1.
Leeward Islands
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The Leeward Islands /ˈliːwərd/ are a group of islands in the West Indies. In English, the term refers to the islands of the Lesser Antilles chain. As a group they start east of Puerto Rico and reach southward to Dominica and they are situated where the northeastern Caribbean Sea meets the western Atlantic Ocean. The more southerly part of the Lesser Antilles chain are called the Windward Islands, the name of this island group, Leeward Islands, dates from previous centuries, when sailing ships were the sole form of transportation across the Atlantic Ocean. In the West Indies, the winds, known as the trade winds. The early Spanish colonizers called Puerto Rico and the islands to the west Sotavento, the islands to the south and east of Puerto Rico were then called Islas de Barlovento, meaning windward islands. When the British gained control of many of the Lesser Antilles, they designated Antigua, Montserrat, guadeloupe and the islands to the south were designated Windward Islands. Later on, all north of Martinique became known as the Leeward Islands. Thus, Dominica is the first of the Leeward islands, the islands along the Venezuelan coast, known in English as the Leeward Antilles, in languages other than English are known as the Leeward Islands. The islands are affected by volcanism, and notable eruptions have occurred in Montserrat in the 1990s. The islands were among the first parts of the Americas to fall under the control of the Spanish Empire, mont serrat in Catalan means saw mountain, referring to the serrated appearance of the mountain range. The Leeward Islands became a British colony in 1671, in 1699, prior to the War of the Spanish Succession, Christopher Codrington became the governor of the Leeward Islands. The war lasted from 1701 to 1714, daniel Parke II was the British governor of the Leeward Islands from 1706 to 1710. He was assassinated during a mutiny triggered by his self-enriching enforcement of Stuart imperialism, although comparatively much smaller than the surrounding islands in the Caribbean, the Leeward Islands posed the most significant rebellion to the British Stamp Act. In 1816 the colony was dissolved, with its last governor being James Leith, in 1833, the colony was reformed. From 1833 until 1871, the Governor of Antigua performed the duties of the Governor of the Leeward Islands, today the Islands are governed by a number of national and colonial administrations. Digital Library of the Caribbean−dloc. org, Antigua, Montserrat and Virgin Islands Gazette — openly−freely available, with searchable text and full page images
2.
French language
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French is a Romance language of the Indo-European family. It descended from the Vulgar Latin of the Roman Empire, as did all Romance languages, French has evolved from Gallo-Romance, the spoken Latin in Gaul, and more specifically in Northern Gaul. Its closest relatives are the other langues doïl—languages historically spoken in northern France and in southern Belgium, French was also influenced by native Celtic languages of Northern Roman Gaul like Gallia Belgica and by the Frankish language of the post-Roman Frankish invaders. Today, owing to Frances past overseas expansion, there are numerous French-based creole languages, a French-speaking person or nation may be referred to as Francophone in both English and French. French is a language in 29 countries, most of which are members of la francophonie. As of 2015, 40% of the population is in Europe, 35% in sub-Saharan Africa, 15% in North Africa and the Middle East, 8% in the Americas. French is the fourth-most widely spoken mother tongue in the European Union, 1/5 of Europeans who do not have French as a mother tongue speak French as a second language. As a result of French and Belgian colonialism from the 17th and 18th century onward, French was introduced to new territories in the Americas, Africa, most second-language speakers reside in Francophone Africa, in particular Gabon, Algeria, Mauritius, Senegal and Ivory Coast. In 2015, French was estimated to have 77 to 110 million native speakers, approximately 274 million people are able to speak the language. The Organisation internationale de la Francophonie estimates 700 million by 2050, in 2011, Bloomberg Businessweek ranked French the third most useful language for business, after English and Standard Mandarin Chinese. Under the Constitution of France, French has been the language of the Republic since 1992. France mandates the use of French in official government publications, public education except in specific cases, French is one of the four official languages of Switzerland and is spoken in the western part of Switzerland called Romandie, of which Geneva is the largest city. French is the language of about 23% of the Swiss population. French is also a language of Luxembourg, Monaco, and Aosta Valley, while French dialects remain spoken by minorities on the Channel Islands. A plurality of the worlds French-speaking population lives in Africa and this number does not include the people living in non-Francophone African countries who have learned French as a foreign language. Due to the rise of French in Africa, the total French-speaking population worldwide is expected to reach 700 million people in 2050, French is the fastest growing language on the continent. French is mostly a language in Africa, but it has become a first language in some urban areas, such as the region of Abidjan, Ivory Coast and in Libreville. There is not a single African French, but multiple forms that diverged through contact with various indigenous African languages, sub-Saharan Africa is the region where the French language is most likely to expand, because of the expansion of education and rapid population growth
3.
Bora Bora
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Bora Bora is a 29.3 km2 island in the Leeward group in the western part of the Society Islands of French Polynesia, an overseas collectivity of France in the Pacific Ocean. The island, located about 230 kilometres northwest of Papeete, is surrounded by a lagoon, in the centre of the island are the remnants of an extinct volcano rising to two peaks, Mount Pahia and Mount Otemanu, the highest point at 727 metres. Bora Bora is an international tourist destination, famous for its aqua-centric luxury resorts. The major settlement, Vaitape, is on the side of the main island. Produce of the island is limited to what can be obtained from the sea and the plentiful coconut trees. According to a 2008 census, Bora Bora has a permanent population of 8,880, in ancient times the island was called Pora pora mai te pora, meaning created by the gods in the local Tahitian dialect. This was often abbreviated Pora Pora meaning simply first born, because of ambiguities in the phonemes of the Tahitian language, this could also be pronounced Bola Bola or Bora Bora. When explorer Jacob Roggeveen first landed on the island, he, the island was inhabited by Polynesian settlers around the 4th century C. E. The first European sighting was made by Jakob Roggeveen in 1722, james Cook sighted the island in 1770 and landed that same year. The London Missionary Society arrived in 1820 and founded a Protestant church in 1890, Bora Bora was an independent kingdom until 1888 when its last queen Teriimaevarua III was forced to abdicate by the French who annexed the island as a colony. In World War II the United States chose Bora Bora as a South Pacific military supply base, and an oil depot, airstrip, seaplane base, and defensive fortifications were constructed. Known as Operation Bobcat, it maintained a force of nine ships,20,000 tons of equipment. Seven artillery guns were set up at points around the island to protect it against potential military attack. However, the island saw no combat as the American presence on Bora Bora went uncontested over the course of the war, the base was officially closed on June 2,1946. The atoll of Tupai has no permanent population apart from about 50 workers in the coconut plantations. The surrounding islets include, Motu Tapu, Motu Ahuna, Tevairoa, Motu Tane, Motu Mute, Motu Tufari, Motu Tehotu, Motu Pitiaau, Sofitel Motu, Motu Toopua, and Toopuaiti. The island is part of the commune of Bora-Bora, itself in the administrative subdivision of the Leeward Islands. President of French Polynesia Édouard Fritch is the current mayor of Bora Bora in addition to being the President, today the islands economy is driven almost solely by tourism
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.
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
6.
Society Islands
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The Society Islands includes a group of islands in the South Pacific Ocean. It is, politically and legally, part of French Polynesia and they have a population of 235,295 inhabitants. They cover an area of 1,590 square kilometres. The islanders explain their origins in term of a myth, the feathered god Taaroa lay in his shell. He called out but no-one answered, so he went back into his shell, when he came out he changed his body into the multi-layered dome of the sky. Other parts of his body he transformed into Papa-fenua, the earth, other parts he made into Te Tuma, the ata, or shadow of his phallus. Taaroa said, Cast your eyes on my phallus, gaze upon it and insert it in the earth. He came down to earth at Opoa in Havaii, one of the most sacred places in the Society Islands, other gods were created, and these ran directly into the time of the people. The high chiefs or arii rahi were descendants from the gods, in their presence commoners showed respect by stripping to the waist. The high chiefs erected marae as places of worship, in the generations before Europeans arrived, a cult called Oro-maro-ura developed, the cult of the red-feathered girdle. This became a symbol of the chiefs power. Key followers of the Oro cult were the arioi, who lived separately from the common people and they wore scented flowers and adorned themselves with scents and scarlet-dyed cloth. The head of each group was heavily tattooed from ankle to thigh. Both male and female blacklegs were a group but they were forbidden to have children. Their babies were all killed at birth and they received and gave lavish presents. They had a range of artistic skills and could be priests, navigators. Only good-looking men or women could become arioi and they played a crucial role in ceremonies associated with birth, deaths and marriage. The first European explorers arrived in 1722, jacob Roggeveens Dutch West Indian Expedition was shipwrecked on Takapoto
7.
Raiatea
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Raiātea, is the second largest of the Society Islands, after Tahiti, in French Polynesia. A traditional name for the island is believed to be Havaii, situated on the south east coast is the historical Taputapuātea which was established by 1000AD. The main township on Raiātea is Uturoa, the centre for the Leeward Islands. There are also colleges which serve as the main location for secondary schools for students from the regional islands of Pora Pora, Tahaa, Huahine. The proper spelling of the name in the Tahitian language is Raiātea, meaning bright sky, the extinct Ulieta bird originated from this island, along with other unknown species, there is only one drawing of it in the world which is in the Natural History Museum London. The islands of Raiātea and Tahaa are enclosed by a coral reef. Raiātea is both the largest and most populated island in the Leeward Islands, with an area of 167.7 km2. The population density is 72 inhabitants per km², the largest commune of Raiātea is Uturoa on the north side of Raiātea and has a population of nearly 10,000. The first European to record sighting Raiātea was Pedro Fernandes de Queirós in 1606, the Polynesian navigator, Tupaia, who sailed with explorer James Cook, was born in Raiātea around 1725. Omai, another man from Raiātea, travelled with European explorers to London in 1774 and also served as an interpreter to Captain Cook on his second. King Tamatoa VI was the last monarch, reigning from 1884-1888, Raiātea has a small road that runs around the entire island. Raiātea Airport is an airport in Uturoa, the island is divided into three administration communes, Uturoa Taputapuātea Tūmāraa These three communes are inside the administrative subdivision of the Leeward Islands. The island economy is agricultural with exports of vanilla, pineapple. The plant Nono is also grown, faaroa Valley is a large and important agricultural region with the rural economy and the cultivation of vanilla supported by a local research facility. Pearl farming is also an important industry while farming cattle, sheep, there is less tourism compared to the other islands in the archipelago. The local tourist infrastructure comprises boarding houses, two marinas, a four star hotel, The Hawaiki Nui and a port for visiting cruise ships, there is also a fledgling local industry in the maintenance of yachts and shipbuilding. The main source of employment is the public service and the consumer market. List of volcanoes in French Polynesia Hawaiki 48 hours live to tell and we had just left an island called Raiātea, which was about 300 miles west of Tahiti
8.
Huahine
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Huahine is an island located among the Society Islands, in French Polynesia, an overseas territory of France in the Pacific Ocean. It is part of the Leeward Islands group, the island has a population of about 6,300. Huahine measures 16 km in length, with a width of 13 km. It is made up of two main islands surrounded by a coral reef with several islets, or motu. Huahine Nui lies to the north and Huahine Iti to the south, the two islands are separated by a few hundred yards of water and joined by a sandspit at low tide. A small bridge was built to connect Huahine Nui and Huahine Iti, in the northwest of Huahine Nui lies a 375 hectares brackish lake known as Lac Fauna Nui. This lake is all that remains of the ancient atoll lagoon, air transportation is available via Huahine airport, located on the northern shore of Huahine Nui. Administratively Huahine is a part of the administrative subdivision of the Leeward Islands. Huahine consists of the associated communes, Faie Fare Fitii Haapu Maeva Maroe Parea Tefarerii The administrative centre of the commune is the settlement of Fare. One of the attractions on Huahine is a bridge that crosses over a stream with 0.9 m -1.8 m long freshwater eels. These eels are deemed sacred by the locals, by local mythology, while viewing these slithering creatures, tourists can buy a can of mackerel and feed the eels. The Faahia archaeological site in the north of the island has revealed remains of several species of extinct birds exterminated by the earliest Polynesian colonists of the island. List of monarchs of Huahine Tahiti Tourism Board website Tourism portal on Huahine Free travel guide - Bilingual french english - 2016-2017
9.
Taha'a
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Taha’a is an island located among the western group, the Leeward Islands, of the Society Islands in French Polynesia, an overseas territory of France in the Pacific Ocean. The islands of Taha’a and neighboring Raiatea to the south are enclosed by the same coral reef. Tahaa has 5,000 people living on 90 square kilometres and it is also known as the Vanilla Island and produces pearls of exceptional quality. Administratively, Taha’a and the surrounding islets emerging from the coral reef form a part of the administrative subdivision of the Leeward Islands. Tahaa consists of the associated communes, Faaaha Haamene Hipu Iripau Niua Ruutia Tapuamu Vaitoare The administrative centre of the commune of Tahaa is the settlement of Patio. Taha’a produces 70-80% of all French Polynesias vanilla, because of the pervasive aroma of vanilla, Taha’a is known as the Vanilla Island. Taha’as pearls are of exceptional quality, Taha’a and its small islets can be reached by boat and outrigger from Raiatea. The short sail drops visitors on a beach with a small lagoon, and in the near distance. These parts of the Society Islands are less modernized, Taha’a is spelled in Tahitian using the apostrophe to represent the glottal stop, as promoted by the Académie Tahitienne and accepted by the territorial government. This apostrophe, however, is often omitted, in old travelogues, the transcription Oataha is sometimes used
10.
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
11.
Uturoa
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Uturoa is a commune of French Polynesia, an overseas territory of France in the Pacific Ocean. The commune of Uturoa is located on the island of Raiatea, the Leeward Islands are themselves part of the Society Islands. Uturoa is the port of Raiatea Island. At the August 2007 census the area of Uturoa had 8,735 inhabitants,3,778 of which lived in the commune of Uturoa proper. Uturoa is about 200 km northwest of Papeete, the Tahitian capital, Raiatea Airport serves the island of Raiatea. The airport is located in eastern Uturoa and many of the islanders come here to travel to different islands, Raiatea Airport has one runway and Air Tahiti is the main airline at the airport. The runway is asphalt and stretches all the way to the side of the island. If the residents want to make a flight, they would take Air Tahiti to Faaa International Airport in Faaa. Sometimes ferries leave Raiatea and sail northward toward nearby Tahaa, other ferries sail to Vaitape/Bora Bora or Tahiti. Uturoa was first settled by early Polynesians coming from Southeast Asia, when the settlers first arrived, they had built houses of branches and grass. Fish, bananas, and apples were the food that the early Polynesians ate. They hunted fish by using spears and sticks, first European that recorded its sight was Pedro Fernandez de Quirós in 1606, it was charted as Fugitiva. During the 1700s, Captain James Cook had arrived in Tahiti, later on, Charles Darwin had come on his expedition. He explored Moorea and other Society Islands, don the Beachcomber had lived here some of his life. Uturoa had a population growth during the 1940s. Container ships and ferries are found throughout the harbour, the ferries sail to other Society Islands such as Bora Bora and Moorea. The harbour will remain relatively small because of the limited coast. The container ships bring in containers and put them into a special area, the containers have come from other countries
12.
Oceania
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Oceania, also known as Oceanica, is a region centred on the islands of the tropical Pacific Ocean. The term is used more specifically to denote a continent comprising Australia. The term was coined as Océanie circa 1812 by geographer Conrad Malte-Brun, the word Océanie is a French word derived from the Latin word oceanus, and this from the Greek word ὠκεανός, ocean. Natives and inhabitants of this region are called Oceanians or Oceanicans, as an ecozone, Oceania includes all of Micronesia, Fiji, and all of Polynesia except New Zealand. New Zealand, along with New Guinea and nearby islands, part of the Philippine islands, Australia, the Solomon Islands, Vanuatu, in geopolitical terms, however, New Zealand, the Solomon Islands, Vanuatu and New Caledonia are almost always considered part of Oceania. Australia and Papua New Guinea are usually considered part of Oceania along with the Maluku Islands, puncak Jaya in Papua is often considered the highest peak in Oceania. Oceania was originally conceived as the lands of the Pacific Ocean and it comprised four regions, Polynesia, Micronesia, Malaysia, and Melanesia. The area extends to Sumatra in the west, the Bonin Islands in the northwest, the Hawaiian Islands in the northeast, Rapa Nui and Sala y Gómez Island in the east, and Macquarie Island in the south. Not included are the Pacific islands of Taiwan, the Ryukyu Islands and the Japanese archipelago, all on the margins of Asia, and the Aleutian Islands of North America. The islands at the extremes of Oceania are Bonin, a politically integral part of Japan, Hawaii, a state of the United States. There is also a geographic definition that excludes land on the Sunda Plate. Biogeographically, Oceania is used as a synonym for either the Australasian ecozone or the Pacific ecozone, Oceania is one of eight terrestrial ecozones, which constitute the major ecological regions of the planet. The Oceania ecozone includes all of Micronesia, Fiji, and all of Polynesia except New Zealand, New Zealand, New Guinea, Melanesia apart from Fiji, and Australia constitute the separate Australasian ecozone. The Malay Archipelago is part of the Indomalaya ecozone, related to these concepts are Near Oceania, that part of western Island Melanesia which has been inhabited for tens of millennia, and Remote Oceania which is more recently settled. The term is used to denote a continent comprising Australia. New Zealand forms the corner of the Polynesian Triangle. Its indigenous Māori constitute one of the cultures of Polynesia. It is also, however, considered part of Australasia, the history of Oceania in the medieval period was synonymous with the history of the indigenous peoples of Australasia, Micronesia, Melanesia, Polynesia
13.
Kiribati
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Kiribati, officially the Republic of Kiribati, is an island nation in the central Pacific Ocean. The permanent population is just over 100,000, more than half of live on Tarawa Atoll. The nation comprises 33 atolls and reef islands and one raised coral island and they have a total land area of 800 square kilometres and are dispersed over 3.5 million square kilometers. Their spread straddles the equator and the 180th meridian, although the International Date Line is indented to bring the Line Islands in the day as the Kiribati Islands. The International Date Line circumscribes Kiribati by swinging far to the east, almost reaching the 150°W meridian, Kiribatis easternmost islands, the southern Line Islands south of Hawaii, have the most advanced time on Earth, UTC+14 hours. Kiribati became independent from the United Kingdom in 1979, the capital and now most populated area, South Tarawa, consists of a number of islets, connected by a series of causeways. These comprise about half the area of Tarawa Atoll, Kiribati is a member of the Commonwealth of Nations, the IMF and the World Bank, and became a full member of the United Nations in 1999. The name Kiribati was adopted at independence and it is local enunciation of Gilberts. This name derives from the archipelago that forms the nation. It was named the Gilbert Islands after the British explorer Thomas Gilbert and he sighted many of the islands in 1788 while mapping out the Outer Passage route from Port Jackson to Canton. The Kiribati archipelago was named Îles Gilbert, in about 1820, by Russian admiral Adam von Krusenstern, both their maps, published in 1820, were written in French. The archipelagos name was incorporated in the entire Gilbert and Ellice Islands Colony from 1916, the spelling of Gilberts in the Gilbertese language as Kiribati may be found in books in Gilbertese prepared by missionaries and others. It is often suggested that the name for the Gilbert Islands proper is Tungaru. The pronunciation differs, Kiribas is the pronunciation as ti in Kiribatese makes an s sound. The area now called Kiribati has been inhabited by Micronesians speaking the same Oceanic language since sometime between 3000 BC and AD1300, the area was not isolated, invaders from Samoa, Tonga, and Fiji, later introduced Polynesian and Melanesian cultural aspects, respectively. Intermarriage tended to blur cultural differences and resulted in a significant degree of cultural homogenisation, chance visits by European ships occurred in the 17th and 18th centuries, as these ships attempted circumnavigations of the world or sought sailing routes from the south to north Pacific Ocean. The passing trade gave rise to European, Chinese, Samoan and other residents from the 1830s, they included beachcombers, castaways, traders and missionaries. In 1892 local authorities on each of the Gilbert Islands agreed to Captain Davis RN declaring them part of a British protectorate with the nearby Ellice Islands
14.
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
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Austral Islands
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The Tuhaa Pae, or Austral Islands, are the southernmost group of islands in French Polynesia, an overseas collectivity of France in the South Pacific. Inhabitants of the islands are known for their pandanus fiber weaving skills, the islands of Maria and Marotiri are not suitable for sustained habitation. Several of the islands have uninhabited islets or rocks off their coastlines, Austral Islands population is about 6,300 on almost 150 km2. The capital of the Austral Islands administrative subdivision is Tupuai, the Tuhaa Pae or Austral Islands are the southernmost group of islands in French Polynesia, an overseas collectivity of France in the South Pacific. Geographically, the Austral Islands consist of two separate archipelagos, from northwest to southeast they are, The Tupuai Islands, named for one of the main islands. Several of the islands have uninhabited islets or rocks off their coastlines, the chain is associated with the Macdonald hotspot. The only active volcano is the Macdonald seamount, in administrative terms, the Austral Islands constitute an administrative subdivision, the Tuhaa Pae or Austral Islands, one of French Polynesias five administrative subdivisions. The capital of the Austral Islands administrative subdivision is Tupuai. com satellite images at the Wayback Machine
16.
Manuae (Society Islands)
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The atoll of Manuae, also known as Scilly, is located approximately 60 km to the northwest of Maupihaa and 255 km to the west of Maupiti. It is the westernmost of the Society Islands Leeward Islands, located 217 mi. west of Bora Bora and 342 mi. west of Papeete. Manuae consists of a ring of islands approximately 6–7 mi. in diameter, separated by unnavigable passages, the motus are covered primarily with coconut palms and tropical scrub with sandy beaches, and comprise a total land area of about 3.5 km2. The atoll is part of the commune of Maupiti, itself in the administrative subdivision of the Leeward Islands. The atolls lagoon, home to a number of species, has been a nature reserve since 1992. The beaches are popular with sea turtles, including the endangered Green Sea Turtle, the atoll is also home to large oyster beds, containing up to 3 or 4 million oysters. Manuaes first European visitor was British navigator Samuel Wallis, in 1767, a small village was established there at the time, the remains of which can still be found on the northern part of the main island. The atoll was the site of the 1855 shipwreck of the three-masted Julia Ann. Its crew and passengers, including women and children, lived on the atoll for two months, during which time they were able to build a boat with which they were able to sail to Raiātea. Beginning in 1952, the islands were visited by copra merchants. During the 1960s, these casual visitors began capturing large numbers of sea turtles until their activities were restricted in 1971. Today the atoll is visited regularly by fishermen from Raiātea, the now-abandoned plantation once produced up to 70 tons of copra annually. On June 25,2005, the Silverwood family of California crashed into the reef in a 55-foot catamaran, the Emerald Jane. Thanks to an EPIRB distress call, the family was spotted by a French Navy airplane, picked up by the resident Taputo family, john Silverwood, the captain of the Emerald Jane, would lose his leg, and the experience is described in the book Black Wave. It was also featured in an episode of I Shouldnt Be Alive, other names given to Manuae include Fenua Ura and Putai, Isla de Pájaros, and Scilly. Maupiti Classification of the French Polynesian atolls by Salvat Manuae at partenaire-info. net Lesser known Society Islands at colonialvoyage. com
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Motu One (Society Islands)
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Motu One, also known as Bellinghausen, is an atoll in the Leeward group of the Society Islands. Motu One is located 550 km northwest from Tahiti and 72 km northeast of Manuae, motu Ones reef encloses totally a lagoon without a pass. All of its sides are covered with low, wooded sandy islands except for its southern side, motu One means Sand Island in Polynesian, that is a low-lying, sandy islet that cannot sustain permanent human habitation. The name Bellinghausen or more rarely Bellingshausen was given to this small atoll by the Baltic German navigator in Russian service Otto von Kotzebue in honour of Fabian Gottlieb von Bellingshausen. It should not be confused with Bellingshausen Island, part of the South Sandwich Islands, motu One Atoll is administratively part of the commune of Maupiti, itself in the administrative subdivision of the Leeward Islands. French Polynesia Atoll list Oceandots. com at the Wayback Machine
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Maupihaa
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Maupihaa, also known as Mopelia, is an atoll in the Leeward group of the Society Islands. This atoll is located 72 km southeast of Manuae, its nearest neighbor, Maupihaa atoll is roughly 8 km in length and contains a lagoon that is up to 40 m in depth and is surrounded by submerged reefs on three sides. The atolls outer reefs are continuous except for a passage on the western side of the atoll. The eastern side consists of a narrow, thickly vegetated, islet, the only village on the atoll is located on Motu Maupihaa and as of 1985, the population consisted of just 10 people. Maupihaa Atoll was inhabited in ancient times by Polynesians, archaeological remains. The first European to arrive on Maupihaa, along with neighboring Fenua Ura, in 1917, the atoll was leased to a Papeete company, with three employees producing copra, and raising pigs and chickens and collecting turtles. It was later leased to another company and entirely planted with coconut palms. The purpose of the stop was to obtain water and fresh stores and to make repairs to the Seeadlers hull after a journey through the Atlantic Ocean. Since SMS Seeadler was too large to enter Mopelia lagoon, she was anchored on the outside of the atoll, after a short time, rough seas and wind caused the Seeadler to run aground on Mopelias reef, leaving Luckner and about 50 others marooned. In Lowell Thomas 1928 book on von Luckner he reports that the loss of Seeadler was the consequence of a tsunami, some of the stranded sailors were American prisoners of war who were captured on the ocean by Luckners raiders. However, the plan did not work well, for while Luckner was able to reach his destination. Four American seamen then sailed an open boat 1,000 mi to Pago Pago, the atoll is administratively part of the commune of Maupiti, itself in the administrative subdivision of the Leeward Islands. Presently Maupihaa is listed as permanently uninhabited, Mopelia Maupelia Mopihaa Maupihoa Mapetia Atoll list
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High island
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In geology, a high island or volcanic island is an island of volcanic origin. The term can be used to such islands from low islands. Volcanic islands normally arise above a so-called hotspot and this hampers or hinders human settlement on many low islands. Atoll Low island Volcanic arc Micronesian culture, High island and low island cultures at Britannica. com
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Maupiti
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For the administrative commune which includes the island, see Maupiti, for the video game, see Maupiti Island Maupiti is a small coral atoll with a volcanic island in its midst. It has a population of 1,200 people living on 11 square kilometres Maupiti is located in the western Leeward Islands in French Polynesia and it is the westernmost volcanic high island in the archipelago,40 kilometres west of Bora Bora. The central island of Maupiti has a peak of 380 metres. The lagoon has large and flat coral islands in its northern reef half, at the August 2007 census, the island population was about 1,200 people. The primary economic activity on Maupiti is noni production, there are ancient Polynesian archaeological artifacts dating from at least AD850 in Maupiti. The first European to arrive on the island was the Dutchman Jakob Roggeveen in 1722, historically, the island has had strong cultural links with Bora Bora. Maupiti is administratively part of the commune of Maupiti, itself in the subdivision of the Leeward Islands
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Western world
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The Western world or the West is a term usually referring to different nations, depending on the context, most often including at least part of Europe. There are many accepted definitions about what they all have in common, the Western world is also known as the Occident. The concept of the Western part of the earth has its roots in Greco-Roman civilization in Europe, before the Cold War era, the traditional Western viewpoint identified Western Civilization with the Western Christian countries and culture. Its political usage was changed by the antagonism during the Cold War in the mid-to-late 20th Century. The term originally had a literal geographic meaning, Western culture was influenced by many older great civilizations of the ancient Near East, such as Phoenicia, Minoan Crete, Sumer, Babylonia, and also Ancient Egypt. It originated in the Mediterranean basin and its vicinity, Greece, over time, their associated empires grew first to the east and west to include the rest of Mediterranean and Black Sea coastal areas, conquering and absorbing. Later, they expanded to the north of the Mediterranean Sea to include Western, Central, numerous times, this expansion was accompanied by Christian missionaries, who attempted to proselytize Christianity. There is debate among some as to whether Latin America is in a category of its own, specifically, Western culture may imply, a Biblical Christian cultural influence in spiritual thinking, customs and either ethic or moral traditions, around the Post-Classical Era and after. European cultural influences concerning artistic, musical, folkloric, ethic and oral traditions, the concept of Western culture is generally linked to the classical definition of the Western world. In this definition, Western culture is the set of literary, scientific, political, artistic, much of this set of traditions and knowledge is collected in the Western canon. The term has come to apply to countries whose history is marked by European immigration or settlement, such as the Americas, and Oceania. The geopolitical divisions in Europe that created a concept of East and West originated in the Roman Empire, Roman Catholic Western and Central Europe, as such, maintained a distinct identity particularly as it began to redevelop during the Renaissance. Even following the Protestant Reformation, Protestant Europe continued to see itself as more tied to Roman Catholic Europe than other parts of the civilized world. Use of the term West as a cultural and geopolitical term developed over the course of the Age of Exploration as Europe spread its culture to other parts of the world. Additionally, closer contacts between the West and Asia and other parts of the world in recent times have continued to cloud the use, herodotus considered the Persian Wars of the early 5th century BC a conflict of Europa versus Asia. The terms West and East were not used by any Greek author to describe that conflict, the Great Schism and the Fourth Crusade confirmed this deviation. The Renaissance in the West emerged partly from currents within the Roman Empire, Ancient Rome was a civilization that grew from a city-state founded on the Italian Peninsula about the 9th century BC to a massive empire straddling the Mediterranean Sea. In its 12-century existence, Roman civilization shifted from a monarchy, to a republic, nonetheless, despite its great legacy, a number of factors led to the eventual decline of the Roman Empire
22.
World War II
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World War II, also known as the Second World War, was a global war that lasted from 1939 to 1945, although related conflicts began earlier. It involved the vast majority of the worlds countries—including all of the great powers—eventually forming two opposing alliances, the Allies and the Axis. It was the most widespread war in history, and directly involved more than 100 million people from over 30 countries. Marked by mass deaths of civilians, including the Holocaust and the bombing of industrial and population centres. These made World War II the deadliest conflict in human history, from late 1939 to early 1941, in a series of campaigns and treaties, Germany conquered or controlled much of continental Europe, and formed the Axis alliance with Italy and Japan. Under the Molotov–Ribbentrop Pact of August 1939, Germany and the Soviet Union partitioned and annexed territories of their European neighbours, Poland, Finland, Romania and the Baltic states. In December 1941, Japan attacked the United States and European colonies in the Pacific Ocean, and quickly conquered much of the Western Pacific. The Axis advance halted in 1942 when Japan lost the critical Battle of Midway, near Hawaii, in 1944, the Western Allies invaded German-occupied France, while the Soviet Union regained all of its territorial losses and invaded Germany and its allies. During 1944 and 1945 the Japanese suffered major reverses in mainland Asia in South Central China and Burma, while the Allies crippled the Japanese Navy, thus ended the war in Asia, cementing the total victory of the Allies. World War II altered the political alignment and social structure of the world, the United Nations was established to foster international co-operation and prevent future conflicts. The victorious great powers—the United States, the Soviet Union, China, the United Kingdom, the Soviet Union and the United States emerged as rival superpowers, setting the stage for the Cold War, which lasted for the next 46 years. Meanwhile, the influence of European great powers waned, while the decolonisation of Asia, most countries whose industries had been damaged moved towards economic recovery. Political integration, especially in Europe, emerged as an effort to end pre-war enmities, the start of the war in Europe is generally held to be 1 September 1939, beginning with the German invasion of Poland, Britain and France declared war on Germany two days later. The dates for the beginning of war in the Pacific include the start of the Second Sino-Japanese War on 7 July 1937, or even the Japanese invasion of Manchuria on 19 September 1931. Others follow the British historian A. J. P. Taylor, who held that the Sino-Japanese War and war in Europe and its colonies occurred simultaneously and this article uses the conventional dating. Other starting dates sometimes used for World War II include the Italian invasion of Abyssinia on 3 October 1935. The British historian Antony Beevor views the beginning of World War II as the Battles of Khalkhin Gol fought between Japan and the forces of Mongolia and the Soviet Union from May to September 1939, the exact date of the wars end is also not universally agreed upon. It was generally accepted at the time that the war ended with the armistice of 14 August 1945, rather than the formal surrender of Japan
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Tourism
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Tourism is travel for pleasure or business, also the theory and practice of touring, the business of attracting, accommodating, and entertaining tourists, and the business of operating tours. Tourism may be international, or within the travellers country, Tourism can be domestic or international, and international tourism has both incoming and outgoing implications on a countrys balance of payments. Today, tourism is a source of income for many countries. International tourism receipts grew to US$1.03 trillion in 2011, the ITB Berlin is the worlds leading tourism trade fair. The word tourist was used by 1772 and tourism by 1811. It is formed from the tour, which is derived from Old English turian, from Old French torner, from Latin tornare, to turn on a lathe. Tourism is an important, even vital, source of income for many regions and it also creates opportunities for employment in the service sector of the economy associated with tourism. This is in addition to goods bought by tourists, including souvenirs, in 1936, the League of Nations defined a foreign tourist as someone traveling abroad for at least twenty-four hours. Its successor, the United Nations, amended this definition in 1945 and it includes movements for all purposes. In 1981, the International Association of Scientific Experts in Tourism defined tourism in terms of particular activities chosen and undertaken outside the home, in this context, travel has a similar definition to tourism, but implies a more purposeful journey. The terms tourism and tourist are sometimes used pejoratively, to imply a shallow interest in the cultures or locations visited, by contrast, traveler is often used as a sign of distinction. The sociology of tourism has studied the values underpinning these distinctions. International tourist arrivals reached 1.035 billion in 2012, up from over 996 million in 2011, the World Tourism Organization reports the following ten destinations as the most visited in terms of the number of international travellers in 2016. International tourism receipts grew to US$1.2 trillion in 2014, based upon air traffic, the MasterCard Global Destination Cities Index reports the following cities as the top ten most popular destinations of international tourism worldwide. MasterCard reports the following cities as the top ten biggest earners on international tourism worldwide in 2015, as early as Shulgi, however, kings praised themselves for protecting roads and building waystations for travelers. During the Roman Republic, spas and coastal resorts such as Baiae were popular among the rich, pausanias wrote his Description of Greece in the 2nd century AD. In ancient China, nobles sometimes made a point of visiting Mount Tai and, on occasion, the Islamic hajj is still central to its faith and Chaucers Canterbury Tales and Wu Chengens Journey to the West remain classics of English and Chinese literature. The 10th- to 13th-century Song dynasty also saw secular travel writers such as Su Shi, under the Ming, Xu Xiake continued the practice
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Tide
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Tides are the rise and fall of sea levels caused by the combined effects of the gravitational forces exerted by the Moon and the Sun and the rotation of the Earth. Some shorelines experience a semi-diurnal tide—two nearly equal high and low tides each day, other locations experience a diurnal tide—only one high and low tide each day. A mixed tide—two uneven tides a day, or one high, Tides vary on timescales ranging from hours to years due to a number of factors. To make accurate records, tide gauges at fixed stations measure water level over time, gauges ignore variations caused by waves with periods shorter than minutes. These data are compared to the level usually called mean sea level. Tidal phenomena are not limited to the oceans, but can occur in other systems whenever a gravitational field varies in time. For example, the part of the Earth is affected by tides. Tide changes proceed via the following stages, Sea level rises over several hours, covering the intertidal zone, the water rises to its highest level, reaching high tide. Sea level falls over several hours, revealing the intertidal zone, the water stops falling, reaching low tide. Oscillating currents produced by tides are known as tidal streams, the moment that the tidal current ceases is called slack water or slack tide. The tide then reverses direction and is said to be turning, slack water usually occurs near high water and low water. But there are locations where the moments of slack tide differ significantly from those of high, Tides are commonly semi-diurnal, or diurnal. The two high waters on a day are typically not the same height, these are the higher high water. Similarly, the two low waters each day are the low water and the lower low water. The daily inequality is not consistent and is small when the Moon is over the equator. From the highest level to the lowest, Highest Astronomical Tide – The highest tide which can be predicted to occur, note that meteorological conditions may add extra height to the HAT. Mean High Water Springs – The average of the two high tides on the days of spring tides, mean High Water Neaps – The average of the two high tides on the days of neap tides. Mean Sea Level – This is the sea level
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Archipelago
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An archipelago, sometimes called an island group or island chain, is a chain, cluster or collection of islands. The word archipelago is derived from the Greek ἄρχι- – arkhi-, in Italian, possibly following a tradition of antiquity, the Archipelago was the proper name for the Aegean Sea and, later, usage shifted to refer to the Aegean Islands. It is now used to refer to any group or, sometimes. Archipelagos may be isolated in large amounts of water or neighbouring a large land mass. For example, Scotland has more than 700 islands surrounding its mainland which form an archipelago, archipelagos are often volcanic, forming along island arcs generated by subduction zones or hotspots, but may also be the result of erosion, deposition, and land elevation. Depending on their origin, islands forming archipelagos can be referred to as oceanic islands, continental fragments. Oceanic islands are mainly of volcanic origin, continental fragments correspond to land masses that have separated from a continental mass due to tectonic displacement. Indonesia, Japan, Taiwan, the Philippines, New Zealand, Maldives, the Bahamas, Greece, Hawaii, the largest archipelagic state in the world by area and population is Indonesia. Island arc List of landforms List of archipelagos by number of islands List of archipelagos List of islands Chisholm, Hugh, ed. Archipelago
26.
Assembly of French Polynesia
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The Assembly of French Polynesia is the unicameral legislature of French Polynesia, located at the Place Tarahoi in Papeete, Tahiti. It consists of 57 members who are elected by popular vote, the only official language of the Assembly is French. The most recent election was in 2013, the number of seats was changed from 49 seats to 57 seats on 23 May 2004, for the 2004 election. On February 13,2005, by-elections for the Assembly in the constituency of the Windward Islands were held. The next elections are to be held May 2009, the members of the Assembly of French Polynesia are elected in 6 different multi-seat constituencies or electoral districts or electoral circumscriptions. Every electoral circumsription of French Polynesia is represented in the Assembly of French Polynesia by at least 3 representatives, since the territorial elections of March 6,2001, the parity bill now binds that the number of women matches the number of men at the Assembly. Antony Géros - May 9,2004 - April 12,2006 Philip Schyle - April 14,2006 - April 12,2007 Édouard Fritch - April 12,2007 -
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Politics of French Polynesia
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Executive power is exercised by the government. Legislative power is vested in both the government and the Assembly of French Polynesia, between 1946 and 2003, French Polynesia had the status of an overseas territory. In 2003 it became an overseas collectivity and its statutory law of 27 February 2004 gives it the particular designation of overseas country to underline the large autonomy of the territory. The President of the French Republic is represented by the High Commissioner of the Republic in French Polynesia, the government is headed by the President of French Polynesia. He submits as Council of Ministers a list of members of the Territorial Assembly, French Polynesia elects the Assembly of French Polynesia, the unicameral legislature on the territorial level. The Assembly of French Polynesia has 57 members, elected for a term by proportional representation in multi-seat constituencies. Since the territorial elections of March 6,2001, the parity bill now binds that the number of matches the number of men at the Assembly
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James Cook
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Captain James Cook FRS RN was a British explorer, navigator, cartographer, and captain in the Royal Navy. Cook joined the British merchant navy as a teenager and joined the Royal Navy in 1755 and he saw action in the Seven Years War, and subsequently surveyed and mapped much of the entrance to the Saint Lawrence River during the siege of Quebec. This helped bring Cook to the attention of the Admiralty and Royal Society, in three voyages Cook sailed thousands of miles across largely uncharted areas of the globe. He mapped lands from New Zealand to Hawaii in the Pacific Ocean in greater detail, as he progressed on his voyages of discovery he surveyed and named features, and recorded islands and coastlines on European maps for the first time. He displayed a combination of seamanship, superior surveying and cartographic skills, physical courage, Cook was attacked and killed while attempting to kidnap the native chief of Hawaii during his third exploratory voyage in the Pacific in 1779. He left a legacy of scientific and geographical knowledge which was to influence his successors well into the 20th century, and numerous memorials worldwide have been dedicated to him. James Cook was born on 7 November 1728 in the village of Marton in Yorkshire and baptised on 14 November in the church of St Cuthbert. He was the second of eight children of James Cook, a Scottish farm labourer from Ednam in Roxburghshire, in 1736, his family moved to Airey Holme farm at Great Ayton, where his fathers employer, Thomas Skottowe, paid for him to attend the local school. In 1741, after five years schooling, he work for his father. For leisure, he would climb a hill, Roseberry Topping, enjoying the opportunity for solitude. Cooks Cottage, his parents last home, which he is likely to have visited, is now in Melbourne, having moved from England and reassembled, brick by brick. In 1745, when he was 16, Cook moved 20 miles to the village of Staithes. Historians have speculated that this is where Cook first felt the lure of the sea while gazing out of the shop window. After 18 months, not proving suitable for work, Cook travelled to the nearby port town of Whitby to be introduced to friends of Sandersons, John. The Walkers, who were Quakers, were prominent local ship-owners in the coal trade and their house is now the Captain Cook Memorial Museum. Cook was taken on as a merchant navy apprentice in their fleet of vessels. His first assignment was aboard the collier Freelove, and he spent several years on this and various other coasters, sailing between the Tyne and London. As part of his apprenticeship, Cook applied himself to the study of algebra, geometry, trigonometry, navigation and his three-year apprenticeship completed, Cook began working on trading ships in the Baltic Sea
29.
Transit of Venus
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A transit of Venus across the Sun takes place when the planet Venus passes directly between the Sun and a superior planet, becoming visible against the solar disk. During a transit, Venus can be seen from Earth as a black disk moving across the face of the Sun. The duration of such transits is usually measured in hours, a transit is similar to a solar eclipse by the Moon. While the diameter of Venus is more than 3 times that of the Moon, Venus appears smaller, Transits of Venus are among the rarest of predictable astronomical phenomena. They occur in a pattern that repeats every 243 years. The periodicity is a reflection of the fact that the periods of Earth. The last transit of Venus was on 5 and 6 June 2012, and was the last Venus transit of the 21st century, the previous pair of transits were in December 1874 and December 1882. The next transits of Venus will be on 10–11 December 2117, Venus transits are historically of great scientific importance as they were used to gain the first realistic estimates of the size of the Solar System. Observations of the 1639 transit, combined with the principle of parallax, the 2012 transit provided scientists with a number of other research opportunities, particularly in the refinement of techniques to be used in the search for exoplanets. Venus, with an orbit inclined by 3. 4° relative to the Earths, although the inclination between these two orbital planes is only 3. 4°, Venus can be as far as 9. 6° from the Sun when viewed from the Earth at inferior conjunction. Since the angular diameter of the Sun is about half a degree, sequences of transits usually repeat every 243 years. After this period of time Venus and Earth have returned to nearly the same point in their respective orbits. During the Earths 243 sidereal orbital periods, which total 88,757.3 days, Venus completes 395 sidereal orbital periods of 224.701 days each and this period of time corresponds to 152 synodic periods of Venus. Prior to 1518, the pattern of transits was 8,113.5 and 121.5 years, the current pattern will continue until 2846, when it will be replaced by a pattern of 105.5,129.5 and 8 years. Thus, the 243-year cycle is relatively stable, but the number of transits, for instance, there is a series which ended in 541 BC, and the series which includes 2117 only started in AD1631. Ancient Indian, Greek, Egyptian, Babylonian and Chinese observers knew of Venus, the early Greek astronomers called Venus by two names—Hesperus the evening star and Phosphorus the morning star. Pythagoras is credited with realizing they were the same planet, there is no evidence that any of these cultures knew of the transits. Venus was important to ancient American civilizations, in particular for the Maya, who called it Noh Ek, the Great Star or Xux Ek, the Wasp Star, they embodied Venus in the form of the god Kukulkán
30.
Royal Society
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Founded in November 1660, it was granted a royal charter by King Charles II as The Royal Society. The society is governed by its Council, which is chaired by the Societys President, according to a set of statutes and standing orders. The members of Council and the President are elected from and by its Fellows, the members of the society. As of 2016, there are about 1,600 fellows, allowed to use the postnominal title FRS, there are also royal fellows, honorary fellows and foreign members, the last of which are allowed to use the postnominal title ForMemRS. The Royal Society President is Venkatraman Ramakrishnan, who took up the post on 30 November 2015, since 1967, the society has been based at 6–9 Carlton House Terrace, a Grade I listed building in central London which was previously used by the Embassy of Germany, London. The Royal Society started from groups of physicians and natural philosophers, meeting at variety of locations and they were influenced by the new science, as promoted by Francis Bacon in his New Atlantis, from approximately 1645 onwards. A group known as The Philosophical Society of Oxford was run under a set of rules still retained by the Bodleian Library, after the English Restoration, there were regular meetings at Gresham College. It is widely held that these groups were the inspiration for the foundation of the Royal Society, I will not say, that Mr Oldenburg did rather inspire the French to follow the English, or, at least, did help them, and hinder us. But tis well known who were the men that began and promoted that design. This initial royal favour has continued and, since then, every monarch has been the patron of the society, the societys early meetings included experiments performed first by Hooke and then by Denis Papin, who was appointed in 1684. These experiments varied in their area, and were both important in some cases and trivial in others. The Society returned to Gresham in 1673, there had been an attempt in 1667 to establish a permanent college for the society. Michael Hunter argues that this was influenced by Solomons House in Bacons New Atlantis and, to a lesser extent, by J. V. The first proposal was given by John Evelyn to Robert Boyle in a letter dated 3 September 1659, he suggested a scheme, with apartments for members. The societys ideas were simpler and only included residences for a handful of staff and these plans were progressing by November 1667, but never came to anything, given the lack of contributions from members and the unrealised—perhaps unrealistic—aspirations of the society. During the 18th century, the gusto that had characterised the early years of the society faded, with a number of scientific greats compared to other periods. The pointed lightning conductor had been invented by Benjamin Franklin in 1749, during the same time period, it became customary to appoint society fellows to serve on government committees where science was concerned, something that still continues. The 18th century featured remedies to many of the early problems
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Tahiti
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Tahiti is the largest island in the Windward group of French Polynesia, this overseas collectivity of the French Republic is sometimes referred to as a French overseas country. The island was formed from volcanic activity and is high and mountainous with surrounding coral reefs, the population is 183,645 inhabitants, making it the most populous island of French Polynesia and accounting for 68.5 percent of its total population. Tahiti is the economic, cultural and political centre of French Polynesia, the capital, Papeete, is located on the northwest coast with the only international airport in the region, Faaā International Airport, situated 5 km from the town centre. Tahiti was originally settled by Polynesians between 300 and 800 CE and they represent about 70 percent of the islands population with the rest made up of Europeans, Chinese and those of mixed heritage. The island was part of the Kingdom of Tahiti until its annexation by France in 1880, when it was proclaimed a colony of France, French is the only official language although the Tahitian language is widely spoken. Tahiti is the highest and largest island in French Polynesia lying close to Moorea island and it is located 4,400 kilometres south of Hawaii,7,900 km from Chile and 5,700 km from Australia. The island is 45 km across at its widest point and covers an area of 1,045 km2, the highest peak is Mont Orohena. Mount Roonui, or Mount Ronui in the southeast rises to 1,332 m, the island consists of two roughly round portions centred on volcanic mountains and connected by a short isthmus named after the small town of Taravao, situated there. The northwestern portion is known as Tahiti Nui, while the much smaller portion is known as Tahiti Iti or Taiarapū. Tahiti Nui is heavily populated along the coast, especially around the capital, the interior of Tahiti Nui is almost entirely uninhabited. Tahiti Iti has remained isolated, as its half is accessible only to those travelling by boat or on foot. The rest of the island is encircled by a road which cuts between the mountains and the sea. A scenic and winding road climbs past dairy farms and citrus groves with panoramic views. Tahitis landscape features lush rainforests and many rivers and waterfalls, including the Papenoo River on the side. November to April is the wet season, the wettest month of which is January with 13.2 in of rain in Papeetē, August is the driest with 1.9 inches. The average temperature ranges between 21 and 31 °C with little seasonal variation, the lowest and highest temperatures recorded in Papeete are 16 and 34 °C, respectively. The first Tahitians arrived from Southeast Asia in about 200 BCE and this hypothesis of an emigration from Southeast Asia is supported by a number of linguistic, biological and archaeological proofs. For example, the languages of Fiji and Polynesia all belong to the same Oceanic sub-group, Fijian-Polynesian, in 1769, for instance, James Cook mentions a great traditional ship in Tahiti that was 33 m long, and could be propelled by sail or paddles
32.
Colony
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In politics and history, a colony is a territory under the immediate political control of a state, distinct from the home territory of the sovereign. For colonies in antiquity, city-states would often found their own colonies, some colonies were historically countries, while others were territories without definite statehood from their inception. The metropolitan state is the state that rules the colony, in Ancient Greece, the city that founded a colony was known as the metropolis. Mother country is a reference to the state from the point of view of citizens who live in its colony. There is a United Nations list of Non-Self-Governing Territories, unlike a puppet state or satellite state, a colony has no independent international representation, and its top-level administration is under direct control of the metropolitan state. The term informal colony is used by historians to refer to a country under the de facto control of another state. The word colony comes from the Latin word colōnia and this in turn derives from the word colōnus, which means colonist but also implies a farmer. Cologne is an example of a settlement preserving this etymology, other, less obvious settlements that began as Roman colonia include cities from Belgrade to York. A tell-tale sign of a settlement once being a Roman Colony is a city centre with a grid pattern. The terminology is taken from architectural analogy, where a column pillar is beneath the head capital, so colonies are not independently self-controlled, but rather are controlled from a separate entity that serves the capital function. Roman colonies first appeared when the Romans conquered neighbouring Italic peoples and these were small farming settlements that appeared when the Romans had subdued an enemy in war. A colony could take many forms, as a trade outpost or a base in enemy territory. Its original definition as a settlement created by migrating from a central region to an outlying one became the modern definition. Kandahar formed as a Greek colony during the Hellenistic era by Alexander the great in 330 BC, alaska, a colony of Russia from the middle 18th century until sold to the United States in 1867. It became the 49th American state in 1959, angola, a colony of Portugal since the 16th century. Australia was formed as an independent country in 1901 from a federation of six distinct British colonies which were founded between 1788 and 1829, barbados, was a colony of Great Britain important in the Atlantic slave trade. It gained its independence in 1966, brazil, a colony of Portugal since the 16th century. Canada, colonized first by France as New France, then under British rule, congo, Democratic Republic of the, a colony of Belgium from 1908 to 1960
33.
Windward Islands (Society Islands)
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The Windward Islands are the eastern group of the Society Islands in French Polynesia, an overseas collectivity of France in the southern Pacific Ocean. These islands were named the Georgian Islands in honor of King George III of England. Tahiti, Moorea, and Mehetia are high islands, tetiaroa and Maiao are coral atolls. The majority of the population speaks French and Tahitian, administratively, the Windward Islands form the administrative subdivision of the Windward Islands, one of French Polynesias five administrative subdivisions
34.
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
35.
Trachyte
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Trachyte is an igneous volcanic rock with an aphanitic to porphyritic texture. It is the equivalent of syenite. The mineral assemblage consists of essential alkali feldspar, relatively minor plagioclase, biotite, clinopyroxene and olivine are common accessory minerals. Chemically, trachyte contains 60 to 65% silica content, less SiO2 than rhyolite and these chemical differences are consistent with the position of trachyte in the TAS classification, and they account for the feldspar-rich mineralogy of the rock type. Trachytes usually consist mainly of sanidine feldspar, very often they have minute irregular steam cavities which make the broken surfaces of specimens of these rocks rough and irregular, and from this character they have derived their name. The trachytes are often described as being the equivalents of the plutonic syenites. Rhomb porphyry is an example with usually large porphyritic rhomb shaped phenocrysts embedded in a very fine-grained matrix, quartz is typically rare in trachyte, but tridymite is by no means uncommon. They often cover the surfaces of the larger feldspars or line the cavities of the rock. In the older trachytes, secondary quartz is not rare, of the mafic minerals present, augite is the most common. It is usually of pale color, and its small crystals are often very perfect in form. Olivine is unusual, though found in some trachytes, like those of the Arso in Ischia, basic varieties of plagioclase, such as labradorite, are known also as phenocrysts in some Italian trachytes. Dark brown varieties of augite and rhombic pyroxene have been observed but are not common, apatite, zircon and magnetite are practically always present as accessory minerals. Trachytes, being rich in potassium feldspar, necessarily contain considerable amounts of alkali. Occasionally minerals of the group, such as nepheline, sodalite and leucite, occur. In many trachytes, however, the phenocrysts are few and small, the ferromagnesian minerals rarely occur in large crystals, and are usually not conspicuous in hand specimens of these rocks. Sometimes granular augite or spongy riebeckite occurs in the groundmass, trachytes are well represented among the Cenozoic volcanic rocks of Europe. In the neighborhood of Rome, Naples and the island of Ischia trachytic lavas, trachytes are also found on the island of Pantelleria. In the United States, trachytes crop out extensively in the Davis Mountains, Chisos Mountains, in England there are Permian trachytes in the Exeter district, and Carboniferous trachytes are found in many parts of the central valley of Scotland
36.
Dolerite
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Diabase or dolerite or microgabbro is a mafic, holocrystalline, subvolcanic rock equivalent to volcanic basalt or plutonic gabbro. Diabase dikes and sills are typically shallow intrusive bodies and often exhibit fine grained to aphanitic chilled margins which may contain tachylite. Diabase normally has a fine, but visible texture of euhedral lath-shaped plagioclase crystals set in a matrix of clinopyroxene, typically augite, with minor olivine, magnetite. Accessory and alteration minerals include hornblende, biotite, apatite, pyrrhotite, chalcopyrite, serpentine, chlorite, the texture is termed diabasic and is typical of diabases. This diabasic texture is also termed interstitial, the feldspar is high in anorthite, the calcium endmember of the plagioclase anorthite-albite solid solution series, most commonly labradorite. Diabase is usually found in relatively shallow intrusive bodies such as dikes. Diabase dikes occur in regions of crustal extension and often occur in swarms of hundreds of individual dikes or sills radiating from a single volcanic center. The Palisades Sill which makes up the New Jersey Palisades on the Hudson River, parts of the Deccan Traps of India, formed at the end of the Cretaceous also includes dolerite. It is also abundant in parts of Curaçao, an island off the coast of Venezuela. West of the Norseman–Wiluna Belt is the Yalgoo–Singleton Belt, where complex dolerite dike swarms obscure the volcaniclastic sediments, large dolerite sills such as the Golden Mile Dolerite can exhibit course grained texture, and show a large diversity in petrography and geochemistry across the width of the sill. The vast areas of mafic volcanism/plutonism associated with the Jurassic breakup of Gondwanaland in the Southern Hemisphere include many large diabase/dolerite sills and dike swarms. These include the Karoo dolerites of South Africa, the Ferrar Dolerites of Antarctica, in Tasmania dolerite dominates much of the landscape, particularly alpine areas. Ring dikes are large, near vertical dikes showing above ground as circular outcrops up to 30 km in diameter, thicker dikes are made up of plutonic rocks, rather than hypabyssal and are centred on deep intrusions. Diabase is crushed and used as an aggregate for road beds, buildings, railroad beds. Diabase can also be cut for use as as ornamental stone for countertops, facing stone on buildings, a form of dolerite, known as bluestone, is one of the materials used as in the construction of Stonehenge. In Tasmania, being one of the most common rocks found, it has used as a building stone, for landscaping. List of rock types Collection of dikes in the Fish River Canyon, Namibia
37.
Basalt
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Basalt is a common extrusive igneous rock formed from the rapid cooling of basaltic lava exposed at or very near the surface of a planet or moon. Flood basalt describes the formation in a series of basalt flows. By definition, basalt is an igneous rock with generally 45-55% silica and less than 10% feldspathoid by volume. Basalt commonly features a very fine-grained or glassy matrix interspersed with visible mineral grains, the average density is 3.0 gm/cm3. Basalt is defined by its content and texture, and physical descriptions without mineralogical context may be unreliable in some circumstances. Basalt is usually grey to black in colour, but rapidly weathers to brown or rust-red due to oxidation of its mafic minerals into hematite, although usually characterized as dark, basaltic rocks exhibit a wide range of shading due to regional geochemical processes. Due to weathering or high concentrations of plagioclase, some basalts can be quite light-coloured and these phenocrysts usually are of olivine or a calcium-rich plagioclase, which have the highest melting temperatures of the typical minerals that can crystallize from the melt. Basalt with a texture is called vesicular basalt, when the bulk of the rock is mostly solid. Gabbro is often marketed commercially as black granite and these ultramafic volcanic rocks, with silica contents below 45% are usually classified as komatiites. Agricola applied basalt to the black rock of the Schloßberg at Stolpen. Tholeiitic basalt is relatively rich in silica and poor in sodium, included in this category are most basalts of the ocean floor, most large oceanic islands, and continental flood basalts such as the Columbia River Plateau. Basalt rocks are in some cases classified after their content in High-Ti and Low-Ti varieties. High-Ti and Low-Ti basalts have been distinguished in the Paraná and Etendeka traps and it has greater than 17% alumina and is intermediate in composition between tholeiite and alkali basalt, the relatively alumina-rich composition is based on rocks without phenocrysts of plagioclase. Alkali basalt is relatively poor in silica and rich in sodium and it is silica-undersaturated and may contain feldspathoids, alkali feldspar and phlogopite. Boninite is a form of basalt that is erupted generally in back-arc basins. Ocean island basalt Lunar basalt On Earth, most basalt magmas have formed by melting of the mantle. Basalt commonly erupts on Io, the third largest moon of Jupiter, and has formed on the Moon, Mars, Venus. The crustal portions of oceanic tectonic plates are composed predominantly of basalt, produced from upwelling mantle below, the mineralogy of basalt is characterized by a preponderance of calcic plagioclase feldspar and pyroxene
38.
Breadfruit
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Breadfruit is a species of flowering tree in the mulberry and jackfruit family originating in the South Pacific and that was eventually spread to the rest of Oceania. Its name is derived from the texture of the ripe fruit when cooked, similar to freshly baked bread. According to DNA fingerprinting studies, breadfruit has its origins in the region of Oceania from New Guinea through the Indo-Malayan Archipelago to western Micronesia, the trees have been widely planted in tropical regions elsewhere, including lowland Central America, northern South America, and the Caribbean. In addition to the serving as a staple food in many cultures. Sir Joseph Banks and others saw the value of breadfruit as a highly productive food in 1769, in 1787, William Bligh was appointed Captain of the HMS Bounty, and ordered to proceed to the South Pacific to collect the plants. Although Bligh won the Royal Society medal for his efforts, the introduction was not entirely successful, Breadfruit trees grow to a height of 26 m. The large and thick leaves are cut into pinnate lobes. All parts of the tree yield latex, which is useful for boat caulking, the trees are monoecious, with male and female flowers growing on the same tree. The male flowers emerge first, followed shortly afterward by the female flowers, the latter grow into capitula, which are capable of pollination just three days later. Pollination occurs mainly by bats, but cultivated varieties produce fruit without pollination. The compound, false fruit develops from the perianth, and originates from 1. Breadfruit is one of the food plants, with a single tree producing up to 200 or more grapefruit-sized fruits per season. In the South Pacific, the trees yield 50 to 150 fruits per year, usually round, productivity varies between wet and dry areas. Studies in Barbados indicate a potential of 16 to 32 tons per hectare. The ovoid fruit has a surface, and each fruit is divided into many achenes, each achene surrounded by a fleshy perianth. Most selectively bred cultivars have seedless fruit, whereas seeded varieties are mainly for their edible seeds. Breadfruit is usually propagated using root cuttings, Breadfruit is closely related to the breadnut, from which it might have been naturally selected. It is noticeably similar in appearance to its relative of the same genus, Breadfruit has hundreds of varieties and thousands of common names varying according to its geographic distribution, and is cultivated in some 90 countries
39.
Pandanus
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Pandanus is a genus of monocots with some 750 accepted species. They are palm-like, dioecious trees and shrubs native to the Old World tropics and subtropics, common names include pandan, screw palm, and screw pine. They are classified in the order Pandanales, family Pandanaceae, often called pandanus palms, these plants are not closely related to palm trees. The species vary in size from small shrubs less than 1 m tall, to medium-sized trees 20 m tall, typically with a canopy, heavy fruit. The trunk is stout, wide-branching, and ringed with leaf scars. Depending on the species, the trunk can be smooth, rough, the roots forms a pyramidal tract to hold the trunk. They commonly have many thick prop roots near the base, which provide support as the tree grows top-heavy with leaves, fruit and these roots are adventitious and often branched. The top of the plant has one or more crowns of strap-shaped leaves that may be spiny and they are dioecious, with male and female flowers produced on different plants. The flowers of the tree are 2–3 cm long and fragrant, surrounded by narrow. The female tree produces flowers with round fruits that are also bract-surrounded, typically, the fruit changes from green to bright orange or red as it matures. The fruits can stay on the tree for more than 12 months and these plants grow from sea level to 3,300 m. Pandanus trees are of cultural, health, and economic importance in the Pacific and they grow wild mainly in seminatural vegetation in littoral habitats throughout the tropical and subtropical Pacific, where they can withstand drought, strong winds, and salt spray. They propagate readily from seed, but also are widely propagated from cuttings by local people. Species growing on exposed headlands and along beaches have thick prop roots as anchors in the loose sand. Those prop roots emerge from the stem, usually close to but above the ground, other species are adapted to mountain habitats and riverine forests. The tree is grown and propagated from shoots that form spontaneously in the axils of lower leaves, Pandanus fruit are eaten by animals including bats, rats, crabs, elephants and monitor lizards, but the vast majority of species are dispersed primarily by water. Its fruit can float and spread to other islands without help from man, craftsmen collect the pandan leaves from plants in the wild. Only the mature leaves are cut so the plant will naturally regenerate, the leaves are sliced in fine strips and sorted for further processing
40.
Coconut
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The coconut tree is a member of the family Arecaceae and the only species of the genus Cocos. The term coconut can refer to the coconut palm or the seed, or the fruit. The spelling cocoanut is a form of the word. The term is derived from the 16th-century Portuguese and Spanish word coco meaning head or skull, coconuts are known for their great versatility, as evidenced by many traditional uses, ranging from food to cosmetics. They form a part of the diets of many people in the tropics and subtropics. Coconuts are distinct from other fruits for their quantity of water. When mature, they can be used as seed nuts or processed to give oil from the kernel, charcoal from the hard shell, the endosperm is initially in its nuclear phase suspended within the coconut water. As development continues, cellular layers of endosperm deposit along the walls of the coconut, when dried, the coconut flesh is called copra. The oil and milk derived from it are used in cooking and frying, as well as in soaps. The husks and leaves can be used as material to make a variety of products for furnishing and decorating, the coconut also has cultural and religious significance in certain societies, particularly in India, where it is used in Hindu rituals. Cocos nucifera is a palm, growing up to 30 m tall, with pinnate leaves 4–6 m long. Coconuts are generally classified into two types, tall and dwarf. On fertile soil, a coconut palm tree can yield up to 75 fruits per year. Given proper care and growing conditions, coconut palms produce their first fruit in six to ten years, botanically, the coconut fruit is a drupe, not a true nut. Like other fruits, it has three layers, the exocarp, mesocarp, and endocarp, the exocarp and mesocarp make up the husk of the coconuts. Coconuts sold in the shops of nontropical countries often have had the exocarp removed, the mesocarp is composed of a fiber, called coir, which has many traditional and commercial uses. The shell has three germination pores or eyes that are visible on its outside surface once the husk is removed. A full-sized coconut weighs about 1.44 kg and it takes around 6,000 full-grown coconuts to produce a tonne of copra
41.
Pig
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A pig is any of the animals in the genus Sus, within the Suidae family of even-toed ungulates. Pigs include the domestic pig and its ancestor, the common Eurasian wild boar, along with species, related creatures outside the genus include the peccary, the babirusa. Pigs, like all suids, are native to the Eurasian and African continents, juvenile pigs are known as piglets. Pigs are highly social and intelligent animals, with around 1 billion individuals alive at any time, the domesticated pig is one of the most numerous large mammals on the planet. Pigs are omnivores and can consume a range of food. Pigs can harbour a range of parasites and diseases that can be transmitted to humans, because of the similarities between pigs and humans, pigs are used for human medical research. The Online Etymology Dictionary provides anecdotal evidence as well as linguistic, saying that the term derives probably from Old English *picg, found in compounds, apparently related to Low German bigge, Dutch big. Another Old English word for pig was fearh, related to furh furrow, from PIE *perk- dig and this reflects a widespread IE tendency to name animals from typical attributes or activities. Synonyms grunter, porker are from sailors and fishermens euphemistic avoidance of uttering the word pig at sea, a superstition perhaps based on the fate of the Gadarene swine and it is entirely likely that the word to call pigs, soo-ie, is similarly derived. A typical pig has a head with a long snout which is strengthened by a special prenasal bone. The snout is used to dig into the soil to find food and is an acute sense organ. There are four hoofed toes on each trotter, with the two larger central toes bearing most of the weight, but the two also being used in soft ground. The dental formula of adult pigs is 3.1.4.33.1.4.3, the rear teeth are adapted for crushing. In the male, the teeth form tusks, which grow continuously and are sharpened by constantly being ground against each other. Occasionally, captive mother pigs may savage their own piglets, often if they become severely stressed, some attacks on newborn piglets are non-fatal. Others may cause the death of the piglets and sometimes, the mother may eat the piglets and it is estimated that 50% of piglet fatalities are due to the mother attacking, or unintentionally crushing, the newborn pre-weaned animals. Scientists have recently discovered that pigs can exhibit a bias and are optimists or pessimests. In a study by the University of Lincoln,36 pigs were tested and they were placed in a room with two food bowls at each end of the room
42.
Rat
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Rats are various medium-sized, long-tailed rodents of the superfamily Muroidea. True rats are members of the genus Rattus, the most important of which to humans are the black rat, Rattus rattus, many members of other rodent genera and families are also referred to as rats, and share many characteristics with true rats. Rats are typically distinguished from mice by their size, generally, when someone discovers a large muroid rodent, its common name includes the term rat, while if it is smaller, the name includes the term mouse. The muroid family is broad and complex, and the common terms rat, scientifically, the terms are not confined to members of the Rattus and Mus genera, for example, the pack rat and cotton mouse. The best-known rat species are the black rat and the brown rat, the group is generally known as the Old World rats or true rats, and originated in Asia. Rats are bigger than most Old World mice, which are their relatives, the term rat is also used in the names of other small mammals which are not true rats. Examples include the North American pack rats, a number of species loosely called kangaroo rats, Rats such as the bandicoot rat are murine rodents related to true rats, but are not members of the genus Rattus. Male rats are called bucks, unmated females are called does, pregnant or parent females are called dams, a group of rats is referred to as a mischief. The common species are opportunistic survivors and often live with and near humans, therefore and they may cause substantial food losses, especially in developing countries. However, the distributed and problematic commensal species of rats are a minority in this diverse genus. Many species of rats are island endemics and some have become endangered due to loss or competition with the brown. Wild rodents, including rats, can carry many different zoonotic pathogens, such as Leptospira, Toxoplasma gondii, another zoonotic disease linked to the rat is the foot-and-mouth disease. The average lifespan of any given rat depends on species is being discussed. The black and brown rats diverged from other Old World rats during the beginning of the Pleistocene in the forests of Asia, specially bred rats have been kept as pets at least since the late 19th century. Pet rats are typically variants of the brown rat, but black rats. Pet rats behave differently from their wild counterparts depending on how many generations they have kept as pets. Pet rats do not pose any more of a risk than pets such as cats or dogs. Tamed rats are generally friendly and can be taught to perform selected behaviors, in 1895, Clark University in Worcester, Massachusetts established a population of domestic albino brown rats to study the effects of diet and for other physiological studies
43.
Lizard
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Lizards are a widespread group of squamate reptiles, with over 6,000 species, ranging across all continents except Antarctica, as well as most oceanic island chains. The group is paraphyletic as it excludes the snakes which are also squamates, Lizards typically have four legs feet and external ears, though some are legless, while snakes lack both of these characteristics. Lizards and snakes share a movable quadrate bone, distinguishing them from the sphenodonts, Lizards form about 60% of all the species of extant non-avian reptiles. Some extinct varanids reached great size, The giant monitor Megalania is estimated to have reached up to 7 m long, vision, including color vision, is particularly well developed in most lizards. Most lizards communicate using body language, using specific postures, gestures, and movements to define territory, resolve disputes, some species of lizards also use pheromones or bright colors, such as the iridescent patches on the belly of Sceloporus. These colors are visible to predators, so are often hidden on the underside or between scales and only revealed when necessary. The particular innovation in this respect is the dewlap, a colored patch of skin on the throat. When a display is needed, a lizard can erect the hyoid bone of its throat, anoles are particularly famous for this display, with each species having specific colors, including patterns only visible under ultraviolet light, as many lizards can see UV light. Lizard tails are often a different and dramatically more vivid color than the rest of the body so as to potential predators to strike for the tail first. Many lizards, including geckos and skinks, are capable of shedding part of their tails through a process called autotomy. This is an example of the pars pro toto principle, sacrificing a part for the whole, the detached tail writhes and wiggles, creating a deceptive sense of continued struggle, distracting the predators attention from the fleeing prey animal. The lizard partially regenerates its tail over a period of weeks, a 2014 research identified 326 genes involved in the regeneration of lizard tails. The new section contains cartilage rather than bone, and the skin may be discolored compared to the rest of the body, most lizards are oviparous, though in some species the eggs are retained until the live young emerge. Parthenogenesis occurs in at least 50 species and may be more widespread in the group. Sexual selection in lizards shows evidence of mate choice, favouring males display fitness indicators. However, doubt has been raised over the age of Tikiguania because it is almost indistinguishable from modern agamid lizards, the Tikiguania remains may instead be late Tertiary or Quaternary in age, having been washed into much older Triassic sediments. Lizards are most closely related to the Rhynchocephalia, which appeared in the Late Triassic, mitochondrial phylogenetics suggest that the first lizards evolved in the late Permian. It had been thought on the basis of data that iguanid lizards diverged from other squamates very early on
44.
Freshwater fish
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Freshwater fish are those that spend some or all of their lives in fresh water, such as rivers and lakes, with a salinity of less than 0. 05%. These environments differ from marine conditions in ways, the most obvious being the difference in levels of salinity. To survive fresh water, the fish need a range of physiological adaptations,41. 24% of all known species of fish are found in fresh water. This is primarily due to the rapid speciation that the scattered habitats make possible, when dealing with ponds and lakes, one might use the same basic models of speciation as when studying island biogeography. Freshwater fish differ physiologically from salt water fish in several respects and their gills must be able to diffuse dissolved gasses while keeping the salts in the body fluids inside. Their scales reduce water diffusion through the skin, freshwater fish that have lost too many scales will die and they also have well developed kidneys to reclaim salts from body fluids before excretion. Many species of fish do reproduce in freshwater, but spend most of their lives in the sea. These are known as fish, and include, for instance, salmon, trout. Some other kinds of fish are, on the contrary, born in salt water and these are known as catadromous fish. Many species solve this problem by associating different habitats with different stages of life, both eels, anadromous salmoniform fish and the sea lamprey have different tolerances in salinity in different stages of their lives. Freshwater fish species are classified by the water temperature in which they survive. The water temperature affects the amount of oxygen available as water contains more oxygen than warm water. Coldwater fish species survive in the coldest temperatures, preferring a water temperature of 50 °F to 60 °F degrees. In North America, air temperatures result in sufficiently cold water temperatures are found in the northern United States, Canada. Common coldwater fish include trout, rainbow trout, and brown trout. Common warmwater fish include bass, bluegill, catfish. Coolwater fish species prefer water temperature between the coldwater and warmwater species, around 60 °F to 80 °F and they are found throughout North America except for the southern portions of the United States. The number of species and subspecies to become endangered has risen from 40 to 61
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This article incorporates text from a publication now in the public domain: Chisholm, Hugh, ed. (1911). "Society Islands". Encyclopædia Britannica. 25 (11th ed.). Cambridge University Press. p. 320.
