Nowanup topographic map
Click on the map to display elevation.
About this map
Name: Nowanup topographic map, elevation, terrain.
Average elevation: 128 m
Minimum elevation: 100 m
Maximum elevation: 163 m
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Click on a map to view its topography, its elevation and its terrain.
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Perth, the capital of Western Australia, is situated on the Swan Coastal Plain, a flat expanse of sandy soil nestled between the Indian Ocean to the west and the Darling Scarp to the east. The Darling Scarp, also known as the Darling Range, is a low escarpment that extends north–south, marking a distinct…
Average elevation: 26 m
Perth
Perth, the capital of Western Australia, is situated on the Swan Coastal Plain, a flat expanse of sandy soil nestled between the Indian Ocean to the west and the Darling Scarp to the east. The Darling Scarp, also known as the Darling Range, is a low escarpment that extends north–south, marking a distinct…
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Australia > Western Australia > Rockingham
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The suburb sits in the south-east corner of the Gnangara Mound, close to the Darling Scarp. Topographically, the majority of Ellenbrook's area sits between 40-50 metres above sea level on the mound, with parts of Coolamon and Malvern Springs situated on hills that reach peaks of 65 metres. The northern village…
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Very early on, because of its altitude and separation from the Swan Coastal Plain, Darlington became established as a popular picnic area, country drive destination, and a place for holiday homes.
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Mount Barker
The peak of Mount Barker lies 3.5 kilometres (2.2 mi) southwest of the town centre, and reaches an elevation of 404 metres (1,325 ft) above sea level. A sealed road leads to the base of a radio and television tower on the summit of the hill. The tower was constructed to a height of 168 metres (551 ft) in 1966,…
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The Bungle Bungle Range, lying fully within the park, has elevations as high as 578 metres (1,896 ft) above sea level. It is famous for the sandstone domes, unusual and visually striking with their striping in alternating orange and grey bands. The banding of the domes is due to differences in clay content and…
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