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Hiva Oa
With its , Hiva Oa is the second largest island in the Marquesas Islands, in French Polynesia, an overseas territory of France in the Pacific Ocean. Located at 9 45' south latitude and 139 W longitude, it is the largest island of the southern Marquesas group. Around 2,200 people reside on the island. A volcano, Temetiu, is Hiva Oa's highest point with . History Colonial period The first recorded sighting of Hiva Oa by the Europeans was by the Spanish expedition of Álvaro de Mendaña on 21 July 1595. They charted it as ''Dominica''. Overview Administratively, Hiva Oa is part of the commune (municipality) of Hiva-Oa, itself in the administrative subdivision of the Marquesas Islands. Atuona, on the coast of Hiva Oa island, is the administrative centre of the commune. Atuona was formerly the seat of government for all of the Marquesas Islands, but it has been replaced by Taiohae on Nuku Hiva island. The island is famous as the final home of French painter Paul Gauguin and Belg ...
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Marquesas Islands
The Marquesas Islands (; french: Îles Marquises or ' or '; Marquesan: ' ( North Marquesan) and ' ( South Marquesan), both meaning "the land of men") are a group of volcanic islands in French Polynesia, an overseas collectivity of France in the southern Pacific Ocean. Their highest point is the peak of Mount Oave (french: Mont Oave, links=no) on Ua Pou island, at 1,230 m (4,035 ft) above sea level. Archaeological research suggests the islands were colonized in the 10th century AD by voyagers from West Polynesia. Over the centuries that followed, the islands have maintained a "remarkably uniform culture, biology and language". The Marquesas were named after the 16th century Spanish Viceroy of Peru, the Marquis of Cañete ( es, Marqués de Cañete, italic=unset) by navigator , who visited them in 1595. The Marquesas Islands constitute one of the five administrative divisions (') of French Polynesia. The capital of the Marquesas Islands' administrative subdivision is t ...
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Calvary Cemetery, Atuona
Calvary Cemetery () is the main cemetery in Atuona, Hiva ‘Oa, French Polynesia. It is located on a hillside on the eastern edge of town, overlooking the anchorage on Atuona Bay. The cemetery is the final resting place of French Post-Impressionist painter Paul Gauguin, as well as of Belgian singer Jacques Brel. See also * Marquesas Islands * French Polynesia * Paul Gauguin Cultural Center The Paul Gauguin Cultural Center (french: Le Centre Culturel Paul Gauguin) was finished in 2003, to coincide with the 100th anniversary of the death of Paul Gauguin, in Atuona, on Hiva Oa, in the Marquesas Islands ( French Polynesia). Atuona was P ... External links * Cemeteries in France Marquesas Islands Cemeteries in Oceania Jacques Brel Paul Gauguin {{cemetery-stub ...
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Tahuata
Tahuata is the smallest of the inhabited Marquesas Islands, in French Polynesia, an overseas territory of France in the Pacific Ocean. It is located 4 km (2.5 mi.) to the south of the western end of Hiva Oa, across the Canal du Bordelais, called Ha‘ava in Marquesan. History Archæological evidence indicates that Tahuata was inhabited by Polynesians as early as AD 200. In later pre-European times, the tribes of Tahuata were allied with the tribes from the Nuku province of Hiva Oa, and the island was considered a dependency of that province. The first recorded sighting by Europeans was by the Spanish expedition of Álvaro de Mandaña on 22 July 1595. They charted the island as ''Santa Cristina''. They landed at Vaitahu that they named ''Madre de Dios'' (God's Mother in Spanish). According to the Spanish accounts Tahuata had fowls, fish, sugar cane, plantains, nuts and fruits. The existent town was built on two sides of a rectangular space, the houses being of timbe ...
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Taha Uku
Taha Uku is a small bay on the north shore of Ta‘a ‘Oa (the Bay of Traitors) on the southern coast of Hiva ‘Oa. The bay is provides one of the best anchorages in the whole of the Marquesas. It lies just to the east of Atuona, the administrative center of the southern Marquesas. Taha Uku is separated from Atuona Bay by a headland called Feki. See also * French Polynesia * Marquesas Islands The Marquesas Islands (; french: Îles Marquises or ' or '; Marquesan: ' ( North Marquesan) and ' ( South Marquesan), both meaning "the land of men") are a group of volcanic islands in French Polynesia, an overseas collectivity of France in th ... Bodies of water of the Marquesas Islands Bays of the Pacific Ocean {{FrenchPolynesia-geo-stub ...
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Volcanic Crater
A volcanic crater is an approximately circular depression in the ground caused by Volcano, volcanic activity. It is typically a bowl-shaped feature containing one or more vents. During Types of volcanic eruptions, volcanic eruptions, molten magma and volcanic gases rise from an underground magma chamber, through a conduit, until they reach the crater's vent, from where the gases escape into the atmosphere and the magma is erupted as lava. A volcanic crater can be of large dimensions, and sometimes of great depth. During certain types of explosive eruptions, a volcano's magma chamber may empty enough for an area above it to subside, forming a type of larger depression known as a caldera. Geomorphology In most volcanoes, the crater is situated at the top of a mountain formed from the erupted volcanic deposits such as lava flows and tephra. Volcanoes that terminate in such a summit crater are usually of a conical form. Other volcanic craters may be found on the flanks of volcanoe ...
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Volcano
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. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and most are found underwater. For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates. Volcanoes can also form where there is stretching and thinning of the crust's plates, such as in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande rift in North America. Volcanism away from plate boundaries has been postulated to arise from upwelling diapirs from the core–mantle boundary, deep in the Earth. This results in hotspot volcanism, of which the Hawaiian hotspot is an example. Volcanoes are usually not created where two tectonic plates slide ...
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Tahiti
Tahiti (; Tahitian ; ; previously also known as Otaheite) is the largest island of the Windward group of the Society Islands in French Polynesia. It is located in the central part of the Pacific Ocean and the nearest major landmass is Australia. Divided into two parts, ''Tahiti Nui'' (bigger, northwestern part) and ''Tahiti Iti'' (smaller, southeastern part), the island was formed from volcanic activity; it is high and mountainous with surrounding coral reefs. Its population was 189,517 in 2017, making it by far the most populous island in French Polynesia and accounting for 68.7% of its total population. Tahiti is the economic, cultural and political centre of French Polynesia, an overseas collectivity and an overseas country of the French Republic. The capital of French Polynesia, Papeete, is located on the northwest coast of Tahiti. The only international airport in the region, Faaā International Airport, is on Tahiti near Papeete. Tahiti was originally settled by Pol ...
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Atuona Airport
Atuona Airport or Hiva Oa Airport is an airport located northeast of Atuona, on the island of Hiva Oa, in the Marquesas Islands of French Polynesia )Territorial motto: ( en, "Great Tahiti of the Golden Haze") , anthem = , song_type = Regional anthem , song = " Ia Ora 'O Tahiti Nui" , image_map = French Polynesia on the globe (French Polynesia centered).svg , map_alt = Location of Frenc .... Previously, that airport had been assigned the HIX IATA location identifier, which has then been deprecated by IATA in 2012. Airlines and destinations Statistics References Airports in French Polynesia {{FrenchPolynesia-geo-stub ...
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Coral Reef
A coral reef is an underwater ecosystem characterized by reef-building corals. Reefs are formed of colonies of coral polyps held together by calcium carbonate. Most coral reefs are built from stony corals, whose polyps cluster in groups. Coral belongs to the class Anthozoa in the animal phylum Cnidaria, which includes sea anemones and jellyfish. Unlike sea anemones, corals secrete hard carbonate exoskeletons that support and protect the coral. Most reefs grow best in warm, shallow, clear, sunny and agitated water. Coral reefs first appeared 485 million years ago, at the dawn of the Early Ordovician, displacing the microbial and sponge reefs of the Cambrian. Sometimes called ''rainforests of the sea'', shallow coral reefs form some of Earth's most diverse ecosystems. They occupy less than 0.1% of the world's ocean area, about half the area of France, yet they provide a home for at least 25% of all marine species, including fish, mollusks, worms, crustaceans, echinoderms, sp ...
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Hiva Oa - Cheval
In Polynesian mythology, (also rendered as in Cook Islands Māori, in Samoan, in Tahitian, in Hawaiian) is the original home of the Polynesians, before dispersal across Polynesia. It also features as the underworld in many Māori stories. Anne Salmond states ''Havaii'' is the old name for Raiatea, the homeland of the Māori. When British explorer James Cook first sighted New Zealand in 1769, he had Tupaia on board, a Raiatean navigator and linguist. Cook's arrival seemed to be a confirmation of a prophecy by Toiroa, a priest from Māhia. At Tolaga Bay, Tupaia conversed with the ''tohunga'' associated with the school of learning located there, called Te Rawheoro. The priest asked about the Maori homelands, 'Rangiatea' (Ra'iatea), 'Hawaiki' (Havai'i, the ancient name for Ra'iatea), and 'Tawhiti' (Tahiti). Etymology Linguists have reconstructed the term to Proto- Nuclear Polynesian ''*sawaiki''. The Māori word figures in legends about the arrival of the Māori in A ...
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