Duff Islands
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Duff Islands
The Duff Islands are a small island group lying to the northeast of the Santa Cruz Islands in the Solomon Islands province of Temotu. They are also sometimes known as the Wilson Islands. Location and geography The islands are located at 9°51'48" S. lat., 167°4'48" E. long. The Duff Islands consist of: *Taumako, the main island, with nearby Tahua, Tohua, and Tatumotu *The Bass Islands: Lua, Kaa and Loreva * Treasurer's Islands: Tuleki (Nula), Elingi (Obelisk Island), Te Aku (Te Ako), Lakao and Ulaka Frequently, Hallie Jackson Reef is mentioned in the context of the Duff islands, although it is located 45 km west of that 32 km long island chain, and although it is not an island, at most a submarine reef. In the Sailing Directions of 1969 Hallie Jackson Reef is described as a reef 24 feet deep, at 9°44'S, 166°07'E. The corresponding current (2017) publication no longer has any mention of the reef. Local population The Duff Islands were settled by the ...
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Santa Cruz Islands
The Santa Cruz Islands are a group of islands in the Pacific Ocean, part of Temotu Province of the nation of Solomon Islands discovered by the Spaniards. They lie approximately 250 miles (400 km) to the southeast of the Solomon Islands archipelago. The Santa Cruz Islands lie just north of the archipelago of Vanuatu, and are considered part of the Vanuatu rain forests ecoregion. Geography The term Santa Cruz Islands is sometimes used to encompass all of the islands of the present-day Solomon Islands province of Temotu. The largest island is Nendö, which is also known as Santa Cruz Island proper (505.5 km2, highest point , population over 5000). Lata, located on Nendö, is the largest town, and the capital of Temotu province. Other islands belonging to the Santa Cruz group are Vanikoro (173.2 km2, population 800, which is actually two islands, Banie and its small neighbor Teanu) and Utupua (69.0 km2, highest point , population 848). The Santa Cru ...
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Duff (1794 Ship)
''Duff'' was a ship launched on the Thames in 1794. In 1796 the London Missionary Society engaged her to take a party of missionaries to the South Pacific. Once she had landed the missionaries she sailed to China and took a cargo back to England for the British East India Company. On this voyage her captain named a variety of South Pacific islands. On her second voyage to deliver missionaries a French privateer captured her in 1799 off the coast of Brazil on the outward-bound leg of her voyage. First voyage ''Duff'' was originally under the command of P. Gordon, with owner J. Carbine and traded between London and Gibraltar. In 1795 the just formed London Missionary Society decided to send missionaries to the South Pacific. Captain James Wilson volunteered his services and the society was able to afford to purchase ''Duff''. ''Lloyd's Register'' for 1796 shows that Wilson replaced Gordon as master of Duff, and Cox & Co. replaced J. Carbine as owner. Also, her trade changed to ...
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Our Lady Of Perpetual Help
Our Lady of Perpetual Help (also known as Our Lady of Perpetual Succour) is a Roman Catholic title of the Blessed Virgin Mary associated with a 15th-century Byzantine icon with an alleged Marian apparition. The icon is believed to have originated from the Keras Kardiotissas Monastery and has been in Rome since 1499. Today it is permanently enshrined in the Church of Saint Alphonse of Liguori, where the official Novena to Our Mother of Perpetual Help text is prayed weekly. Pope Pius IX granted a Pontifical decree of Canonical Coronation along with its present title on 5 May 1866. The Latin Patriarch of Constantinople, Cardinal Ruggero Luigi Emidio Antici Mattei, executed the rite of coronation on 23 June 1867. The Redemptorist Congregation of priests and brothers are the only religious order currently entrusted by the Holy See to protect and propagate a Marian religious work of art. In the Eastern Orthodox Church iconography, the image is known as the “''Virgin ...
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Pedro Fernandes De Queirós
Pedro Fernandes de Queirós ( es, Pedro Fernández de Quirós) (1563–1614) was a Portuguese navigator in the service of Spain. He is best known for his involvement with Spanish voyages of discovery in the Pacific Ocean, in particular the 1595–1596 voyage of Álvaro de Mendaña y Neira, and for leading a 1605–1606 expedition that crossed the Pacific in search of Terra Australis. Early life Queirós (or Quirós as he signed) was born in Évora, Portugal in 1563. As the Portuguese and Spanish monarchies had been unified under the king of Spain in 1580 (following the vacancy of the Portuguese throne, which lasted for sixty years, until 1640, when the Portuguese monarchy was restored), Queirós entered Spanish service as a young man and became an experienced seaman and navigator. In April 1595 he joined Álvaro de Mendaña y Neira on his voyage to colonize the Solomon Islands, serving as chief pilot. After Mendaña's death in October 1595, Queirós is credited with taking comma ...
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Polynesian Languages
The Polynesian languages form a genealogical group of languages, itself part of the Oceanic branch of the Austronesian family. There are 38 Polynesian languages, representing 7 percent of the 522 Oceanic languages, and 3 percent of the Austronesian family. While half of them are spoken in geographical Polynesia (the Polynesian triangle), the other half – known as Polynesian outliers – are spoken in other parts of the Pacific: from Micronesia to atolls scattered in Papua New Guinea, the Solomon Islands or Vanuatu. The most prominent Polynesian languages, in number of speakers, are Tahitian, Samoan, Tongan, Māori and Hawaiian. The ancestors of modern Polynesians were Lapita navigators, who settled in the Tonga and Samoa areas about 3,000 years ago. Linguists and archaeologists estimate that this first population went through common development during about 1000 years, giving rise to Proto-Polynesian, the linguistic ancestor of all modern Polynesian languages. ...
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Samoic Languages
The Samoic–Outlier languages, also known as Samoic languages, are a purported group of Polynesian languages, encompassing the Polynesian languages of Samoa, Tuvalu, American Samoa, Tokelau, Wallis and Futuna, and Polynesian outlier languages in New Caledonia, the Solomon Islands, Vanuatu, Papua New Guinea, and the Federated States of Micronesia. The name "Samoic-Outlier" recognizes Sāmoan. Classification According to ''Ethnologue'' 16, the Samoic languages are as follows: * East Uvean–Niuafoou ** Niuafoou (in Tonga) ** Uvea (also called Wallisian or East Uvean, on Uvea or Wallis island, Wallis and Futuna) *Pukapukan (Pukapuka in the Cook Islands) * Samoan (Samoa and American Samoa) *Tokelauan (Tokelau) *Niuatoputapu (on Niuatoputapu in Tonga, extinct) * Ellicean ** Tuvaluan (Tuvalu) **Kapingamarangi (Kapingamarangi in the Federated States of Micronesia) **Nukuoro (Nukuoro in the Federated States of Micronesia) ** Ontong Java ( Ontong Java in the Solomon Islands) **Sik ...
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Vaeakau-Taumako Language
Vaeakau-Taumako (formerly known as ''Pileni'') is a Polynesian language spoken in some of the Reef Islands as well as in the Taumako Islands (also known as the Duff Islands) in the Temotu province of the Solomon Islands. The language is spoken throughout the Taumako Islands, while in the Reef Islands, it is spoken on Aua, Matema, Nifiloli, Nupani, Nukapu, and Pileni. Speakers are thought to be descendants of people from Tuvalu. Vaeakau-Taumako was described by linguists Even Hovdhaugen and Åshild Næss, in the form of a dictionary and a grammar. Classification Vaeakau-Taumako is a Polynesian outlier. Within that group, it has traditionally been considered one of the Futunic branch, but a 2008 study (exclusively based on lexical evidence) concluded that this membership is weakly supported. Phonology Vowels Vaeakau-Taumako does not vary from the standard Polynesian and Austronesian vowel system, featuring five vowels that can be used either in a long or short form. Sh ...
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Polynesians
Polynesians form an ethnolinguistic group of closely related people who are native to Polynesia (islands in the Polynesian Triangle), an expansive region of Oceania in the Pacific Ocean. They trace their early prehistoric origins to Island Southeast Asia and form part of the larger Austronesian ethnolinguistic group with an Urheimat in Taiwan. They speak the Polynesian languages, a branch of the Oceanic subfamily of the Austronesian language family. there were an estimated 2 million ethnic Polynesians (full and part) worldwide, the vast majority of whom either inhabit independent Polynesian nation-states ( Samoa, Niue, Cook Islands, Tonga, and Tuvalu) or form minorities in countries such as Australia, Chile (Easter Island), New Zealand, France ( French Polynesia and Wallis and Futuna), and the United States (Hawaii and American Samoa), in addition to the British Overseas Territory of the Pitcairn Islands. New Zealand had the highest population of Polynesians, estima ...
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Lapita People
The Lapita culture is the name given to a Neolithic Austronesian peoples, Austronesian people and their material culture, who settled Island Melanesia via a seaborne migration at around 1600 to 500 BCE. They are believed to have originated from the northern Philippines, either directly, via the Mariana Islands, or both. They were notable for their distinctive geometric designs on dentate-stamped pottery, which closely resemble the pottery recovered from the Nagsabaran archaeological site in northern Luzon. The Lapita intermarried with the Papuans, Papuan populations to various degrees, and are the direct ancestors of the Austronesian peoples of Polynesia, eastern Micronesia, and Island Melanesia. Etymology The term 'Lapita' was coined by archaeologists after mishearing a word in the local Haveke language, ''xapeta'a'', which means 'to dig a hole' or 'the place where one digs', during the 1952 excavation in New Caledonia. The Lapita archaeological culture is named after the type ...
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Reef
A reef is a ridge or shoal of rock, coral or similar relatively stable material, lying beneath the surface of a natural body of water. Many reefs result from natural, abiotic processes— deposition of sand, wave erosion planing down rock outcrops, etc.—but there are also reefs such as the coral reefs of tropical waters formed by biotic processes dominated by corals and coralline algae, and artificial reefs such as shipwrecks and other anthropogenic underwater structures may occur intentionally or as the result of an accident, and sometimes have a designed role in enhancing the physical complexity of featureless sand bottoms, to attract a more diverse assemblage of organisms. Reefs are often quite near to the surface, but not all definitions require this. Earth's largest coral reef system is the Great Barrier Reef in Australia, at a length of over . Biotic There is a variety of biotic reef types, including oyster reefs and sponge reefs, but the most massive and w ...
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