Mappa topografica Macleay Park

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…

Altitudine media: 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…

Altitudine media: 185 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…

Altitudine media: 185 m

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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…

Altitudine media: 49 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,…

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Gentle, rolling hills extend from east of the Yarra River flood plains, along Templestowe Road (towards the Eastern Freeway) for seven km (4.3 miles), to the north-east. The altitude of the plain above sea level is 50 m, and the topography is subdued and mostly flat; the hills are just below 60 m, the slopes…

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Collingwood's topography is mostly flat, but a prominent slope extends from Hoddle Street up to Smith Street, and also along sections of Hoddle Street.

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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…

Altitudine media: 319 m

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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A comprehensive geological survey of Victoria's Great Dividing Range reveals a distinct north-south alignment in its bedrock, a vestige of the bygone epochs of plate tectonics. This enduring geological framework, coupled with ongoing tectonic activity, contributes to the dynamic topography witnessed in the…

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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…

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Fitzroy's topography is flat. It is laid out in grid plan and is characterised by a fairly tightly spaced rectangular grid of medium-sized streets, with many of its narrow streets and back lanes facilitating only one-way traffic. Its built form is a legacy of its early history when a mixture of land uses was…

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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…

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The topography consists of a series of ridges dissected by deeply cut streams. Sheltered gullies in the south of the range are home to temperate rain forest, fern gullies and Mountain Ash forest Eucalyptus regnans, whereas the drier ridges and exposed northern slopes are covered by dry sclerophyll forest of…

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The topography consists of a series of ridges dissected by deeply cut streams. Sheltered gullies in the south of the range are home to temperate rain forest, fern gullies and Mountain Ash forest Eucalyptus regnans, whereas the drier ridges and exposed northern slopes are covered by dry sclerophyll forest of…

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