1.
Geographic coordinate system
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A geographic coordinate system is a coordinate system used in geography that enables every location on Earth to be specified by a set of numbers, letters or symbols. The coordinates are chosen such that one of the numbers represents a vertical position. A common choice of coordinates is latitude, longitude and elevation, to specify a location on a two-dimensional map requires a map projection. The invention of a coordinate system is generally credited to Eratosthenes of Cyrene. Ptolemy credited him with the adoption of longitude and latitude. Ptolemys 2nd-century Geography used the prime meridian but measured latitude from the equator instead. Mathematical cartography resumed in Europe following Maximus Planudes recovery of Ptolemys text a little before 1300, in 1884, the United States hosted the International Meridian Conference, attended by representatives from twenty-five nations. Twenty-two of them agreed to adopt the longitude of the Royal Observatory in Greenwich, the Dominican Republic voted against the motion, while France and Brazil abstained. France adopted Greenwich Mean Time in place of local determinations by the Paris Observatory in 1911, the latitude of a point on Earths surface is the angle between the equatorial plane and the straight line that passes through that point and through the center of the Earth. Lines joining points of the same latitude trace circles on the surface of Earth called parallels, as they are parallel to the equator, the north pole is 90° N, the south pole is 90° S. The 0° parallel of latitude is designated the equator, the plane of all geographic coordinate systems. The equator divides the globe into Northern and Southern Hemispheres, the longitude of a point on Earths surface is the angle east or west of a reference meridian to another meridian that passes through that point. All meridians are halves of great ellipses, which converge at the north and south poles, the prime meridian determines the proper Eastern and Western Hemispheres, although maps often divide these hemispheres further west in order to keep the Old World on a single side. The antipodal meridian of Greenwich is both 180°W and 180°E, the combination of these two components specifies the position of any location on the surface of Earth, without consideration of altitude or depth. The grid formed by lines of latitude and longitude is known as a graticule, the origin/zero point of this system is located in the Gulf of Guinea about 625 km south of Tema, Ghana. To completely specify a location of a feature on, in, or above Earth. Earth is not a sphere, but a shape approximating a biaxial ellipsoid. It is nearly spherical, but has an equatorial bulge making the radius at the equator about 0. 3% larger than the radius measured through the poles, the shorter axis approximately coincides with the axis of rotation
2.
Flag of the Cook Islands
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The flag of the Cook Islands, officially known as the Cook Islands Ensign, is based on the traditional design for former British colonies in the Pacific region. It is a blue ensign containing the Union Flag in the upper left, the Union Flag is symbolic of the nations historic ties to the United Kingdom and to the Commonwealth of Nations. The stars stand for the fifteen islands that make up the Cook Islands, the blue represents the ocean and the peaceful nature of the inhabitants. From 1973 to 1979, the flag was green with the stars in yellow shifted towards the fly, the green colour represented the continuous growth and life of the islands, the yellow represented the faith, love, happiness, and commitment shown by the islanders. The circle represented the union of the islands and the union between the islanders and the land itself, list of New Zealand flags Cook Islands at Flags of the World World Statesmen - Cook Islands
3.
Te Atua Mou E
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Te Atua mou e is the national anthem of the Cook Islands. It was adopted in 1982, replacing the previous New Zealand anthem God Defend New Zealand, the music is by Sir Tom Davis, then Prime Minister of the Cook Islands. The words are by his wife, Pa Tepaeru Terito Ariki Lady Davis, Te Atua mou e on YouTube Te Atua mou e on YouTube
4.
Ethnic group
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An ethnic group or ethnicity is a category of people who identify with each other based on similarities, such as common ancestral, language, social, cultural or national experiences. Unlike other social groups, ethnicity is often an inherited status based on the society in which one lives, in some cases, it can be adopted if a person moves into another society. Ethnic groups, derived from the historical founder population, often continue to speak related languages. By way of language shift, acculturation, adoption and religious conversion, it is possible for individuals or groups to leave one ethnic group. Ethnicity is often used synonymously with terms such as nation or people. In English, it can also have the connotation of something exotic, generally related to cultures of more recent immigrants, the largest ethnic groups in modern times comprise hundreds of millions of individuals, while the smallest are limited to a few dozen individuals. Conversely, formerly separate ethnicities can merge to form a pan-ethnicity, whether through division or amalgamation, the formation of a separate ethnic identity is referred to as ethnogenesis. The term ethnic is derived from the Greek word ἔθνος ethnos, the inherited English language term for this concept is folk, used alongside the latinate people since the late Middle English period. In Early Modern English and until the mid-19th century, ethnic was used to mean heathen or pagan, as the Septuagint used ta ethne to translate the Hebrew goyim the nations, non-Hebrews, non-Jews. The Greek term in antiquity could refer to any large group, a host of men. In the 19th century, the term came to be used in the sense of peculiar to a race, people or nation, the abstract ethnicity had been used for paganism in the 18th century, but now came to express the meaning of an ethnic character. The term ethnic group was first recorded in 1935 and entered the Oxford English Dictionary in 1972, depending on the context that is used, the term nationality may either be used synonymously with ethnicity, or synonymously with citizenship. The process that results in the emergence of an ethnicity is called ethnogenesis, the Greeks at this time did not describe foreign nations but had also developed a concept of their own ethnicity, which they grouped under the name of Hellenes. Herodotus gave an account of what defined Greek ethnic identity in his day, enumerating shared descent. Whether ethnicity qualifies as a universal is to some extent dependent on the exact definition used. Many social scientists, such as anthropologists Fredrik Barth and Eric Wolf and they regard ethnicity as a product of specific kinds of inter-group interactions, rather than an essential quality inherent to human groups. According to Thomas Hylland Eriksen, the study of ethnicity was dominated by two distinct debates until recently, one is between primordialism and instrumentalism. In the primordialist view, the participant perceives ethnic ties collectively, as a given, even coercive
5.
Cook Islanders
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Cook Islanders or Cook Islands Māori are residents of the Cook Islands, which is composed of 15 islands and atolls in Polynesia in the Pacific Ocean. From a legal standpoint, there is no such thing as a Cook Islands citizenship, the Cook Islands is a self-governing country in free association with New Zealand and is part of the Realm of New Zealand. As such, Cook Islanders are New Zealand citizens, on the other hand, Cook Islands nationality is differentiated from that of the rest of the New Zealand citizens. Nationality in this sense may be distinguished from citizenship, while it does not have distinct citizenship legislation, the Cook Islands has determined under its own laws who are its nationals and what privileges they enjoy by virtue of that status. Cook Islanders possess New Zealand citizenship with the rights and privileges that status entails. Well over 90 percent of Cook Islanders are either of full or partial descent of the native Polynesian people of the islands, Cook Islands Māori share many ancestral links with the Māori of New Zealand and the native people of French Polynesia. Some Cook Islanders are also of other Polynesian, European, or Asian descent, Cook Islands permanent residency Arrangement between US and the Compact of Free Association states The Cook Islands’ unique constitutional and international status, page 9
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 the Cook Islands
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The politics of the Cook Islands, an associated state, takes place in a framework of a parliamentary representative democracy within a constitutional monarchy. The Queen of New Zealand, represented in the Cook Islands by the Queens Representative, is the Head of State, the Islands are self-governing in free association with New Zealand and are fully responsible for internal affairs. New Zealand retains some responsibility for external affairs, in consultation with the Cook Islands, in recent years, the Cook Islands have taken on more of its own external affairs, as of 2005, it has diplomatic relations in its own name with eighteen other countries. Executive power is exercised by the government, while power is vested in both the government and the islands parliament. The judiciary is independent of the executive and the legislatures, the Constitution of the Cook Islands took effect on August 4,1965, when the Cook Islands became a self-governing territory in free association with New Zealand. The anniversary of these events in 1965 is commemorated annually on Constitution Day, the monarch is hereditary, her representative is appointed by the monarch on the recommendation of the Cook Islands Government. The cabinet is chosen by the minister and collectively responsible to Parliament. Ten years of rule by the Cook Islands Party came to an end 18 November 1999 with the resignation of Prime Minister Joe Williams, Williams had led a minority government since October 1999 when the New Alliance Party left the government coalition and joined the main opposition Democratic Party. On 18 November 1999, DAP leader Dr. Terepai Maoate was sworn in as prime minister and he was succeeded by his co-partisan Robert Woonton. When Dr Woonton lost his seat in the 2004 elections, Jim Marurai took over, in the 2010 elections, the CIP regained power and Henry Puna was sworn in as prime minister on 30 November 2010. Jim Marurais Democratic Party retained the Treasury benches with an increased majority, the New Zealand High Commissioner is appointed by the New Zealand Government. The Parliament of the Cook Islands has 24 members, elected for a term in single-seat constituencies. There is also a House of Ariki, composed of chiefs, the Koutu Nui is a similar organization consisting of sub-chiefs. It was established by an amendment in 1972 of the 1966 House of Ariki Act, the current President is Te Tika Mataiapo Dorice Reid. On June 13,2008, a majority of members of the House of Ariki attempted a coup, claiming to dissolve the elected government. Basically we are dissolving the leadership, the minister and the deputy prime minister. The Cook Islands Herald suggested that the ariki were attempting thereby to regain some of their traditional prestige or mana, Prime Minister Jim Marurai described the take-over move as ill-founded and nonsensical. By June 23, the situation appeared to have normalised, with members of the House of Ariki accepting to return to their regular duties, the 1999 election produced a hung Parliament
8.
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
9.
Monarchy in the Cook Islands
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The Cook Islands are a constitutional monarchy within the Realm of New Zealand. Under the Cook Islands Constitution, the monarch in right of New Zealand has been Head of State of the Cook Islands since 4 August 1965, the vice-regal position is currently held by Sir Frederick Goodwin. The Queens official title is, Elizabeth the Second, By the Grace of God, Queen of New Zealand and Her other Realms and Territories, Head of the Commonwealth, the heir apparent is Elizabeth IIs eldest son, Prince Charles, Prince of Wales. In 1965 Queen Elizabeth II became Head of State of the Cook Islands when the country obtained a position of free-association with New Zealand. Article 2 of the Cook Islands Constitution states that Her Majesty the Queen in Right of New Zealand shall be the Head of State of the Cook Islands. In clause 1, the Realm of New Zealand is defined as including New Zealand, the state of the Cook Islands, the self-governing state of Niue, Tokelau. The New Zealand - Cook Islands Joint Centenary Declaration states that and this legislation lays out the rules that the Monarch cannot be a Roman Catholic, and must be in communion with the Church of England upon ascending the throne. The Queens constitutional roles in the Cook Islands have been almost entirely delegated to the Queens Representative, further, the 1981 Constitution Amendment decreed that the Queens representative was appointed directly by the Queen herself, not the Governor-General of New Zealand. The text states that shall be a representative of Her Majesty the Queen in the Cook Islands, however, the relationship between the Governor-General of New Zealand and the Queens Representative is quite different. Under the Cook Islands Constitution, executive power is vested in Her Majesty the Queen in right of New Zealand, the executive authority of the Cook Islands may be exercised on behalf of Her Majesty by the Queens Representative either directly or through officers subordinate to him. Any vice-regal powers and responsibilities in the Cook Islands are vested in the Queens Representative, Royal assent and proclamation are required for all acts of Parliament, usually granted by the Queen’s Representative. References to the Monarchy are commonplace in public life in the Cook Islands, unlike in the United Kingdom, the Queens Official Birthday is a public holiday on the first Monday in June. The Queens portrait appears on the obverse of coins, and all feature the portrait of the Queen as the watermark. However, only the $20 banknote bears her image as the main feature, the Queen undertook a royal tour of the Cook Islands between 28 January and 29 January 1974. Monarchy in New Zealand Monarchy of the United Kingdom
10.
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
11.
Henry Puna
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Henry Tuakeu Puna is the Prime Minister of the Cook Islands. He is leader of the Cook Islands Party and has been Prime Minister since November 2010 and he was educated on Aitutaki and Rarotonga before studying law at the University of Auckland in New Zealand and the University of Tasmania in Australia. He worked as a lawyer before entering politics, Puna first stood for Parliament at the 2004 election, contesting Prime Minister Robert Woontons seat of Manihiki. He narrowly lost the seat on election night, but challenged the result in an election petition, the petition was upheld, with several voters being disqualified, the subsequent recount produced a tie, precipitating a by-election which Puna ultimately won. In September 2006, following the retirement of party leader Geoffrey Henry and he subsequently lost his seat in the Manihiki constituency to Apii Piho in the 2006 election, but continued to serve as leader outside Parliament. Because he was not a member of Parliament, Puna was not the leader of the opposition, Puna worked as a lawyer and pearl farmer during his time out of parliament. In September 2009, Puna was unanimously re-elected party leader, Puna was elected as MP for Manihiki during the 2010 election, in which his party won 16 of the 24 seats. On 30 November 2010 he was sworn in as Prime Minister of the Cook Islands, Puna made his first official visit to New Zealand as Prime Minister in August 2011. List of foreign ministers in 2017 List of current foreign ministers
12.
House of Ariki
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The House of Ariki is a parliamentary body in the Cook Islands. It is composed of Cook Islands high chiefs, appointed by the Queens Representative, there are up to twenty four members, representing different islands of the Cooks. It was established in 1967 by Prime Minister Albert Henry, shortly after the country obtained self-government from New Zealand, Henry stated that the ariki were the Cook Islands royal heritage. The House of Ariki was intended to confer additional legitimacy and strength to the newly self-governing nation, Henry stated, The ariki and their tribes are the backbone of all nations in this world. For any nation to allow this backbone to be broken or to disappear would mean that they are relying on a backbone for their survival. The vice-president is Kainuku Kapiriterangi Ariki, according to Ron Crocombe and Jon Tikivanotau Jonassen, The House of Ariki was created to marginalize the ariki. Most of them had opposed the party won the election at self-government, so it created and quarantined them in a House with dignity. To marginalize ariki further, that party later created a Koutu Nui of mataiapo, on 13 June 2008, a small majority of members of the House of Ariki attempted a coup, claiming to dissolve the elected government and to take control of the countrys leadership. Basically we are dissolving the leadership, the minister and the deputy prime minister. The Cook Islands Herald suggested that the Ariki were attempting thereby to regain some of their traditional prestige or mana, Prime Minister Jim Marurai described the take-over move as ill-founded and nonsensical. Police commissioner Pat Tasker added that it was laughable, and that the police did not intend to take it seriously, by 23 June, the situation appeared to have normalised, with members of the House of Ariki accepting to return to their regular duties. List of Presidents of the House of Ariki House of Lords Chamber of Peers NZ Māori stirs Cooks sovereignty stoush
13.
Parliament of the Cook Islands
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The Parliament of the Cook Islands is the legislature of the Cook Islands. Originally established under New Zealand colonial rule, it became the legislature on independence in 1965. The Parliament consists of 24 members directly elected by universal suffrage from single-seat constituencies, Members are elected for a limited term, and hold office until Parliament is dissolved. It meets in the capital of Rarotonga, the Cook Islands follows the Westminster system of government, and is governed by a cabinet and Prime Minister commanding a majority in Parliament. The Speaker of the House is currently Niki Rattle, the Deputy Speaker is Rose Toki-Brown. The Cook Islands Parliament is descended from the Cook Islands Legislative Council established in October 1946, established to provide for political representation and better local government in the islands, the Legislative Council was a subordinate legislature. Later regulations provided for the members to be split between the various islands,3 from Rarotonga,6 from the outer islands and 1 representing the islands European population. The island representatives were elected annually, while the European representative was elected to a three-year term, the Legislative Council was reorganised in 1957 as the Legislative Assembly with 22 elected members and 4 appointed officials. Fifteen of the members were elected directly by secret ballot, in 1962, the Assembly was given full control of its own budget. In that year it also debated the political future and chose self-government in free association with New Zealand. On independence in 1965 it gained full legislative power and it was renamed the Parliament of the Cook Islands in 1981. Both the size and term of Parliament have fluctuated since independence, in 1965, it consisted of 22 members elected for a period of 3 years. The size was increased to 24 members in 1981, and again to 25 in 1991 and it was reduced again to 24 members in 2003 when the overseas constituency created under the 1980–81 Constitution Amendment was abolished. The original three-year term was increased to four years in 1969, a referendum to reduce it to four years failed to gain the necessary two-thirds majority in 1999, but passed in 2004. See, Elections in the Cook Islands, the Cook Islands Parliament takes the British House of Commons as its model. It consists of 24 members, known as Members of Parliament, Members are elected by universal suffrage using the first-past-the-post system from single-seat constituencies. The executive branch of the Cook Islands government draws its membership exclusively from Parliament, the Prime Minister leads the government, the Queens Representative appoints the Prime Minister from the party or coalition which has or appears to have enough support to govern. The Prime Minister and Cabinet hold office until the next election, the Democratic Party is currently in government
14.
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
15.
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
16.
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
17.
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
18.
Cook Islands dollar
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The dollar is the currency of the Cook Islands. The dollar is subdivided into 100 cents, although some 50 cent coins carry the denomination as 50 tene, until 1967, the New Zealand pound was used on the Cook Islands, when it was replaced by the New Zealand dollar. In 1972, coins were issued specifically for the Cook Islands, the Cook Islands dollar is pegged at par to the New Zealand dollar. The currency of New Zealand and the Cook Islands circulate concurrently within the country, coins have been struck on different occasions mainly by the Royal Australian Mint, the Franklin Mint, and the Perth Mint with the paper currency being printed by De La Rue. In 1972, bronze 1 and 2 cents, and cupro-nickel 5,10,20 and 50 cents, and 1-dollar coins were introduced. All were the size, weight, and composition as the corresponding New Zealand coins, however. Each coin depicted plants, animals, and items unique to the Cook Islands, in 1983, production of the 1 and 2-cent coins was ceased and the two coins were later demonetized. In 1987, a smaller, lighter scallop-edged $1 coin with a similar size and this coin was issued to replace its bulky predecessor. 2003 saw the reintroduction of a 1-cent coin, this time composed of aluminium rather than bronze and these were issued with five different reverses, each commemorating a few of the nations historical themes. A large, stainless steel 5 cent coin was issued in 2000 centred on FAO, the Cook Islands has a long reputation for frequent monetary oddities. It was one of the last countries to hold on to large crown-sized coins while elsewhere,1988 brought the redesign of the 50-cent piece, quite unique in becoming the first coin in the country to bear a denomination name. Although widely recognized as cents this coin depicts tene, the language equivalent to the English word cent. It also abandoned its 1 and 2-cent pieces almost 10 years before both New Zealand and Australia, only to bring the 1 cent back 20 years later. It also replaced $1 and $2 notes for two years before New Zealand did, even though the Cook Islands dollar is pegged to the NZD at par. Amidst minting $2 and $5 coins, it issued an oddball $3 note in between the dollar coins as part of the same series. With the reduction in size of the New Zealand 10,20 and 50-cent coins in 2006, however, $1, $2, and $5 pieces remained in use. As part of a reform, new coins were minted in 2015 by the Royal Australian Mint. The new coins carry similar designs to the ones with the 10,20, and 50 cents struck in nickel-plated steel, while the 1,2
19.
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
20.
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
21.
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
22.
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
23.
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
24.
Exclusive economic zone
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It stretches from the baseline out to 200 nautical miles from its coast. In colloquial usage, the term may include the continental shelf, the term does not include either the territorial sea or the continental shelf beyond the 200 nmi limit. The surface waters, as can be seen in the map, are international waters, generally, a states exclusive economic zone is an area beyond and adjacent to the territorial sea, extending seaward to a distance of no more than 200 nautical miles out from its coastal baseline. The exception to this occurs when exclusive economic zones would overlap. When an overlap occurs, it is up to the states to delineate the actual maritime boundary, generally, any point within an overlapping area defaults to the nearest state. A states exclusive economic zone starts at the edge of its territorial sea. The exclusive economic zone stretches much further into sea than the territorial waters, thus, the exclusive economic zones includes the contiguous zone. The idea of allotting nations EEZs to give more control of maritime affairs outside territorial limits gained acceptance in the late 20th century. Initially, a countrys sovereign territorial waters extended 3 nautical miles or 6 km beyond the shore, in modern times, a countrys sovereign territorial waters extend to 12 nautical miles beyond the shore. One of the first assertions of exclusive jurisdiction beyond the territorial seas was made by the United States in the Truman Proclamation of September 28,1945. The exact extent of economic zones is a common source of conflicts between states over marine waters. One well-known example of such dispute was the Cod Wars between the United Kingdom and Iceland, Norway and Russia dispute both territorial sea and EEZ with regard to the Svalbard archipelago as it affects Russias EEZ due to its unique treaty status. A treaty was agreed in principle in April 2010 between the two states and subsequently ratified, resolving this demarcation dispute, the agreement was signed in Murmansk on September 15,2010. The South China Sea is the site of a dispute between several neighboring nations. Croatias ZERP in the Adriatic Sea caused friction with Italy and Slovenia, a wedge-shaped section of the Beaufort Sea is disputed between Canada and the United States, as the area reportedly contains substantial oil reserves. France claims a portion of Canadas EEZ for Saint-Pierre-et-Miquelon based on a new definition of the continental shelf, Saint-Pierre-et-Miquelon is entirely surrounded by Canadas EEZ. Mauritius claims EEZ for Tromelin from France and EEZ for British Indian Ocean Territory from the UK, Northern Cyprus claims a portion of Cyprus EEZ overlaps with that of Northern Cyprus in the south/southeastern part of the Cyprus island. Turkey claims a portion of Cypruss EEZ overlaps with its own EEZ, Lebanon claims that the agreement between Cyprus and Israel overlapped its own EEZ
25.
New Zealand nationality law
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New Zealand nationality law determines who is and who is not a New Zealand citizen. The status of New Zealand citizenship was created on 1 January 1949 by the British Nationality, prior to this date, New Zealanders were only British subjects and New Zealand had the same nationality legislation as the United Kingdom and other Commonwealth countries. The 1948 legislation was replaced by the Citizenship Act 1977, which came into force on 1 January 1978 and this was substantially amended in 2005 by the Citizenship Act 2005, in force from 21 April 2005. The Citizenship Office of the Department of Internal Affairs is in charge of processing applications, in the mid-19th century, all aliens were able to enter and live freely in the British Queen’s dominions, although their property rights were restricted. On 1 January 1978, the Citizenship Act 1977 came into force, New Zealand passports no longer contained the status of British subject and New Zealand citizen, but instead only stated New Zealand citizen. Foreign nationals who wanted to become New Zealand citizens were no longer naturalised, māori were granted ‘all the Rights and Privileges of British Subjects’ under Article 3 of the Treaty of Waitangi in 1840. Their status as British subjects was re-affirmed by the Native Rights Act 1865, when the Cook Islands and Niue became New Zealand territories in 1901, their inhabitants were already British subjects. In 1920, Tokelauans became recognised as British subjects, in 1920, New Zealand started governing Western Samoa under a mandate from the League of Nations. When Western Samoa achieved independence from New Zealand in 1962, the status of Western Samoans living in New Zealand became uncertain. As a result, many Western Samoans were staying in New Zealand illegally, the Privy Council ruling would have meant recognising over 100,000 Samoans as New Zealand citizens. In 1866, the Aliens Act imposed a fee of £1 on all immigrants to New Zealand who were perceived to be undesirable. When this naturalisation fee was abolished in the 1890s, Chinese people continued to be discriminated against as they still had to pay the fee whilst all other applicants did not, in 1908, Chinese people in New Zealand were subjected to even more discrimination. They were denied any possibility for permanent residence and citizenship and were required to apply periodically for permission to remain in New Zealand, despite being treated as third-class citizens, during the Second World War, Chinese people in New Zealand were forced to serve in the armed forces. It was not until 1951 that Chinese people were allowed by law to apply for permanent residence. However, in practice, they continued to be subject to discrimination, on 12 February 2002, Prime Minister Helen Clark made a formal apology in Parliament to the Chinese community in New Zealand for the discrimination which they had faced in the past. However, for Samoan citizens applying for a grant of New Zealand citizenship, the Cook Islands, Niue. Similarly, all born or naturalised in New Zealand in 1949 or later are New Zealand citizens otherwise than by descent. In general, any person born in New Zealand on or before 31 December 2005 is a New Zealand citizen by birth, children born to a parent who is a permanent resident of the Cook Islands, Niue or Tokelau also qualify
26.
Rarotonga
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Rarotonga is the most populous island of the Cook Islands, with a population of 10,572, out of the countrys total resident population of 14,974. Captain John Dibbs, master of the colonial brig Endeavour, is credited as the European discoverer on 25 August 1823, the Cook Islands Parliament buildings and international airport are on Rarotonga. Because it is the most populous island, Cook Islanders may often be referred to as Rarotongan, Rarotonga is a very popular tourist destination with many resorts, hotels and motels. The chief town, Avarua, on the north coast, is the capital of the Cook Islands, the volcanic island of Rarotonga stands over 14,750 feet above the ocean floor. It is 32 km in circumference and has an area of 67.19 km2, at a depth of 4,000 m the volcano is nearly 50 km in diameter. Te Manga, at 658 m above sea level, is the highest peak on the island, the island is surrounded by a lagoon, which often extends more than a hundred metres to the reef, then slopes steeply to deep water. This part of the island is the most popular with tourists for swimming, snorkelling and boating, agricultural terraces, flats and swamps surround the central mountain area. Along the southeast coast off Muri Beach are four small islets within a few hundred metres of the shore. Paved and unpaved roads allow access to valleys but the interior of the island remains largely unpopulated due to forbidding terrain and lack of infrastructure. A large tract of land has set aside in the south east as the Takitumu Conservation Area to protect native birds and plants, especially the endangered kakerori. On May 30,1965, five sounding rockets were launched from Rarotonga for studying a solar eclipse, Rarotonga is divided into three main districts or vaka. Te Au O Tonga on the side of the island, Takitumu on the eastern and southern side. On the other hand, the island is divided into five Land Districts. In 2008, the three councils of Rarotonga were abolished. It passes the Te Rua Manga, the prominent needle-shaped rock visible from the air, hikes can also be taken to the Raemaru, or flat-top mountain. Other stops should include Wigmore Falls and the ancient marae, Arai te Tonga, there are many churches open for service on Sunday, with a cappella singing. The pace of life is so relaxed that at night people congregate at the sea wall that skirts the end of the runway to be jetblasted by incoming planes. Large cruise ships have to anchor off shore, Rarotonga is encircled by a main road, Ara Tapu, that traces the coast
27.
French Polynesia
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It is composed of 118 geographically dispersed islands and atolls stretching over an expanse of more than 2,000 kilometres in the South Pacific Ocean. Its total land area is 4,167 square kilometres, among its 118 islands and atolls,67 are inhabited. Tahiti, which is located within the Society Islands, is the most populous island and it has more than 68% of the population of the islands in 2012. Although not a part of its territory, Clipperton Island was administered from French Polynesia until 2007. Following the Great Polynesian Migration, European explorers visited the islands of French Polynesia on several occasions, traders and whaling ships also visited. In 1842, the French took over the islands and established a French protectorate they called Etablissements des français en Océanie, in 1946, the EFOs became an overseas territory under the constitution of the French Fourth Republic, and Polynesians were granted the right to vote through citizenship. In 1957, the EFOs were renamed French Polynesia, French Polynesia as we know it today was one of the last places on Earth to be settled by humans. Scientists believe the Great Polynesian Migration happened around 1500 BC as Austronesian people went on a journey using celestial navigation to find islands in the South Pacific Ocean, the first islands of French Polynesia to be settled were the Marquesas Islands in about 200 BC. The Polynesians later ventured southwest and discovered the Society Islands around AD300, European encounters began in 1521 when Portuguese explorer Ferdinand Magellan, sailing at the service of the Spanish Crown, sighted Puka-Puka in the Tuāmotu-Gambier Archipelago. Over a century later, British explorer Samuel Wallis visited Tahiti in 1767, French explorer Louis Antoine de Bougainville also visited Tahiti in 1768, while British explorer James Cook arrived in 1769. A short-lived Spanish settlement was created in 1774, and for a time some maps bore the name Isla de Amat after Viceroy Amat, in 1772, Dutchman Jakob Roggeveen came across Bora Bora in the Society Islands. Christian missions began with Spanish priests who stayed in Tahiti for a year, protestants from the London Missionary Society settled permanently in Polynesia in 1797. King Pōmare II of Tahiti was forced to flee to Moorea in 1803, he, French Catholic missionaries arrived on Tahiti in 1834, their expulsion in 1836 caused France to send a gunboat in 1838. In 1842, Tahiti and Tahuata were declared a French protectorate, the capital of Papeetē was founded in 1843. In 1880, France annexed Tahiti, changing the status from that of a protectorate to that of a colony, the island groups were not officially united until the establishment of the French protectorate in 1889. In the 1880s, France claimed the Tuamotu Archipelago, which belonged to the Pōmare Dynasty. Having declared a protectorate over Tahuata in 1842, the French regarded the entire Marquesas Islands as French, in 1885, France appointed a governor and established a general council, thus giving it the proper administration for a colony. The islands of Rimatara and Rūrutu unsuccessfully lobbied for British protection in 1888, postage stamps were first issued in the colony in 1892
28.
American Samoa
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American Samoa is an unincorporated territory of the United States located in the South Pacific Ocean, southeast of Samoa. American Samoa consists of five islands and two coral atolls. The largest and most populous island is Tutuila, with the Manuʻa Islands, Rose Atoll, All islands except for Swains Island are part of the Samoan Islands, located west of the Cook Islands, north of Tonga, and some 300 miles south of Tokelau. To the west are the islands of the Wallis and Futuna group, the 2010 census showed a total population of 55,519 people. The total land area is 199 square kilometers, slightly more than Washington, American Samoa is the southernmost territory of the U. S. and one of two U. S. territories south of the Equator, along with the uninhabited Jarvis Island. Tuna products are the exports, and the main trading partner is the United States. American Samoa is noted for having the highest rate of enlistment of any U. S. state or territory. Most American Samoans are bilingual and can speak English and Samoan fluently, Samoan is the same language spoken in neighboring independent Samoa. Contact with Europeans began in the early 18th century, dutchman Jacob Roggeveen 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, when English missionaries and traders began arriving. The site of battle is called Massacre Bay. Mission work in the Samoas had begun in late 1830 when John Williams of the London Missionary Society arrived from the Cook Islands, by that time, the Samoans had gained a reputation for being savage and warlike, as violent altercations had occurred between natives and European visitors. In March 1889, an Imperial German naval force entered a village on Samoa, three American warships then entered the Apia harbor and prepared to engage the three German warships found there. Before any shots were fired, a typhoon wrecked both the American and German ships, a compulsory armistice was then called because of the lack of any warships. Forerunners to the Tripartite Convention of 1899 were the Washington Conference of 1887, the Treaty of Berlin of 1889, the following year, the USA formally occupied its portion, a smaller group of eastern islands, one of which contains the noted harbor of Pago Pago. The Navy secured a Deed of Cession of Tutuila in 1900, the territory became known as the US Naval Station Tutuila. On July 17,1911, the US Naval Station Tutuila, in 1918 during the final stages of World War I, the flu pandemic had taken its toll, spreading rapidly from country to country. The result of Poyers quick actions earned him the Navy Cross from the US Navy, with this distinction, American Samoans regarded Poyer as their hero for what he had done to prevent the deadly disease
29.
Atoll
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An atoll, sometimes called a coral atoll, is a ring-shaped coral reef including a coral rim that encircles a lagoon partially or completely. There may be coral islands/cays on the rim, the coral of the atoll often sits atop the rim of an extinct seamount or volcano which has eroded or subsided partially beneath the water. The lagoon forms over the crater or caldera while the higher rim remains above water or at shallow depths that permit the coral to grow. For the atoll to persist, continued erosion or subsidence must be at a slow enough to permit reef growth upwards and outwards to replace the lost height. The word atoll comes from the Dhivehi word atholhu, meaning an administrative subdivision, the distribution of atolls around the globe is instructive, most of the worlds atolls are in the Pacific Ocean and Indian Ocean. The Atlantic Ocean has no large groups of atolls, other than eight atolls east of Nicaragua that belong to the Colombian department of San Andres and Providencia in the Caribbean. Reef-building corals will thrive only in tropical and subtropical waters of oceans and seas. The northernmost atoll of the world is Kure Atoll at 28°24 N, the southernmost atolls of the world are Elizabeth Reef at 29°58 S, and nearby Middleton Reef at 29°29 S, in the Tasman Sea, both of which are part of the Coral Sea Islands Territory. The next southerly atoll is Ducie Island in the Pitcairn Islands Group, at this latitude coral reefs would not develop without the warming waters of the Gulf Stream. However, Bermuda is termed a pseudo-atoll because its general form, while there is no atoll directly on the equator, the closest atoll to the Equator is Aranuka of Kiribati, with its southern tip just 12 km north of the equator. In most cases, the area of an atoll is very small in comparison to the total area. Atoll islands are low lying, with their elevations less than 5 meters, measured by total area, Lifou is the largest raised coral atoll of the world, followed by Rennell Island. More sources however list as the largest atoll in the world in terms of land area Kiritimati, the remains of an ancient atoll as a hill in a limestone area is called a reef knoll. The second largest atoll by dry land area is Aldabra with 155 km², the largest atoll in terms of island numbers is Huvadhu Atoll in the south of the Maldives with 255 islands. In 1842, Charles Darwin explained the creation of coral atolls in the southern Pacific Ocean based upon observations made during a voyage aboard the HMS Beagle from 1831 to 1836. In time, subsidence carries the old volcano below the ocean surface, at this point, the island has become an atoll. Atolls are the product of the growth of marine organisms. Volcanic islands located beyond the water temperature requirements of hermatypic organisms become seamounts as they subside and are eroded away at the surface
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Volcano
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A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. Earths volcanoes occur because its crust is broken into 17 major, therefore, on Earth, volcanoes are generally found where tectonic plates are diverging or converging. This type of volcanism falls under the umbrella of plate hypothesis volcanism, Volcanism away from plate boundaries has also been explained as mantle plumes. These so-called hotspots, for example Hawaii, are postulated to arise from upwelling diapirs with magma from the boundary,3,000 km deep in the Earth. Volcanoes are usually not created where two plates slide past one another. Erupting volcanoes can pose hazards, not only in the immediate vicinity of the eruption. Historically, so-called volcanic winters have caused catastrophic famines, the word volcano is derived from the name of Vulcano, a volcanic island in the Aeolian Islands of Italy whose name in turn comes from Vulcan, the god of fire in Roman mythology. The study of volcanoes is called volcanology, sometimes spelled vulcanology, at the mid-oceanic ridges, two tectonic plates diverge from one another as new oceanic crust is formed by the cooling and solidifying of hot molten rock. Most divergent plate boundaries are at the bottom of the oceans, therefore, most volcanic activity is submarine, black smokers are evidence of this kind of volcanic activity. Where the mid-oceanic ridge is above sea-level, volcanic islands are formed, for example, subduction zones are places where two plates, usually an oceanic plate and a continental plate, collide. In this case, the plate subducts, or submerges under the continental plate forming a deep ocean trench just offshore. In a process called flux melting, water released from the subducting plate lowers the temperature of the overlying mantle wedge. This magma tends to be very viscous due to its high content, so it often does not reach the surface. When it does reach the surface, a volcano is formed, typical examples of this kind of volcano are Mount Etna and the volcanoes in the Pacific Ring of Fire. Because tectonic plates move across them, each volcano becomes dormant and is eventually re-formed as the plate advances over the postulated plume and this theory is currently under criticism, however. The most common perception of a volcano is of a mountain, spewing lava and poisonous gases from a crater at its summit, however. The features of volcanoes are more complicated and their structure. Some volcanoes have rugged peaks formed by lava domes rather than a summit crater while others have features such as massive plateaus
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Oceanic climate
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Oceanic climates are defined as having a monthly mean temperature below 22 °C in the warmest month, and above 0 °C in the coldest month. It typically lacks a dry season, as precipitation is evenly dispersed throughout the year. Oceanic climates generally have cool summers and mild to cool winters, Oceanic climates are most dominant in Europe, where they spread much farther inland than in other continents. Oceanic climates can have much storm activity as they are located in the belt of the stormy westerlies, many oceanic climates have frequent cloudy or overcast conditions due to the near constant storms and lows tracking over or near them. Precipitation is both adequate and reliable throughout the year in oceanic climates, extended months of rain and cloudy conditions are common in oceanic climates. Seattle is an example of this, between October and May, Seattle experiences high rainfall and is mostly or partly cloudy six out of every seven days. In most areas with a climate, precipitation comes in the form of rain for the majority of the year. However, some areas with this climate see some snowfall annually during winter, outside of Australia and parts of New Zealand, most areas with an oceanic climate experience at least one snowstorm per year. In the poleward locations of the climate zone, snowfall is more frequent. Overall temperature characteristics of the oceanic climates feature cool temperatures and infrequent extremes of temperature, summers are cool, with the warmest month having a mean temperature below 22 °C. Poleward of the latter is a zone of the subpolar oceanic climate, with long and cold winters and cool. Examples of this climate include parts of coastal Iceland in the Northern Hemisphere and extreme southern Chile, Oceanic climates are not necessarily always found in coastal locations on the aforementioned parallels, however, in most cases oceanic climates parallel higher middle latitude oceans. The polar jet stream, which moves in a west to east direction across the middle latitudes, advancing low pressure systems, storms, in coastal areas of the higher middle latitudes, the prevailing onshore flow creates the basic structure of most oceanic climates. Oceanic climates are a product and reflection of the adjacent to them. In summer, high pressure pushes the prevailing westerlies north of many oceanic climates. As a result of the Gulf Stream, west-coast areas located in high latitudes like Ireland, the UK, Oceanic climates in Europe occur mostly in Northwest Europe, from Ireland and Great Britain eastward to central Europe. Most of France, Germany, Norway, the north coast of Spain, examples of oceanic climates are found in London, Bergen, Dublin, Berlin, Bilbao, Donostia-San Sebastian, Biarritz, Bayonne, Zürich, Copenhagen and Paris. With decreasing distance to the Mediterranean Sea, the climate of Northwest Europe gradually changes to the subtropical dry-summer or Mediterranean climate of southern Europe
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