1.
Flag of Niue
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The flag of Niue was adopted on 15 October 1975. It consists of the Union Jack in the left corner with a star in the middle of the Union Jack. It is very unusual for a flag based on a British ensign design, in having not only a yellow background, the symbolism represented by the flag is described in the Act. The Union Jack symbolises the protection granted by the United Kingdom in 1900 after petitioning by the Kings, the golden yellow is inspired by the bright sunshine of Niue and also said to symbolise the warm feelings of the Niuean people towards New Zealand and his people. The association with New Zealand, which took responsibility and administration of Niue in 1901, is also represented by the four small stars that depict the Southern Cross. Finally the blue disc containing a star represents the deep blue sea surrounding the self-governing island of Niue. Seal of Niue List of New Zealand flags Flags of the World - Niue Niue Flag Act 1975
2.
Seal of Niue
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The Seal of Niue, or the Public Seal of Niue, is the official seal of Niue. It was created in 1974 when Niue gained independence and joined into free association with New Zealand, before 1974 Niue used the Coat of Arms of New Zealand. The Niue Constitution Act, passed in 1974, provided for a seal to be created for Niue. The Seal was to be held by the Speaker of the Niue Assembly, the Speaker is also responsible for ensuring that the Seal is not misused. All judicial notices in Niue are affixed with the Seal, before 2007 the Seal of Niue was used in Tokelau to confirm the passage of legislation. In 2007 the Tokelau Amendment Act 2007 was passed, which replaced the use of the Seal of Niue in Tokelau, the Seal of Niue has at its centre the coat of arms of New Zealand, which is a shield divided into quarters. In the first quarter is the constellation of the Southern Cross, in the second a golden fleece, a sheaf of wheat in the third, over the four-quarters in the centre appears a white band on which there are three black ships. At the head of the shield is a crown, and at the foot of the shield is a ribbon with the words New Zealand, the Seal is on a white circle, with Public Seal of Niue along the top, and Niue at the bottom. Flag of Niue Media related to Coats of arms of Niue at Wikimedia Commons
3.
Ko e Iki he Lagi
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Ko e Iki he Lagi, also titled in English as Lord in heaven, Thou art merciful, is the national anthem of Niue. It was adopted in 1974 when Niue became a self-governing state, during Niues history as a territory of New Zealand, the national anthem of Niue was New Zealands God Defend New Zealand. God Save the Queen was also used and is used as the royal anthem for the Monarchy of New Zealand. Ko e Iki he Lagi was created before the 1970s and it is not known who wrote it but it is known that it was prepared by Sioeli Fusikata. When it was written, it had become a song on Niue. In the 1963 South Pacific Games, Niue used the Flag of New Zealand as the flag to represent them in keeping with the rest of the colonies of the British Empire not using the Union Jack at the games. However, Niue failed to win any events so Ko e Iki he Lagi was not performed at the games, God Save the Queen was retained as the royal anthem for when the monarch is present in Niue
4.
Pacific Ocean
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The Pacific Ocean is the largest and deepest of the Earths oceanic divisions. It extends from the Arctic Ocean in the north to the Southern Ocean in the south and is bounded by Asia and Australia in the west, the Mariana Trench in the western North Pacific is the deepest point in the world, reaching a depth of 10,911 metres. Both the center of the Water Hemisphere and the Western Hemisphere are in the Pacific Ocean, the oceans current name was coined by Portuguese explorer Ferdinand Magellan during the Spanish circumnavigation of the world in 1521, as he encountered favourable winds on reaching the ocean. He called it Mar Pacífico, which in both Portuguese and Spanish means peaceful sea, important human migrations occurred in the Pacific in prehistoric times. Long-distance trade developed all along the coast from Mozambique to Japan, trade, and therefore knowledge, extended to the Indonesian islands but apparently not Australia. By at least 878 when there was a significant Islamic settlement in Canton much of trade was controlled by Arabs or Muslims. In 219 BC Xu Fu sailed out into the Pacific searching for the elixir of immortality, from 1404 to 1433 Zheng He led expeditions into the Indian Ocean. The east side of the ocean was discovered by Spanish explorer Vasco Núñez de Balboa in 1513 after his expedition crossed the Isthmus of Panama and he named it Mar del Sur because the ocean was to the south of the coast of the isthmus where he first observed the Pacific. Later, Portuguese explorer Ferdinand Magellan sailed the Pacific East to West on a Castilian expedition of world circumnavigation starting in 1519, Magellan called the ocean Pacífico because, after sailing through the stormy seas off Cape Horn, the expedition found calm waters. The ocean was often called the Sea of Magellan in his honor until the eighteenth century, sailing around and east of the Moluccas, between 1525 and 1527, Portuguese expeditions discovered the Caroline Islands, the Aru Islands, and Papua New Guinea. In 1542–43 the Portuguese also reached Japan, in 1564, five Spanish ships consisting of 379 explorers crossed the ocean from Mexico led by Miguel López de Legazpi and sailed to the Philippines and Mariana Islands. The Manila galleons operated for two and a half centuries linking Manila and Acapulco, in one of the longest trade routes in history, Spanish expeditions also discovered Tuvalu, the Marquesas, the Cook Islands, the Solomon Islands, and the Admiralty Islands in the South Pacific. In the 16th and 17th century Spain considered the Pacific Ocean a Mare clausum—a sea closed to other naval powers, as the only known entrance from the Atlantic the Strait of Magellan was at times patrolled by fleets sent to prevent entrance of non-Spanish ships. On the western end of the Pacific Ocean the Dutch threatened the Spanish Philippines, Spain also sent expeditions to the Pacific Northwest reaching Vancouver Island in southern Canada, and Alaska. The French explored and settled Polynesia, and the British made three voyages with James Cook to the South Pacific and Australia, Hawaii, and the North American Pacific Northwest, one of the earliest voyages of scientific exploration was organized by Spain in the Malaspina Expedition of 1789–1794. It sailed vast areas of the Pacific, from Cape Horn to Alaska, Guam and the Philippines, New Zealand, Australia, and the South Pacific. Growing imperialism during the 19th century resulted in the occupation of much of Oceania by other European powers, and later, Japan, in Oceania, France got a leading position as imperial power after making Tahiti and New Caledonia protectorates in 1842 and 1853 respectively. After navy visits to Easter Island in 1875 and 1887, Chilean navy officer Policarpo Toro managed to negotiate an incorporation of the island into Chile with native Rapanui in 1888, by occupying Easter Island, Chile joined the imperial nations
5.
Alofi
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Alofi is the capital of the Pacific Ocean island nation of Niue, which is located within the Realm of New Zealand. With a population of 1,611, Alofi has the distinction of being the second smallest national capital city in terms of population and it consists of the two villages, Alofi North and Alofi South where the government headquarters are located. It is located at the centre of Alofi Bay on the west coast of the island, the bay stretches for 30% of the islands length from Halagigie Point in the south to Makapu Point in the north. It is also notable that Alofi contains the worlds largest toothbrush fence, in January 2004, Niue was hit by the fierce tropical storm Cyclone Heta which killed two people and did extensive damage to the entire island. Many of Alofis buildings were destroyed, including the hospital, government buildings were shifted to a less exposed site 3 km inland from the west coast, named Fonuakula, after the storm. This site is still within the boundaries of Alofi South. Alofi features a tropical rainforest climate under the Köppen climate classification, the city has a noticeably drier stretch from June through September. However, all of these months average more than 60 mm of rain, like other cities with this climate, average temperatures remain relatively constant throughout the year, at 25 °C. The town is serviced by Niue International Airport, and there are numerous roads, Niue recovery at $23 million, Alofi to be relocated. Kalauni, Hubert M. DECLARATION OF FINAL RESULT OF POLL FOR THE NIUE LEGISLATIVE ASSEMBLY GENERAL ELECTION ¶ SATURDAY7 JUNE2008, NZ Ministry of Foreign Affairs and Trade. Niue – Country Information Paper – NZ Ministry of Foreign Affairs, NZ Ministry of Foreign Affairs and Trade. Niue population profile based on 2006 census of population and housing, nouméa, New Caledonia, Secretariat of the Pacific Community. Archived from the original on 3 August 2009, weatherbase, Historical Weather for Alofi, Niue. History of Niue Cyclone aftermath pictures
6.
Demonym
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A demonym is a word that identifies residents or natives of a particular place, which is derived from the name of that particular place. It is a neologism, previously gentilic was recorded in English dictionaries, e. g. the Oxford English Dictionary, thus a Thai may be any resident or citizen of Thailand, of any ethnic group, or more narrowly a member of the Thai people. Conversely, some groups of people may be associated with multiple demonyms, for example, a native of the United Kingdom may be called a British person, a Brit, or a Briton. In some languages, when a parallel demonym does not exist, in English, demonyms are capitalized and are often the same as the adjectival form of the place, e. g. Egyptian, Japanese, or Greek. Significant exceptions exist, for instance the adjectival form of Spain is Spanish, English widely includes country-level demonyms such as Ethiopian or Guatemalan and more local demonyms such as Seoulite, Wisconsinite, Chicagoan, Michigander, Fluminense, and Paulista. Some places lack a commonly used and accepted demonym and this poses a particular challenge to those toponymists who research demonyms. The word gentilic comes from the Latin gentilis and the English suffix -ic, the word demonym was derived from the Greek word meaning populace with the suffix for name. National Geographic attributes the term demonym to Merriam-Webster editor Paul Dickson in a recent work from 1990 and it was subsequently popularized in this sense in 1997 by Dickson in his book Labels for Locals. However, in What Do You Call a Person From, a Dictionary of Resident Names attributed the term to George H. Scheetz, in his Names Names, A Descriptive and Prescriptive Onymicon, which is apparently where the term first appears. Several linguistic elements are used to create demonyms in the English language, the most common is to add a suffix to the end of the location name, slightly modified in some instances. Cairo → Cairene Cyrenaica → Cyrene Damascus → Damascene Greece → Greek Nazareth → Nazarene Slovenia → Slovene Often used for Middle Eastern locations and European locations. Kingston-upon-Hull → Hullensian Leeds → Leodensian Spain → Spaniard Savoy → Savoyard -ese is usually considered proper only as an adjective, thus, a Chinese person is used rather than a Chinese. Monaco → Monégasque Menton → Mentonasque Basque Country → Basque Often used for French locations, mostly they are from Africa and the Pacific, and are not generally known or used outside the country concerned. In much of East Africa, a person of an ethnic group will be denoted by a prefix. For example, a person of the Luba people would be a Muluba, the plural form Baluba, similar patterns with minor variations in the prefixes exist throughout on a tribal level. And Fijians who are indigenous Fijians are known as Kaiviti and these demonyms are usually more informal and colloquial. In the United States such informal demonyms frequently become associated with mascots of the sports teams of the state university system. In other countries the origins are often disputed and these will typically be formed using the standard models above
7.
Politics of Niue
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Politics of Niue takes place in a framework of a parliamentary representative democratic dependency, whereby the Chief Minister is the head of government, and of a multi-party system. Niue is self-governing in free association with New Zealand and is responsible for internal affairs. New Zealand retains some responsibility for external affairs, in consultation with Niue, the Niue Constitution Act 1974 vests executive authority in Her Majesty the Queen in Right of New Zealand and the Governor-General of New Zealand. The constitution specifies that in practice, it is exercised by a Cabinet of the Premier of Niue. The premier and ministers must be members of the Niue Assembly, the Judiciary is independent of the executive and the legislature. The monarch is hereditary, her representative in relation to Niue is appointed by the monarch, the New Zealand high commissioner is appointed by, and acts solely as a diplomatic agent of, the New Zealand Government. The cabinet is chosen by the premier and appointed by the Speaker of the Niue Assembly and collectively responsible to Parliament, the Assembly has 20 members elected for a three-year term,6 elected on a common roll and 14 representatives of the villages. Electors must be New Zealand citizens, resident for at least three months, and candidates must have been electors, resident for twelve months, the speaker is elected from among the members. In Niue, political parties have never played an important role, there is, at present, no political party, and candidates to elections therefore run as independents. The only party ever to have existed, the Niue Peoples Party, as there are no political parties, there is no formal parliamentary Opposition, though there are MPs who oppose the government. Below is a list of recent by-elections, The Judicial Committee of the Privy Council sitting in the United Kingdom is Niues highest court, on the island, there is a Court of Appeal, and the High Court of Niue. The current chief justice is Patrick Savage, previous chief justices include Gaven Donne and Heta Kenneth Hingston, who served as such for 14 years prior to Patrick Savage. Niue is divided in 14 villages each with its own village council members are elected. ACP, ESCAP, Intelsat, PIF, Sparteca, SPC, UNESCO, WHO, every village in Niue have a Village council, the term in office is three years before going back to the polls. The election of the members of the village follows the same rules. At the first meeting of the Village Council the Chairman will be elected, including the Deputy Chair, the Village Council receives grants from the Government, donor agencies also fund some development projects. The Council use to organize show days and conduct fundraising activities to generate revenue to help run some of the activities of the village, Cabinet of Niue Electoral calendar Electoral system Foreign relations of Niue List of political parties by country to browse parties by country Government of Niue
8.
Unitary state
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The majority of states in the world have a unitary system of government. Of the 193 UN member states,165 of them are governed as unitary states, unitary states are contrasted with federal states. In a unitary state, sub-national units are created and abolished, the United Kingdom of Great Britain and Northern Ireland is an example of a unitary state. Many unitary states have no areas possessing a degree of autonomy, in such countries, sub-national regions cannot decide their own laws. Examples are the Republic of Ireland and the Kingdom of Norway, in federal states, the sub-national governments share powers with the central government as equal actors through a written constitution, to which the consent of both is required to make amendments. This means that the units have a right of existence. The United States of America is an example of a federal state, under the U. S. Constitution, powers are shared between the federal government and the states
9.
Parliamentary system
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In a parliamentary system, the head of state is usually a different person from the head of government. Since ancient times, when societies were tribal, there were councils or a headman whose decisions were assessed by village elders, eventually these councils have slowly evolved into the modern Parliamentary system. The first parliaments date back to Europe in the Middle Ages, for example in 1188 Alfonso IX, the modern concept of parliamentary government emerged in the Kingdom of Great Britain and its contemporary, the Parliamentary System in Sweden. In England, Simon de Montfort is remembered as one of the fathers of representative government for holding two famous parliaments, the first, in 1258, stripped the King of unlimited authority and the second, in 1265, included ordinary citizens from the towns. Later, in the 17th century, the Parliament of England pioneered some of the ideas and systems of liberal democracy culminating in the Glorious Revolution, in the Kingdom of Great Britain, the monarch, in theory, chaired cabinet and chose ministers. In practice, King George Is inability to speak English led the responsibility for chairing cabinet to go to the minister, literally the prime or first minister. By the nineteenth century, the Great Reform Act of 1832 led to parliamentary dominance, with its choice invariably deciding who was prime minister, hence the use of phrases like Her Majestys government or His Excellencys government. Nineteenth century urbanisation, industrial revolution and, modernism had already fueled the political struggle for democracy. In the radicalised times at the end of World War I, a parliamentary system may be either bicameral, with two chambers of parliament or unicameral, with just one parliamentary chamber. Scholars of democracy such as Arend Lijphart distinguish two types of parliamentary democracies, the Westminster and Consensus systems, the Westminster system is usually found in the Commonwealth of Nations and countries which were influenced by the British political tradition. These parliaments tend to have a more style of debate. The Australian House of Representatives is elected using instant-runoff voting, while the Senate is elected using proportional representation through single transferable vote, regardless of which system is used, the voting systems tend to allow the voter to vote for a named candidate rather than a closed list. The Western European parliamentary model tends to have a more consensual debating system, Consensus systems have more of a tendency to use proportional representation with open party lists than the Westminster Model legislatures. The committees of these Parliaments tend to be more important than the plenary chamber, some West European countries parliaments implement the principle of dualism as a form of separation of powers. In countries using this system, Members of Parliament have to resign their place in Parliament upon being appointed minister, ministers in those countries usually actively participate in parliamentary debates, but are not entitled to vote. Some countries such as India also require the prime minister to be a member of the legislature, the head of state appoints a prime minister who will likely have majority support in parliament. The head of state appoints a minister who must gain a vote of confidence within a set time. The head of state appoints the leader of the party holding a plurality of seats in parliament as prime minister
10.
Constitutional monarchy
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A constitutional monarchy is a form of monarchy in which the sovereign exercises their authorities in accordance with a written or unwritten constitution. A constitutional monarchy may refer to a system in which the acts as a non-party political head of state under the constitution. Political scientist Vernon Bogdanor, paraphrasing Thomas Macaulay, has defined a constitutional monarch as a sovereign who reigns, in addition to acting as a visible symbol of national unity, a constitutional monarch may hold formal powers such as dissolving parliament or giving royal assent to legislation. Many constitutional monarchies still retain significant authorities or political influence however, such as through certain reserve powers, the United Kingdom and the other Commonwealth realms are all constitutional monarchies in the Westminster tradition of constitutional governance. Three states – Malaysia, Cambodia and the Holy See – are elective monarchies, the oldest constitutional monarchy dating back to ancient times was that of the Hittites. These were scattered noble families that worked as representatives of their subjects in an adjutant or subaltern federal-type landscape, the most recent country to move from an absolute monarchy to a constitutional monarchy was Bhutan, between 2007 and 2008. At the same time, in Scotland the Convention of Estates enacted the Claim of Right Act 1689, although Queen Anne was the last monarch to veto an Act of Parliament when in 1707 she blocked the Scottish Militia Bill, Hanoverian monarchs continued to selectively dictate government policies. For instance George III constantly blocked Catholic Emancipation, eventually precipitating the resignation of William Pitt the Younger as Prime Minister in 1801, Queen Victoria was the last monarch to exercise real personal power but this diminished over the course of her reign. In 1839 she became the last sovereign to keep a Prime Minister in power against the will of Parliament when the Bedchamber crisis resulted in the retention of Lord Melbournes administration, today, the role of the British monarch is by convention effectively ceremonial. No person may accept significant public office without swearing an oath of allegiance to the Queen, with few exceptions, the monarch is bound by constitutional convention to act on the advice of the Government. Constitutional monarchy also occurred briefly in the years of the French Revolution. As originally conceived, a monarch was head of the executive branch and quite a powerful figure even though his or her power was limited by the constitution. In many cases the monarchs, while still at the top of the political and social hierarchy, were given the status of servants of the people to reflect the new. In the course of Frances July Monarchy, Louis-Philippe I was styled King of the French rather than King of France, following the Unification of Germany, Otto von Bismarck rejected the British model. However this model of constitutional monarchy was discredited and abolished following Germanys defeat in the First World War. Later, Fascist Italy could also be considered as a constitutional monarchy and this eventually discredited the Italian monarchy and led to its abolition in 1946. After the Second World War, surviving European monarchies almost invariably adopted some variant of the constitutional monarchy model originally developed in Britain, nowadays a parliamentary democracy that is a constitutional monarchy is considered to differ from one that is a republic only in detail rather than in substance. However, three important factors distinguish monarchies such as the United Kingdom from systems where greater power might otherwise rest with Parliament, other privileges may be nominal or ceremonial
11.
Elizabeth II
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Elizabeth II has been Queen of the United Kingdom, Canada, Australia, and New Zealand since 6 February 1952. Elizabeth was born in London as the eldest child of the Duke and Duchess of York, later King George VI and Queen Elizabeth and her father acceded to the throne on the abdication of his brother Edward VIII in 1936, from which time she was the heir presumptive. She began to undertake duties during the Second World War. Elizabeths many historic visits and meetings include a visit to the Republic of Ireland. She has seen major changes, such as devolution in the United Kingdom, Canadian patriation. She has reigned through various wars and conflicts involving many of her realms and she is the worlds oldest reigning monarch as well as Britains longest-lived. In October 2016, she became the longest currently reigning monarch, in 2017 she became the first British monarch to commemorate a Sapphire Jubilee. Elizabeth has occasionally faced republican sentiments and press criticism of the family, however, support for the monarchy remains high. Elizabeth was born at 02,40 on 21 April 1926, during the reign of her paternal grandfather and her father, Prince Albert, Duke of York, was the second son of the King. Her mother, Elizabeth, Duchess of York, was the youngest daughter of Scottish aristocrat Claude Bowes-Lyon, 14th Earl of Strathmore and she was delivered by Caesarean section at her maternal grandfathers London house,17 Bruton Street, Mayfair. Elizabeths only sibling, Princess Margaret, was born in 1930, the two princesses were educated at home under the supervision of their mother and their governess, Marion Crawford, who was casually known as Crawfie. Lessons concentrated on history, language, literature and music, Crawford published a biography of Elizabeth and Margarets childhood years entitled The Little Princesses in 1950, much to the dismay of the royal family. The book describes Elizabeths love of horses and dogs, her orderliness, others echoed such observations, Winston Churchill described Elizabeth when she was two as a character. She has an air of authority and reflectiveness astonishing in an infant and her cousin Margaret Rhodes described her as a jolly little girl, but fundamentally sensible and well-behaved. During her grandfathers reign, Elizabeth was third in the line of succession to the throne, behind her uncle Edward, Prince of Wales, and her father, the Duke of York. Although her birth generated public interest, she was not expected to become queen, many people believed that he would marry and have children of his own. When her grandfather died in 1936 and her uncle succeeded as Edward VIII, she became second-in-line to the throne, later that year, Edward abdicated, after his proposed marriage to divorced socialite Wallis Simpson provoked a constitutional crisis. Consequently, Elizabeths father became king, and she became heir presumptive, if her parents had had a later son, she would have lost her position as first-in-line, as her brother would have been heir apparent and above her in the line of succession
12.
Governor-General of New Zealand
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The Governor-General of New Zealand is the viceregal representative of the monarch of New Zealand, currently Queen Elizabeth II. The office is mandated by letters patent and the officeholder is formally titled the Governor-General, when travelling abroad, the governor-general is seen as the representative of New Zealand, and of the Queen of New Zealand. For this reason, the governor-general is viewed by some as the de facto head of state, under the Niue Constitution Act, the governor-general also represents the monarch in Niue. The governor-general initially represented the British monarch and the government of the United Kingdom, therefore, many officeholders have been British statesmen. In 1972, Sir Denis Blundell became the first New Zealand resident to be appointed to the office, governors-general are not appointed for a specific term, but are generally expected to serve for five years. The current Governor-General is Dame Patsy Reddy, who has served since 28 September 2016, administrative support for the governor-general is provided by the Department of the Prime Minister and Cabinet. Appointment to the Office is made by the Queen on the advice of the Prime Minister of New Zealand, the Prime Ministers advice has sometimes been the result of a decision by Cabinet, although there is no requirement for this. The appointment of Anand Satyanand met with the approval of every leader in the House of Representatives, by convention the Leader of the Opposition is also consulted on the appointment, however this too has not always been the case. This suggestion was in turn criticised by the Government, as Sir Edmund had backed Labour in 1975 as part of the Citizens for Rowling campaign, however, the right granted by the convention was not exercised directly by a New Zealand Prime Minister until 1967. Although non-partisan while in office, there have been a number of appointments of Governors-General to the office that have attracted considerable controversy, despite their political backgrounds, neither of these appointments could be said to have discharged their duties in a partisan way. There has often been speculation that a member of the Royal Family might take up the position, before the Governor-General enters office, his or her commission of appointment is publicly read in the presence of the Chief Justice of New Zealand and the members of the Executive Council. The Governor-General must take the Oath of Allegiance and the oath for the due execution of the office, from time to time, there have been proposals to elect the Governor-General. When first drafted by then Governor George Grey, the New Zealand Constitution Act 1852 contained provision for the Governor to be elected by New Zealands Parliament. This provision was removed from the enactment, probably because the Colonial Office wanted to keep a check on New Zealands colonial government. In 1887 Sir George Grey, by then also a former Premier, the Bill was narrowly defeated 46–48, being opposed by the government of Harry Atkinson. In 2006 political commentator Colin James suggested that the Governor-General could be elected by a 60% majority of votes cast in Parliament, James argued that the New Zealand public should be given the ability to choose the Queens representative, and that the current system is undemocratic and not transparent. National MP Nikki Kaye queried whether several one-member parties in parliament could veto the decision, the Republican Movement responded that the method would ensure appointments were made that most MPs and parties found acceptable. The Governor-General holds office at the pleasure of the Queen, under clause II of the Letters Patent
13.
Toke Talagi
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Sir Toke Tufukia Talagi KNZM is the current premier of Niue. He was elected premier by the Niue Assembly on 19 June 2008, defeating the standing premier Young Vivian by fourteen votes to five and he is the current Foreign Minister of Niue. Talagi has been, at times, deputy prime minister, minister of Finance. He was re-elected easily in 2008, there are no political parties in Niue, Talagi is therefore an independent. Talagi is also president of the Niue Rugby Union, in 2008, he was elected chair of the Pacific Islands Forum. In May 2009, Talagi co-chaired the 5th Pacific Alliance Leaders Meeting with then Japanese Prime Minister Taro Aso in Hokkaido, in March 2017, Toke made the announcement he would run in that years election and for a fourth term as premier. In the 2017 New Year Honours, Talagi was appointed Knight Companion of the New Zealand Order of Merit
14.
Niue Assembly
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The Niue Assembly is the legislature of Niue. It consists of 20 members,14 representatives of the villages and 6 elected on a common roll, members are directly elected by universal suffrage, and serve a three-year term. Niue follows the Westminster system of government, with the Premier elected by the Assembly, the Assembly is descended from the Island Council established under the Cook Islands Act 1915. This was disbanded in 1959 and reconstituted as the Assembly, which was granted greater control. The Assembly assumed full law-making power within the constitution upon self-government in 1974, the Assembly is physically located in Alofi. The Assembly is presided over by a Speaker, elected by its members from outside their ranks, if a member of the Assembly is elected Speaker, they must resign their seat. The Speaker does not vote in proceedings, and does not enjoy a casting vote, the current Speaker is Togiavalu Pihigia. Elections are held under a plurality system, with electors in the fourteen villages electing one member per village by majority vote. Electors must be New Zealand citizens, resident for at least three months, and candidates must have been electors, resident for twelve months, the Assembly is currently in its 14th term. The 14th Assembly was elected at the 2011 elections, the power of the Assembly to pass legislation is circumscribed by the constitution. Any member may introduce a bill, but the Assembly may not proceed on bills dealing with financial matters without the consent of the Premier, a bill becomes law when passed by the Assembly and certified by the Speaker. List of Speakers of the Niue Assembly
15.
Niue Constitution Act 1974 (NZ)
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The Schedules of the Niue Constitution Act 1974 form the Niue constitution. It stipulates the make-up of the branch of the government, the legislative branch. The Niue Constitution Act 1974 is the law of Niue. Its granting by the New Zealand Parliament in 1974 is celebrated yearly as Niues independence on Constitution Day on 19 October, the road towards self-government for Niue started with the UN Decolonisation Committee putting pressure on New Zealand for Niue to decide what form of status Niue wanted. The people of Niue voted in 1974 choosing the self-government option as the best direction for Niue, the Niue Constitution is the legal doctrine that put the wishes of the Niue people for self-government into practice. The Niue Constitution requires 2/3 majority in the three readings in the Legislative Assembly and also requires 2/3 support from the electors before it can be amended. There is a committee that have been working on reviewing the constitution but have made little progress. The Niue Constitution Act 1974 is available at the legislation. govt. nz site, New Zealand Statutes at legislation. govt. nz site Niue Constitution Act 1974 Niue Constitution Act 1974 at the University of the South Pacific Law School web site in Vanuatu
16.
Geography of Niue
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Niue is a small island in the South Pacific Ocean, to the east of Tonga. It has an area of 260 square kilometres, and a coastline of 64 km and it claims an exclusive economic zone of 200 nm, and a territorial sea of 12 nm. It is one of worlds largest coral islands, niues climate is tropical, modified by south-east trade winds. The terrain consists of coastal cliffs made from limestone and a central plateau. The lowest point is at sea level, and the highest is a point near Mutalau settlement. The islands natural resources are fish and arable land, Niue is a party to the following international agreements regarding the environment, Biodiversity, Climate Change, Climate Change-Kyoto Protocol, Desertification. Niue has signed but not ratified the Law of the Sea agreement, Niue has signed a treaty with the United States in which the parties delimited the east–west maritime boundary between Niue and American Samoa. Niue is south of American Samoa and this is a list of the extreme points of Niue, the points that are farther north, south, east or west than any other location. Northernmost point – unnamed headland north-west of Uluvehi Easternmost point – unnamed headland south-east of Liku Southernmost point – Limufuafua Point Westernmost point - Halagigie Point
17.
Niue
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Niue is an island country in the South Pacific Ocean,2,400 kilometres northeast of New Zealand, and east of Tonga, south of Samoa and west of the Cook Islands. Its land area is 260 square kilometres and its population, predominantly Polynesian, is around 1,612 as of November 2016 and they commonly refer to the island as The Rock, a reference to the traditional name Rock of Polynesia. Niue, whose capital is the village of Alofi, is a state in free association with New Zealand. Niueans are citizens of New Zealand, and Queen Elizabeth II is head of state in her capacity as Queen of New Zealand, between 90–95% of Niuean people live in New Zealand, along with about 70% of the speakers of the Niuean language. A bilingual country, over 30% speak both Niuean and English, though the percentage of monolingual English-speaking people is only 11%, while 46% are monolingual Niuean speakers, Rugby is the most played sport in Niue. In October 2016, Niue officially declared that all its debt was paid off. Niue is not a member of the United Nations, but UN organisations have accepted its status as a state as equivalent to independence for the purposes of international law. As such, Niue is a member of some UN specialised agencies, and is invited, alongside the other non-UN member state. Niue is subdivided into 14 villages, each village has a village council that elects its chairman. The villages are at the same electoral districts. Each village sends an assemblyman to the Parliament of Niue, in 2003, Niue became the first country in the world to offer free wireless internet to all its inhabitants. Niue Island Organic Farmers Association is currently paving way to an MEA committed to making Niue the worlds first fully organic nation, a leader in green growth, Niue is also transitioning to solar power, with help from the European Union. In 2015, Niue started providing phone landlines to all of its inhabitants, in 2008, Niue became the first country in the world where laptops are provided to all its school students. A highly democratic nation, Niueans enjoy high freedom, with elections every 3 years, there are no political parties in Niue, all are independents. The last political party, Niue Peoples Party, won once, in January 2004, Niue was hit by Cyclone Heta, which caused extensive damage to the entire island, including wiping out most of the south of the capital, Alofi. The disaster set the island back about two years from its planned timeline to implement the Niue Integrated Strategic Plan, since national efforts concentrated on recovery, in 2008, Niue had yet to fully recover. Niue is one of the worlds largest coral islands, the terrain consists of steep limestone cliffs along the coast with a central plateau rising to about 60 metres above sea level. A coral reef surrounds the island, with the only break in the reef being in the central western coast, close to the capital
18.
Gross domestic product
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Gross Domestic Product is a monetary measure of the market value of all final goods and services produced in a period. Nominal GDP estimates are used to determine the economic performance of a whole country or region. The OECD defines GDP as a measure of production equal to the sum of the gross values added of all resident and institutional units engaged in production. ”An IMF publication states that GDP measures the monetary value of final goods and services - that is. Total GDP can also be broken down into the contribution of industry or sector of the economy. The ratio of GDP to the population of the region is the per capita GDP. William Petty came up with a concept of GDP to defend landlords against unfair taxation during warfare between the Dutch and the English between 1652 and 1674. Charles Davenant developed the method further in 1695, the modern concept of GDP was first developed by Simon Kuznets for a US Congress report in 1934. In this report, Kuznets warned against its use as a measure of welfare, after the Bretton Woods conference in 1944, GDP became the main tool for measuring a countrys economy. The switch from GNP to GDP in the US was in 1991, the history of the concept of GDP should be distinguished from the history of changes in ways of estimating it. The value added by firms is relatively easy to calculate from their accounts, but the value added by the sector, by financial industries. GDP can be determined in three ways, all of which should, in principle, give the same result and they are the production approach, the income approach, or the expenditure approach. The most direct of the three is the approach, which sums the outputs of every class of enterprise to arrive at the total. The income approach works on the principle that the incomes of the factors must be equal to the value of their product. This approach mirrors the OECD definition given above, deduct intermediate consumption from gross value to obtain the gross value added. Gross value added = gross value of output – value of intermediate consumption, value of output = value of the total sales of goods and services plus value of changes in the inventories. The sum of the value added in the various economic activities is known as GDP at factor cost. GDP at factor cost plus indirect taxes less subsidies on products = GDP at producer price, for measuring output of domestic product, economic activities are classified into various sectors. Subtracting each sectors intermediate consumption from gross output gives the GDP at factor cost, adding indirect tax minus subsidies in GDP at factor cost gives the GDP at producer prices
19.
Purchasing power parity
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Observed deviations of the exchange rate from purchasing power parity are measured by deviations of the real exchange rate from its PPP value of 1. PPP exchange rates help to minimize misleading international comparisons that can arise with the use of exchange rates. For example, suppose that two countries produce the same amounts of goods as each other in each of two different years. But if one countrys GDP is converted into the countrys currency using PPP exchange rates instead of observed market exchange rates. The idea originated with the School of Salamanca in the 16th century, the best-known purchasing power adjustment is the Geary–Khamis dollar. The real exchange rate is equal to the nominal exchange rate. If purchasing power parity held exactly, then the exchange rate would always equal one. However, in practice the exchange rates exhibit both short run and long run deviations from this value, for example due to reasons illuminated in the Balassa–Samuelson theorem. There can be marked differences between purchasing power adjusted incomes and those converted via market exchange rates. This discrepancy has large implications, for instance, when converted via the exchange rates GDP per capita in India is about US$1,965 while on a PPP basis it is about US$7,197. At the other extreme, Denmarks nominal GDP per capita is around US$62,100, the purchasing power parity exchange rate serves two main functions. PPP exchange rates can be useful for making comparisons between countries because they stay fairly constant from day to day or week to week and only change modestly, if at all, from year to year. The PPP exchange-rate calculation is controversial because of the difficulties of finding comparable baskets of goods to compare purchasing power across countries, people in different countries typically consume different baskets of goods. It is necessary to compare the cost of baskets of goods and this is a difficult task because purchasing patterns and even the goods available to purchase differ across countries. Thus, it is necessary to make adjustments for differences in the quality of goods, furthermore, the basket of goods representative of one economy will vary from that of another, Americans eat more bread, Chinese more rice. Hence a PPP calculated using the US consumption as a base will differ from that calculated using China as a base, additional statistical difficulties arise with multilateral comparisons when more than two countries are to be compared. Various ways of averaging bilateral PPPs can provide a stable multilateral comparison. These are all issues of indexing, as with other price indices there is no way to reduce complexity to a single number that is equally satisfying for all purposes
20.
New Zealand dollar
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The New Zealand dollar is the currency and legal tender of New Zealand, the Cook Islands, Niue, the Ross Dependency, Tokelau, and a British territory, the Pitcairn Islands. Within New Zealand, it is almost always abbreviated with the dollar sign, in the context of currency trading, it is often informally called the Kiwi, since New Zealand is commonly associated with the indigenous bird and the $1 coin depicts a kiwi. Introduced in 1967, the dollar is subdivided into 100 cents, altogether there are ten denominations—five coins and five banknotes—with the smallest being the 10-cent coin. Formerly there were lower denominations, but those were discontinued due to inflation, the New Zealand dollar is consistently one of the 10 most-traded currencies in the world, being approximately 2. 0% of global foreign exchange market daily turnover in 2013. Prior to the introduction of the New Zealand dollar in 1967, the New Zealand pound was the currency of New Zealand, which had been distinct from the pound sterling since 1933. The pound used the £sd system, in which the pound was divided into 20 shillings and one shilling was divided into 12 pence, switching to decimal currency had been proposed in New Zealand since the 1930s, although only in the 1950s did any plans come to fruition. In 1957, a committee was set up by the Government to investigate decimal currency, the idea fell on fertile ground, and in 1963, the Government decided to decimalise New Zealand currency. The Decimal Currency Act was passed in 1964, setting the date of transition to 10 July 1967, words such as fern, kiwi and zeal were proposed to avoid confusion with the word dollar, which many people at the time associated with the United States dollar. In the end, the dollar was chosen anyway. On Monday 10 July 1967, the New Zealand dollar was introduced to replace the pound at a rate of two dollars to one pound, some 27 million new banknotes were printed and 165 million new coins were minted for the changeover. The New Zealand dollar was pegged to the US dollar at US$1.43 = NZ$1. This rate changed on 21 November of the year to US$1.12 = NZ$1 after the devaluation of the British pound. In 1971 the US devalued its dollar relative to gold, leading New Zealand on 23 December to peg its dollar at US$1.216 with a 4. 5% fluctuation range, keeping the same gold value. From 9 July 1973 to 4 March 1985 the dollars value was determined from a basket of currencies. The NZ$ was floated on 4 March 1985 at the rate of US$0.4444. Since then the value has been determined by the financial markets. The dollars post-float minimum average daily value was US$0.3922 on 22 November 2000, much of this medium-term variation in the exchange rate has been attributed to differences in interest rates. The New Zealand dollars value is often affected by currency trading
21.
ISO 4217
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The ISO4217 code list is used in banking and business globally. ISO4217 codes are used on tickets and international train tickets to remove any ambiguity about the price. The first two letters of the code are the two letters of the ISO 3166-1 alpha-2 country codes and the third is usually the initial of the currency itself, so Japans currency code is JPY—JP for Japan and Y for yen. This eliminates the problem caused by the dollar, franc, peso and pound being used in dozens of different countries. Also, if a currency is revalued, the currency codes last letter is changed to distinguish it from the old currency. Other changes can be seen, however, the Russian ruble, for example, changed from RUR to RUB and these currency units are denominated as one troy ounce of the specified metal as opposed to USD1 or EUR1. The code XTS is reserved for use in testing, the code XXX is used to denote a transaction involving no currency. There are also codes specifying certain monetary instruments used in international finance, the codes for most supranational currencies, such as the East Caribbean dollar, the CFP franc, the CFA franc BEAC and the CFA franc BCEAO. The predecessor to the euro, the European Currency Unit, had the code XEU, the use of an initial letter X for these purposes is facilitated by the ISO3166 rule that no official country code beginning with X will ever be assigned. Because of this rule ISO4217 can use X codes without risk of clashing with a country code. ISO3166 country codes beginning with X are used for private custom use, consequently, ISO4217 can use X codes for non-country-specific currencies without risk of clashing with future country codes. The inclusion of EU in the ISO 3166-1 reserved codes list, the ISO4217 standard includes a crude mechanism for expressing the relationship between a major currency unit and its corresponding minor currency unit. This mechanism is called the exponent and assumes a base of 10. For example, USD is equal to 100 of its currency unit the cent. So the USD has exponent 2, the code JPY is given the exponent 0, because its minor unit, the sen, although nominally valued at 1/100 of a yen, is of such negligible value that it is no longer used. Usually, as with the USD, the currency unit has a value that is 1/100 of the major unit, but in some cases 1/1000 is used. Mauritania does not use a decimal division of units, setting 1 ouguiya equal to 5 khoums, some currencies do not have any minor currency unit at all and these are given an exponent of 0, as with currencies whose minor units are unused due to negligible value. There is also a code number assigned to each currency
22.
Coordinated Universal Time
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Coordinated Universal Time, abbreviated to UTC, is the primary time standard by which the world regulates clocks and time. It is within about 1 second of mean time at 0° longitude. It is one of closely related successors to Greenwich Mean Time. For most purposes, UTC is considered interchangeable with GMT, the first Coordinated Universal Time was informally adopted on 1 January 1960. This change also adopted leap seconds to simplify future adjustments, a number of proposals have been made to replace UTC with a new system that would eliminate leap seconds, but no consensus has yet been reached. Leap seconds are inserted as necessary to keep UTC within 0.9 seconds of universal time, see the Current number of leap seconds section for the number of leap seconds inserted to date. The official abbreviation for Coordinated Universal Time is UTC and this abbreviation arose from a desire by the International Telecommunication Union and the International Astronomical Union to use the same abbreviation in all languages. English speakers originally proposed CUT, while French speakers proposed TUC, the compromise that emerged was UTC, which conforms to the pattern for the abbreviations of the variants of Universal Time. Time zones around the world are expressed using positive or negative offsets from UTC, the westernmost time zone uses UTC−12, being twelve hours behind UTC, the easternmost time zone, theoretically, uses UTC+12, being twelve hours ahead of UTC. In 1995, the nation of Kiribati moved those of its atolls in the Line Islands from UTC-10 to UTC+14 so that the country would all be on the same day. UTC is used in internet and World Wide Web standards. The Network Time Protocol, designed to synchronise the clocks of computers over the internet, computer servers, online services and other entities that rely on having a universally accepted time use UTC as it is more specific than GMT. If only limited precision is needed, clients can obtain the current UTC from a number of official internet UTC servers, for sub-microsecond precision, clients can obtain the time from satellite signals. UTC is also the standard used in aviation, e. g. for flight plans. Weather forecasts and maps all use UTC to avoid confusion about time zones, the International Space Station also uses UTC as a time standard. Amateur radio operators often schedule their radio contacts in UTC, because transmissions on some frequencies can be picked up by many time zones, UTC is also used in digital tachographs used on large goods vehicles under EU and AETR rules. UTC divides time into days, hours, minutes and seconds, days are conventionally identified using the Gregorian calendar, but Julian day numbers can also be used. Each day contains 24 hours and each hour contains 60 minutes, the number of seconds in a minute is usually 60, but with an occasional leap second, it may be 61 or 59 instead
23.
Left- and right-hand traffic
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This is so fundamental to traffic flow that it is sometimes referred to as the rule of the road. About two-thirds of the population use RHT, with the remaining 76 countries and territories using LHT. Countries that use LHT account for about a sixth of the worlds area, in the early 1900s some countries including Canada, Spain, and Brazil had different rules in different parts of the country. During the 1900s many countries standardised within their jurisdictions, and changed from LHT to RHT, in 1919,104 of the worlds territories were LHT and an equal number were RHT. From 1919 to 1986,34 of the LHT territories switched to RHT, many of the countries with LHT are former British colonies in the Caribbean, Southern Africa, Southeast Asia, Australia, and New Zealand. Japan, Thailand, Nepal, Bhutan, Mozambique, Suriname, East Timor, in Europe, only four countries still drive on the left, the United Kingdom, Ireland, Malta, and Cyprus, all of which are islands. Nearly all countries use one side or the other throughout their entire territory, most exceptions are due to historical considerations and involve islands with no road connection to the main part of a country. China is RHT except the Special Administrative Regions of China of Hong Kong, the United States is RHT except the United States Virgin Islands. The United Kingdom is LHT, but its overseas territories of Gibraltar, according to the International Regulations for Preventing Collisions at Sea, water traffic is RHT. For aircraft the US Federal Aviation Regulations provide for passing on the right, light rail vehicles generally operate on the same side as other road traffic in the country. Many countries use RHT for automobiles but LHT for trains, often because of the influence of the British on early railway systems, in some countries rail traffic remained LHT after automobile traffic switched to RHT, for example in China, Brazil, and Argentina. However, France, Belgium, and Switzerland have used RHT for automobiles since their introduction, there is no technical reason to prefer one side over the other. Ancient Greek, Egyptian, and Roman troops kept to the left when marching, in 1998, archaeologists found a well-preserved double track leading to a Roman quarry near Swindon. The first reference in English law to an order for LHT was in 1756, northcote Parkinson, believed that ancient travellers on horseback or on foot generally kept to the left, since most people were right handed. If two men riding on horseback were to start a fight, each would edge toward the left, in the year 1300, Pope Boniface VIII directed pilgrims to keep left. In the late 1700s, traffic in the United States was RHT based on use of large freight wagons pulled by several pairs of horses. The wagons had no seat, so a postilion sat on the left rear horse. Seated on the left, the driver preferred that other wagons pass him on the left so that he could be sure to keep clear of the wheels of oncoming wagons, in France, traditionally foot traffic had kept right, while carriage traffic kept left
24.
.nu
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. nu is the Internet country code top-level domain assigned to the island state of Niue. It was one of the first ccTLDs to be marketed to the Internet at large as an alternative to the gTLDs. com. net, and. org. Playing on the similarity between nu and new, it was promoted as a new TLD in which there was an abundance of good domain names available. As of September 2,2013. SE has assumed responsibility for administration, the. nu domain is particularly popular in Sweden, Denmark, the Netherlands and Belgium, as nu is the word for now in Swedish, Danish and Dutch - an example of a domain hack. Nu is also an archaic adverb meaning now in Norwegian, but nå is the frequently used word. In March 2000. NU Domain Ltd became the first TLD to offer registration of Internationalized domain names, a few days later the site also had its domain name revoked by domain registrar Nunames. The domain revocation was recorded in screenshots taken at the time, Domain names can be as short as one character. In June,2008. NU Domain began permitting registration of domain names. A2005 UDRP case regarding nudomain. com made the assertion under Factual background that The Complainants own, the case does, however, point out that these companies own a registered trademark to. nudomain in several countries. In March 2007, McAfee SiteAdvisor issued a report explaining the functionality of SiteAdvisor, as part of that report. nu domain websites were stated to be among the highest-risk TLDs for browser exploits. However, in most other respects. nu sites were ranked overall as a low to moderate risk, shortly thereafter. NU Domain issued a press release stating that SiteAdvisor had ranked. nu sites among the lowest for risk. In 2008 McAfee reported that. net and. com had become the riskiest TLDs, IANA WHOIS record for. nu IUSN Foundation IUSNs WiFi Nation Internet Niue Niue is dead. The Register Official website of the government of Niue
25.
Fixed exchange-rate system
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There are benefits and risks to using a fixed exchange rate. In doing so, the rate between the currency and its peg does not change based on market conditions, the way floating currencies do. A fixed exchange-rate system can also be used as a means to control the behavior of a currency, however, in doing so, the pegged currency is then controlled by its reference value. In other words, a currency is dependent on its reference value to dictate how its current worth is defined at any given time. The central bank provides the assets and/or the foreign currency or currencies which are needed in order to any payments imbalances. In the 21st century, the associated with large economies typically do not fix or peg exchange rates to other currencies. The last large economy to use a fixed exchange system was the Peoples Republic of China which, in July 2005. The European Exchange Rate Mechanism is also used on a basis to establish a final conversion rate against the Euro from the local currencies of countries joining the Eurozone. The gold standard or gold standard of fixed exchange rates prevailed from about 1870 to 1914. The period between the two wars was transitory, with the Bretton Woods system emerging as the new fixed exchange rate regime in the aftermath of World War II. It was formed with an intent to rebuild war-ravaged nations after World War II through a series of currency stabilization programs, the early 1970s saw the breakdown of the system and its replacement by a mixture of fluctuating and fixed exchange rates. Timeline of the exchange rate system, The earliest establishment of a gold standard was in the United Kingdom in 1821 followed by Australia in 1852. Under this system, the value of all currencies was denominated in terms of gold with central banks ready to buy. Each central bank maintained gold reserves as their official reserve asset, for example, during the “classical” gold standard period, the U. S. dollar was defined as 0.048 troy oz. of pure gold. Following the Second World War, the Bretton Woods system replaced gold with the U. S. dollar as the reserve asset. The regime intended to combine binding legal obligations with multilateral decision-making through the International Monetary Fund, the rules of this system were set forth in the articles of agreement of the IMF and the International Bank for Reconstruction and Development. S. Dollar and to exchange rates within 1% of parity by intervening in their foreign exchange markets. In December 1971, the Smithsonian Agreement paved the way for the increase in the value of the price of gold from US$35.50 to US$38 an ounce
26.
Coin collecting
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Coin collecting is the collecting of coins or other forms of minted legal tender. Coins of interest to collectors often include those that circulated for only a time, coins with mint errors. Coin collecting can be differentiated from numismatics, in that the latter is the study of currency. Though closely related, the two disciplines are not necessarily the same, a numismatist may or may not be a coin collector, and vice versa. A coins grade is a determinant of its value. For a tiered fee, a third party service like PCGS or NGC will grade, authenticate, attribute. Over 80 million coins have been certified by the four largest services, people have hoarded coins for their bullion value for as long as coins have been minted. However, the collection of coins for their value was a later development. Evidence from the archaeological and historical record of Ancient Rome and medieval Mesopotamia indicates that coins were collected and catalogued by scholars and it also seems probable that individual citizens collected old, exotic or commemorative coins as an affordable, portable form of art. Contemporary coin collecting and appreciation began around the fourteenth century, during the Renaissance, it became a fad among some members of the privileged classes, especially kings and queens. The Italian scholar and poet Petrarch is credited with being the pursuits first and most famous aficionado, following his lead, many European kings, princes, and other nobility kept collections of ancient coins. Perhaps because only the wealthy could afford the pursuit, in Renaissance times coin collecting became known as the Hobby of Kings. During the 17th and 18th centuries coin collecting remained a pursuit of the well-to-do, but rational, Enlightenment thinking led to a more systematic approach to accumulation and study. During the 19th and 20th centuries, coin collecting increased further in popularity, the market for coins expanded to include not only antique coins, but foreign or otherwise exotic currency. Coin shows, trade associations, and regulatory bodies emerged during these decades, as one of the oldest and most popular world pastimes, coin collecting is now often referred to as the King of Hobbies. The motivations for collecting are varied, possibly the most common type of collector is the hobbyist, who amasses a collection purely for fun with no real expectation of profit. This is especially true of casual collectors and children who collect items on the basis of chance, another frequent reason for purchasing coins is as an investment. As with stamps, precious metals or other commodities, coin prices are based on supply
27.
Island country
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An island country is a country whose primary territory consists of one or more islands or parts of islands. As of 2011,46 of the 193 UN member states are island countries, the percentage of island countries that are democratic is higher than that of continental countries. Historically they have been prone to political stability than their continental counterparts. Island countries have often been the basis of maritime conquest and historical rivalry between other countries, Island countries are more susceptible to attack by large, continental countries due to their size and dependence on sea and air lines of communication. Many island countries are vulnerable to predation by mercenaries and other foreign invaders. Many island countries rely heavily on fish for their supply of food. Some are turning to renewable energy—such as wind power, hydropower, geothermal power, some island countries are more affected than other countries by climate change, which produces problems such as reduced land use, water scarcity and sometimes even resettlement issues. Some low-lying island countries are slowly being submerged by the water levels of the Pacific Ocean. Climate change also impacts island countries by causing natural disasters such as cyclones, hurricanes, flash floods. In 2011, the Center for Climate Change Law held a conference attended by 272 registrants from 39 island nations titled Legal Issues for Threatened Island Nations, many island countries rely heavily on imports and are greatly affected by changes in the global economy. The dominant industry for many countries is tourism. Island countries are small with low populations, although some, like Indonesia. Some island countries are centred on one or two islands, such as the United Kingdom, Trinidad and Tobago, New Zealand, Cuba, Bahrain, Singapore, Malta. Others are spread out over hundreds or thousands of islands, such as Indonesia, the Philippines, Seychelles. Geographically, the country of Australia is considered a continental landmass rather than an island, in the past, however, it was considered an island country for tourism purposes and is still often referred to as such
28.
South Seas
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The Pacific Ocean is the largest and deepest of the Earths oceanic divisions. It extends from the Arctic Ocean in the north to the Southern Ocean in the south and is bounded by Asia and Australia in the west, the Mariana Trench in the western North Pacific is the deepest point in the world, reaching a depth of 10,911 metres. Both the center of the Water Hemisphere and the Western Hemisphere are in the Pacific Ocean, the oceans current name was coined by Portuguese explorer Ferdinand Magellan during the Spanish circumnavigation of the world in 1521, as he encountered favourable winds on reaching the ocean. He called it Mar Pacífico, which in both Portuguese and Spanish means peaceful sea, important human migrations occurred in the Pacific in prehistoric times. Long-distance trade developed all along the coast from Mozambique to Japan, trade, and therefore knowledge, extended to the Indonesian islands but apparently not Australia. By at least 878 when there was a significant Islamic settlement in Canton much of trade was controlled by Arabs or Muslims. In 219 BC Xu Fu sailed out into the Pacific searching for the elixir of immortality, from 1404 to 1433 Zheng He led expeditions into the Indian Ocean. The east side of the ocean was discovered by Spanish explorer Vasco Núñez de Balboa in 1513 after his expedition crossed the Isthmus of Panama and he named it Mar del Sur because the ocean was to the south of the coast of the isthmus where he first observed the Pacific. Later, Portuguese explorer Ferdinand Magellan sailed the Pacific East to West on a Castilian expedition of world circumnavigation starting in 1519, Magellan called the ocean Pacífico because, after sailing through the stormy seas off Cape Horn, the expedition found calm waters. The ocean was often called the Sea of Magellan in his honor until the eighteenth century, sailing around and east of the Moluccas, between 1525 and 1527, Portuguese expeditions discovered the Caroline Islands, the Aru Islands, and Papua New Guinea. In 1542–43 the Portuguese also reached Japan, in 1564, five Spanish ships consisting of 379 explorers crossed the ocean from Mexico led by Miguel López de Legazpi and sailed to the Philippines and Mariana Islands. The Manila galleons operated for two and a half centuries linking Manila and Acapulco, in one of the longest trade routes in history, Spanish expeditions also discovered Tuvalu, the Marquesas, the Cook Islands, the Solomon Islands, and the Admiralty Islands in the South Pacific. In the 16th and 17th century Spain considered the Pacific Ocean a Mare clausum—a sea closed to other naval powers, as the only known entrance from the Atlantic the Strait of Magellan was at times patrolled by fleets sent to prevent entrance of non-Spanish ships. On the western end of the Pacific Ocean the Dutch threatened the Spanish Philippines, Spain also sent expeditions to the Pacific Northwest reaching Vancouver Island in southern Canada, and Alaska. The French explored and settled Polynesia, and the British made three voyages with James Cook to the South Pacific and Australia, Hawaii, and the North American Pacific Northwest, one of the earliest voyages of scientific exploration was organized by Spain in the Malaspina Expedition of 1789–1794. It sailed vast areas of the Pacific, from Cape Horn to Alaska, Guam and the Philippines, New Zealand, Australia, and the South Pacific. Growing imperialism during the 19th century resulted in the occupation of much of Oceania by other European powers, and later, Japan, in Oceania, France got a leading position as imperial power after making Tahiti and New Caledonia protectorates in 1842 and 1853 respectively. After navy visits to Easter Island in 1875 and 1887, Chilean navy officer Policarpo Toro managed to negotiate an incorporation of the island into Chile with native Rapanui in 1888, by occupying Easter Island, Chile joined the imperial nations
29.
New Zealand
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New Zealand /njuːˈziːlənd/ is an island nation in the southwestern Pacific Ocean. The country geographically comprises two main landmasses—the North Island, or Te Ika-a-Māui, and the South Island, or Te Waipounamu—and around 600 smaller islands. New Zealand is situated some 1,500 kilometres east of Australia across the Tasman Sea and roughly 1,000 kilometres south of the Pacific island areas of New Caledonia, Fiji, because of its remoteness, it was one of the last lands to be settled by humans. During its long period of isolation, New Zealand developed a distinct biodiversity of animal, fungal, the countrys varied topography and its sharp mountain peaks, such as the Southern Alps, owe much to the tectonic uplift of land and volcanic eruptions. New Zealands capital city is Wellington, while its most populous city is Auckland, sometime between 1250 and 1300 CE, Polynesians settled in the islands that later were named New Zealand and developed a distinctive Māori culture. In 1642, Dutch explorer Abel Tasman became the first European to sight New Zealand, in 1840, representatives of Britain and Māori chiefs signed the Treaty of Waitangi, which declared British sovereignty over the islands. In 1841, New Zealand became a colony within the British Empire, today, the majority of New Zealands population of 4.7 million is of European descent, the indigenous Māori are the largest minority, followed by Asians and Pacific Islanders. Reflecting this, New Zealands culture is derived from Māori and early British settlers. The official languages are English, Māori and New Zealand Sign Language, New Zealand is a developed country and ranks highly in international comparisons of national performance, such as health, education, economic freedom and quality of life. Since the 1980s, New Zealand has transformed from an agrarian, Queen Elizabeth II is the countrys head of state and is represented by a governor-general. In addition, New Zealand is organised into 11 regional councils and 67 territorial authorities for local government purposes, the Realm of New Zealand also includes Tokelau, the Cook Islands and Niue, and the Ross Dependency, which is New Zealands territorial claim in Antarctica. New Zealand is a member of the United Nations, Commonwealth of Nations, ANZUS, Organisation for Economic Co-operation and Development, Pacific Islands Forum, and Asia-Pacific Economic Cooperation. Dutch explorer Abel Tasman sighted New Zealand in 1642 and called it Staten Landt, in 1645, Dutch cartographers renamed the land Nova Zeelandia after the Dutch province of Zeeland. British explorer James Cook subsequently anglicised the name to New Zealand, Aotearoa is the current Māori name for New Zealand. It is unknown whether Māori had a name for the country before the arrival of Europeans. Māori had several names for the two main islands, including Te Ika-a-Māui for the North Island and Te Waipounamu or Te Waka o Aoraki for the South Island. Early European maps labelled the islands North, Middle and South, in 1830, maps began to use North and South to distinguish the two largest islands and by 1907, this was the accepted norm. The New Zealand Geographic Board discovered in 2009 that the names of the North Island and South Island had never been formalised and this set the names as North Island or Te Ika-a-Māui, and South Island or Te Waipounamu
30.
Tonga
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Tonga, officially the Kingdom of Tonga, is a Polynesian sovereign state and archipelago comprising 169 islands of which 36 are inhabited. The total surface area is about 750 square kilometres scattered over 700,000 square kilometres of the southern Pacific Ocean and it has a population of 103,000 people of whom 70% reside on the main island of Tongatapu. Tonga stretches across approximately 800 kilometres in a north-south line and it is surrounded by Fiji and Wallis and Futuna to the northwest, Samoa to the northeast, Niue to the east, Kermadec to the southwest, and New Caledonia and Vanuatu to the farther west. Tonga became known in the West as the Friendly Islands because of the reception accorded to Captain James Cook on his first visit in 1773. He arrived at the time of the festival, the yearly donation of the First Fruits to the Tuʻi Tonga. According to the writer William Mariner, the wanted to kill Cook during the gathering. From 1900 to 1970, Tonga had British protected state status, the country never relinquished its sovereignty to any foreign power. In many Polynesian languages including Tongan, the word tonga means south, the name of Tonga is cognate to the Hawaiian region of Kona. In Malay, the name of Tonga is also cognate to the word Tenggara, an Austronesian-speaking group linked to the archaeological construct known as the Lapita cultural complex reached and inhabited Tonga around 1500–1000 BCE. Scholars have much debated the exact dates of the settlement of Tonga. Not much is known before European contact because of the lack of a writing system, in the 15th century and again in the 17th, civil war erupted. The Tongan people first encountered Europeans in 1616 when the Dutch vessel Eendracht, captained by Willem Schouten, later came other Dutch explorers, including Jacob Le Maire, and in 1643 Abel Tasman. In 1845, the young warrior, strategist, and orator Tāufaʻāhau united Tonga into a kingdom. He held the title of Tuʻi Kanokupolu, but had been baptised by Methodist missionaries with the name Siaosi in 1831. Tonga became a state under a Treaty of Friendship with Britain on 18 May 1900. The treaty posted no higher permanent representative on Tonga than a British Consul, under the protection of Britain, Tonga maintained its sovereignty, and remained the only Pacific nation to retain its monarchical government. The Tongan monarchy follows a succession of hereditary rulers from one family. The 1918 flu pandemic, brought to Tonga by a ship from New Zealand, killed 1,800 Tongans, the Treaty of Friendship and Tongas protection status ended in 1970 under arrangements established by Queen Salote Tupou III prior to her death in 1965
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Samoa
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The Independent State of Samoa, commonly known as Samoa and, until 1997, known as Western Samoa, is a unitary parliamentary democracy with eleven administrative divisions. The two main islands are Savaii and Upolu with four smaller islands surrounding the landmasses, the Lapita people discovered and settled the Samoan islands around 3,500 years ago. They developed a language and cultural identity. Samoa is a member of the Commonwealth of Nations, Western Samoa was admitted to the United Nations on 15 December 1976. The entire island group, which includes American Samoa, was called Navigator Islands by European explorers before the 20th century because of the Samoans seafaring skills. The oldest date so far for remains in Samoa has been calculated by New Zealand scientists to a true age of circa 3,000 years ago from a Lapita site at Mulifanua during the 1970s. The origins of the Samoans are closely studied in research about Polynesia in various scientific disciplines such as genetics, linguistics. Contact with Europeans began in the early 18th century, jacob Roggeveen, a Dutchman, was the first known European to sight the Samoan islands in 1722. This visit was followed by French explorer Louis-Antoine de Bougainville, who named them the Navigator Islands in 1768, contact was limited before the 1830s, which is when English missionaries and traders began arriving. Christian missionary work in Samoa began in 1830 by John Williams, of the London Missionary Society arriving in Sapapalii from The Cook Islands and Tahiti. However, Robert Louis Stevenson, who lived in Samoa from 1889 until his death in 1894, wrote in A Footnote to History, Eight Years of Trouble in Samoa, … the Samoans are gentle people. The Germans in particular began to show great commercial interest in the Samoan Islands, especially on the island of Upolu, the United States laid its own claim and formed alliances with local native chieftains, most conspicuously on the islands of Tutuila and Manua. Britain also sent troops to protect British business enterprise, harbour rights and this was followed by an eight-year civil war, during which each of the three powers supplied arms, training and in some cases combat troops to the warring Samoan parties. The Samoan crisis came to a critical juncture in March 1889 when all three colonial contenders sent warships into Apia harbour, and a larger-scale war seemed imminent, a massive storm on 15 March 1889 damaged or destroyed the warships, ending the military conflict. The Second Samoan Civil War reached a head in 1898 when Germany, the United Kingdom, the Siege of Apia occurred in March 1899. Samoan forces loyal to Prince Tanu were besieged by a force of Samoan rebels loyal to Mataafa Iosefo. Supporting Prince Tanu were landing parties from four British and American warships, after several days of fighting, the Samoan rebels were finally defeated. American and British warships shelled Apia on 15 March 1899, including the USS Philadelphia, the eastern island-group became a territory of the United States and was known as American Samoa
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Cook Islands
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The Cook Islands is a self-governing island country in the South Pacific Ocean in free association with New Zealand. It comprises 15 islands whose total area is 240 square kilometres. The Cook Islands Exclusive Economic Zone, however, covers 1,800,000 square kilometres of ocean, the Cook Islands defence and foreign affairs are the responsibility of New Zealand, but they are exercised in consultation with the Cook Islands. In recent times, the Cook Islands have adopted an independent foreign policy. Although Cook Islanders are citizens of New Zealand, they have the status of Cook Islands nationals, the Cook Islands main population centres are on the island of Rarotonga, where there is an international airport. There is a population of Cook Islanders in New Zealand. In the 2006 census,58,008 self-identified as being of ethnic Cook Islands Māori descent, the Cook Islands are in the South Pacific Ocean, northeast of New Zealand, between French Polynesia and American Samoa. There are 15 major islands spread over 2,200,000 km2 of ocean, the islands were formed by volcanic activity, the northern group is older and consists of six atolls, which are sunken volcanoes topped by coral growth. The climate is moderate to tropical, palmerston Island sometimes grouped with the Northern Group. Manuae Winslow Reef The Cook Islands were first settled in the 6th century by Polynesian people who migrated from Tahiti, in 1813 John Williams, a missionary on the Endeavour made the first recorded sighting of Rarotonga. The first recorded landing on Rarotonga by Europeans was in 1814 by the Cumberland, the islands saw no more Europeans until missionaries arrived from England in 1821. Christianity quickly took hold in the culture and many continue to be Christian believers today. The Cook Islands became a British protectorate in 1888, due largely to community fears that France might occupy the territory as it had Tahiti, on 6 September 1900, the leading islanders presented a petition asking that the islands should be annexed as British territory. These instruments did not include Aitutaki and it appears that, though the inhabitants regarded themselves as British subjects, the Crowns title was uncertain, and the island was formally annexed by Proclamation dated 9 October 1900. The islands were included within the boundaries of the Colony of New Zealand in 1901 by Order in Council under the Colonial Boundaries Act,1895 of the United Kingdom. The boundary change became effective on 11 June 1901 and the Cook Islands have had a relationship with New Zealand ever since. When the British Nationality and New Zealand Citizenship Act 1948 came into effect on 1 January 1949, the country remained a New Zealand dependent territory until 1965, when the New Zealand Government decided to offer self-governing status to its colony. In that year, Albert Henry of the Cook Islands Party was elected as the first Premier, Henry led the country until he was accused of vote-rigging
33.
Polynesians
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The Polynesian people consist of various ethnic Austronesian groups that speak Polynesian languages, a branch of the Oceanic languages, and inhabit Polynesia. The native Polynesian people of New Zealand and Hawaii are minorities in their homelands, Polynesians, including Samoans, Tongans, Niueans, Cook Islands Māori, Tahitian Māohi, Hawaiian Māoli, Marquesans and New Zealand Māori, are a subset of the Austronesian peoples. They share the same origins as the peoples of maritime Southeast Asia, Madagascar. This is supported by genetic, linguistic, and archaeological evidence, the origins of the Polynesian people are addressed in the theories regarding migration into the Pacific that began about 3000 years ago. These are outlined well by Kayser et al, however, Soares et al. have argued for an older pre-Holocene Sundaland origin within Island Southeast Asia based on mitochondrial DNA. Paternal Y chromosome analysis by Kayser et al. also showed that Polynesians have significant Melanesian genetic admixture. However, a study by Kayser et al. discovered that only 21% of the Polynesian autosomal gene pool is of Melanesian origin. Another study by Friedlaender et al. also confirmed that Polynesians are closer genetically to Micronesians, Taiwanese Aborigines, the study concluded that Polynesians moved through Melanesia fairly rapidly, allowing only limited admixture between Austronesians and Melanesians. Thus the high frequencies of mtDNA B4a1a1 in the Polynesians are the result of drift, the Polynesian population experienced a population bottleneck and genetic drift. DNA analysis of modern Polynesians indicates that there has been intermarriage that results in a mixed Asian-Papuan ancestry of the Polynesians. The preliminary analysis of skulls found at the Teouma and Talasiu Lapita sites is that the skulls lacks Australian or Papuan affinities, there is an estimated 2 million ethnic Polynesians and their descendants worldwide, majority of which live in Polynesia, United States, Australia and New Zealand
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Polynesia
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Polynesia is a subregion of Oceania, made up of over 1,000 islands scattered over the central and southern Pacific Ocean. The indigenous people who inhabit the islands of Polynesia are termed Polynesians and they share many similar traits including the language family, culture, and beliefs. Historically, they were experienced sailors who used stars to navigate at night, the term Polynesia was first used in 1756 by French writer Charles de Brosses, and originally applied to all the islands of the Pacific. In 1831, Jules Dumont dUrville proposed a restriction on its use during a lecture to the Geographical Society of Paris, historically, these islands have also been referred to as the South Sea Islands. Polynesia is characterized by an amount of land spread over a very large portion of the mid. Most Polynesian islands and archipelagos, including the Hawaiian Islands and Samoa, are composed of volcanic islands built by hotspots, New Zealand, Norfolk Island, and Ouvéa, the Polynesian outlier near New Caledonia, are the unsubmerged portions of the largely sunken continent of Zealandia. At first, the Pacific plate was subducted under the Australian plate, the Alpine Fault that traverses the South Island is currently a transform fault while the convergent plate boundary from the North Island northwards is called the Kermadec-Tonga Subduction Zone. The volcanism associated with subduction zone is the origin of the Kermadec. Out of approximately 300,000 or 310,000 square kilometres of land, over 270,000 km2 are within New Zealand, the Zealandia continent has approximately 3,600,000 km2 of continental shelf. The oldest rocks in the region are found in New Zealand and are believed to be about 510 million years old, the oldest Polynesian rocks outside of Zealandia are to be found in the Hawaiian Emperor Seamount Chain, and are 80 million years old. Polynesia is generally defined as the islands within the Polynesian Triangle, geographically, the Polynesian Triangle is drawn by connecting the points of Hawaii, New Zealand and Easter Island. The other main island groups located within the Polynesian Triangle are Samoa, Tonga, there are also small Polynesian settlements in Papua New Guinea, the Solomon Islands, the Caroline Islands, and in Vanuatu. An island group with strong Polynesian cultural traits outside of this triangle is Rotuma. The people of Rotuma have many common Polynesian traits but speak a non-Polynesian language, some of the Lau Islands to the southeast of Fiji have strong historic and cultural links with Tonga. However, in essence, Polynesia is a term referring to one of the three parts of Oceania. Some islands of Polynesian origin are outside the triangle that geographically defines the region. The Phoenix Islands and Line Islands, most of which are part of Kiribati, are geographically Polynesian islands, tracing Polynesian languages places their prehistoric origins in the Malay Archipelago, and ultimately, in Taiwan. Between about 3000 and 1000 BC speakers of Austronesian languages began spreading from Taiwan into Island Southeast Asia, there are three theories regarding the spread of humans across the Pacific to Polynesia
35.
Coral
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Corals are marine invertebrates in the class Anthozoa of phylum Cnidaria. They typically live in colonies of many identical individual polyps. The group includes the important reef builders that inhabit tropical oceans, a coral group is a colony of myriad genetically identical polyps. Each polyp is an animal typically only a few millimeters in diameter. A set of tentacles surround a central mouth opening, an exoskeleton is excreted near the base. Over many generations, the colony creates a large skeleton that is characteristic of the species. Individual heads grow by reproduction of polyps. Corals also breed sexually by spawning, polyps of the same species release gametes simultaneously over a period of one to several nights around a full moon and these are commonly known as zooxanthellae and the corals that contain them are zooxanthellate corals. Such corals require sunlight and grow in clear, shallow water, other corals do not rely on zooxanthellae and can live in much deeper water, with the cold-water genus Lophelia surviving as deep as 3,000 metres. Some have been found on the Darwin Mounds, north-west of Cape Wrath, Corals have also been found as far north as off the coast of Washington State and the Aleutian Islands. In his Scala Naturae, Aristotle classified corals as zoophyta, animals that had characteristics of plants and were therefore hypothetically in between animals and plants, the Persian polymath Al-Biruni classified sponges and corals as animals, arguing that they respond to touch. The phylogeny of Anthozoans is not clearly understood and a number of different models have been proposed, within the Hexacorallia, the sea anemones, coral anemones and stony corals may constitute a monophyletic grouping united by their eight-fold symmetry and cnidocyte trait. The Octocorallia appears to be monophyletic, and primitive members of this group may have been stolonate, the cladogram presented here comes from a 2014 study by Stampar et al. which was based on the divergence of mitochondrial DNA within the group and on nuclear markers. Corals are classified in the class Anthozoa of the phylum Cnidaria and they are divided into three subclasses, Hexacorallia, Octocorallia, and Ceriantharia. The Hexacorallia include the stony corals, the sea anemones and the zoanthids and these groups have polyps that generally have 6-fold symmetry. The Octocorallia include blue coral, soft corals, sea pens and these groups have polyps with 8-fold symmetry, each polyp having eight tentacles and eight mesenteries. Fire corals are not true corals, being in the order Anthomedusa of the class Hydrozoa, Corals are sessile animals in the class Anthozoa and differ from most other cnidarians in not having a medusa stage in their life cycle. The body unit of the animal is a polyp, most corals are colonial, the initial polyp budding to produce another and the colony gradually developing from this small start
36.
Limestone
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Limestone is a sedimentary rock, composed mainly of skeletal fragments of marine organisms such as coral, forams and molluscs. Its major materials are the minerals calcite and aragonite, which are different crystal forms of calcium carbonate, about 10% of sedimentary rocks are limestones. The solubility of limestone in water and weak acid solutions leads to karst landscapes, most cave systems are through limestone bedrock. The first geologist to distinguish limestone from dolomite was Belsazar Hacquet in 1778, like most other sedimentary rocks, most limestone is composed of grains. Most grains in limestone are skeletal fragments of organisms such as coral or foraminifera. Other carbonate grains comprising limestones are ooids, peloids, intraclasts and these organisms secrete shells made of aragonite or calcite, and leave these shells behind when they die. Limestone often contains variable amounts of silica in the form of chert or siliceous skeletal fragment, some limestones do not consist of grains at all, and are formed completely by the chemical precipitation of calcite or aragonite, i. e. travertine. Secondary calcite may be deposited by supersaturated meteoric waters and this produces speleothems, such as stalagmites and stalactites. Another form taken by calcite is oolitic limestone, which can be recognized by its granular appearance, the primary source of the calcite in limestone is most commonly marine organisms. Some of these organisms can construct mounds of rock known as reefs, below about 3,000 meters, water pressure and temperature conditions cause the dissolution of calcite to increase nonlinearly, so limestone typically does not form in deeper waters. Limestones may also form in lacustrine and evaporite depositional environments, calcite can be dissolved or precipitated by groundwater, depending on several factors, including the water temperature, pH, and dissolved ion concentrations. Calcite exhibits a characteristic called retrograde solubility, in which it becomes less soluble in water as the temperature increases. Impurities will cause limestones to exhibit different colors, especially with weathered surfaces, Limestone may be crystalline, clastic, granular, or massive, depending on the method of formation. Crystals of calcite, quartz, dolomite or barite may line small cavities in the rock, when conditions are right for precipitation, calcite forms mineral coatings that cement the existing rock grains together, or it can fill fractures. Travertine is a banded, compact variety of limestone formed along streams, particularly there are waterfalls. Calcium carbonate is deposited where evaporation of the leaves a solution supersaturated with the chemical constituents of calcite. Tufa, a porous or cellular variety of travertine, is found near waterfalls, coquina is a poorly consolidated limestone composed of pieces of coral or shells. During regional metamorphism that occurs during the building process, limestone recrystallizes into marble
37.
Cliff
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In geography and geology, a cliff is a vertical, or nearly vertical, rock exposure. Cliffs are formed as erosion landforms by the processes of weathering, Cliffs are common on coasts, in mountainous areas, escarpments and along rivers. Cliffs are usually formed by rock that is resistant to weathering, sedimentary rocks most likely to form cliffs include sandstone, limestone, chalk, and dolomite. Igneous rocks such as granite and basalt also often form cliffs, an escarpment is a type of cliff, formed by the movement of a geologic fault or a landslide. Most cliffs have some form of slope at their base. In arid areas or under high cliffs, they are generally exposed jumbles of fallen rock, in areas of higher moisture, a soil slope may obscure the talus. Many cliffs also feature tributary waterfalls or rock shelters, sometimes a cliff peters out at the end of a ridge, with tea tables or other types of rock columns remaining. Coastal erosion may lead to the formation of sea cliffs along a receding coastline, the Ordnance Survey distinguishes between cliffs and outcrops. Cliff is a Romance loanword that has its origins in the Latin forms clivus / clevus. Given that a cliff need not be vertical, there can be ambiguity about whether a given slope is a cliff or not. For example, given a vertical rock wall above a very steep slope. Listings of cliffs are thus inherently uncertain, some of the largest cliffs on Earth are found underwater. For example, an 8,000 m drop over a 4,250 m span can be found at a ridge sitting inside the Kermadec Trench. One candidate for highest cliff in the world is Nanga Parbats Rupal Face, according to other sources, the highest cliff in the world, about 1,340 m high, is the east face of Great Trango in the Karakoram mountains of northern Pakistan. The location of the worlds highest sea cliffs depends also on the definition of cliff that is used, guinness World Records states it is Kalaupapa, Hawaii, at 1,010 m high. Another contender is the face of Mitre Peak, which drops 1,683 m to Milford Sound. These are subject to a less stringent definition, as the slope of these cliffs at Kaulapapa is about 1.7, corresponding to an angle of 60 degrees. A more vertical drop into the sea can be found at Maujit Qaqarssuasia which is situated in the Torssukátak fjord area at the tip of South Greenland
38.
Plateau
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Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Magma rises from the mantle, causing the ground to swell upward, in way, large, flat areas of rock are uplifted. Plateaus can also be built up by lava spreading outward from cracks, plateaus can also be formed by the erosional processes of glaciers on mountain ranges, leaving them sitting between the mountain ranges. Water can also erode mountains and other landforms down into plateaus, volcanic plateaus are produced by volcanic activity. The Columbia Plateau in the northwestern United States is an example, dissected plateaus are highly eroded plateaus cut by rivers and broken by deep narrow valleys. Plateaus are classified according to their surrounding environment, intermontane plateaus are the highest in the world, bordered by mountains. The Tibetan Plateau is one such plateau, Piedmont plateaus are bordered on one side by mountains and on the other by a plain or a sea. The Piedmont Plateau of the Eastern United States between the Appalachian Mountains and the Atlantic Coastal Plain is an example, continental plateaus are bordered on all sides by plains or oceans, forming away from the mountains. The Tibetan plateau covers approximately 2,500,000 km2, the plateau is sufficiently high enough to reverse the Hadley cell convection cycles and to drive the monsoons of India towards the south. The second-highest plateau is the Deosai Plateau of the Deosai National Park at an elevation of 4,114 m. It is located in the Astore and Skardu districts of Gilgit-Baltistan, Deosai means the land of giants. The park protects an area of 3,000 km2 and it is known for its rich flora and fauna of the Karakoram-West Tibetan Plateau alpine steppe ecoregion. In spring it is covered by sweeps of wildflowers and a variety of butterflies. The highest point in Deosai is Deosai Lake, or Sheosar Lake from the Shina language meaning Blind lake near the Chilim Valley. The lake lies at an elevation of 4,142 m, one of the highest lakes in the world, and is 2.3 km long,1.8 km wide, and 40 m deep on average. Some other major plateaus in Asia are, Armenian Highlands, Iranian plateau, Anatolian Plateau, Mongolian Plateau, and the Deccan Plateau. This polar ice cap is so massive that the echolocation sound measurements of ice thickness have shown that parts of the Antarctic dry land surface have been pressed below sea level. Thus, if that same ice cap were removed, the large areas of the frozen white continent would be flooded by the surrounding Antarctic Ocean or Southern Ocean
39.
Sea level
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Mean sea level is an average level of the surface of one or more of Earths oceans from which heights such as elevations may be measured. A common and relatively straightforward mean sea-level standard is the midpoint between a low and mean high tide at a particular location. Sea levels can be affected by factors and are known to have varied greatly over geological time scales. The careful measurement of variations in MSL can offer insights into ongoing climate change, the term above sea level generally refers to above mean sea level. Precise determination of a sea level is a difficult problem because of the many factors that affect sea level. Sea level varies quite a lot on several scales of time and this is because the sea is in constant motion, affected by the tides, wind, atmospheric pressure, local gravitational differences, temperature, salinity and so forth. The easiest way this may be calculated is by selecting a location and calculating the mean sea level at that point, for example, a period of 19 years of hourly level observations may be averaged and used to determine the mean sea level at some measurement point. One measures the values of MSL in respect to the land, hence a change in MSL can result from a real change in sea level, or from a change in the height of the land on which the tide gauge operates. In the UK, the Ordnance Datum is the sea level measured at Newlyn in Cornwall between 1915 and 1921. Prior to 1921, the datum was MSL at the Victoria Dock, in Hong Kong, mPD is a surveying term meaning metres above Principal Datum and refers to height of 1. 230m below the average sea level. In France, the Marégraphe in Marseilles measures continuously the sea level since 1883 and it is used for a part of continental Europe and main part of Africa as official sea level. Elsewhere in Europe vertical elevation references are made to the Amsterdam Peil elevation, satellite altimeters have been making precise measurements of sea level since the launch of TOPEX/Poseidon in 1992. A joint mission of NASA and CNES, TOPEX/Poseidon was followed by Jason-1 in 2001, height above mean sea level is the elevation or altitude of an object, relative to the average sea level datum. It is also used in aviation, where some heights are recorded and reported with respect to sea level, and in the atmospheric sciences. An alternative is to base height measurements on an ellipsoid of the entire Earth, in aviation, the ellipsoid known as World Geodetic System 84 is increasingly used to define heights, however, differences up to 100 metres exist between this ellipsoid height and mean tidal height. The alternative is to use a vertical datum such as NAVD88. When referring to geographic features such as mountains on a topographic map, the elevation of a mountain denotes the highest point or summit and is typically illustrated as a small circle on a topographic map with the AMSL height shown in metres, feet or both. In the rare case that a location is below sea level, for one such case, see Amsterdam Airport Schiphol
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