Swan Coastal Plain
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Swan Coastal Plain
The Swan Coastal Plain in Western Australia is the geographic feature which contains the Swan River as it travels west to the Indian Ocean. The coastal plain continues well beyond the boundaries of the Swan River and its tributaries, as a geological and biological zone, one of Western Australia's Interim Biogeographic Regionalisation for Australia (IBRA) regions.IBRA Version 6.1
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It is also one of the distinct physiographic provinces of the larger West Australian Shield division.


Location and description

The coastal plain is a strip on the Indian Ocean coast directly west of the

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Australasian Realm
The Australasian realm is a biogeographic realm that is coincident with, but not (by some definitions) the same as, the geographical region of Australasia. The realm includes Australia, the island of New Guinea (comprising Papua New Guinea and the Indonesian province of Papua), and the eastern part of the Indonesian archipelago, including the island of Sulawesi, the Moluccan islands (the Indonesian provinces of Maluku and North Maluku), and the islands of Lombok, Sumbawa, Sumba, Flores, and Timor, often known as the Lesser Sundas. The Australasian realm also includes several Pacific island groups, including the Bismarck Archipelago, Vanuatu, the Solomon Islands, and New Caledonia. New Zealand and its surrounding islands are a distinctive sub-region of the Australasian realm. The rest of Indonesia is part of the Indomalayan realm. In the classification scheme developed by Miklos Udvardy, New Guinea, New Caledonia, Solomon Islands and New Zealand are placed in the Oceania ...
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Coquina
Coquina () is a sedimentary rock that is composed either wholly or almost entirely of the transported, abraded, and mechanically sorted fragments of the shells of mollusks, trilobites, brachiopods, or other invertebrates. The term ''coquina'' comes from the Spanish word for " cockle" and "shellfish". For a sediment to be considered to be a coquina, the particles composing it should average or greater in size. Coquina can vary in hardness from poorly to moderately cemented. Incompletely consolidated and poorly cemented coquinas are considered grainstones in the Dunham classification system for carbonate sedimentary rocks. A well-cemented coquina is classified as a biosparite (fossiliferous limestone) according to the Folk classification of sedimentary rocks. Coquinas accumulate in high-energy marine and lacustrine environments where currents and waves result in the vigorous winnowing, abrasion, fracturing, and sorting of the shells that compose them. As a result, they typi ...
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Lake Pinjar
A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic drainage patterns left over from the last ice ...
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Wanneroo Wetlands
The Wanneroo wetlands are a series of wetlands, swamps and lakes that occur on the Swan Coastal Plain of Perth, Western Australia. They are linked very closely to the Gnangara Mound. They are in part, incorporated into the Yellagonga Regional Park and also referred to as Yellagonga wetlands. Description The wetlands comprise a series of named lakes, including Lake Joondalup (or Craigie Lake), Lake Goolelal (or Welshes Lake), Jandabup Lake (or Big Dundebar Lake), Yonderup Lake, Nowergup Lake (or Narago Lake), Coogee Springs, Neerabup Lake (or Pappas Swamp), Lake Gnangara, Mariginiup Lake, Pippidinny and Boonaddy Swamps, and Loch McNess (or Yanchep Lake). See also * List of lakes of Western Australia The following lists of lakes of Western Australia are arranged alphabetically: * List of lakes of Western Australia, A–C (plus numerals) * List of lakes of Western Australia, D–K * List of lakes of Western Australia, L–P * List of lakes of ... Notes Swan Coastal Pl ...
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Peel Inlet
The Peel-Harvey Estuarine System ( nys, Djilba) is a natural estuarine system that lies roughly parallel to the coast of Western Australia and south of the town of Mandurah. The strip of land between the Indian Ocean and the estuarine system carries the Old Coast Road and to the east is the Forrest Highway which is the main thoroughfare between Perth and the coastal towns of the south west corner of the state including Bunbury and Busselton. Description The estuarine system, which the Bindjareb Noongar people call , covers an area of approximately in total, with an average water depth of about . The Harvey River discharges into the extreme southern end of the elongated Harvey Estuary, which has an area of about . This in turn feeds into the south-western corner of the more northerly Peel Inlet which is roughly circular and occupies an area of about . The Serpentine River and Murray Rivers discharge into the eastern edges of Peel Inlet. A long channel, the Mandurah Estu ...
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Serpentine River (Western Australia)
The Serpentine River is a river in the South West region of Western Australia. It is known as Waangaamaap Bilya to the Indigenous Bindjareb people, who met, lived and fished there before British settlement. The river rises in the Darling Scarp below Bowerling Hill and flows westward crossing Albany Highway north of North Bannister. The river continues north west through the Youarling State Forest then the Serpentine National Park. The river flows through Serpentine Dam then flows over Serpentine Falls just south of Jarrahdale as it comes off the Scarp and onto the Swan Coastal Plain. The river continues west and crosses the South Western Highway then flows past the town of Serpentine. The river then veers south and continues until it discharges into the Peel Inlet near Mandurah. The upper reaches of the river flow into Serpentine Dam, which provides drinking water to the Perth metropolitan area. The only tributary to Serpentine River is Big Brook. Additionally, the Pee ...
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Ellen Brook
Ellen Brook is an ephemeral stream which runs from south of Gingin to the Swan River in Western Australia. Overview The headwaters of Ellen Brook start south of Gingin, in the Wheatbelt region. From there, Ellen Brook travels south, generally parallel and to the east of Brand Highway, through agricultural land. Near Muchea, Ellen Brook passes under Brand Highway, Granary Drive and Tonkin Highway. From there, it heads south, between Great Northern Highway and Muchea South Road, passing to the west of RAAF Base Pearce in Bullsbrook, before reaching Upper Swan, where it passes under Muchea South Road, past residential areas in The Vines and Belhus, before joining the Swan River in the Swan Valley. Tributaries to the west of Ellen Brook are sourced by groundwater flowing from the Gnangara Mound. Tributaries to the east have aquifers on the Dandaragan plateau as their source. The brook only flows from May to December. At a size of , Ellen Brook is the largest sub catchme ...
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Cardup Brook
Cardup is an outer suburb of the Western Australian capital city of Perth, located in the Shire of Serpentine-Jarrahdale The Shire of Serpentine-Jarrahdale is a local government area in the outer southeastern metropolitan area of Perth, the capital of Western Australia, and has an area of and a population of almost 27,000 as at the 2016 Census. The Shire's seat ... to the north of the town Mundijong. In the , it had a population of 972 people. History In 1844, surveyor Robert Austin recorded that Cockburn Sound Location 22 was called Cardoup. The brook joining the northern boundary of this location has been shown at various times as either Cardoup or Cadup Brook. In 1851, the location was purchased by H. Mead, who gave his address as Cardup and this spelling was used for the brook on most subsequent plans and surveys. By 1927, a railway siding had been erected nearby and was called Cardup after the brook and although the siding is no longer in use, the place still retains ...
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