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The maximum water depth is 41.8 metres (137 ft) and at 100% capacity the dam wall impounds enough water from the Barron River to create a lake approximately 75% the size of Sydney Harbour with a capacity of 438,919 megalitres (15,500.3 × 10 ^ 6 cu ft) of water at 670 metres (2,200 ft) AHD. The surface area of the Lake Tinaroo is 3,500 hectares ...
Lake Tinaroo is a rural locality in the Tablelands Region of Queensland, Australia. [2] In the 2021 census , Lake Tinaroo had "no people or a very low population". [ 1 ]
The Tinaroo Hydro Power Station is an electricity power station in Tinaroo, Tablelands Region, Queensland, Australia. It is located at the spillway of Tinaroo Dam. It has been designed to take advantage of water being released for irrigation, and water released when the dam is full. [1] It was opened in 2004. [2]
Tinaroo is located on the shore of Lake Tinaroo, a man-made reservoir created by the impoundment of the Barron River by the Tinaroo Dam. [4]Despite the town's name, the waterfall of the same name is not in the town nor the locality, but it is very close by in the neighbouring locality of Lake Tinaroo, which includes the dam wall, the lake it impounds and the shoreline around the lake.
The principal river flowing across the plateau is the Barron River, which was dammed to form the irrigation reservoir named Lake Tinaroo. Unlike many other rural areas, the Tablelands is experiencing a significant growth in population.
Burdekin Falls Dam [7] Bjelke-Petersen Dam [7] Kinchant Dam [8] Wuruma Dam [7] SunWater constructed, and owns and operates the Tinaroo Hydro Power Station, a mini–hydroelectric power station at Lake Tinaroo; [7] and the Paradise Mini-Hydro, a mini–hydroelectric power station at Paradise Dam, impacted by flooding near Bundaberg in 2010.
The largest of the natural volcanic lakes in the area, Lake Barrine is 730 m above sea level. It is about 1 km in diameter, with a shoreline of almost 4.5 km, an average depth of 35 m and a maximum depth of 65 m. [4] No streams or springs feed the crystal clear lake; it is filled only by rainwater.
To develop the M-y Diagram, we plot the value of M as a function of depth with M on the x-axis and depth on the y-axis since this is more naturally conducive to visualizing the change in momentum with depth. This example is a very basic hydraulic jump situation where the flow approaches at a supercritical depth, y 1, and jumps to its ...
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