Scotts Peak Dam | |
---|---|
Location of the Edgar Dam in Tasmania | |
Country | Australia |
Location | South West Tasmania |
Coordinates | 43°01′52″S146°17′46″E / 43.03111°S 146.29611°E |
Purpose | Power |
Status | Operational |
Opening date | 1973 |
Owner(s) | Hydro Tasmania |
Dam and spillways | |
Type of dam | Embankment dam |
Impounds | Huon River |
Height | 43 metres (141 ft) |
Length | 1,067 metres (3,501 ft) |
Dam volume | 584×10 3 m3 (20.6×10 6 cu ft) |
Spillways | 0 |
Reservoir | |
Creates | Lake Pedder |
Total capacity | 2,937,930 ML (103,752×10 6 cu ft) |
Catchment area | 734 km2 (283 sq mi) |
Surface area | 242 km2 (93 sq mi) |
Maximum water depth | 43 m (141 ft) |
Website hydro | |
[1] |
The Scotts Peak Dam is a rockfill embankment dam without a spillway across the Huon River, located in the South West region of Tasmania, Australia.
The impounded reservoir, also formed with the Edgar Dam and the Serpentine Dam, is called Lake Pedder which flooded Lake Edgar, a naturally forming fault scarp pond. The dam was constructed in 1973 by the Hydro Electric Corporation (TAS) as part of the Gordon River Power Development Scheme for the purpose of generating hydro-electric power via the conventional Gordon Power Station. Water from Lake Pedder is diverted to Lake Gordon (formed by the Gordon Dam) via the McPartlan Pass Canal. [2] [3] [4]
The Scotts Peak Dam, together with the Edgar 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 [5] in the upper reaches of the Huon 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 upper reaches of the Huon River. At the northwestern end of the lake is impounded by the Serpentine Dam across the Serpentine 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. [2] Water from Lake Gordon then exits through the Gordon Dam.
Built on a foundation of rock and soil, the Scotts Peak Dam wall was constructed with 584 thousand cubic metres (20.6×10 6 cu ft) of rockfill and faced with asphalt. The dam wall is 43 metres (141 ft) high and 1,067 metres (3,501 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. [1]
This non-hydroelectric dam helps retain water in the new impoundment, which then flows to Lake Gordon via the McPartlans Pass Canal at 42°50′51″S146°11′45″E / 42.84750°S 146.19583°E . In 2001 the dam was recorded as an Historic Engineering Marker along with twenty-four other dams by Engineers Australia. [3]
The construction of Scotts Peak Dam was controversial as it was built to flood Lake Pedder and extend the reservoir for the Gordon Dam. A small greens movement was formed it response, which mobilised in the 1980s to stop the proposed Franklin River Dam. [6]
In the 2008 edition of Ticklebelly Tales engineers associated with the dam acknowledge that there were issues leaks as soon as it was built. [7] [8] [9] Evidence of deformation is still current in the 2010s.
Due to its far southwestern location, this site is frequently lashed by severe weather; with a mean annual wind speed of 27.1 kilometres per hour (16.8 mph), peaking at a mean of 32.9 kilometres per hour (20.4 mph) in September. Cloud cover is likewise extreme, with precipitation falling on 269 days of the year and over 25 days in each winter month. Snow is a common occurrence throughout the year and can even occur in the summer.
Climate data for Scotts Peak Dam (1998–2023); 408 m AMSL; 43.04° S, 146.27° E | |||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Month | Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec | Year |
Record high °C (°F) | 38.6 (101.5) | 35.9 (96.6) | 37.5 (99.5) | 29.1 (84.4) | 22.0 (71.6) | 15.7 (60.3) | 17.1 (62.8) | 22.5 (72.5) | 25.2 (77.4) | 30.6 (87.1) | 34.8 (94.6) | 37.9 (100.2) | 38.6 (101.5) |
Mean daily maximum °C (°F) | 21.4 (70.5) | 21.1 (70.0) | 18.5 (65.3) | 14.9 (58.8) | 11.6 (52.9) | 9.8 (49.6) | 9.3 (48.7) | 10.4 (50.7) | 12.5 (54.5) | 14.9 (58.8) | 17.8 (64.0) | 19.1 (66.4) | 15.1 (59.2) |
Mean daily minimum °C (°F) | 9.5 (49.1) | 9.4 (48.9) | 8.5 (47.3) | 6.9 (44.4) | 5.5 (41.9) | 4.1 (39.4) | 3.3 (37.9) | 3.4 (38.1) | 4.4 (39.9) | 5.2 (41.4) | 6.9 (44.4) | 8.1 (46.6) | 6.3 (43.3) |
Record low °C (°F) | 2.6 (36.7) | 3.3 (37.9) | 1.3 (34.3) | −0.4 (31.3) | −1.1 (30.0) | −1 (30) | −2.3 (27.9) | −2.1 (28.2) | −1.6 (29.1) | −1 (30) | −0.5 (31.1) | 1.5 (34.7) | −2.3 (27.9) |
Average precipitation mm (inches) | 92.8 (3.65) | 82.8 (3.26) | 122.1 (4.81) | 131.4 (5.17) | 193.2 (7.61) | 183.0 (7.20) | 214.2 (8.43) | 227.0 (8.94) | 205.6 (8.09) | 161.9 (6.37) | 114.4 (4.50) | 141.5 (5.57) | 1,869.9 (73.62) |
Average precipitation days (≥ 0.2 mm) | 17.3 | 16.0 | 19.5 | 21.9 | 26.0 | 25.9 | 27.2 | 26.5 | 25.2 | 23.9 | 19.8 | 20.0 | 269.2 |
Average afternoon relative humidity (%) | 58 | 59 | 66 | 74 | 82 | 86 | 85 | 81 | 76 | 69 | 62 | 63 | 72 |
Source: [10] |
Lake Pedder, once a glacial outwash lake, is a man-made impoundment and diversion lake located in the southwest of Tasmania, Australia. In addition to its natural catchment from the Frankland Range, the lake is formed by the 1972 damming of the Serpentine and Huon rivers by the Hydro-Electric Commission for the purpose of hydroelectric power generation. Consequently, the lake is also known, somewhat derisively, as the Huon-Serpentine Impoundment.
Lake Gordon is a man-made reservoir created by the Gordon Dam, located on the upper reaches of the Gordon River in the south-west region of Tasmania, Australia.
The Gordon River is a major perennial river located in the central highlands, south-west, and western regions of Tasmania, Australia.
Hydro Tasmania, known for most of its history as the Hydro-Electric Commission (HEC) or The Hydro, is the trading name of the Hydro-Electric Corporation, a Tasmanian Government business enterprise which is the predominant electricity generator in the state of Tasmania, Australia. The Hydro was originally oriented towards hydro-electricity, due to Tasmania's dramatic topography and relatively high rainfall in the central and western parts of the state. Today Hydro Tasmania operates thirty hydro-electric and one gas power station, and is a joint owner in three wind farms.
The Huon River is a perennial river located in the south-west and south-east regions of Tasmania, Australia. At 174 kilometres (108 mi) in length, the Huon River is the fifth-longest in the state, with its course flowing east through the fertile Huon Valley and emptying into the D'Entrecasteaux Channel, before flowing into the Tasman Sea.
The Crotty Dam, also known during construction as the King Dam, or the King River Dam on initial approval, is a rockfill embankment dam with a controlled and uncontrolled spillway across the King River, between Mount Jukes and Mount Huxley, located in Western Tasmania, Australia.
Jindabyne Dam is a major ungated rockfill embankment dam across the Snowy River in the Snowy Mountains of New South Wales, Australia. The dam's main purpose is to redirect water from the Snowy River to the Murray, for the generation of hydro-power and irrigation. It is one of the sixteen major dams that comprise the Snowy Mountains Scheme, a vast hydroelectricity and irrigation complex constructed in south-east Australia between 1949 and 1974 and now run by Snowy Hydro.
The Darwin Dam is an offstream earthfill embankment saddle dam without a spillway, located in Western Tasmania, Australia. The impounded reservoir, also formed by Crotty Dam, is called Lake Burbury.
The Gordon Power Station is the largest conventional hydroelectric power station in Tasmania, Australia; located in the South West region of the state. The power station is situated on Gordon River. Water from Lake Gordon descends 183 metres (600 ft) underground past the Gordon Dam and into the power station.
The Gordon River Road, sometimes called the Strathgordon Road, (B61), is a road in the south western region of Tasmania, Australia.
The Gordon Dam, also known as the Gordon River Dam, is a major gated double curvature concrete arch dam with a controlled spillway across the Gordon River, located in Southwest National Park, Tasmania, Australia. The impounded reservoir is called Lake Gordon.
The Serpentine River is a major perennial river located in the south-west and western regions of Tasmania, Australia.
The Scotts Peak Dam Road is the most southerly point of road access into Southwest National Park, Tasmania, Australia.
The Serpentine Dam is a rockfill embankment dam with a concrete face and a controlled spillway across the Serpentine River, located in the South West region of Tasmania, Australia.
The Edgar Dam is an earthfill embankment saddle dam without a spillway, located offstream in the South West region of Tasmania, Australia.
The Anthony Power Development Scheme, part of the Pieman River power development scheme, was a proposed scheme for damming parts of the upper catchment of the Pieman River in Western Tasmania, Australia.
Lake Edgar was a natural fault scarp pond on the upper reaches of the Huon River in South West Tasmania.
The Frankland Range is a mountain range that is located in the south-west region of Tasmania, Australia. The range forms part of a natural south-western border to the impounded Lake Pedder, formed by the damming of the Serpentine and Huon rivers.
This page discusses the rivers and hydrography of the state of Tasmania, Australia.
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.