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Hughenden, Queensland
Hughenden is a rural town and locality in the Flinders Shire, Queensland, Australia. In the , the locality of Hughenden had a population of 1,136 people. Geography Hughenden is situated on the banks of the Flinders River. Hughenden has the following mountains (from west to east): * Mount Walker () * Mount Mowbray () * Mount Devlin () * Mount Castor () * Mount Beckford () Hughenden is located on the Flinders Highway, west of Townsville and north-west of Brisbane, the state capital. The region around Hughenden is a major centre for the grazing of sheep and cattle. The main feed is annual grasses known as Flinders grass, which grow rapidly on the (by Australian standards) fertile grey or brown cracking clay soils after rain between November and March. However, because the rainfall is extremely erratic – at Hughenden itself it has ranged from in 1926 to in 1950 – droughts and floods are normal and stock numbers fluctuate greatly. The runoff from the Flinders R ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
AEST
Australia uses three main time zones: Australian Western Standard Time (AWST; UTC+08:00), Australian Central Standard Time (ACST; UTC+09:30), and Australian Eastern Standard Time (AEST; UTC+10:00). Time is regulated by the individual state governments, some of which observe daylight saving time (DST). Australia's external territories observe different time zones. Standard time was introduced in the 1890s when all of the Australian colonies adopted it. Before the switch to standard time zones, each local city or town was free to determine its local time, called local mean time. Now, Western Australia uses Western Standard Time; South Australia and the Northern Territory use Central Standard Time; while New South Wales, Queensland, Tasmania, Victoria (Australia), Victoria, Jervis Bay Territory, and the Australian Capital Territory use Eastern Standard Time. Daylight saving time (+1 hour) is used in jurisdictions in the south and south-east: South Australia, New South Wales, Vict ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Flinders River
The Flinders River is the longest river in Queensland, Australia, at approximately . It was named in honour of the explorer Matthew Flinders. The catchment is sparsely populated and mostly undeveloped. The Flinders rises on the western slopes of the Great Dividing Range in North West Queensland and flows generally north-west through the Gulf Country, across a large, flat clay pan, before entering the Gulf of Carpentaria. Course and features The River rises in the Burra Range, part of the Great Dividing Range, north-east of Hughenden and flows in a westerly direction past Hughenden, Richmond and Julia Creek, then north-west to the Gulf of Carpentaria west of . The catchment is bordered to the south by the Selwyn Range. At in length, it is the eighth-longest river in Australia. The catchment covers . The primary land use in the catchment is grazing and other agriculture, the catchment covers 1.5% of the continent. A total of 36 tributaries flow into the Flinders, the pr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Australian Aboriginal Language
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] |
Yirandhali Language
Yirandhali (Yirandali, Jirandali), also known as Pooroga, is an extinct Australian Aboriginal language of Hughenden in Central Queensland. Yirandhali is a Pama–Nyungan language. Dixon (2002) speculates that it may belong in the Maric branch of that family, but further research is required before this can be verified, due to the limited lexical material that is available in the language.Dixon, Robert (2002) ''Australian Languages: Their Nature and Development''. . There is very little information available about the languages of this region. Oral recounts suggest that the town area of Hughenden was a place that was passed through rather than a place that was used as a regular campsite. The Flinders River is often a dry river bed. At the nearby Porcupine Gorge, in an area known locally as 'the Tattoos', there are signs of Aboriginal rock drawings. This area would have been a more reliable source of water. Classification A Pama–Nyungan language, Dixon (2002) speculat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yirandhali
The Yirandhali are an indigenous Australian people, who lived in the area of the present day Shire of Flinders in the state of Queensland. Language Yirandhali may possibly. according to Robert Dixon, belong to the Maric branch of the Pama–Nyungan language family. According to Peter Sutton, the list of words given by an early settler, M. Armstrong of the language of the Upper Cape River, which Tindale ascribes to the Yilba, actually refers to the Yirandhali language. Country The Yirandhali had an estimated territorial estate, according to Norman Tindale, of around . The heartland of their country lay west of the Great Dividing Range, around the upper Dutton and Flinders rivers and stretched from neaMount Sturgeonsouthwards as far as Caledonia. Their western limits lay close to Richmond, Corfield, and the area east of Winton. The Yirandhali were the indigenous peoples of Torrens, Tower Hill, and Landsborough Creeks, of Lammermoor, Hughenden and Tangorin. Watering on Yir ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hughenden-Winton Railway Line
The Hughenden-Winton railway line was a railway line in Queensland, Australia, branching from the Mt Isa line at Hughenden and connecting to the Central West line at Winton. It was originally part of the Great Northern Railway (Mt Isa line), but was later downgraded to branch line status when the extension west of Hughenden opened. History Queensland is the second largest of the Australian States and Territories by area. Its vast interior was largely opened up by the construction of three east-west railway lines that connected the interior of the State to the eastern coastal towns of Brisbane, Rockhampton and Townsville. The trunk lines were the Main Line and Western Line from Brisbane to Roma and Charleville (completed in 1888), the Central West line from Rockhampton to Emerald and Longreach (completed in 1892), and the Great Northern Line from Townsville to Charters Towers and Hughenden (completed in 1887). But those termini were still some 500 kilometres from Quee ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Great Northern Railway (Mt Isa Line)
The Great Northern Railway is a railway line in Queensland, Australia. The line stretches nearly 1,000 kilometres linking the port city of Townsville, Australia to the mining town of Mount Isa in north-west Queensland. Along with a passenger service called the Inlander, it is a major freight route connecting the Mount Isa Mines to the Port of Townsville. In 2010 the line moved 5.8 million tonnes of cargo, and this is expected to increase significantly in coming years. History Originally approved in 1877, its construction over nearly thirty years along with the building of other lines in Queensland was dictated by the pressing need to transport minerals and wool from isolated inland areas to the coast for shipment. To the goldfields In Townsville’s case it was given impetus by the discovery of gold at Ravenswood, Queensland and Charters Towers, Queensland in 1868 and 1872 respectively. The first section of the railway opened on 20 December 1880 and followed a sou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Irrigation
Irrigation (also referred to as watering) is the practice of applying controlled amounts of water to land to help grow Crop, crops, Landscape plant, landscape plants, and Lawn, lawns. Irrigation has been a key aspect of agriculture for over 5,000 years and has been developed by many cultures around the world. Irrigation helps to grow crops, maintain landscapes, and revegetation, revegetate disturbed soils in dry areas and during times of below-average rainfall. In addition to these uses, irrigation is also employed to protect crops from frost, suppress weed growth in grain fields, and prevent soil consolidation. It is also used to cool livestock, reduce dust, dispose of sewage, and support mining operations. Drainage, which involves the removal of surface and sub-surface water from a given location, is often studied in conjunction with irrigation. There are several methods of irrigation that differ in how water is supplied to plants. Surface irrigation, also known as gravity irri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Runoff (water)
Surface runoff (also known as overland flow) is the flow of water occurring on the ground surface when excess rainwater, stormwater, meltwater, or other sources, can no longer sufficiently rapidly infiltrate in the soil. This can occur when the soil is saturated by water to its full capacity, and the rain arrives more quickly than the soil can absorb it. Surface runoff often occurs because impervious areas (such as roofs and pavement) do not allow water to soak into the ground. Furthermore, runoff can occur either through natural or man-made processes. Surface runoff is a major component of the water cycle. It is the primary agent of soil erosion by water. The land area producing runoff that drains to a common point is called a drainage basin. Runoff that occurs on the ground surface before reaching a channel can be a nonpoint source of pollution, as it can carry man-made contaminants or natural forms of pollution (such as rotting leaves). Man-made contaminants in runoff in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Flood
A flood is an overflow of water ( or rarely other fluids) that submerges land that is usually dry. In the sense of "flowing water", the word may also be applied to the inflow of the tide. Floods are an area of study of the discipline hydrology and are of significant concern in agriculture, civil engineering and public health. Human changes to the environment often increase the intensity and frequency of flooding, for example land use changes such as deforestation and removal of wetlands, changes in waterway course or flood controls such as with levees, and larger environmental issues such as climate change and sea level rise. In particular climate change's increased rainfall and extreme weather events increases the severity of other causes for flooding, resulting in more intense floods and increased flood risk. Flooding may occur as an overflow of water from water bodies, such as a river, lake, or ocean, in which the water overtops or breaks levees, resulting ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Drought
A drought is defined as drier than normal conditions.Douville, H., K. Raghavan, J. Renwick, R.P. Allan, P.A. Arias, M. Barlow, R. Cerezo-Mota, A. Cherchi, T.Y. Gan, J. Gergis, D. Jiang, A. Khan, W. Pokam Mba, D. Rosenfeld, J. Tierney, and O. Zolina, 2021Water Cycle Changes In Climate Change 2021: The Physical Science Basis. Contribution of Working Group I to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change [Masson-Delmotte, V., P. Zhai, A. Pirani, S.L. Connors, C. Péan, S. Berger, N. Caud, Y. Chen, L. Goldfarb, M.I. Gomis, M. Huang, K. Leitzell, E. Lonnoy, J.B.R. Matthews, T.K. Maycock, T. Waterfield, O. Yelekçi, R. Yu, and B. Zhou (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, pp. 1055–1210, doi:10.1017/9781009157896.010. This means that a drought is "a moisture deficit relative to the average water availability at a given location and season". A drought can last for days, months or years. Drought ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vertisol
A vertisol, or vertosol, is a soil type in which there is a high content of expansive clay minerals, many of them known as montmorillonite, that form deep cracks in drier seasons or years. In a phenomenon known as argillipedoturbation, alternate shrinking and swelling causes ''self-ploughing'', where the soil material consistently mixes itself, causing some vertisols to have an extremely deep A horizon and no B horizon. (A soil with no B horizon is called an ''A/C soil''). This heaving of the underlying material to the surface often creates a microrelief known as ''gilgai''. Vertisols typically form from highly basic rocks, such as basalt, in climates that are seasonally humid or subject to erratic droughts and floods, or that impeded drainage. Depending on the parent material and the climate, they can range from grey or red to the more familiar deep black (known as "black earths" in Australia, "black gumbo" in East Texas, "black cotton" soils in East Africa, and "vlei soils" ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
