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The Great Dividing Range creates the drainage basins of the Australian south-east coast drainage division and the Australian north-east coast drainage division, whose water flows to the east coast and into the Pacific Ocean, Tasman Sea, and Bass Strait with the westerly Murray–Darling basin which flow inland, away from the coast into the ...
The Great Escarpment in eastern Australia is an escarpment that runs east of the Great Dividing Range along most of the east of the continent. It was created due to formation of a new continental margin in the Mesozoic, followed by tectonic uplifting of the divide and then scarp retreat. [2]
Aspects of traditional Aboriginal land use and culture have been documented from the period of first contact [8] to present. [9] Aboriginal people with ties to the region seek to maintain their culture today, [10] despite a long period of forced removal from their lands following European occupation in the late 19th-early 20th century. [11] [12]
This area is a distinct physiographic section of the larger Western Victorian Highlands province, which, in turn, is part of the larger East Australian Cordillera physiographic division — commonly known as the Great Dividing Range — a series of mountain ranges, plateaus and rolling hills forming out of the Wimmera plains just to the west of the Grampians, staying close to the east ...
Cordillera Central of Luzon and Southern Pacific Cordillera of Mindanao in the Philippines; Cordilleras Béticas, Central and Cantábrica (including the Picos de Europa) in Spain; East Australian Cordillera, more commonly known as the Great Dividing Range, the most significant topographic feature of the east coast of Australia
The Victorian Alps, also known locally as the High Country, is a large mountain system in the southeastern Australian state of Victoria.Occupying the majority of eastern Victoria, it is the southwestern half of the Australian Alps (the other half being the Snowy Mountains), the tallest portion of the Great Dividing Range.
The geologic history of the Australian continental mass is extremely prolonged and involved, continuing from the Archaean to the recent. In a gross pattern, continental Australia grew from west to east, with Archean rocks mostly in the west, Proterozoic rocks in the centre, and Phanerozoic rocks in the east.
The eastern Australian states. States in red are always defined as eastern. The term can sometimes be applied to the states in orange. The eastern states of Australia are the states adjoining the east continental coastline of Australia. These are the mainland states of Victoria, New South Wales and Queensland, and the island state of Tasmania.