|
Anindilyakwa People
The Anindilyakwa people (''Warnumamalya)'' are Aboriginal Australian people living on Groote Eylandt, Bickerton Island, and Woodah Island in the Gulf of Carpentaria in the Northern Territory of Australia. Names The accepted names for the Traditional Owners of the Groote archipelago are the Anindilyakwa people or Warnumamalya ('True People' in the Anindilyakwa language). Although they have a strong sense of identity, the fourteen clans on Groote Eylandt and the surrounding islands did not have a collective name that they referred to themselves. They have been called the Warnindilyakwa in the past. However, this term refers to a specific clan from the Dilyakburra peninsula on the southeastern part of the island. Anthropologist Norman Tindale previously used , the Nunggubuyu word for Groote Eylandt people. History Macassan traders Macassans from Sulawesi traded with northern Australian Aboriginal people long before the arrival of Europeans. Exploiting the monsoonal winds in D ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Groote Eylandt
Groote Eylandt ( Anindilyakwa: ''Ayangkidarrba'' meaning "island" ) is the largest island in the Gulf of Carpentaria and the fourth largest island in Australia. It was named by the explorer Abel Tasman in 1644 and is Dutch for "Large Island" in archaic spelling. The modern Dutch spelling is ''Groot Eiland''. The original inhabitants of Groote Eylandt are the Anindilyakwa, an Aboriginal Australian people, who speak the Anindilyakwa language (also known as Amamalya Ayakwa). They consist of 14 clan groups which make up the two moieties on the island. The clans maintain their traditions and have strong ties with the people in the community of Numbulwar and on Bickerton Island. The island's population was 2,811 in the 2016 census. There are four communities on Groote Eylandt. The mining company GEMCO established the township of Alyangula for its workers. The three main Aboriginal communities are Angurugu and Umbakumba, and Milyakburra on Bickerton Island. There are also a number ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Makassar People
The Makassar or Makassarese people are an ethnic group that inhabits the southern part of the South Peninsula, Sulawesi (formerly Celebes) in Indonesia. They live around Makassar, the capital city of the province of South Sulawesi, as well as the Konjo highlands, the coastal areas, and the Selayar and Spermonde islands. They speak Makassarese, which is closely related to Buginese and also a Malay creole called Makassar Malay. History The Makassar are an ethnic group originally from the southern coast of the island of Sulawesi. Their exploratory spirits have led to successful overseas explorations. This is exemplified by the Kingdom of Gowa (14-17th century), which succeeded in forming a vast Islamic empire with a large and strong naval force. Its territory included almost the entire island of Sulawesi, eastern Kalimantan, East Nusa Tenggara, part of West Nusa Tenggara, part of Maluku and some small surrounding islands. The Makassar people made treaties with Bali and coopera ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cycas Angulata
''Cycas angulata'' is a species of cycad in the genus ''Cycas'', native to Australia in northeast Northern Territory (lower reaches of the Foelsche, Robinson and Wearyan Rivers near Borroloola) and northwest Queensland ( Bountiful Islands). It is the largest Australian ''Cycas'' species, with arborescent and frequently branched stems growing to 5 m (rarely 12 m) tall, and 15–25 cm in diameter. Older specimens lose the leaf base scars and gain a more checkerboard appearance. The leaves are 1.1-1.7 m long, pinnate with 180-320 leaflets, the leaflets 14–23 cm long and 4.5-6.5 mm wide, grey-green to glaucous; there are to 40 leaves in the crown. The leaf petioles are armed with spines in younger individuals (a few millimetres long) with this trait being lost in older individuals. The female cones are open type sporophylls 25–50 cm long, brown, each with 6-12 ovules each. The lamina is triangular ending in a sharp narrow spine. The male cones are solitary, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Laterite
Laterite is both a soil and a rock type rich in iron and aluminium and is commonly considered to have formed in hot and wet tropical areas. Nearly all laterites are of rusty-red coloration, because of high iron oxide content. They develop by intensive and prolonged weathering of the underlying parent rock, usually when there are conditions of high temperatures and heavy rainfall with alternate wet and dry periods. Tropical weathering (''laterization'') is a prolonged process of chemical weathering which produces a wide variety in the thickness, grade, chemistry and ore mineralogy of the resulting soils. The majority of the land area containing laterites is between the tropics of Cancer and Capricorn. Laterite has commonly been referred to as a soil type as well as being a rock type. This and further variation in the modes of conceptualizing about laterite (e.g. also as a complete weathering profile or theory about weathering) has led to calls for the term to be abandoned alto ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mudflat
Mudflats or mud flats, also known as tidal flats or, in Ireland, slob or slobs, are coastal wetlands that form in intertidal areas where sediments have been deposited by tides or rivers. A global analysis published in 2019 suggested that tidal flat ecosystems are as extensive globally as mangroves, covering at least of the Earth's surface. / They are found in sheltered areas such as bays, bayous, lagoons, and estuaries; they are also seen in freshwater lakes and salty lakes (or inland seas) alike, wherein many rivers and creeks end. Mudflats may be viewed geologically as exposed layers of bay mud, resulting from deposition of estuarine silts, clays and aquatic animal detritus. Most of the sediment within a mudflat is within the intertidal zone, and thus the flat is submerged and exposed approximately twice daily. A recent global remote sensing analysis estimated that approximately 50% of the global extent of tidal flats occurs within eight countries (Indonesia, China, Austral ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mangrove
A mangrove is a shrub or tree that grows in coastal saline water, saline or brackish water. The term is also used for tropical coastal vegetation consisting of such species. Mangroves are taxonomically diverse, as a result of convergent evolution in several plant families. They occur worldwide in the tropics and subtropics and even some temperate coastal areas, mainly between latitudes 30° N and 30° S, with the greatest mangrove area within 5° of the equator. Mangrove plant families first appeared during the Late Cretaceous to Paleocene epochs, and became widely distributed in part due to the plate tectonics, movement of tectonic plates. The oldest known fossils of Nypa fruticans, mangrove palm date to 75 million years ago. Mangroves are salt-tolerant trees, also called halophytes, and are adapted to live in harsh coastal conditions. They contain a complex salt filtration system and a complex root system to cope with saltwater immersion and wave action. They are ad ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sand Dune
A dune is a landform composed of wind- or water-driven sand. It typically takes the form of a mound, ridge, or hill. An area with dunes is called a dune system or a dune complex. A large dune complex is called a dune field, while broad, flat regions covered with wind-swept sand or dunes with little or no vegetation are called ''ergs'' or ''sand seas''. Dunes occur in different shapes and sizes, but most kinds of dunes are longer on the stoss (upflow) side, where the sand is pushed up the dune, and have a shorter ''slip face'' in the lee side. The valley or trough between dunes is called a ''dune slack''. Dunes are most common in desert environments, where the lack of moisture hinders the growth of vegetation that would otherwise interfere with the development of dunes. However, sand deposits are not restricted to deserts, and dunes are also found along sea shores, along streams in semiarid climates, in areas of glacial outwash, and in other areas where poorly cemented san ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Loanword
A loanword (also loan word or loan-word) is a word at least partly assimilated from one language (the donor language) into another language. This is in contrast to cognates, which are words in two or more languages that are similar because they share an etymological origin, and calques, which involve translation. Loanwords from languages with different scripts are usually transliterated (between scripts), but they are not translated. Additionally, loanwords may be adapted to phonology, phonotactics, orthography, and morphology of the target language. When a loanword is fully adapted to the rules of the target language, it is distinguished from native words of the target language only by its origin. However, often the adaptation is incomplete, so loanwords may conserve specific features distinguishing them from native words of the target language: loaned phonemes and sound combinations, partial or total conserving of the original spelling, foreign plural or case forms or indecli ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Laminal Consonant
A laminal consonant is a phone (speech sound) produced by obstructing the air passage with the blade of the tongue, the flat top front surface just behind the tip of the tongue in contact with upper lip, teeth, alveolar ridge, to possibly, as far back as the prepalatal arch, although in the last contact may involve as well parts behind the blade. It is distinct from an apical consonant, produced by creating an obstruction with the tongue apex (tongue tip) only. Sometimes laminal is used exclusively for an articulation that involves only the blade of the tongue with the tip being lowered and apicolaminal for an articulation that involves both the blade of the tongue and the raised tongue tip. The distinction applies only to coronal consonants, which use the front of the tongue. Compared to apical Although most languages do not contrast laminal and apical sounds, the distinction is found in a number of languages: *The contrast is very common in Australian Aboriginal languages, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pama–Nyungan Languages
The Pama–Nyungan languages are the most widespread family of Australian Aboriginal languages, containing 306 out of 400 Aboriginal languages in Australia. The name "Pama–Nyungan" is a merism: it derived from the two end-points of the range: the Pama languages of northeast Australia (where the word for "man" is ) and the Nyungan languages of southwest Australia (where the word for "man" is ). The other language families indigenous to the continent of Australia are occasionally referred to, by exclusion, as non-Pama–Nyungan languages, though this is not a taxonomic term. The Pama–Nyungan family accounts for most of the geographic spread, most of the Aboriginal population, and the greatest number of languages. Most of the Pama–Nyungan languages are spoken by small ethnic groups of hundreds of speakers or fewer. The vast majority of languages, either due to disease or elimination of their speakers, have become extinct, and almost all remaining ones are endangered in some ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Australian Aboriginal Languages
The Indigenous languages of Australia number in the hundreds, the precise number being quite uncertain, although there is a range of estimates from a minimum of around 250 (using the technical definition of 'language' as non-mutually intelligible varieties) up to possibly 363. The Indigenous languages of Australia comprise numerous language families and isolates, perhaps as many as 13, spoken by the Indigenous peoples of mainland Australia and a few nearby islands. The relationships between the language families are not clear at present although there are proposals to link some into larger groupings. Despite this uncertainty, the Indigenous Australian languages are collectively covered by the technical term "Australian languages", or the "Australian family". The term can include both Tasmanian languages and the Western Torres Strait language, but the genetic relationship to the mainland Australian languages of the former is unknown, while the latter is Pama–Nyungan, thoug ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arthur Capell
Arthur Capell (28 March 1902 – 10 August 1986) was an Australian linguist, who made major contributions to the study of Australian languages, Austronesian languages and Papuan languages. Early life Capell was born in Newtown, New South Wales in 1902, the only child of Sarah Ann (née Scott) and her husband, Henry Capell. He attended North Sydney Boys' High School. Career Capell graduated from the Sydney Teachers' College in Modern Languages in 1922 and the University of Sydney in the same year as the University medallist in Classics. He taught in high schools for three years at Canterbury Boys' Intermediate High and Tamworth High School. He was then ordained deacon in 1925 and priest in 1926 in the Church of England in Australia. He worked in Newcastle for a decade, as Curate, St Peter's, Hamilton (1926–28); Priest-in-Charge, All Saints, Belmont (1928–29); as a teacher at Broughton School for Boys in Newcastle (1929–32), where he was introduced to the anthropologist ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
.JPG "Click for more on -> Mangrove")
