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St. Michael's Cathedral, Rikitea
St. Michael's Cathedral (french: Cathédrale Saint-Michel, Rikitea), also known as the Rikitea Cathedral, is a parish of the Catholic Church located on Mangareva Island in the Gambier Islands of French Polynesia. Its historic neo-Gothic church was built on the eastern side of Rikitea between 1839 and 1848 by missionaries of the Congregation of the Sacred Hearts of Jesus and Mary. It formerly served as cathedral for what is now the Archdiocese of Papeete, and was extensively renovated in 2011. The parish community remains very active, within the limitations of the small population of the island. History The cathedral was built under the auspices of the Picpus Fathers by Father Cyprien Liausu, Superior of the Mission of Our Lady of Peace in the Gambiers, after he arrived in Rikitea in 1835. The cornerstone for the cathedral was laid on 17 January 1839, and Bishop Étienne Jérôme Rouchouze blessed the site on 4 April 1839. Lay brothers Gilbert Soulié and Fabien Costes were res ...
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Catholic Church
The Catholic Church, also known as the Roman Catholic Church, is the largest Christian church, with 1.3 billion baptized Catholics worldwide . It is among the world's oldest and largest international institutions, and has played a prominent role in the history and development of Western civilization. O'Collins, p. v (preface). The church consists of 24 ''sui iuris'' churches, including the Latin Church and 23 Eastern Catholic Churches, which comprise almost 3,500 dioceses and eparchies located around the world. The pope, who is the bishop of Rome, is the chief pastor of the church. The bishopric of Rome, known as the Holy See, is the central governing authority of the church. The administrative body of the Holy See, the Roman Curia, has its principal offices in Vatican City, a small enclave of the Italian city of Rome, of which the pope is head of state. The core beliefs of Catholicism are found in the Nicene Creed. The Catholic Church teaches that it ...
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Papeete
Papeete ( Tahitian: ''Papeete'', pronounced ) is the capital city of French Polynesia, an overseas collectivity of the French Republic in the Pacific Ocean. The commune of Papeete is located on the island of Tahiti, in the administrative subdivision of the Windward Islands, of which Papeete is the administrative capital.Décret n° 2005-1611 du 20 décembre 2005 pris pour l'application du statut d'autonomie de la Polynésie française
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Religion In 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 French Polynesia , map_caption = Location of French Polynesia (circled in red) , mapsize = 290px , subdivision_type = Sovereign state , subdivision_name = , established_title = Protectorate proclaimed , established_date = 9 September 1842 , established_title2 = Territorial status , established_date2 = 27 October 1946 , established_title3 = Collectivity status , established_date3 = 28 March 2003 , established_title4 = Country status (nominal title) , established_date4 = 27 February 2004 , official_languages = French , regional_languages = , capital = Papeete , coordinates = , largest_city = Fa'a'ā , demonym = French Polynesian , ethnic_groups = 66.5% unmixed Polynesians7.1% mixed Polynesians9.3% Demis11. ...
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Maputeoa
Te Maputeoa (baptized Gregorio Stanislas; reigned as Gregorio I; born c. 1814 – 20 June 1857) was a monarch of the Polynesian island of Mangareva and the other Gambier Islands. He was the King or ''ʻAkariki'' (paramount chief), as well as the penultimate king of the island of Mangareva, and other Gambier Islands including Akamaru, Aukena, Taravai and Temoe. He reigned from 1830 until his death in 1857. During Maputeoa's reign, the country, which was deeply rooted in native beliefs and even cannibalism, became a Roman Catholic community. This was accomplished by removing all vestiges of native beliefs, such as destroying the traditional wooden images of their indigenous faith deified in ''maraes'' and replacing them with churches. The king was baptized into Catholicism on 25 August 1836. He learned about Christianity from the island's missionaries, headed by the French Picpus priests, Honoré Laval and François Caret. His uncle Matua, the High Priest of the local temp ...
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François Caret
François d'Assise Caret, SS.CC., (born François Toussaint Caret; 4 July 1802 – 26 October 1844) was a French Catholic priest of the Congregation of the Sacred Hearts of Jesus and Mary, a religious institute of the Roman Catholic Church. Life François d'Assise Caret was born 4 July 1802 in Miniac-sous-Bécherel ( Ille-et-Vilaine). He was already a priest by 1829, when he became a professed member of the Congregation of the Sacred Hearts of Jesus and Mary. In February 1834, he sailed from Bordeaux for Valparaiso with Father Honoré Laval. Advised by one Captain Mauruc that Protestant missionaries had not yet reached the Gambier archipelago, they took passage on the ''Peruvian'', out of Boston, and arrived 8 August on Akamaru, where they found a representatives of the London Missionary Society already established. Caret and Laval established a thriving mission and planned to expand their work to Tahiti.
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Tahitian Pearl
The Tahitian pearl (or black pearl) is an organic gem formed from the black lip oyster ('' Pinctada margaritifera'').Newman, Renee. ''Pearl Buying Guide''. "Black Pearls." Los Angeles: International Jewelry Publications, c2005, p. 73 These pearls derive their name from the fact that they are primarily cultivated around the islands of French Polynesia, around Tahiti. Description Tahitian pearls come in a range of colors from white to black. They can contain various undertones and overtones of green, pink, blue, silver and yellow. The most valuable of these are of the darker variety, as the naturally dark tones of the Tahitian pearls is a unique quality among pearls. A true black Tahitian pearl is extremely rare, and largely considered one of the most beautiful kinds of pearls in the world. Most Tahitian pearls that are identified as “black” are actually charcoal grey, silver, or dark green. An advantage of the Tahitian pearl is that the oyster inside of which they grow is quit ...
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Nacre
Nacre ( , ), also known as mother of pearl, is an organicinorganic composite material produced by some molluscs as an inner shell layer; it is also the material of which pearls are composed. It is strong, resilient, and iridescent. Nacre is found in some of the most ancient lineages of bivalves, gastropods, and cephalopods. However, the inner layer in the great majority of mollusc shells is porcellaneous, not nacreous, and this usually results in a non-iridescent shine, or more rarely in non-nacreous iridescence such as ''flame structure'' as is found in conch pearls. The outer layer of cultured pearls and the inside layer of pearl oyster and freshwater pearl mussel shells are made of nacre. Other mollusc families that have a nacreous inner shell layer include marine gastropods such as the Haliotidae, the Trochidae and the Turbinidae. Physical characteristics Structure and appearance Nacre is composed of hexagonal platelets of aragonite (a form of calcium ...
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Mother Of Pearl
Nacre ( , ), also known as mother of pearl, is an organicinorganic composite material produced by some molluscs as an inner shell layer; it is also the material of which pearls are composed. It is strong, resilient, and iridescent. Nacre is found in some of the most ancient lineages of bivalves, gastropods, and cephalopods. However, the inner layer in the great majority of mollusc shells is porcellaneous, not nacreous, and this usually results in a non-iridescent shine, or more rarely in non-nacreous iridescence such as ''flame structure'' as is found in conch pearls. The outer layer of cultured pearls and the inside layer of pearl oyster and freshwater pearl mussel shells are made of nacre. Other mollusc families that have a nacreous inner shell layer include marine gastropods such as the Haliotidae, the Trochidae and the Turbinidae. Physical characteristics Structure and appearance Nacre is composed of hexagonal platelets of aragonite (a form of calcium carbo ...
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Kouaku
Kouaku is an island of the Gambier Islands of French Polynesia. See also * Desert island * List of islands This is a list of the lists of islands in the world grouped by country, by continent, by body of water A body of water or waterbody (often spelled water body) is any significant accumulation of water on the surface of Earth or another plane ... References {{coord, 23.2092, S, 134.8589, W, source:wikidata-and-enwiki-cat-tree_region:FR, display=title Islands of the Gambier Islands Uninhabited islands of French Polynesia ...
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Tekava
Tekava is an island of the Gambier Islands of French Polynesia. See also * Desert island * List of islands This is a list of the lists of islands in the world grouped by country, by continent, by body of water A body of water or waterbody (often spelled water body) is any significant accumulation of water on the surface of Earth or another plane ... References {{coord, -23.1647, -134.8527, type:isle_region:PF, display=title Islands of the Gambier Islands Uninhabited islands of French Polynesia ...
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Tauna
Tauna is an islet of the Gambier Islands of French Polynesia. In and around Polynesia, islets are widely known by the term Motu, from the term for the coral-rubble islets common to the region. During a recent filming of the television show GT Hunters shot on Tauna in April 2014, the locals of the village RikiteaRikitea have come to unofficially call this small island, Motu Topher, after the cinematographer who fell madly in love with the island. See also * Desert island * List of islands This is a list of the lists of islands in the world grouped by country, by continent, by body of water A body of water or waterbody (often spelled water body) is any significant accumulation of water on the surface of Earth or another plane ... References Islands of the Gambier Islands Uninhabited islands of French Polynesia {{FrenchPolynesia-geo-stub ...
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Oolite
Oolite or oölite (''egg stone'') is a sedimentary rock formed from ooids, spherical grains composed of concentric layers. The name derives from the Ancient Greek word for egg (ᾠόν). Strictly, oolites consist of ooids of diameter 0.25–2 millimetres; rocks composed of ooids larger than 2 mm are called pisolites. The term ''oolith'' can refer to oolite or individual ooids. Composition Ooids are most commonly composed of calcium carbonate (calcite or aragonite), but can be composed of phosphate, clays, chert, dolomite or iron minerals, including hematite. Dolomitic and chert ooids are most likely the result of the replacement of the original texture in limestone. Oolitic hematite occurs at Red Mountain near Birmingham, Alabama, along with oolitic limestone. They are usually formed in warm, supersaturated, shallow, highly agitated marine water intertidal environments, though some are formed in inland lakes. The mechanism of formation starts with a small fra ...
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