Dookie topographic map

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

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

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Average elevation: 191 m

Port Phillip's mostly flat topography and moderate waves make perfect conditions for recreational swimming, kitesurfing, windsurfing, sailing, boating, snorkeling, scuba diving, stand up paddle boarding (SUP) and other sports.

Average elevation: 18 m

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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…

Average elevation: 824 m

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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

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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

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Average elevation: 32 m

Olivers Hill is the most prominent elevation in Frankston which rises to 55 metres above sea level (180 feet) at its highest point in the suburb. Its origins date to approximately 415 to 360 million years ago. Its base is Mount Eliza Granite dating from the Devonian period, which was covered in lava tuffs in…

Average elevation: 40 m

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The streets are designed in a curvilinear way typical of Griffin's design, often following the topography of the land.

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