Lake Amadeus topographic map

Sydney's topography is characterized by a diverse landscape that seamlessly blends coastal features with inland plateaus. The city is divided into two primary regions: the relatively flat Cumberland Plain to the south and west of Sydney Harbour, and the elevated Hornsby Plateau to the north. The Cumberland…

Average elevation: 53 m

Victoria, Australia, exhibits a remarkably varied topography shaped by the Great Dividing Range, which forms a west-to-east spine across the state. In the northeast, the Victorian Alps rise to the state’s highest point, Mount Bogong at 1,986 meters, amid deep valleys and snow-capped ridges, while westward,…

Average elevation: 179 m

Melbourne's topography is characterized by a diverse landscape that transitions from flat coastal plains to rolling hills and mountainous regions. The city is situated at the northern end of Port Phillip Bay, where the terrain is predominantly flat, facilitating urban development. As one moves eastward, the…

Average elevation: 18 m

Average elevation: 45 m

Perth, the capital of Western Australia, is situated on the Swan Coastal Plain, a flat expanse of sandy soil nestled between the Indian Ocean to the west and the Darling Scarp to the east. The Darling Scarp, also known as the Darling Range, is a low escarpment that extends north–south, marking a distinct…

Average elevation: 26 m

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…

Average elevation: 638 m

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…

Average elevation: 154 m

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…

Average elevation: 220 m

Ballarat has a moderate oceanic climate (Köppen climate classification Cfb) with four distinct seasons. Its elevation, ranging between 400 and 630 metres (1,310 and 2,070 feet) above sea level, causes its mean monthly temperatures to tend to be on average 3 to 5 °C (5 to 9 °F) below those of Melbourne,…

Average elevation: 470 m

Queensland's topography is characterized by a diverse landscape that includes coastal plains, mountain ranges, plateaus, and expansive inland areas. The Great Dividing Range runs parallel to the state's eastern coast, forming a series of mountain ranges, plateaus, and upland areas. This range influences the…

Average elevation: 122 m

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…

Average elevation: 154 m

Adelaide is north of the Fleurieu Peninsula, on the Adelaide Plains between the Gulf St Vincent and the low-lying Mount Lofty Ranges. The city stretches 20 km (12 mi) from the coast to the foothills, and 90 km (56 mi) from Gawler at its northern extent to Sellicks Beach in the south. According to the Regional…

Average elevation: 148 m

Average elevation: 110 m

Average elevation: 46 m

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: 185 m

Average elevation: 23 m

Average elevation: 42 m

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…

Average elevation: 194 m

Average elevation: 5 m

Brisbane's topography is characterized by a series of hills and ranges that define its landscape. The city is situated on a low-lying floodplain, with the Brisbane River meandering through its heart, creating a winding course with many steep curves from the southwest to its mouth at Moreton Bay in the east.…

Average elevation: 71 m

Victoria, Australia, exhibits a remarkably varied topography shaped by the Great Dividing Range, which forms a west-to-east spine across the state. In the northeast, the Victorian Alps rise to the state’s highest point, Mount Bogong at 1,986 meters, amid deep valleys and snow-capped ridges, while westward,…

Average elevation: 179 m

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…

Average elevation: 638 m

Average elevation: 2 m

Average elevation: 31 m

Orange is a city in the Central Tablelands region of New South Wales, Australia. It is 254 km (158 mi) west of the state capital, Sydney [206 km (128 mi) on a great circle], at an altitude of 862 metres (2,828 ft). Orange had an estimated urban population of 40,493 as of June 2018 making the city a significant…

Average elevation: 852 m

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: 185 m

Mount Dandenong has a cool oceanic climate (Cfb), with cool to mild summers and cold, damp winters. Daytime temperatures are usually 4−6 °C cooler than downtown Melbourne due to its elevation and distance from the urban heat island effect of Melbourne. It is significantly cloudier than Melbourne,…

Average elevation: 395 m

Average elevation: 690 m

Average elevation: 318 m

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: 49 m

Average elevation: 23 m

Average elevation: 525 m

Average elevation: 580 m

Average elevation: 115 m

Average elevation: 18 m

Phillip had been given no instructions for urban development, but in July 1788 submitted a plan for the new town at Sydney Cove. It included a wide central avenue, a permanent Government House, law courts, hospital and other public buildings, but no provision for warehouses, shops, or other commercial…

Average elevation: 32 m

Average elevation: 305 m

Average elevation: 103 m

Average elevation: 85 m

Average elevation: 8 m

Average elevation: 644 m

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,…

Average elevation: 179 m

Average elevation: 986 m

Average elevation: 748 m

Average elevation: 52 m

Average elevation: 59 m

Owing to its elevation, Goulburn has an oceanic climate (Cfb) with warm summers and cool winters; with a high diurnal range. Its climate is variable much of the year, though generally dry with maximum temperatures ranging from 11.8 °C (53.2 °F) in July to 28.3 °C (82.9 °F) in January. Rainfall is…

Average elevation: 666 m

Average elevation: 223 m

The city occupies the edge of the range and the low ridges behind it. Two valleys run north from the southern boundary, each arising from springs either side of Middle Ridge near Spring Street at an altitude of around 680 m. These waterways, East Creek and West Creek, flow together just north of the CBD to…

Average elevation: 458 m

Average elevation: 87 m

Average elevation: 370 m

Average elevation: 31 m

Average elevation: 713 m

Average elevation: 598 m

The Sunshine Coast in Queensland, Australia, showcases a diverse topography that harmoniously blends coastal plains with rugged hinterlands. Along its eastern edge, the region features expansive sandy beaches and coastal dunes that transition smoothly into fertile lowlands. Inland, the terrain becomes more…

Average elevation: 109 m

Average elevation: 5 m

Average elevation: 416 m

Average elevation: 596 m

Toolangi has a cold rainforest climate, significantly cooler and wetter than Melbourne due to elevation (of 595 metres) and being outside of the Yarra rainshadow; with annual cloud cover resembling that of Southern England in the British Isles and the Pacific Northwest of North America, more than the typical…

Average elevation: 562 m

Average elevation: 614 m

Average elevation: 232 m

Mount William is known within the gliding community for the "Grampians Wave", a weather phenomenon that sometimes enables glider pilots to reach extreme altitudes of the order of 28,000 ft (8,500 m). This predominantly occurs during the months of May, June, September and October when strong westerly winds flow…

Average elevation: 262 m

Average elevation: 9 m

Average elevation: 53 m

Average elevation: 6 m

Average elevation: 713 m

Average elevation: 491 m

The Castlemaine goldfields' legendary prosperity raised expectations of Castlemaine becoming Victoria's second city. That is reflected in imposing buildings erected in the town's first few years. Though the rich alluvial diggings were largely exhausted within 15–20 years causing the town's population to…

Average elevation: 319 m

Average elevation: 883 m

South of Smithfield and inland from the Northern Beaches along the edge of the Barron River flood plain are the suburbs of Caravonica, Kamerunga, Freshwater, and Stratford. This area is sometimes referred to as Freshwater Valley, though it is actually the lower part of Redlynch Valley; further up the valley…

Average elevation: 176 m

Average elevation: 48 m

Average elevation: 693 m

Average elevation: 21 m

Average elevation: 399 m

Average elevation: 7 m

Average elevation: 589 m

Average elevation: 799 m

Average elevation: 253 m

Average elevation: 366 m

Average elevation: 310 m

Average elevation: 740 m

Average elevation: 189 m

Average elevation: 17 m

Average elevation: 5 m

Average elevation: 845 m

Average elevation: 521 m

Average elevation: 904 m

Average elevation: 37 m

Average elevation: 285 m

Average elevation: 588 m

Average elevation: 590 m

Average elevation: 20 m

Average elevation: 18 m

The tropical landscapes are among the most stable in the world. Long undisturbed by tectonic activity, the peninsula is an extremely eroded, almost level low plain dominated by meandering rivers and vast floodplains, with some very low hills rising to 800 m (2,600 ft) elevation in the McIlwraith Range on the…

Average elevation: 71 m

South Australia was officially established as a British Province in England in February 1836. The first governor proclaimed the commencement of colonial government in South Australia on 28 December 1836, near The Old Gum Tree in what is now the suburb of Glenelg North. The event is commemorated in South…

Average elevation: 146 m

Average elevation: 151 m

Average elevation: 443 m

Average elevation: 20 m

Average elevation: 601 m

Average elevation: 273 m