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Edgar Dam

From Wikipedia, the free encyclopedia

Dam in South West Tasmania
Edgar Dam
Edgar Dam is located in Tasmania
Edgar Dam
Edgar Dam
Location of the Edgar Dam inTasmania
Map
Interactive map of Edgar Dam
CountryAustralia
LocationSouth WestTasmania
PurposePower
StatusOperational
Opening date1973 (1973)
OwnerHydro Tasmania
Dam and spillways
Type of damEmbankment dam
ImpoundsOff stream
Height17 metres (56 ft)
Length460 metres (1,510 ft)
Dam volume96×10^3 m3 (3.4×10^6 cu ft)
Spillways0
Reservoir
CreatesLake Pedder
Total capacity2,937,930 ML (103,752×10^6 cu ft)
Catchment area734 km2 (283 sq mi)
Surface area241 km2 (93 sq mi)
Maximum water depth43 m (141 ft)
Website
hydro.com.au/energy/our-power-stations/gordon-pedder

TheEdgar Dam is anearthfillembankmentsaddledam without aspillway, located offstream in theSouth West region ofTasmania, Australia.

The impoundedreservoir, also formed with theScotts Peak Dam and theSerpentine Dam, is calledLake Pedder which floodedLake Edgar, a naturally formingfault scarp pond. The dam was constructed in 1973 by theHydro Electric Corporation (TAS) as part of the Gordon River Power Development Scheme for the purpose of generatinghydro-electric power via theGordon Power Station. Water from Lake Pedder is diverted toLake Gordon (formed by theGordon Dam) via the McPartlan Pass Canal.[1]

Location and features

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The Edgar Dam, together with the Scotts Peak Dam and the Serpentine Dam, are three major dams that form the headwaters for the Gordon River Power Development Scheme. The dam is located near Lake Pedder's most easterly point[2] in the upper reaches of theHuon River where the river descends from the Marsden Range and descends into what is now known as the Huon Basin. Also at the southern end of the Lake Pedder, the Scotts Peak Dam impounds the Huon River. At the northwestern end of the lake is impounded by the Serpentine Dam across theSerpentine River. The water in Lake Pedder provides around 40% of the water used in the Gordon Power Station. The water flows to Lake Gordon via McPartlan Canal.[1] Water from Lake Gordon then exits through the Gordon Dam.

The Edgar Dam wall, constructed with 96 thousand cubic metres (3.4×10^6 cu ft) of earth core, is 17 metres (56 ft) high and 460 metres (1,510 ft) long. At 100% capacity the dam wall holds back 2,937,930 megalitres (103,752×10^6 cu ft) of water. The surface area of Lake Pedder is 241,330 hectares (596,300 acres) and the catchment area is 734 square kilometres (283 sq mi). The dam wall does not have a spillway.[3]

The dam draws its name from the flooded Lake Edgar.

Lake Edgar Fault

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The Lake Edgar Fault is a 30-kilometre (19 mi) long north–south trending scarp that occurs within the boundary of theSouthwest National Park. The scarp traverses the button grass of the Huon Plains and is notable because faulting resulted in the defeat of westerly flowing drainage and the consequent formation of the fault-bound sag pond of Lake Edgar.[4] In January 2001 a tremor measuring 3.2 on theRichter magnitude scale occurred near the Lake Edgar fault, which runs adjacent to the Edgar Dam, however damage was negligible.[5][6][7][8][9]

In 2002 it was reported that a dam safety manager from Hydro Tasmania, was confident that the eventuality of the Edgar dam being destroyed by an earthquake was an extremely remote possibility, with a University of Tasmania Geophysicist agreeing that the risk of collapse was remote.[10]

See also

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References

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  1. ^ab"Gordon - Pedder".Energy: Our power stations.Hydro Tasmania. Retrieved21 June 2015.
  2. ^"Edgar Dam camp ground".Community.Hydro Tasmania. 2015. Archived fromthe original on 1 July 2015. Retrieved29 June 2015.
  3. ^"Register of Large Dams in Australia".Dams information.Australian National Committee on Large Dams. 2012. Archived fromthe original(Excel (requires download)) on 4 March 2015. Retrieved28 June 2015.
  4. ^"Lake Edgar Earthquake"(PDF).Geoscience Australia. 22 June 2004. Retrieved28 June 2015.
  5. ^Taylor, Sam (April 2002)."Dam failure"(PDF).Reflections (9). The Lake Pedder Restoration Committee: 7. Archived fromthe original(PDF) on 26 March 2016. Retrieved28 June 2015.
  6. ^"Earthquakes".Mineral Resources Tasmania, Department of State Growth.Government of Tasmania. Retrieved29 June 2015.
  7. ^McCue, K; Boreham, B; van Dissen, R; Gibson, G; Jensen, V; McKavanagh, B (1996),A paleoseismology case study: the Lake Edgar Fault Scarp in Tasmania, Geological Society of Australia, retrieved30 October 2017
  8. ^McCue, K; Van Dissen, R; Gibson, G; Jensen, V; Boreham, B (2003),The Lake Edgar Fault: an active fault in Southwestern Tasmania, Australia, with repeated displacement in the Quaternary, Istituto Nazionale di Geofisics e Vulcanologia, retrieved30 October 2017
  9. ^Clark, D; Cupper, M; Sandiford, M; Kiernan, K (2011),Style and timing of late Quaternary faulting on the Lake Edgar fault, southwest Tasmania, Australia: Implications for hazard assessment in intracratonic areas, retrieved30 October 2017
  10. ^Taylor, Sam (April 2002)."Dam failure"(PDF).Reflections (9). The Lake Pedder Restoration Committee: 7. Archived fromthe original(PDF) on 26 March 2016. Retrieved28 June 2015.

Further reading

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  • Reid, Vern (1976)Edgar Dam B&W photo between p. 248 and p249 (not indexed) of theTasmanian Year Book No.10 1976. Australian Bureau of Statistics Tasmanian Office ISSN 0082-2116
  • Tasmania. Hydro-Electric Commission. Survey Section; Tasmania. Department of Lands and Surveys (December 1967).Gordon River power development Stage 1 (Map). Hobart:Hydro-Electric Commission.
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