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Perth Canyon is a submarine canyon located on the edge of the continental shelf off the coast of Perth, Western Australia, approximately 22 kilometres (14 mi) west of Rottnest Island. It was carved by the Swan River , likely before the Tertiary , when this part of the continental shelf was above sea level.
The Avon rises near Yealering, 221 kilometres (137 mi) southeast of Perth: it meanders north-northwest to Toodyay about 90 kilometres (56 mi) northeast of Perth, then turns southwest in Walyunga National Park – at the confluence of the Wooroloo Brook, it becomes the Swan River.
A geologic cross section of the Grand Canyon. [ 5 ] The Tonto Group is a name for an assemblage of related sedimentary strata , collectively known by geologists as a Group , that comprises the basal sequence Paleozoic strata exposed in the sides of the Grand Canyon.
Kings Park is a 399.9-hectare (988-acre) [1] [2] park overlooking Perth Water and the central business district of Perth, Western Australia. The park is a mixture of grassed parkland, botanical gardens and natural bushland on Mount Eliza with two-thirds of the grounds conserved as native bushland.
Mount Eliza is a hill that overlooks the city of Perth, Western Australia and forms part of Kings Park. It is known as Kaarta Gar-up [ 1 ] and Mooro Katta [ 1 ] in the local Noongar dialect. As part of Kings Park, Mount Eliza has received more than 5 million visitors each year (2019), [ 2 ] due to events such as; the Anzac Day Memorial service ...
The Perth Basin is a thick, elongated sedimentary basin in Western Australia. It lies beneath the Swan Coastal Plain west of the Darling Scarp, representing the western limit of the much older Yilgarn Craton, and extends further west offshore. Cities and towns including Perth, Busselton, Bunbury, Mandurah and Geraldton are built over the Perth ...
Geologic stratigraphic column of strata exposed in and near the Grand Canyon. The term Great Unconformity is frequently applied to the unconformity observed by John Wesley Powell in the Grand Canyon in 1869. [1] It is an exceptional example of relatively young sedimentary rock strata overlying much older sedimentary or crystalline strata.
The Neoproterozoic Chuar Group consists of 1,600 m (5,200 ft) of exceptionally well-preserved, unmetamorphosed sedimentary strata that is composed of about 85% mudrock.The Group is the approximate upper half of the Grand Canyon Supergroup, overlain by the thin, in comparison, Sixtymile Formation, the top member of the multi-membered Grand Canyon Supergroup.
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