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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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Flag Of The Marquesas Islands
The flag of the Marquesas Islands is the flag chosen by the regional government to represent the islands. However, it is not formally recognized by France, the administrative government of the region. Description The flag is divided into two horizontal stripes with yellow on top and red on bottom, with a white equilateral triangle emerging from the hoist. The yellow represents youth and joy, while the red and white are ''tapu'', or sacred, to the chiefs and priests respectively. In the white triangle, a black design of '' Matatiki'' (English: the gaze of Tiki) represents the first man in Polynesian mythology, and the inventor of sculpture and tattooing. The tattoo design on Tiki's cheeks are ''tapu'' symbols. History The first version of the flag was revealed December 30, 1978 by the Motu Haka Association. The flag was formally adopted by the local government on November 30, 1998. The flag was used informally for many years, having been first raised on December 14, 1980, at ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcano
A volcano is a rupture in the Crust (geology), crust of a Planet#Planetary-mass objects, planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and volcanic gas, gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where list of tectonic plates, tectonic plates are divergent boundary, diverging or convergent boundary, 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eiao
Eiao is the largest of the extreme northwestern Marquesas Islands. The island is uninhabited, but is administratively part of the commune (municipality) of Nuku-Hiva, itself in the administrative subdivision of the Marquesas Islands. Geography The center of this island is a high plateau, rising on the east side to 576 metres above sea level (1,890 feet), much of which has been devastated by herds of feral sheep brought here by mankind. There is one good anchorage, found on the western side of the island at Vaituha. History In pre-European times, the bodies of chiefs from parts of Te I'i were taken to Eiao for burial. Eiao was at one time home to a Marquesan tribe called the Tuametaki. Archaeological investigations have discovered workshops for the production of stone tools, especially adzes, made from local basalt. These tools have been found in archaeological sites on other islands, providing evidence for prehistoric interisland voyaging within this island group. The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marquesas Hotspot
The Marquesas hotspot is a volcanic hotspot in the southern Pacific Ocean. It is responsible for the creation of the Marquesas Islands – a group of eight main islands and several smaller ones – and a few seamounts. The islands and seamounts formed between 5.5 and 0.4 million years ago and constitute the northernmost volcanic chain in French Polynesia. There are two competing theories concerning the origins of volcanism associated with the Marquesas hotspot. Many geoscientists maintain that the area is underlain by a mantle plume which has transported hot material from the lower mantle to the surface, forming the chain of islands and seamounts as the Pacific Plate moved in a north-westerly direction relative to the stationary plume. Radiometric dating of the youngest volcanic rocks suggests that volcanism is still active. Evidence for a plume origin comes mainly from seismic imaging, with large-scale low velocity anomalies being observed from the core-mantle boundary to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Magma
Magma () is the molten or semi-molten natural material from which all igneous rocks are formed. Magma is found beneath the surface of the Earth, and evidence of magmatism has also been discovered on other terrestrial planets and some natural satellites. Besides molten rock, magma may also contain suspended crystals and gas bubbles. Magma is produced by melting of the mantle or the crust in various tectonic settings, which on Earth include subduction zones, continental rift zones, mid-ocean ridges and hotspots. Mantle and crustal melts migrate upwards through the crust where they are thought to be stored in magma chambers or trans-crustal crystal-rich mush zones. During magma's storage in the crust, its composition may be modified by fractional crystallization, contamination with crustal melts, magma mixing, and degassing. Following its ascent through the crust, magma may feed a volcano and be extruded as lava, or it may solidify underground to form an intrusion, such ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 Polyn ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Taiohae
Taiohae is the main town on Nuku Hiva island. The town is located on a former volcanic crater A volcanic crater is an approximately circular depression in the ground caused by volcanic activity. It is typically a bowl-shaped feature containing one or more vents. During volcanic eruptions, molten magma and volcanic gases rise from an und ..., which has partly collapsed into the ocean, creating a bay. This is the site of Fort Madison, set up by Porter in 1813. External links References Populated places in the Marquesas Islands {{FrenchPolynesia-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Administrative Divisions Of French Polynesia
In French Polynesia, there are two levels of administrative divisions: five administrative subdivisions (french: subdivisions administratives) and 48 communes.Codification des collectivités d'outre-mer (COM) INSEE, 1 March 2017Loi n° 2004-193 du 27 février 2004 complétant le statut d'autonomie de la Polynésie française (1) |
Álvaro De Mendaña De Neira
Álvaro de Mendaña y Neira (or Neyra) (1 October 1542 – 18 October 1595) was a Spanish navigator and discoverer, best known for two of the earliest recorded expeditions across the Pacific in 1567 and 1595. His voyages led to the discovery of the Marquesas, Cook Islands and Solomons among other archipelagos. Born in Congosto, in El Bierzo Region ( León), he was the nephew of Lope García de Castro, viceroy of Peru. Search for Terra Australis Between 1565 and 1605, three important Spanish voyages of exploration left Peru bound for the southwest Pacific. One inspiration for these voyages was Spanish soldier Pedro Sarmiento de Gamboa who arrived in Peru in 1557. Sarmiento de Gamboa developed an interest in Inca stories of gold and riches being collected from lands further to the west. Sarmiento's proposal for an expedition to find land in the Pacific was put to Governor Lope García de Castro, finding favour as it matched common Spanish belief in the existence of a great ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
García Hurtado De Mendoza, 5th Marquis Of Cañete
García Hurtado de Mendoza y Manrique, 5th Marquis of Cañete (July 21, 1535 – May 19, 1609) was a Spanish Governor of Chile, and later Viceroy of Peru (from January 8, 1590 to July 24, 1596). He is often known simply as "Marquis of Cañete". Belonging to an influential family of Spanish noblemen Hurtado de Mendoza successfully fought in the Arauco War during his stay as Governor of Chile. The city of Mendoza is named after him. In his later position as Viceroy of Peru he sponsored Álvaro de Mendaña's transpacific expedition of 1595, who named the Marquesas Islands after him. Early life He was the son of Andrés Hurtado de Mendoza, 3rd Marquis of Cañete — also a viceroy of Peru — and Magdalena Manrique, daughter of the Count of Osorno. Both his parents belonged to some of the most influential families in the Spanish aristocracy. In 1552 Hurtado de Mendoza ran away from home with the intention of serving his king, Charles I (Emperor Charles V), in an exped ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Viceroy Of Peru
The viceroys of Peru ruled the Viceroyalty of Peru from 1544 to 1824 in the name of the monarch of Spain. The territories under ''de jure'' rule by the viceroys included in the 16th and 17th century almost all of South America except eastern Brazil. Governors of New Castile (1532–1544) Viceroys of Peru (1544–1824) See also *Viceroyalty of Peru *History of Peru * List of presidents of Peru References {{DEFAULTSORT:Viceroys Of Peru, List Of Viceroyalty of Peru * *Peru Colonial Peru Viceroy A viceroy () is an official who reigns over a polity in the name of and as the representative of the monarch of the territory. The term derives from the Latin prefix ''vice-'', meaning "in the place of" and the French word ''roy'', meaning " ... Peru, viceroys Viceroys 16th-century Peruvian people 17th-century Peruvian people 18th-century Peruvian people 19th-century Peruvian people Viceroy of Peru Viceroy of Peru Viceroy of Peru Viceroy of Peru Viceroy o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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