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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 ...
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 ]
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 ]
Danbulla National Park and Danbulla State Forest are on the central part of the Atherton Tableland.The Danbulla forest is a spectacular part of the Atherton Tableland. covering 12.000ha between the Tinaroo and Lamb ranges. and bordering Lake Tinaroo. It includes eucalypt and acacia forests. pine plantations and Wet Tropics World Heritage ...
The Barron River forms most of the western boundary of the locality flowing into Lake Tinaroo (created by the Tinaroo Dam) which then forms the northern boundary of the locality. Peterson Creek, also flowing into Lake Tinaroo, forms the north-east boundary of the locality, while Gwynne Creek forms the south-western boundary of the locality ...
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.
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 ...
The method consists of filling the flow area with stream and equipotential lines, which are everywhere perpendicular to each other, making a curvilinear grid.Typically there are two surfaces (boundaries) which are at constant values of potential or hydraulic head (upstream and downstream ends), and the other surfaces are no-flow boundaries (i.e., impermeable; for example the bottom of the dam ...