlled by an iwi ('tribe'). Usually no two iwi had overlapping rohe. Māori adapted to eating the local marine resources, flora and fauna for food, hunting the giant flightless moa (which soon became extinct), and ate the Polynesian Rat and kumara (sweet potato), which they introduced to the country. The first Europeans known to reach New Zealand were led by Abel Janszoon Tasman, who sailed up the west coast of the South and North islands in 1642. He named it Staten Landt, believing it to be part of the land Jacob Le Maire had discovered in 1616 off the coast of Chile. Staten Landt appeared on Tasman's first maps of New Zealand, but this was changed by Dutch cartographers to Nova Zeelandia, after the Dutch province of Zeeland, some time after Hendrik Brouwer proved the South American land to be an island in 1643. The Latin Nova Zeelandia became Nieuw Zeeland in Dutch. Lieutenant James Cook subsequently called the archipelago New Zealand, although the names he chose for the North and South islands were rejected, and the main three islands became known as North, Middle and South, with the Middle Island being later called the South Island. Cook began extensive surveys of the islands in 1769, leading to European whaling expeditions and eventually significant European colonisation. From as early as the 1780s, Māori had encounters with European sealers and whalers. Acquisition of muskets by those iwi in close contact with European visitors destabilised the existing balance of power between Māori tribes and there was a temporary but intense period of bloody inter-tribal warfare, known as the Musket Wars, that only ceased when all iwi were so armed. Concern about the exploitation of Māori by Europeans, Church Missionary Society lobbying and French interest in the region led the British to annex New Zealand by Royal Proclamation in January 1840. To legitimise the British annexation, Lieutenant Governor William Hobson had been dispatched in 1839; he hurriedly negotiated the Treaty of Waitangi with northern iwi on his arrival. The Treaty was signed in February, and in recent years it has come to be seen as the founding document of New Zealand. The Māori translation of the treaty promised the Māori tribes "tino rangatiratanga" would be preserved in return for cedeing kawanatanga, which the English versions translates as "chieftainship" for "sovereignty"; the real meanings are now disputed. Disputes over land sales and sovereignty caused the New Zealand land wars which took place between 1845 and 1872. In 1975 the Treaty of Waitangi Act established the Waitangi Tribunal, charged with hearing claims of Crown violations of the Treaty of Waitangi dating back to 1840. Some Māori tribes and the Moriori never signed the treaty. Although New Zealand was initially administered as a part of the Australian colony of New South Wales, it became a colony in its own right in 1841. European settlement progressed more rapidly than anyone anticipated, and settlers soon outnumbered Māori. Self-government was granted to the settler population in 1852. The first capital of New Zealand was Kororareka (known today as Russell) but shortly afterwards moved to Auckland. There were political concerns following the discovery of gold in Central Otago in 1861 that the South Island would form a separate colony. So in 1865 the capital was offically moved to the more central city of Wellington. New Zealand was involved in a Constitutional Convention in March 1891 in Sydney, New South Wales, along with the then-colonies of Australia. This was to consider a potential constitution for the proposed federation between the then-British Colonies of Australasia. New Zealand lost interest in joining Australia in a federation following this convention. New Zealand became an independent dominion on 26 September 1907 by royal proclamation. Full independence was granted by the United Kingdom Parliament with the Statute of Westminster in 1931; it was taken up upon the Statute's adoption by the New Zealand Parliament in 1947. Since then New Zealand has been a sovereign constitutional monarchy within the Commonwealth of Nations.

Politics

New Zealand is a constitutional monarchy with a parliamentary democracy. Under the New Zealand Royal Titles Act (1953), Queen Elizabeth II is Queen of New Zealand and is represented as head of state by the Governor-General, Dame Silvia Cartwright. The New Zealand Parliament has only one chamber, the House of Representatives which usually seats 120 members of Parliament. Parliamentary elections are every three years under a form of proportional representation called Mixed Member Proportional (MMP). The 2005 General Election created an 'overhang' of one extra seat (occupied by the Māori Party), due to that party winning more seats in constituencies than its proportional entitlement. There is no single written constitution; however, the Constitution Act (1986) is the principal formal statement of New Zealand's constitutional structure. The Governor-General has the power to appoint and dismiss Prime Ministers and to dissolve Parliament. The Governor-General also chairs the Executive Council which is a formal committee consisting of all ministers of the Crown. Members of the Executive Council are required to be members of Parliament, and most are also in Cabinet. Cabinet is the most senior policy-making body and is led by the Prime Minister who is also the Parliamentary leader of the governing party or coalition. The current Prime Minister is Helen Clark of the Labour Party. She has served two complete terms as Prime Minister and has begun her third. On 17 October 2005 she announced that she had come to a complex arrangement that guaranteed the support of enough parties for her Labour-led coalition to govern. The core of the coalition is a cabinet consisting of Labour Party ministers and Jim Anderton, the Progressive Party's only MP. In addition to the parties represented in cabinet the leaders of New Zealand First and United Future are to be appointed as Ministers outside Cabinet. An arrangement of this kind has never been attempted before in New Zealand. A further arrangement has been made with the Green Party, which has given a commitment not to vote against the government on confidence and supply. This commitment assures the government of a majority of seven MPs on confidence. The Leader of the Opposition is National Party leader Don Brash who was formerly Governor of the Reserve Bank. Also in opposition are the Māori Party and ACT New Zealand. The highest court in New Zealand is the Supreme Court of New Zealand. The Supreme Court was established in 2004 following the passage of the Supreme Court Act in 2003. The Act abolished the option to appeal Court of Appeal rulings to the Privy Council in London. The current Chief Justice is Dame Sian Elias. New Zealand's judicary also has a High Court which deals with serious criminal offences and civil matters, and a Court of Appeal, as well as subordinate courts.

Foreign relations and military

New Zealand maintains a strong profile on environmental protection, human rights and free trade, particularly for agriculture. New Zealand is a member of the following geo-political organisations: APEC, Commonwealth of Nations, OECD and the United Nations. It has signed up to a number of free trade agreements, of which the most important is Closer Economic Relations with Australia. For its first hundred years, New Zealand followed Britain's lead on foreign policy. "Where she goes, we go, where she stands, we stand", said Prime Minister Michael Savage, in declaring war on Germany on 3 September 1939. However, Britain's inability to protect New Zealand from Japanese aggression in World War II led New Zealand to come under the influence of the United States of America for the generation following the war. New Zealand has traditionally also worked closely with Australia, whose foreign policy followed a similar historical trend. In turn, many Pacific Islands such as Western Samoa have looked to New Zealand's lead. The American influence on New Zealand was weakened by the disappointment with the Vietnam War, the nuclear danger presented by the Cold War, the Sinking of the Rainbow Warrior by France and by disagreements over environmental and agricultural trade issues. New Zealand is a party to the ANZUS security treaty between Australia, New Zealand and the United States. In 1984 New Zealand refused nuclear-powered or nuclear-armed ships access to its ports. In 1986 the United States announced that it was suspending its treaty security obligations to New Zealand pending the restoration of port access. The New Zealand Nuclear Free Zone, Disarmament and Arms Control Act of 1987 prohibits the stationing of nuclear weapons on the territory of New Zealand and the entry into New Zealand waters of nuclear armed or propelled ships. This legislation remains a source of contention and the basis for the United States' continued suspension of treaty obligations to New Zealand. In addition to the various wars between Iwi, and between the British, settlers and Iwi, New Zealand has fought in the Boer War, World War I, (sustaining the highest casualties per head of population of any combatant nation), World War II, the Korean War, the Malayan Emergency (and committed troops, fighters and bombers to the subsequent confrontation with Indonesia), the Vietnam War, the Gulf War and the Afghanistan War and has briefly sent a unit of army engineers to help with rebuilding Iraqi infrastructure. The New Zealand military has three branches: the New Zealand Army, the Royal New Zealand Navy, and the Royal New Zealand Air Force. New Zealand considers its own national defence needs to be modest; it dismantled its air combat capability in 2001. New Zealand has contributed forces to recent regional and global peacekeeping missions, including those in Cyprus, Somalia, Bosnia, the Sinai, Angola, Cambodia, the Iran/Iraq border, Bougainville and East Timor.

Local government and external territories

East Timor The early European settlers divided New Zealand into provinces. These were abolished in 1876 so that government could be centralised for financial reasons. As a result, New Zealand has no separately represented subnational entities such as provinces, states or territories apart from its local government. The spirit of the provinces however still lives on, and there is fierce rivalry exhibited in sporting and cultural events. Since 1876, local government has administered the various regions of New Zealand. In 1989, the government completely reorganised local government, implementing the current two-tier structure of regional councils and territorial authorities. Today New Zealand has 12 regional councils for the administration of environmental and transport matters and 74 territorial authorities that administer roading, sewerage, building consents, and other local matters. The territorial authorities are 16 city councils, 57 district councils, and the Chatham Islands County Council. Four of the territorial councils (one city and three districts) and the Chatham Islands County Council also perform the functions of a regional council and thus are known as unitary authorities. Territorial authority districts are not subdivisions of regional council districts, and a few of them straddle regional council boundaries. Regions are (asterisks denote unitary authorities): Northland, Auckland, Waikato, Bay of Plenty, Gisborne
- , Hawke's Bay, Taranaki, Manawatu-Wanganui, Wellington, Marlborough
- , Nelson
- , Tasman
- , West Coast, Canterbury, Otago, Southland, Chatham Islands
- . As a major South Pacific nation, New Zealand has a close working relationship with many of the smaller Pacific Island nations, and continues a political association with the Cook Islands, Niue, and Tokelau. New Zealand operates Scott Base in its Antarctic territory, the Ross Dependency. Other countries also use Christchurch to support their Antarctic bases and the city is sometimes known as the "Gateway to Antarctica".

Geography

Ross Dependency are visible in the centre of the North Island. The Southern Alps and the rain shadow they create are clearly visible on the South Island]] New Zealand comprises two main islands (simply called the North and South Islands in English, or usually Te-Ika-a-Maui and Te Wai Pounamu in Māori) and a number of smaller islands. The total land area of New Zealand, 268,680 km², is a little less than that of Japan and a little more than the United Kingdom. The country extends more than 1600 km along its main, north-north-east axis. The most significant of the smaller inhabited islands of New Zealand include Stewart Island/Rakiura, Waiheke Island, an island in Auckland's Hauraki Gulf, Great Barrier Island, east of the Hauraki Gulf and the Chatham Islands, named Rekohu by Moriori. The country has extensive marine resources, with the fifth largest Exclusive Economic Zone in the world covering over 4 million km², more than 15 times its land area. The South Island is the largest land mass, and is divided along its length by the Southern Alps, the highest peak of which is Aoraki/Mount Cook, at 3,754 metres (12,316 feet). There are 18 peaks of more than 3,000 metres in the South Island. The North Island is less mountainous than the South, but is marked by volcanism. The tallest North Island mountain, Mount Ruapehu (2,797 metres), is an active cone volcano. The dramatic and varied landscape of New Zealand has made it a popular location for the production of television programmes and films, including the Lord of the Rings trilogy. Lord of the Rings The usual climate throughout the country is mild, mostly cool temperate to warm temperate, with temperatures rarely falling below 0°C or rising above 30°C. Conditions vary from wet and cold on the West Coast of the South Island to dry and continental in the Mackenzie Basin of inland Canterbury and subtropical in Northland. Of the main cities, Christchurch is the driest, receiving only some 640 millimetres of rain per year. Auckland, the wettest, receives a little less than three times that amount.

Flora and fauna

Northland Because of its long isolation from the rest of the world, and its island biogeography New Zealand has extraordinary flora and fauna. About 80 percent of the New Zealand flora only occurs in New Zealand, including more than 40 endemic genera. The main two types of forest have been dominated by podocarps including the giant kauri and southern beech. The remaining vegetation types in New Zealand are grassland of grass and tussock, usually associated with the subalpine areas, and the low shrublands between grasslands and forests. Until the arrival of the first humans, 80% of the land was forested and, barring two species of bat, there were no non-marine mammals at all. Instead, New Zealand's forests were inhabited by a diverse range of birds including the flightless Moa which is now extinct, the Kiwi, Kakapo, and Takahē which are all endangered due to human actions. Unique birds capable of flight include the Haast's eagle which was the world's largest bird of prey before it became extinct and the large parrots the Kaka and Kea. Reptiles present in New Zealand include skinks and geckos and the Tuatara. There are no snakes but there are many species of insects— including the weta which may grow as large as a House Mouse.

Economy

House Mouse New Zealand has a thriving, modern, developed economy. The country has a high standard of living, ranking 19th on the 2005 Human Development Index and 15th of The Economists 2005 world-wide quality-of-life index. Since 1984 successive governments have engaged in major macroeconomic restructuring, transforming New Zealand from a highly protectionist and regulated economy to a liberalised free-trade economy. During the late 1980s, the New Zealand Government sold a number of major trading enterprises, including its telecommunications company, railway network, a number of radio stations and two financial institutions in a series of asset sales. Although the New Zealand Government continues to own a number of significant businesses, collectively known as State-Owned Enterprises (SOEs), they are operated through arms-length shareholding arrangements as stand-alone businesses that are required to operate profitably, just like any privately owned enterprise. Unfortunately, due in part to the sudden transition to a market economy, an economic bubble developed in the New Zealand stock market starting in 1984. This burst in October 1987 and the total value of the market halved within a year (it has still to recover this lost value). The effect of this bubble was a period of poor economic growth which lasted until the mid 90s. It also led the government to begin a programme of massive immigration to boost GDP. However, since 1999 New Zealand has enjoyed a period of relatively strong and sustained growth, and contained inflationary pressures. The current New Zealand government's economic objectives are centred around moving from being ranked among the lower end of the OECD countries to regaining a higher placing again, pursuing free-trade agreements, "closing the gaps" between ethnic groups, and building a "knowledge economy." In 2004 it began discussing free trade with China, one of the first countries to do so. New Zealand is heavily dependent on trade—particularly in agricultural products—to drive growth, and it has been affected by global economic slowdowns and slumps in commodity prices. Since agricultural exports are highly sensitive to currency values and a large percentage of consumer goods are imported, any changes in the value of the New Zealand dollar has a strong impact on the economy. Its primary export industries are agriculture, horticulture, fishing, forestry and information technology. There are also substantial tourism and export education industries. The film and wine industries are considered to be up-and-coming.

Demographics

New Zealand has a population of about 4.1 million. About 70% of the population are whites of European descent. New Zealanders of Anglo-Celtic ancestry are known as Pākeha - this term is used variously and some Māori use it to refer to all non-Māori New Zealanders. A large proportion of white New Zealanders are of Scottish ancestry. Māori people are the second largest ethnic group (the percentage of the population of full or part-Māori ancestry is 14.7%; those who checked only Māori are 7.9%). Between the 1996 and 2001 censuses, the number of people of Asian origin (6.6%) overtook the number of people of Pacific Island origin (6.5%) (note that the census allowed multiple ethnic affiliations). Virtually all Māori are of mixed heritage (Māori/Pākeha), but a large portion of them marked themselves as Māori-only on the Census. New Zealand is positive about immigration and is committed to increasing its population by approx 1% per annum. At present migrants from the UK constitute the largest single group (30%) but new migrants are drawn from many nations, increasingly from East Asia. Christianity is the predominant religion in New Zealand, although nearly 40% of the population has no religious affiliation. The main Christian denominations are Anglicanism, Presbyterianism, Roman Catholicism and Methodism. There are also significant numbers who identify themselves with Pentecostal and Baptist churches and with the Mormon church. The New Zealand-based Ratana church has many adherents among Māori. According to census figures, other significant minority religions include Hinduism, Buddhism and Islam.

Culture

IslamNew Zealand has a diverse contemporary culture with influences from British, the Māori,and other European immigrants and most recently Polynesian cultures. There were many people from Scotland amongst the early British settlers and elements of their culture persist; New Zealand is said to have more bagpipe bands than Scotland. Cultural links between New Zealand and the UK are maintained by a common language, sustained migration from the UK and the fact that many young New Zealanders spend time in the UK on their "overseas experience (OE)". Pre-European contact Māori culture had no metal tools, relying on stone and wood. Modern Māori do not live a traditional lifestyle. Elements of Māori culture survive and the Government actively promotes it to all New Zealanders. Use of the Māori language (Te Reo Māori) as a living, community language remained only in a few remote areas in the post war years but it is currently going through a renaissance; with generous state support for Māori language medium schools and a Māori language television channel. New Zealand's landscape has appeared in a number of television programmes and films. In particular, the television series Hercules and Xena were filmed around Auckland, and the film Heavenly Creatures in Christchurch. The television series The Tribe is set and filmed in New Zealand as well. Director Peter Jackson shot the epic The Lord of the Rings trilogy in various locations around the country, taking advantage of the spectacular and relatively unspoiled landscapes, and Mount Taranaki was used as a stand-in for Mount Fuji in The Last Samurai. The latest of such major international films to be released are King Kong and The Chronicles of Narnia: The Lion, the Witch and the Wardrobe.

Sport

New Zealand's most popular sports are rugby union, cricket, netball, lawn bowling, soccer (the most popular sport amongst children) and rugby league. Also popular are golf, tennis, cycling and a variety of water sports, particularly sailing, whitewater kayaking, Surf Lifesaving and rowing. In the latter, New Zealand enjoyed an extraordinary Magic 45 minutes when winning four successive gold medals at the 2005 world championships. Snow sports such as skiing and snowboarding are also popular. Equestrian sportsmen and sportswomen make their mark in the world (Mark Todd being chosen international "Horseman of the Century"), and all the way down to the juniors at pony club level.

Olympic Games

The country is internationally recognised as achieving extremely well on a medals-to-population ratio at Olympic Games and Commonwealth Games. See, for example, New Zealand Olympic medallists and New Zealand at the 2004 Summer Olympics.

Rugby

Rugby as a sport is closely linked to New Zealand's national identity. The national rugby team is called the All Blacks and has the best winning record of any national team in the world, including being the inaugural winners of the World Cup in 1987. The style of name has been followed in naming the national team in several other sports. For instance, the nation's basketball team is known as the Tall Blacks. New Zealand is to host the 2011 Rugby Union World Cup. New Zealand's national sporting colours are not the colours of its flag, but are black and white (silver). The silver fern is a national emblem worn by New Zealanders representing their country in sport. The haka—a traditional Māori challenge—is often performed at sporting events. The All Blacks traditionally perform a haka before the start of international matches.

Yachting, America's Cup

New Zealand is one of the leading nations in world yachting, especially open water long distance or around the world races. Round-the-world yachtsman, Sir Peter Blake was something of a national hero before his untimely death at the hands of river pirates while on an environmental exploration trip on the Amazon. In inshore yachting, Auckland hosted the last two America's Cup regattas (2000 and 2003). In 2000, Team New Zealand successfully defended the trophy they had won in 1995 in San Diego, which made them the only team in the history of the Cup to successfully defend a challenge other than a United States team, but in 2003 they lost to a team headed by Ernesto Bertarelli of Switzerland, whose Alinghi syndicate was skippered by Russell Coutts, the former skipper of Team New Zealand. Team New Zealand will compete for the America's Cup at the next regatta in Valencia in 2007. The team manager is Grant Dalton.

Public holidays

Statutory Holidays
(These holidays are legislated by several Acts of Parliament, such as the Holidays Act. New Zealand Statutes can be viewed at [http://www.legislation.govt.nz/browse_vw.asp?content-set=pal_statutes legislation.govt.nz]) There are also Provincial Anniversary Days to celebrate the founding days or landing days of the first colonists of the various colonial provinces. The actual observance of Anniversary days can vary even within each province due to local custom, convenience or the proximity of seasonal events or other holidays. This may differ from the historical observance day, and may be several weeks from the historic date of the events being commemorated. A full list of Anniversary days is listed in the article Holidays in New Zealand.

International rankings


- UN Human Development Index (HDI), 2005: 19th out of 177 behind Norway; United Nations Development Programme (pdf) [http://hdr.undp.org/reports/global/2005/pdf/HDR05_complete.pdf]
- Quality of Life Index, 2005: 15th out of 111 behind Ireland; The Economist Intelligence Unit (pdf) [http://www.economist.com/media/pdf/QUALITY_OF_LIFE.pdf]
- Environmental Sustainability Index, 2005: 14th (out of 146) behind Finland; Yale University Center for Environmental Law and Policy & Columbia University Center for International Earth Science Information Network (pdf) [http://www.yale.edu/esi/ESI2005_Main_Report.pdf]
- Index of Economic Freedom, 2005: 5th= (out of 155) behind Hong Kong; Heritage Foundation/Wall Street Journal [http://www.heritage.org/research/features/index/]
- GDP Ranking, 2005: 25th out of 111 behind Luxembourg; The Economist Intelligence Unit (pdf) [http://www.economist.com/media/pdf/QUALITY_OF_LIFE.pdf]
- Transparency International 2005: 2nd= (out of 159) behind Iceland on its list of least corrupt countries in the world. [http://ww1.transparency.org/cpi/2005/cpi2005_infocus.html#cpi]

See also

Notes

McGlone, S.M. and Wilmshurst, J.M. 1999. Dating initial Māori environmental impact in New Zealand. Quaternary International 59:5 - 16
Ministry for the Environment. 2005. Offshore Options: Managing Environmental Effects in New Zealand's Exclusive Economic Zone. [http://www.mfe.govt.nz/publications/water/offshore-options-jun05/html/page3.html Introduction]
Allan, H.H. 1982. Indigenous Tracheophyta - Psilopsida, Lycopsida, Filicopsida, Gymnospermae, Dicotyledons, Flora of New Zealand Volume I. Botany Division, Department of Scientific and Industrial Research

External links


- [http://www.teara.govt.nz/ Te Ara, the Encyclopedia of New Zealand]
- [http://webdirectory.natlib.govt.nz/index.htm Te Puna Web Directory ] - A directory to New Zealand web sites
- [http://www.mch.govt.nz/ Ministry for Culture and Heritage] - includes information on flag, anthems and coat of arms.
- [http://www.govt.nz/ New Zealand Government Portal]
- [http://www.nzte.govt.nz/ New Zealand Trade and Enterprise] - New Zealand's trade and economic development agency.
- [http://wikitravel.org/en/article/New_Zealand Wikitravel] - New Zealand travel guide.
- [http://www.metservice.co.nz/ New Zealand weather]
- [http://www.nzhistory.net.nz/ NZHistory.net.nz New Zealand history website]
- [http://www.stats.govt.nz/ Statistics New Zealand] - Official statistics.
- [http://www.newzealand.com/ Tourism New Zealand]
- [http://www.astronomy.net.nz/ Astronomy in New Zealand] The guide to astronomy in New Zealand
- [http://www.nzherald.co.nz/ New Zealand Herald] - New Zealand newspaper online A
Category:Island nations Category:Members of the Commonwealth of Nations Category:Former British colonies Category:Monarchies Category:Oceanic countries Category:Polynesia als:Neuseeland zh-min-nan:Aotearoa ko:뉴질랜드 ms:New Zealand ja:ニュージーランド simple:New Zealand th:ประเทศนิวซีแลนด์

Territory

A territory is a defined area (including land and waters), usually considered to be a possession of an animal, person, organization, or institution (from the word 'terra', meaning 'land').
- In politics, a territory is an area of land under the jurisdiction of a governmental authority. Territory can, though, include any geographical area under the jurisdiction of a sovereign and does not have a political division status. The remainder of this article deals with political territories.
- In biology, an organism which defends an area against intrusion (usually from members of its own species) is said to be territorial. For further details see