Lardner Park地形図

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…

平均標高：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…

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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…

平均標高：824 m

The Yarra Valley is the region surrounding the Yarra River in Victoria, Australia. The river originates approximately 240 km (150 mi) east of the Melbourne central business district and flows towards it and out into Port Phillip Bay. The name Yarra Valley is used in reference to the upper regions surrounding…

平均標高：305 m

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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.

平均標高：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…

平均標高：49 m

平均標高：275 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…

平均標高：36 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…

平均標高：319 m

平均標高：91 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…

平均標高：185 m

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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,…

平均標高：470 m

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平均標高：550 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…

平均標高：262 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,…

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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…

平均標高：40 m

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

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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,…

平均標高：470 m

平均標高：1,467 m

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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Due to its relatively high elevation of approximately 620 metres (2,030 ft) AHD, the area experiences much cooler temperatures on average relative to nearby Melbourne. The area also receives high rainfall relative to the surrounding plains and much of the Melbourne area. This combination of geographic factors…

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