Victoria topographic maps

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: 491 m

Average elevation: 56 m

Average elevation: 43 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

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

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Average elevation: 533 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: 36 m

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Average elevation: 86 m

Average elevation: 672 m

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Average elevation: 50 m

Average elevation: 191 m

Average elevation: 573 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: 103 m

Average elevation: 11 m

Average elevation: 441 m

Within and around the area, at least 15 volcanic eruption points formed small cones. The eruptions produced deposits of scoria, ash, and tuff near these cones. In between eruptions, clay layers formed between the basalt flows. Mount Kooroocheang, known locally as Mount Smeaton, just north of Kingston, is the…

Average elevation: 518 m

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