Undera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…

平均標高：185 m

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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…

平均標高：345 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…

平均標高：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…

平均標高：185 m

平均標高：50 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

Horsham's topography is flat, approximately 128 metres (420 ft) above sea level. The central business district (CBD) is laid out in a grid plan south of the train line and is characterised by wide streets and several roundabouts. Firebrace Street, running north–south through the middle of the CBD is one of…

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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

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There are bus routes from Bright and Bairnsdale. The Bairnsdale bus runs weekdays, once both directions, and the Bright bus (Alps Link) timetable is less frequent in Summer and runs additional services during the ski season. Alps Link is the highest altitude public bus in Australia. The town sits at the…

平均標高：861 m

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Beaufort has an elevation-influenced oceanic climate (Köppen: Cfb), with tepid, relatively dry summers and cool, wetter winters. Average maxima vary from 25.3 °C (77.5 °F) in January to 10.1 °C (50.2 °F) in July, while average minima fluctuate between 11.5 °C (52.7 °F) in February and 3.2 °C (37.8 °F)…

平均標高：390 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.

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Newspaper articles from the late 19th and early 20th century describe the wide variety of plants that flourished at the State Nursery in spite of its poor topsoil and craggy terrain. Cool-climate trees like cypress, larch, cedar and pine thrived at the high altitude; deciduous species of oak, ash and birch…

平均標高：542 m

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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…

平均標高：212 m

Formerly a major river drainage system, it was inundated together with Port Phillip by the rising sea in the Holocene period; the Western Port sunkland now forms an extensive tidal bay. The waters of Western Port cover an area of 680 km² of which 270 km² are exposed as mud flats at low tide. The topography…

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