Canberra topographic map
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Canberra
The area chosen for the capital had been inhabited by Indigenous Australians for up to 21,000 years, with the principal group being the Ngunnawal people. European settlement commenced in the first half of the 19th century, as evidenced by surviving landmarks such as St John's Anglican Church and Blundells Cottage. On 1 January 1901, federation of the colonies of Australia was achieved. Following a long dispute over whether Sydney or Melbourne should be the national capital, a compromise was reached: the new capital would be built in New South Wales, so long as it was at least 100 miles (160 km) from Sydney. The capital city was founded and formally named as Canberra in 1913. A blueprint by American architects Walter Burley Griffin and Marion Mahony Griffin was selected after an international design contest, and construction commenced in 1913. Unusual among Australian cities, it is an entirely planned city. The Griffins' plan featured geometric motifs and was centred on axes aligned with significant topographical landmarks such as Black Mountain, Mount Ainslie, Capital Hill and City Hill. Canberra's mountainous location makes it the only mainland Australian city where snow-capped mountains can be seen in winter; although snow in the city itself is uncommon.
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Other topographic maps
Click on a map to view its topography, its elevation and its terrain.
Sydney
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City of Melbourne
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Victoria
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Average elevation: 587 ft
New South Wales
New South Wales (NSW), located on Australia's eastern seaboard, boasts a diverse topography that significantly influences its landscapes and ecosystems. The state's eastern edge is dominated by a narrow coastal plain, featuring regions such as the Illawarra and Shoalhaven near Nowra, characterized by rolling…
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Western Australia
Because the only mountain-building since then has been of the Stirling Range with the rifting from Antarctica, the land is extremely eroded and ancient, with no part of the state above 1,245 metres (4,085 ft) AHD (at Mount Meharry in the Hamersley Range of the Pilbara region). Most of the state is a low…
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Melbourne
Melbourne is also prone to isolated convective showers forming when a cold pool crosses the state, especially if there is considerable daytime heating. These showers are often heavy and can include hail, squalls, and significant drops in temperature, but they often pass through very quickly with a rapid…
Average elevation: 607 ft
Queensland
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Tasmania
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Average elevation: 722 ft
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Average elevation: 384 ft
Melbourne
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Average elevation: 607 ft
Cape York Peninsula
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Orange
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Lord Howe Island
Australia > New South Wales > Unincorporated New South Wales > Lord Howe Island
Average elevation: 89 ft
Mount Coot-tha
Australia > Queensland > City of Brisbane
It is often claimed that Mount Coot-tha is the "highest point in Brisbane", but, as the elevations above show, the peak known as Mount Coot-tha is not even the highest peak of the mountain as a whole with both Constitution Hill and The Summit being higher. However, Mount Coot-tha has a lookout with unobscured…
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Penrith
Australia > New South Wales > Sydney > Penrith
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New South Wales
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Camberwell
Australia > Victoria > Melbourne
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Average elevation: 217 ft
Queensland
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Average elevation: 400 ft
Ellenbrook
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Frankston
Australia > Victoria > Melbourne
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Goulburn
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Adaminaby
Another site 20 km to the north (Yaouk, since 1969) records significantly greater rainfall due to its higher elevation and proximity to the dividing range. This site is most representative of the areas situated on and around Lake Eucumbene. Rainfall total and pattern here approach those of Khancoban and very…
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Castlereagh River
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Blue Mountains
A sandstone plateau dominated by a landscape of endless eucalyptus forests, the Blue Mountains are located at the top of a 470-million-year-old quartzite. In the Permian period, a shallow sea covered the region, when rivers brought shales, siltstones and mudstones. Then during the Mesozoic period, rivers…
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Sunshine Coast Regional
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Launceston
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