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Woady Yaloak Creek
The Woady Yaloak River is a perennial river of the Corangamite catchment, located in the Western District Lakes region of the Australian state of Victoria. Location and features The Woady Yaloak River rises below Black Hill, west of Ballarat and flows generally south joined by three minor tributaries through the towns of , and before reaching its river mouth and emptying into Lake Martin and then Lake Corangamite. From its highest point, the river descends over its meandering course. The river is crossed by the Glenelg Highway west of Scarsdale and the Hamilton Highway at Cressy, and McMillans Bridge McMillans Bridge, is a riveted wrought iron open web truss bridge, located over the Woady Yaloak River on the Rokewood-Skipton Road between Rokewood and Werneth, Victoria, Werneth on a historical route between Geelong and the 1850s goldfields at ... on the Rokewood-Skipton Road between Rokewood and Werneth. Etymology In the Aboriginal Australian Wathawurrung language ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Government Of Victoria (Australia)
The Victoria State Government, also referred to as just the Victorian Government, is the state-level authority for Victoria, Australia. Like all state governments, it is formed by three independent branches: the executive, the judicial, and the parliament. As a parliamentary constitutional monarchy, the State Government was first formed in 1851 when Victoria first gained the right to responsible government. The Constitution of Australia regulates the relationship between the Victorian Government and the Australian Government, and cedes legislative and judicial supremacy to the federal government on conflicting matters. The Victoria State Government enforces acts passed by the parliament through government departments, statutory authorities, and other public agencies. The Government is formally presided over by the Governor, who exercises executive authority granted by the state's constitution through the Executive Council, a body consisting of senior cabinet ministers. In re ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Perennial River
A perennial stream is a stream that has continuous flow of surface water throughout the year in at least parts of its catchment during seasons of normal rainfall, Water Supply Paper 494. as opposed to one whose flow is intermittent. In the absence of irregular, prolonged or extreme drought, a perennial stream is a watercourse, or segment, element or emerging body of water which continually delivers groundwater. For example, an artificial disruption of stream, variability in flow or stream selection associated with the activity in hydropower installations, do not affect this status. Perennial streams do not include stagnant water (pools and waterholes), reservoirs, cutoff lakes and ponds that persist throughout the year. All other streams, or parts of them, should be considered seasonal rivers or lakes. The stream can cycle from intermittent to perpetual through multiple iterations. Stream Definition The basic concept means flowing bodies of water. In hydrology, the strea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rivers Of Barwon South West (region)
A river is a natural flowing watercourse, usually freshwater, flowing towards an ocean, sea, lake or another river. In some cases, a river flows into the ground and becomes dry at the end of its course without reaching another body of water. Small rivers can be referred to using names such as creek, brook, rivulet, and rill. There are no official definitions for the generic term river as applied to geographic features, although in some countries or communities a stream is defined by its size. Many names for small rivers are specific to geographic location; examples are "run" in some parts of the United States, "burn" in Scotland and northeast England, and "beck" in northern England. Sometimes a river is defined as being larger than a creek, but not always: the language is vague. Rivers are part of the water cycle. Water generally collects in a river from precipitation through a drainage basin from surface runoff and other sources such as groundwater recharge, springs, a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Corangamite Catchment
{{Disambig ...
Corangamite may refer to: *Division of Corangamite *Lake Corangamite *Corangamite Shire *Corangamite Catchment Management Authority Corangamite may refer to: *Division of Corangamite *Lake Corangamite Lake Corangamite , a hypersaline endorheic lake, is located near Colac in the Lakes and Craters region of the Victorian Volcanic Plains of south-west Victoria, Australia. The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
McMillans Bridge
McMillans Bridge, is a riveted wrought iron open web truss bridge, located over the Woady Yaloak River on the Rokewood-Skipton Road between Rokewood and Werneth, Victoria, Werneth on a historical route between Geelong and the 1850s goldfields at Ararat and Streatham. McMillans Bridge was originally constructed in 1856 with stone abutments and timber truss, by the Victorian Central Road Board to a design of Charles Rowland, a student of prominent colonial engineer David Lennox. In 1888-9 the timber span was replaced with a riveted wrought iron truss designed be Charles Anthony Corbett Wilson by for the Shires of Shire of Leigh, Leigh and Shire of Grenville, Grenville. Wilson was a particularly prolific Victorian shire engineer who was influenced in this and Pitfield Bridge by the lightweight and efficient metal truss designs of Professor W. C. Kernot of Melbourne University.Alsop, P. F. B, 1999, A History of McMillans Bridge over Mt Misery Creek on the Rokewood-Skipton Road in th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hamilton Highway
Hamilton Highway is a rural highway in western Victoria, Australia, linking Geelong and the town of Hamilton, through the localities of Inverleigh, Cressy, Lismore, Derrinallum, Darlington, Mortlake, and Penshurst. Glenelg Highway links Hamilton across the South Australian border to Mount Gambier, making Hamilton Highway a popular alternative Melbourne-Mount Gambier route (being roughly 50 km shorter than a corresponding journey via the Victorian coast along Highway 1). History The passing of the ''Highways and Vehicles Act of 1924'' through the Parliament of Victoria provided for the declaration of State Highways, roads two-thirds financed by the State government through the Country Roads Board (later VicRoads). The Hamilton Highway was declared a State Highway in the 1959/60 financial year, from Geelong via Cressy and Mortlake to Hamilton (for a total of 143 miles); before this declaration, this road was referred to as the Geelong-Hamilton Road. The Geelong end of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glenelg Highway
Glenelg Highway is a rural highway in south-eastern Australia, linking Mount Gambier with Ballarat. Most of the highway is located within the Western part of the state of Victoria, though a short, 15 km stretch from the South Australia/Victoria state border near Ardno to Glenburnie (6 km east of central Mount Gambier) is located in South Australia. Some maps identify the South Australian stretch as Casterton Road. Major towns along its route include Casterton, Coleraine and Hamilton. History The passing of the ''Highways and Vehicles Act of 1924'' through the Parliament of Victoria provided for the declaration of State Highways, roads two-thirds financed by the State government through the Country Roads Board (later VicRoads). The Glenelg Highway was declared a State Highway in the 1947/48 financial year, from Ballarat via Skipton, and Hamilton to Casterton (for a total of 149 miles); before this declaration, the roads were referred to as Hamilton-Coleraine-Casterton ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Watercourse
A stream is a continuous body of surface water flowing within the bed and banks of a channel. Depending on its location or certain characteristics, a stream may be referred to by a variety of local or regional names. Long large streams are usually called rivers, while smaller, less voluminous and more intermittent streams are known as streamlets, brooks or creeks. The flow of a stream is controlled by three inputs – surface runoff (from precipitation or meltwater), daylighted subterranean water, and surfaced groundwater (spring water). The surface and subterranean water are highly variable between periods of rainfall. Groundwater, on the other hand, has a relatively constant input and is controlled more by long-term patterns of precipitation. The stream encompasses surface, subsurface and groundwater fluxes that respond to geological, geomorphological, hydrological and biotic controls. Streams are important as conduits in the water cycle, instruments in groundwater ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Meander
A meander is one of a series of regular sinuous curves in the channel of a river or other watercourse. It is produced as a watercourse erodes the sediments of an outer, concave bank ( cut bank) and deposits sediments on an inner, convex bank which is typically a point bar. The result of this coupled erosion and sedimentation is the formation of a sinuous course as the channel migrates back and forth across the axis of a floodplain. The zone within which a meandering stream periodically shifts its channel is known as a meander belt. It typically ranges from 15 to 18 times the width of the channel. Over time, meanders migrate downstream, sometimes in such a short time as to create civil engineering challenges for local municipalities attempting to maintain stable roads and bridges.Neuendorf, K.K.E., J.P. Mehl Jr., and J.A. Jackson, J.A., eds. (2005) ''Glossary of Geology'' (5th ed.). Alexandria, Virginia, American Geological Institute. 779 pp. Charlton, R., 2007. ''Fundamentals ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mouth (river)
A river mouth is where a river flows into a larger body of water, such as another river, a lake/reservoir, a bay/gulf, a sea, or an ocean. At the river mouth, sediments are often deposited due to the slowing of the current reducing the carrying capacity of the water. The water from a river can enter the receiving body in a variety of different ways. The motion of a river is influenced by the relative density of the river compared to the receiving water, the rotation of the earth, and any ambient motion in the receiving water, such as tides or seiches. If the river water has a higher density than the surface of the receiving water, the river water will plunge below the surface. The river water will then either form an underflow or an interflow within the lake. However, if the river water is lighter than the receiving water, as is typically the case when fresh river water flows into the sea, the river water will float along the surface of the receiving water as an overflow. Alon ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Corangamite
Lake Corangamite , a hypersaline endorheic lake, is located near Colac in the Lakes and Craters region of the Victorian Volcanic Plains of south-west Victoria, Australia. The lake's salinity levels have increased dramatically as the lake level has dropped in recent decades. It is Australia's largest permanent saline lake, covering approximately with a circumference of . It forms part of the Ramsar-listed Western District Lakes wetland site. The indigenous name of the lake is recorded as ''Kronimite''. Physical features and hydrology The waterbody is surrounded to the south and east by rocky outcrops (known locally as the ''stony rises'') which were formed by lava flows from Mount Porndon to the south-west and Mount Warrion to the east. The Red Rock volcanic complex overlooks the south east shore at Alvie. The Mount Warrion flows caused the lake to form by blocking drainage to the east. As is typical of lakes in the area, the eastern flanks of the lake consist of lunettes for ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wathawurrung Language
Wadawurrung, also rendered as Wathawurrung, Wathaurong or Wada wurrung, and formerly sometimes Barrabool, is the Aboriginal Australian language spoken by the Wathaurong people of the Kulin Nation of Central Victoria. It was spoken by 15 clans south of the Werribee River and the Bellarine Peninsula to Streatham. Glottolog classifies Wathawurrung as extinct, however various regional programs and initiatives promote the usage and revitalisation of Wathaurong language Phonology Blake reconstructs Wadawurrung consonants as such; Due to the varied nature of attestations of the language, Blake reconstructs Wadawurrung consonants in complacence to the standard features of the Australian Languages. It is presumed that Wadawurrung did not distinguish between voiced and unvoiced consonants ('Parrwong ~ Barwon' - Magpie). What Blake attributes as a distinction between 'alveolar' and 'laminal' consonants is better described as a distinction between dental and post-alveolar pronunciation ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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