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Bairnsdale Dragway
Bairnsdale () ( Ganai: ''Wy-yung'') is a city in East Gippsland, Victoria, Australia in a region traditionally owned by the Tatungalung clan of the Gunaikurnai people. The estimated population of Bairnsdale urban area was 15,411 at June 2018. Estimated resident population, 30 June 2018. The city is a major regional centre of eastern Victoria along with Traralgon and Sale and the commercial centre for the East Gippsland region and the seat of local government for the Shire of East Gippsland. Bairnsdale was first proclaimed a shire on 16 July 1868 and it was proclaimed as a city on 14 July 1990. Accessed at State Library of Victoria, La Trobe Reading Room. The origin of the city's name is uncertain. It was possibly Bernisdale, with "Bernis-dale" originating from "Bjorn's dale, or glen", which indicates the Viking origins of the Skye Village. Legend has it that Macleod was so impressed by the large number of children on the run, the children of his stockmen, that he call ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Australian Bureau Of Statistics
The Australian Bureau of Statistics (ABS) is the independent statutory agency of the Australian Government responsible for statistical collection and analysis and for giving evidence-based advice to federal, state and territory governments. The ABS collects and analyses statistics on economic, population, environmental and social issues, publishing many on their website. The ABS also operates the national Census of Population and Housing that occurs every five years. History In 1901, statistics were collected by each state for their individual use. While attempts were made to coordinate collections through an annual Conference of Statisticians, it was quickly realized that a National Statistical Office would be required to develop nationally comparable statistics. The Commonwealth Bureau of Census and Statistics (CBCS) was established under the Census and Statistics Act in 1905. Sir George Knibbs was appointed as the first Commonwealth Statistician. Initially, the bureau w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Henry Lawson
Henry Archibald Hertzberg Lawson (17 June 1867 – 2 September 1922) was an Australian writer and bush poet. Along with his contemporary Banjo Paterson, Lawson is among the best-known Australian poets and fiction writers of the colonial period and is often called Australia's "greatest short story writer". A vocal nationalist and republican, Lawson regularly contributed to '' The Bulletin'', and many of his works helped popularise the Australian vernacular in fiction. He wrote prolifically into the 1890s, after which his output declined, in part due to struggles with alcoholism and mental illness. At times destitute, he spent periods in Darlinghurst Gaol and psychiatric institutions. After he died in 1922 following a cerebral haemorrhage, Lawson became the first Australian writer to be granted a state funeral. He was the son of the poet, publisher and feminist Louisa Lawson. Family and early life Henry Lawson was born 17 June 1867 in a town on the Grenfell goldfields of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geomorphological
Geomorphology (from Ancient Greek: , ', "earth"; , ', "form"; and , ', "study") is the scientific study of the origin and evolution of topographic and bathymetric features created by physical, chemical or biological processes operating at or near Earth's surface. Geomorphologists seek to understand why landscapes look the way they do, to understand landform and terrain history and dynamics and to predict changes through a combination of field observations, physical experiments and numerical modeling. Geomorphologists work within disciplines such as physical geography, geology, geodesy, engineering geology, archaeology, climatology, and geotechnical engineering. This broad base of interests contributes to many research styles and interests within the field. Overview Earth's surface is modified by a combination of surface processes that shape landscapes, and geologic processes that cause tectonic uplift and subsidence, and shape the coastal geography. Surface processes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alluvial
Alluvium (from Latin ''alluvius'', from ''alluere'' 'to wash against') is loose clay, silt, sand, or gravel that has been deposited by running water in a stream bed, on a floodplain, in an alluvial fan or beach, or in similar settings. Alluvium is also sometimes called alluvial deposit. Alluvium is typically geologically young and is not consolidated into solid rock. Sediments deposited underwater, in seas, estuaries, lakes, or ponds, are not described as alluvium. Floodplain alluvium can be highly fertile, and supported some of the earliest human civilizations. Definitions The present consensus is that "alluvium" refers to loose sediments of all types deposited by running water in floodplains or in alluvial fans or related landforms. However, the meaning of the term has varied considerably since it was first defined in the French dictionary of Antoine Furetière, posthumously published in 1690. Drawing upon concepts from Roman law, Furetière defined ''alluvion'' (the F ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Delta
A river delta is a landform shaped like a triangle, created by deposition (geology), deposition of sediment that is carried by a river and enters slower-moving or stagnant water. This occurs where a river enters an ocean, sea, estuary, lake, reservoir, or (more rarely) another river that cannot carry away the supplied sediment. It is so named because its triangle shape resembles the Greek letter Delta. The size and shape of a delta is controlled by the balance between watershed processes that supply sediment, and receiving basin processes that redistribute, sequester, and export that sediment. The size, geometry, and location of the receiving basin also plays an important role in delta evolution. River deltas are important in human civilization, as they are major agricultural production centers and population centers. They can provide Coast, coastline defense and can impact drinking water supply. They are also Ecology, ecologically important, with different species' assemblages ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Levees
A levee (), dike (American English), dyke (Commonwealth English), embankment, floodbank, or stop bank is a structure that is usually earthen and that often runs parallel to the course of a river in its floodplain or along low-lying coastlines. The purpose of a levee is to keep the course of rivers from changing and to protect against flooding of the area adjoining the river or coast. Levees can be naturally occurring ridge structures that form next to the bank of a river, or be an artificially constructed fill or wall that regulates water levels. Ancient civilizations in the Indus Valley, ancient Egypt, Mesopotamia and China all built levees. Today, levees can be found around the world, and failures of levees due to erosion or other causes can be major disasters. Etymology Speakers of American English (notably in the Midwest and Deep South) use the word ''levee'', from the French word (from the feminine past participle of the French verb , 'to raise'). It originated i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Floodplains
A floodplain or flood plain or bottomlands is an area of land adjacent to a river which stretches from the banks of its channel to the base of the enclosing valley walls, and which experiences flooding during periods of high discharge.Goudie, A. S., 2004, ''Encyclopedia of Geomorphology'', vol. 1. Routledge, New York. The soils usually consist of clays, silts, sands, and gravels deposited during floods. Because the regular flooding of floodplains can deposit nutrients and water, floodplains frequently have high soil fertility; some important agricultural regions, such as the Mississippi river basin and the Nile, rely heavily on the flood plains. Agricultural regions as well as urban areas have developed near or on floodplains to take advantage of the rich soil and fresh water. However, the risk of flooding has led to increasing efforts to control flooding. Formation Most floodplains are formed by deposition on the inside of river meanders and by overbank flow. Wherever ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Thomson River (Victoria)
The Thomson River, a perennial river of the West Gippsland catchment, is located in the Gippsland region of the Australian state of Victoria. Location and features The Thomson River rises below Newlands at the north western end of the Baw Baw Plateau of the Great Dividing Range, where it shares a watershed with the Yarra and Tanjil rivers. From its source, the river flows generally north, then east, then south southeast through its impoundment, then southeast, then east, and finally east by south, joined by seventeen tributaries including the Jordan, Aberfeldy, and Macalister rivers, before reaching its confluence with the Latrobe River near Sale. The river descends over its course. The Thomson Valley was intensively mined for gold during the latter half of the 19th and early 20th centuries. Prospector "Ned" Stringer discovered significant quantities of alluvial gold at the junction of what is now known as Stringers Creek. A short distance up that creek the gold mining tow ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Latrobe River
The Latrobe River (or sometimes La Trobe or LaTrobe) is a perennial river of the West Gippsland catchment, located in the West Gippsland region of the Australian state of Victoria. The Latrobe River and its associated sub-catchment is an important source for the Gippsland Lakes, draining the south eastern slopes of the Great Dividing Range. Course and features The Latrobe River rises below Dick Hill, from the southern slopes of the Baw Baw plateau, part of the Great Dividing Range, between Powelltown and Noojee where it shares a watershed with the Little Yarra River, in a state forestry area. The river flows generally in an easterly direction, then south, and then east again through the Latrobe Valley, joined by seventeen tributaries including the Ada, Toorongo, Loch, Tanjil, Morwell, Tyers, and Thomson rivers, before reaching its mouth in Lake Wellington east of where it forms its confluence with the Avon. It then goes to flow out of Lake Wellington and into Lake V ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gigalitre
The litre (international spelling) or liter (American English spelling) (SI symbols L and l, other symbol used: ℓ) is a metric unit of volume. It is equal to 1 cubic decimetre (dm3), 1000 cubic centimetres (cm3) or 0.001 cubic metre (m3). A cubic decimetre (or litre) occupies a volume of (see figure) and is thus equal to one-thousandth of a cubic metre. The original French metric system used the litre as a base unit. The word ''litre'' is derived from an older French unit, the '' litron'', whose name came from Byzantine Greek—where it was a unit of weight, not volume—via Late Medieval Latin, and which equalled approximately 0.831 litres. The litre was also used in several subsequent versions of the metric system and is accepted for use with the SI,Bureau International des Poids et Me ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nicholson River (Victoria)
The Nicholson River is a perennial river of the Mitchell River catchment, located in the East Gippsland region of the Australian state of Victoria. Course and features The Nicholson River rises below the Angora Range in the lower reaches of the Victorian Alps within the Great Dividing Range, near the small settlement of Marthavale, west of . The river flows generally southeast passing through the small town of before entering Lake King, one of the main lakes in the extensive Gippsland Lakes system. Within the lake, the Nicholson River forms its confluence with the Mitchell River, which joins with the Tambo River; with the Mitchell River draining into Bass Strait southwest of , in the Shire of East Gippsland. The river descends over its course. The river is impounded by the Nicholson River Dam, that forms a water reservoir used for the supply of town water to Lakes Entrance, until 1995. In its lower reaches, the river is traversed by the Great Alpine Road, the Princes H ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tambo River (Victoria)
The Tambo River or ''Berrawan'' is a perennial river of the Mitchell River catchment, located in the East Gippsland region of the Australian state of Victoria. With a total length in excess of , the Tambo River is one of the longest rivers in the East Gippsland drainage basin, extending from the steep forested southern slopes of the Victorian Alps through forest and farmland to the Gippsland Lakes. Physical aspects Course The Tambo River rises in the Bowen Mountains, below Mount Leinster in the Victorian Alps, part of the Great Dividing Range, about east of . The river flows generally south by south southeast by south southwest, joined by sixteen tributaries including the Little and Timbarra rivers, before reaching its mouth and emptying into Lake King, one of the main lakes in the extensive Gippsland Lakes system. Within the lake, the Tambo River forms confluence with the Mitchell River, west of the village of , with the Mitchell River draining into Bass Strait southwest of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
