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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.
It is bounded to the west by Lake Tinaroo, to the north by Tinaroo Range, to the north-east and east by Lamb Range, to the south-east by Main Range, and to the south-west by Surprise Creek, a tributary of Lake Tinaroo. [3] It is within the world-heritage-listed Wet Tropics of Queensland. [4] Danbulla has the following mountains, from north to ...
It has very deep, rich basaltic soils and the main industry is agriculture. 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. [2]
This can be seen in Figure 6 by the decrease in depth from y 1,q=30 to y 1,q=10 and the increase in depth between y 2,q=30 and y 2,q=10. From this analysis of the change in depth due to a change in flow rate, we can also imagine that the energy lost in a jump with a value of q = 10 ft 2 /s would be different from that of a jump with q = 30 ft 2 ...
Gardiner Dam [6] Canada: 1967 65.4 64 9.4 186 TE 8 Oroville Dam United States: 1968 59.6 230 4.36 819 TE/ER 9 San Luis Dam (BF Sisk Dam) United States: 1967 59.6 93 2.52 424 TE 10 Nurek Dam Tajikistan: 1980 54 300 10.5 3,200 TE 11 Samara Dam Russia: 1955 54 [4] 52 57.3 2,315 TE or ER 12 Garrison Dam [2] United States: 1954 50.8 64 29 583.3 TE ...
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