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Sophia River
The Sophia River, part of the Pieman River catchment, is a perennial river located in the West Coast region of Tasmania, Australia. Course and features The Sophie River rises below Sophie Peak, part of the West Coast Range within the Granite Tor Conservation Area. The river flows generally west by north and reaches its confluence with the Mackintosh River within Lake Mackintosh. The river descends over its course. Lake Mackintosh and several adjoining reservoirs form part of the Pieman River Power Development scheme and some of the flow of the Sophie River supplies the Mackintosh Power Station for the generation of hydroelectricity Hydroelectricity, or hydroelectric power, is Electricity generation, electricity generated from hydropower (water power). Hydropower supplies one sixth of the world's electricity, almost 4500 TWh in 2020, which is more than all other Renewabl .... The Sophia Tunnel feeder from Murchison Dam has its outlet near Sophia River. The Sophia Adit, ... [...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] |
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] |
Lake Murchison
Lake Murchison is a man-made water reservoir located in the western region of Tasmania, Australia. The lake is situated within the northern part of Tasmania's West Coast Range and is fed by the Murchison River, the George Creek, the Anthony River, and discharge from the Tribute Power Station. Location and features The Murchison Dam across the Murchison River was built by the Hydro-Electric Commission in 1982. The dam created a reservoir, called Lake Murchison, with a surface area ranging from , drawn from a catchment area of . Lake Murchison forms part of the Pieman River power development that was completed in the 1980s. Upstream of Lake Murchison is the White Spur Lake and dam, Henty Lake and dam, Lake Newton and dam, Lake Plimsoll and Anthony Dam, and the Tribute Power Station. Downstream from Lake Murchison is Lake Mackintosh, Tullabardine Dam, Mackintosh Dam, Mackintosh Power Station, Lake Rosebery, Bastyan Dam, Bastyan Power Station, Lake Pieman, Reece Dam and the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hydroelectricity
Hydroelectricity, or hydroelectric power, is Electricity generation, electricity generated from hydropower (water power). Hydropower supplies one sixth of the world's electricity, almost 4500 TWh in 2020, which is more than all other Renewable energy, renewable sources combined and also more than nuclear power. Hydropower can provide large amounts of Low-carbon power, low-carbon electricity on demand, making it a key element for creating secure and clean electricity supply systems. A hydroelectric power station that has a dam and reservoir is a flexible source, since the amount of electricity produced can be increased or decreased in seconds or minutes in response to varying electricity demand. Once a hydroelectric complex is constructed, it produces no direct waste, and almost always emits considerably less greenhouse gas than fossil fuel-powered energy plants. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mackintosh Power Station
The Mackintosh Power Station is a conventional hydroelectric power station located in Western Tasmania, Australia. Technical details Part of the Pieman River scheme that comprises four hydroelectric power stations, the Mackintosh Power Station is the second station in the scheme. The power station is located aboveground at the foot of the rock-filled concrete faced Mackintosh Dam across the Mackintosh River and the Tullabardine Dam across the Tullabardine Creek that together form Lake Mackintosh. Water from the lake is fed to the power station by a -long single tunnel. The power station was commissioned in 1982 by the Hydro Electric Corporation (TAS) and the station has one Fuji Francis turbine, with a generating capacity of of electricity. The station output, estimated to be annually, is fed to TasNetworks' transmission grid via a 13.8 k V/220 kV Fuji generator transformer to the outdoor switchyard. The water discharged from Mackintosh Power Station flows into ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pieman River Power Development
Pieman River Power Development was a major 1970s and 1980s hydroelectric development of the Pieman River and its tributaries on the west coast of Tasmania. Development The ''Pieman River Power Development'' was approved by the Tasmanian government in 1971, construction began in 1974 and it was completed in 1987. page 24 The damming of the river was the subject of a struggle between conservation groups and Hydro Tasmania, similar to Lake Pedder . The struggle went relatively unnoticed on mainland Australia - and it was the proposed Franklin Dam issue that was to catch a much wider Australian audience, than the damming of the Pieman or King Rivers. The development included three power stations and five dams:- * Lake Murchison and Murchison Dam * Lake Mackintosh, Tullabardine Dam and Mackintosh Dam (Mackintosh Power Station), commissioned in 1982 * Lake Rosebery and Bastyan Dam (Bastyan Power Station), commissioned in 1983 * Lake Pieman and Reece Dam (Reece Power Station), com ... [...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] |
Confluence
In geography, a confluence (also: ''conflux'') occurs where two or more flowing bodies of water join to form a single channel. A confluence can occur in several configurations: at the point where a tributary joins a larger river (main stem); or where two streams meet to become the source of a river of a new name (such as the confluence of the Monongahela and Allegheny rivers at Pittsburgh, forming the Ohio); or where two separated channels of a river (forming a river island) rejoin at the downstream end. Scientific study of confluences Confluences are studied in a variety of sciences. Hydrology studies the characteristic flow patterns of confluences and how they give rise to patterns of erosion, bars, and scour pools. The water flows and their consequences are often studied with mathematical models. Confluences are relevant to the distribution of living organisms (i.e., ecology) as well; "the general pattern ownstream of confluencesof increasing stream flow and decreasing s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Reservoir
A reservoir (; from French ''réservoir'' ) is an enlarged lake behind a dam. Such a dam may be either artificial, built to store fresh water or it may be a natural formation. Reservoirs can be created in a number of ways, including controlling a watercourse that drains an existing body of water, interrupting a watercourse to form an embayment within it, through excavation, or building any number of retaining walls or levees. In other contexts, "reservoirs" may refer to storage spaces for various fluids; they may hold liquids or gasses, including hydrocarbons. ''Tank reservoirs'' store these in ground-level, elevated, or buried tanks. Tank reservoirs for water are also called cisterns. Most underground reservoirs are used to store liquids, principally either water or petroleum. Types Dammed valleys Dammed reservoirs are artificial lakes created and controlled by a dam A dam is a barrier that stops or restricts the flow of surface water or underground streams ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tasmania
) , nickname = , image_map = Tasmania in Australia.svg , map_caption = Location of Tasmania in AustraliaCoordinates: , subdivision_type = Country , subdivision_name = Australia , established_title = Before federation , established_date = Colony of Tasmania , established_title2 = Federation , established_date2 = 1 January 1901 , named_for = Abel Tasman , demonym = , capital = Hobart , largest_city = capital , coordinates = , admin_center = 29 local government areas , admin_center_type = Administration , leader_title1 = Monarch , leader_name1 = Charles III , leader_title2 = Governor , leader_name2 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pieman River
The Pieman River is a major perennial river located in the west coast region of Tasmania, Australia. Course and features Formed by the confluence of the Mackintosh River and Murchison River, the Pieman River rises in what is now known as Lake Rosebury, an artificial lake formed by the Bastyan Dam. The river flows generally west and northwest and then west again, joined by 21 tributaries including the Mackintosh, Murchison, Marionoak, Ring, Wilson, Stitt, Huskisson, Stanley, Heemskirk, Paradise, Owen Meredith, Savage, Whyte and Donaldson rivers before emptying into Hardwicke Bay and reaching its mouth in the Southern Ocean. The river descends over its course. The river is impounded at Bastyan by the Bastyan Dam (and adjacent hydroelectric power station to form Lake Rosebury; and at Reece by the Reece Dam (and adjacent hydroelectric power station to form Lake Pieman. Both reservoir and power stations from part of the Hydro Tasmania-operated Pieman River Powe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Mackintosh
Lake Mackintosh is a reservoir with a surface area of that forms part of the Pieman power development running north–south past Mount Farrell, adjacent to the town of Tullah in Tasmania. Features Fed by the damming of the Mackintosh, Sophia, Fury, Southwell, and Brougham rivers and Mackintosh Creek, water from the lake feeds Mackintosh Power Station through Lake Rosebery. The lake was created in the 1980s and the main basin of the lake was originally a Button Grass swamp prior to inundation. Lake Mackintosh is impounded by two dams, the main Mackintosh Dam and the smaller Tullabardine Dam. The lake's deepest point is roughly deep at the base of the main dam. It is one of the larger sized water impoundments of the Pieman power scheme. The Murchison River is feeds into Lake Mackintosh through the Murchison Dam, to the south. The Murchison Highway borders the lake to the west. The Cradle Mountain-Lake St Clair National Park as a component part of the Tasmanian Wildernes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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