Mappa topografica Kingston

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…

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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: 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…

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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…

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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.

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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…

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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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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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Like most of south-western Victoria, Hamilton has a temperate mediterranean climate (Csb). Cold fronts regularly sweep in from the Southern Ocean. Although daytime temperatures occasionally reach into the 30s even 40s during summer, daytime temperatures in the mid teens will often linger into December and are…

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Hemmed in by a rising ocean that stabilised about 7000 years ago, the uplifted sedimentary rocks of the Otway Range run from north-east to south-west at an elevation of about 500 metres above the sea. A few isolated peaks reach up to 675 metres, and at many points along this coastline bare mountains and…

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The town has a prominent winter rainfall peak, with a yearly average of 1,264.6 millimetres (49.79 in). It rains on 142 days of the year; heavily concentrated between May and October. On account of its southern latitude nearing the 37th parallel, summers have a notable chill about them when compared to…

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