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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 on the Rokewood-Skipton Road between Rokewood and Werneth. Etymology In the Aboriginal Australian Wathawurrung language Wadawurrung, also rendered as Wathawurrung, Wathaurong or Wada wurrung, and formerly sometimes Barrabool, is the Aboriginal Australian language spoken by the Wadawurrung people of the Kulin Nation, Kulin Nation of Central Victoria (Australia), ... dif ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Government Of Victoria (Australia)
The Victoria State Government, also referred to as the Victorian Government, is the executive government of the Australian state of Victoria. As a parliamentary constitutional monarchy, the State Government was first formed in 1851 when Victoria first gained responsible government. The Constitution of Australia regulates the relationship between the Victorian Government and the Commonwealth level of 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 reality, both the governor and the Executive Council are largely ceremonial, with the premier and ministers having c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Perennial River
A stream is a continuous body of water, body of surface water Current (stream), flowing within the stream bed, bed and bank (geography), banks of a channel (geography), 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 river, intermittent streams are known, amongst others, as brook, creek, rivulet, rill, run, tributary, feeder, freshet, narrow river, and streamlet. The flow of a stream is controlled by three inputs – surface runoff (from precipitation or meltwater), daylighting (streams), daylighted subterranean river, subterranean water, and surfaced groundwater (Spring (hydrology), 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 pr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rivers Of Barwon South West (region)
A river is a natural stream of fresh water that flows on land or inside caves towards another body of water at a lower elevation, such as an ocean, lake, or another river. A river may run dry before reaching the end of its course if it runs out of water, or only flow during certain seasons. Rivers are regulated by the water cycle, the processes by which water moves around the Earth. Water first enters rivers through precipitation, whether from rainfall, the runoff of water down a slope, the melting of glaciers or snow, or seepage from aquifers beneath the surface of the Earth. Rivers flow in channeled watercourses and merge in confluences to form drainage basins, or catchments, areas where surface water eventually flows to a common outlet. Rivers have a great effect on the landscape around them. They may regularly overflow their banks and flood the surrounding area, spreading nutrients to the surrounding area. Sediment or alluvium carried by rivers shapes the landscape aro ... [...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 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 Leigh and 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 the Shires of Leigh and Grenville Victoria The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hamilton Highway
Hamilton Highway is a rural highway through the Barwon South West region of Victoria, Australia, linking Geelong and the town of Hamilton. Route Hamilton Highway commences at the intersection of Latrobe Terrace and Portarlington Road in Geelong and heads in a westerly direction as a two-lane, single carriageway through Fyansford, crossing the Barwon River and an interchange with Geelong Ring Road, before leaving the Geelong suburbs and continuing west as a rural highway through the localities of Inverleigh, Cressy, Lismore, Mortlake, and Penshurst to eventually terminate at the intersection with Glenelg Highway at the eastern edge of Hamilton. Glenelg Highway continues west across the border with South Australia 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 ''Country Roads Act of 1912'' throu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glenelg Highway
Glenelg Highway is a rural highway in south-eastern Australia, linking the major regional centres of Mount Gambier in south-eastern South Australia with Ballarat in western Victoria. Route Glenelg Highway commences at the intersection with Princes Highway in Glenburnie, South Australia and heads on a north-easterly direction as a two-lane, single carriageway rural highway, crossing the interstate border into Victoria 15km later (some maps identify the South Australian section as Casterton Road), continuing northeast to Casterton, then heading in an easterly direction through the towns of Hamilton, Dunkeld and Skipton, before eventually terminating at the intersection with Midland Highway in the south-eastern suburb of Sebastopol in Ballarat. History The passing of the ''Country Roads Act of 1912'' through the Parliament of Victoria provided for the establishment of the Country Roads Board (later VicRoads) and their ability to declare Main Roads, taking responsibility for t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Watercourse
A stream is a continuous body of water, body of surface water Current (stream), flowing within the stream bed, bed and bank (geography), banks of a channel (geography), 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 river, intermittent streams are known, amongst others, as brook, creek, rivulet, rill, run, tributary, feeder, freshet, narrow river, and streamlet. The flow of a stream is controlled by three inputs – surface runoff (from precipitation or meltwater), daylighting (streams), daylighted subterranean river, subterranean water, and surfaced groundwater (Spring (hydrology), 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 pr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Meander
A meander is one of a series of regular sinuous curves in the Channel (geography), channel of a river or other watercourse. It is produced as a watercourse erosion, erodes the sediments of an outer, concave bank (cut bank, cut bank or river cliff) 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 I ... [...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. Along ... [...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 Aboriginal 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 ... [...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 Wadawurrung people of the Kulin Nation, Kulin Nation of Central Victoria (Australia), Victoria. It was spoken by 15 clans south of the Werribee River and the Bellarine Peninsula to Streatham, Victoria, Streatham. Various regional programs and initiatives promote the usage and revitalisation of Wadawurrung language. Phonology Consonants 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 Australian Aboriginal languages, the Australian Languages. It is presumed that Wadawurrung did not distinguish between voiced and unvoiced consonants ('Parrwong ~ Barwon' - Australian magpie, Magpie). What Blake attributes as a distinction between 'alveolar' and 'laminal' consonants is better des ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
