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The Brisbane River (Turrbal: Maiwar) is the longest river in South East Queensland, Australia, and flows through the city of Brisbane, before emptying into Moreton Bay on the Coral Sea. John Oxley , the first European to explore the river, named it after the Governor of New South Wales , Sir Thomas Brisbane in 1823.
A drainage basin is an extent of land where water from rain and melting snow or ice drains downhill into a body of water, such as a river, lake, reservoir, estuary, wetland, sea or ocean. The drainage basin includes both the streams and rivers that convey the water as well as the land surfaces from which water drains into those channels, and is ...
The Great Artesian Basin (GAB) [1] of Australia is the largest and deepest artesian basin in the world, extending over 1,700,000 square kilometres (660,000 sq mi). Measured water temperatures range from 30 to 100 °C (86 to 212 °F). The basin provides the only source of fresh water through much of inland Australia. [2]
However, the river frontages have become gentrified in the last 30 years, with wharf facilities and industrial buildings replaced by parklands, residential apartments and the arts precinct. [4] The Brisbane River is a wide tidal estuary and its waters throughout most of the metropolitan area are brackish and navigable.
Between the Eastern Highlands and the Western Plateau lies the Central Lowlands, which are made up of the Great Artesian Basin and Australia's largest river systems, the Murray-Darling Basin and the Lake Eyre Basin. Off the north-eastern coast of Australia is the world's largest coral reef complex, the Great Barrier Reef.
The range drains into both the Bremer River Basin (sub-basin of Brisbane River Basin) and via Teviot Brook into the Logan River Basin (sub-basin of Logan-Albert River Basin). Teviot Brook is a major tributary of the Logan River that also supplies water to Wyaralong Dam. [17] [18] [19]
A subbasin or sub-basin is a structural geologic feature where a larger basin is divided into a series of smaller basins with intervening intrabasinal highs.
The oceans drain approximately 83% of the land in the world. The other 17% – an area larger than the basin of the Arctic Ocean – drains to internal endorheic basins. There are also substantial areas of the world that do not "drain" in the commonly understood sense.
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