Mapa topográfico Mount Cole

Sydney's topography is characterized by a diverse landscape that seamlessly blends coastal features with inland plateaus. The city is divided into two primary regions: the relatively flat Cumberland Plain to the south and west of Sydney Harbour, and the elevated Hornsby Plateau to the north. The Cumberland…

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A sandstone plateau dominated by a landscape of endless eucalyptus forests, the Blue Mountains are located at the top of a 470-million-year-old quartzite. In the Permian period, a shallow sea covered the region, when rivers brought shales, siltstones and mudstones. Then during the Mesozoic period, rivers…

Altitude média: 566 m

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Byron Bay, located in northeastern New South Wales, Australia, is characterized by diverse topography shaped by its geological history. The town is part of the erosion caldera of the ancient Tweed Volcano, which erupted approximately 23 million years ago, resulting in the rich volcanic soils that define the…

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Owing to its elevation, Goulburn has an oceanic climate (Cfb) with warm summers and cool winters; with a high diurnal range. Its climate is variable much of the year, though generally dry with maximum temperatures ranging from 11.8 °C (53.2 °F) in July to 28.3 °C (82.9 °F) in January. Rainfall is…

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The park includes areas of land which are part of Ku-ring-gai, Ryde, and Hornsby local government areas with small areas of the park in Willoughby, Lane Cove and Hunter's Hill local government areas on the banks of the lower reaches of the river. The park is surrounded on all sides by developed suburban areas…

Altitude média: 81 m

Orange is a city in the Central Tablelands region of New South Wales, Australia. It is 254 km (158 mi) west of the state capital, Sydney [206 km (128 mi) on a great circle], at an altitude of 862 metres (2,828 ft). Orange had an estimated urban population of 40,493 as of June 2018 making the city a significant…

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The highest mountain in the range is Mount Budawang, which has an elevation of 1,129 metres (3,704 ft) above sea level.

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