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Volow
Volow (formerly known as ''Valuwa'' or ''Valuga'') is an Oceanic language variety which used to be spoken in the area of Aplow, in the eastern part of the island of Motalava, in Vanuatu. Name The name ''Volow'' is originally a placename: it corresponds to the area known as Aplow, but in the local language Volow rather than in Mwotlap. This form, pronounced , is derived from Proto-Torres-Banks *''βaluwa''. In neighboring Mwotlap, the same area is called ''Aplow'' (with locative prefix ''a-''), and in Mota, it is called ''Valuwa'' . Both of these are nowadays used as alternative names for the area. Sociolinguistics Volow has receded historically in favour of the now dominant language Mwotlap. It is now only remembered by a single passive speaker, who lives in the village of Aplow — the new name of what was previously known as Volow. The similarity of Volow with Mwotlap is such that the two communalects may be considered dialects of a single language. Phonology Volow ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mwotlap Language
Mwotlap (pronounced ; formerly known as ''Motlav'') is an Oceanic language spoken by about 2,100 people in Vanuatu. The majority of speakers are found on the island of Motalava in the Banks Islands, with smaller communities in the islands of Ra (or ''Aya'') and Vanua Lava, as well as migrant groups in the two main cities of the country, Santo and Port Vila. Mwotlap was first described in any detail in 2001, by the linguist Alexandre François. Volow, which used to be spoken on the same island, may be considered a dialect or a separate language. The language Name The language is named after the island. Geographic distribution Mwotlap is spoken by about 2,100 people in the Banks Islands, in the North of Vanuatu. Among them, 1,640 live on the island of Mota Lava and its neighbor island, Ra. It is also spoken by a few hundred people living elsewhere in Vanuatu: * Vanua Lava, particularly in the northeast * Several other northern Vanuatu islands including Ureparapara, Gaua, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Torres–Banks Languages
The Torres–Banks languages form a linkage of Southern Oceanic languages spoken in the Torres Islands and Banks Islands of northern Vanuatu. Languages François (2011) recognizes 17 languages spoken by 9,400 people in 50 villages, including 16 living (3 of which are moribund) and one extinct language. François (2011). The 17 languages, ranked from northwest to southeast, are: : Comparative studies A. François has published several studies comparing various features of the Torres–Banks languages: * François (2005): Inventories of vowel systems, and their historical development; * François (2007): Systems of noun articles, and their historical development; * François (2009): How several languages grammaticalized a set of light personal pronouns into markers for “aorist” aspect; * François (2011): How Torres–Banks languages tend to show structural isomorphism, yet lexical diversity; * François (2013): Etymological reconstruction of spiritual terms in Torres–B ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Labial–velar Consonant
Labial–velar consonants are doubly articulated at the velum and the lips, such as . They are sometimes called "labiovelar consonants", a term that can also refer to labialized velars, such as the stop consonant and the approximant . Labial-velars are often written as digraphs. In the Kâte language, however, is written Q q, and as Ɋ ɋ. Globally, these types of consonants are quite rare, only existing in two regions: West and Central Africa on the one hand, Eastern New Guinea and northern Vanuatu on the other. Labial-velar stops Truly doubly articulated labial-velars include the stops and the nasal . To pronounce them, one must attempt to say the velar consonants but then close their lips for the bilabial component, and then release the lips. While 90% of the occlusion overlaps, the onset of the velar occurs slightly before that of the labial, and the release of the labial occurs slightly after that of the velar so the preceding vowel sounds as if it were followed by a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aplow
Aplow, or ''Valuwa'', is a village located on the eastern part of Motalava island, in the Banks Islands of Vanuatu. Located close to it is the island's airport, ''Valua airport''. Aplow also designates the whole district around this village, corresponding to the eastern side of the island; in this sense, Aplow contrasts with ''Mwotlap'', which strictly speaking designates the western half of Motalava island. The area of Aplow used to be home of a communalect (language or dialect) known as Volow. Volow become extinct in the 1980s, as its speakers adopted the dominant language Mwotlap from the western side. Name The name ''Aplow'' is the name of the village in Mwotlap, which is the dominant language spoken today on the island. The same village was originally known as ''Volow'' in the now extinct language of the same name. Finally, the village, as well as the district around it, are sometimes designated as ''Valuwa'' (or wrongly as ''Valua''). this reflects the form of the w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Labialization
Labialization is a secondary articulatory feature of sounds in some languages. Labialized sounds involve the lips while the remainder of the oral cavity produces another sound. The term is normally restricted to consonants. When vowels involve the lips, they are called rounded. The most common labialized consonants are labialized velars. Most other labialized sounds also have simultaneous velarization, and the process may then be more precisely called labio-velarization. In phonology, labialization may also refer to a type of assimilation process. Occurrence Labialization is the most widespread secondary articulation in the world's languages. It is phonemically contrastive in Northwest Caucasian (e.g. Adyghe), Athabaskan, and Salishan language families, among others. This contrast is reconstructed also for Proto-Indo-European, the common ancestor of the Indo-European languages; and it survives in Latin and some Romance languages. It is also found in the Cushitic and E ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North Vanuatu Languages
The North Vanuatu languages form a Linkage (linguistics), linkage of Southern Oceanic languages spoken in northern Vanuatu. Languages Clark (2009) Clark (2009) provides the following classification of the North Vanuatu languages, divided into two main geographic areas (Torres–Banks–Maewo–Ambae–Pentecost and Espiritu Santo, Santo). Outlier (aberrant) languages identified by Clark (2009) are in ''italics''.The language names used by Clark have often been superseded by other names; in that case, the glottonym used by Clark is indicated in brackets. *North Vanuatu **Northern (Torres–Banks–Maewo–Ambae–Pentecost) ***Torres–Banks languages ****Torres Islands: Hiw language, Hiw, Lo-Toga language, Lo-Toga (“Loh”) ****Banks Islands: Lehali language, Lehali–Löyöp language, Löyöp (“Ureparapara”), Mwotlap language, Mwotlap–Volow language, Volow (“Mwotlav”), Lemerig language, Lemerig–Vera'a language, Vera’a (“Vera'a”), Vurës language, Vurës–Mwe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Banks Islands
The Banks Islands (in Bislama ''Bankis'') are a group of islands in northern Vanuatu. Together with the Torres Islands to their northwest, they make up the northernmost province of Torba. The island group lies about north of Maewo, and includes Gaua and Vanua Lava, two of the 13 largest islands in Vanuatu. In 2009, the islands had a population of 8,533. The island group's combined land area is 780 km2. Geography The largest island is Gaua (formerly called Santa Maria), which has a rugged terrain, rising to Mount Gharat, an active volcano at the centre of the island, at . Gaua's freshwater Lake Letas, in its volcanic crater, is the largest lake in Vanuatu. A slightly smaller island in the group, Vanua Lava, is higher, at ; it too has an active volcano: Mount Suretamate (also spelled Süretimiat or Sere'ama, ). To the east of Vanua Lava are two islets in the groupo, Ravenga and Kwakea (also spelled Qakea). Sola, the provincial capital, is on Vanua Lava. The third largest ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Motalava
Mota Lava or Motalava is an island of the Banks group, in the north of Vanuatu. It forms a single coral system with the small island of Ra. The 2009 census figures give a population of 1640 inhabitants (Mota Lava + Ra), which amounts to a population density of 67 people per km². Geography Geography and geology With an area of 24 km2 (9.3 sq mi), Mota Lava is the fourth largest island in the Banks Islands, after Gaua, Vanua Lava and Ureparapara. It is the highest () of the eastern chain of islands, as well as the largest. Ra, a small island of , is located off the southern coast of Mota Lava. It is attached to it by high corals that one can wade through at low tide. The climate on Mota Lava is humid tropical. The average annual rainfall exceeds 4000 mm. The island is subject to frequent earthquakes and cyclones. The island is served by Mota Lava Airport. Geology Mota Lava is composed of at least five basaltic stratovolcanoes. Two of the cones, Vetman ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mota Lava
Mota Lava or Motalava is an island of the Banks Islands, Banks group, in the north of Vanuatu. It forms a single coral system with the Ra Island, small island of Ra. The 2009 Vanuatu Census, 2009 census figures give a population of 1640 inhabitants (Mota Lava + Ra island, Ra), which amounts to a population density of 67 people per km². Geography Geography and geology With an area of 24 km2 (9.3 sq mi), Mota Lava is the fourth largest island in the Banks Islands, after Gaua, Vanua Lava and Ureparapara. It is the highest () of the eastern chain of islands, as well as the largest. Ra Island, Ra, a small island of , is located off the southern coast of Mota Lava. It is attached to it by high corals that one can wade through at low tide. The climate on Mota Lava is humid tropical. The average annual rainfall exceeds 4000 mm. The island is subject to frequent earthquakes and cyclones. The island is served by Mota Lava Airport. Geology Mota Lava is composed of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Approximant Consonant
Approximants are speech sounds that involve the articulators approaching each other but not narrowly enough nor with enough articulatory precision to create turbulent airflow. Therefore, approximants fall between fricatives, which do produce a turbulent airstream, and vowels, which produce no turbulence. This class is composed of sounds like (as in ''rest'') and semivowels like and (as in ''yes'' and ''west'', respectively), as well as lateral approximants like (as in ''less''). Terminology Before Peter Ladefoged coined the term "approximant" in the 1960s, the terms "frictionless continuant" and "semivowel" were used to refer to non-lateral approximants. In phonology, "approximant" is also a distinctive feature that encompasses all sonorants except nasals, including vowels, taps and trills. Semivowels Some approximants resemble vowels in acoustic and articulatory properties and the terms ''semivowel'' and ''glide'' are often used for these non-syllabic vowel-like segme ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Prenasalization
Prenasalized consonants are phonetic sequences of a nasal and an obstruent (or occasionally a non-nasal sonorant such as ) that behave phonologically like single consonants. The primary reason for considering them to be single consonants, rather than clusters as in English ''finger'' or ''member'', lies in their behaviour; however, there may also be phonetic correlates which distinguish prenasalized consonants from clusters. Because of the additional difficulty in both articulation and timing, prenasalized fricatives and sonorants are not as common as prenasalized stops or affricates, and the presence of the former implies the latter. In most languages, when a prenasalized consonant is described as "voiceless", it is only the oral portion that is voiceless, and the nasal portion is modally voiced. Thus, a language may have "voiced" and "voiceless" . However, in some Southern Min (including Taiwanese) dialects, voiced consonants are preceded by voiceless prenasalization: . Yeyi ha ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dorsal Consonant
Dorsal consonants are consonants articulated with the back of the tongue (the dorsum). They include the palatal, velar and, in some cases, alveolo-palatal and uvular consonants. They contrast with coronal consonants, articulated with the flexible front of the tongue, and laryngeal consonants, articulated in the pharyngeal cavity. Function The dorsum of the tongue can contact a broad region of the roof of the mouth, from the hard palate (palatal consonants), the flexible velum behind that (velar consonants), to the uvula at the back of the mouth cavity (uvular consonants). These distinctions are not clear cut, and sometimes finer gradations such as ''pre-palatal, pre-velar,'' and ''post-velar'' will be noted. Because the tip of the tongue can curl back to also contact the hard palate for retroflex consonants (''subapical-palatal''), consonants produced by contact between the dorsum and the palate are sometimes called ''dorso-palatal.'' Examples See also *Place of articulation ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
