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  2. Great Dividing Range - Wikipedia

    en.wikipedia.org/wiki/Great_Dividing_Range

    Great Dividing Range sign on the Kings Highway between Braidwood and Bungendore, New South Wales. The Great Dividing Range was formed during the Carboniferous period—over 300 million years ago—when Australia collided with what are now parts of South America and New Zealand. [12] The range has experienced significant erosion since.

  3. Australian Alps - Wikipedia

    en.wikipedia.org/wiki/Australian_Alps

    The range comprises an area of 1,232,981 ha (3,046,760 acres). [3] The Australian Alps are part of the Great Dividing Range, the series of mountain and hill ranges and tablelands that runs about 3,000 km (1,900 mi) from northern Queensland, through New South Wales, and into the northern part of Victoria. [4]

  4. List of mountains in Australia - Wikipedia

    en.wikipedia.org/wiki/List_of_mountains_in_Australia

    States and Territories of Australia [1] State / Territory Highest point Elevation AHD Notes m ft; ... Great Dividing Range: 1,913 6,276 [13] 2 Mount Gingera: 1,857 6,093

  5. Snowy Mountains - Wikipedia

    en.wikipedia.org/wiki/Snowy_Mountains

    The Snowy Mountains, known informally as "The Snowies", is an IBRA subregion in southern New South Wales, Australia, and is the tallest mountain range in mainland Australia, being part of the continent's Great Dividing Range cordillera system.

  6. Mount Townsend (Snowy Mountains) - Wikipedia

    en.wikipedia.org/wiki/Mount_Townsend_(Snowy...

    Mount Townsend, a mountain in the Main Range of the Great Dividing Range, is located in the Snowy Mountains region of New South Wales, Australia.. With an elevation of 2,209 metres (7,247 ft) above sea level, [1] Mount Townsend is the second-highest peak of mainland Australia.

  7. Great Escarpment, Australia - Wikipedia

    en.wikipedia.org/wiki/Great_Escarpment,_Australia

    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]