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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 mi (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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About this map
Name: Canberra topographic map, elevation, terrain.
Average elevation: 638 m
Minimum elevation: 395 m
Maximum elevation: 1,238 m
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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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Queensland
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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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New South Wales
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Average elevation: 220 m
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Melbourne
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Great Dividing Range
The Great Dividing Range, also known as the East Australian Cordillera or the Eastern Highlands, is a cordillera system in eastern Australia consisting of an expansive collection of mountain ranges, plateaus and rolling hills, that runs roughly parallel to the east coast of Australia and forms the…
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Mount Buller
Due to its far south-western location in the alpine region, Mount Buller is more susceptible to cold airmasses which allow it to record some of the lowest maximum temperatures and daytime readings in the country, despite being considerably lower in elevation than other mountain sites to the north-east. On 5…
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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…
Average elevation: 88 m
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Australia > New South Wales > Unincorporated New South Wales > Lord Howe Island
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Inman Valley
Australia > South Australia > The District Council of Yankalilla
In the valley is Selwyn Rock (35°29′47″S 138°30′45″E / 35.4965°S 138.5124°E / -35.4965; 138.5124) a glaciated pavement in the bed of the Inman River. It was first described in 1859 by, and later named for, A.R.C. Selwyn,[17] who was Victorian Government geologist at the time. Glacial…
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Tasmania
The most mountainous region is the Central Highlands area, which covers most of the central western parts of the state. The Midlands located in the central east, is fairly flat, and is predominantly used for agriculture, although farming activity is scattered throughout the state. Tasmania's tallest mountain…
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Penrith
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Hobart
Although Hobart itself rarely receives snow during the winter due to the foehn effect created by the Central Highlands (the city's geographic position causes a rainshadow), the adjacent Kunanyi/Mount Wellington is frequently seen with a snowcap throughout the year including in summer. During the 20th century,…
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Bruny Island
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