Culham Inlet Western Australia | |
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Coordinates | 33°54′29″S120°04′07″E / 33.90806°S 120.06861°E |
LGA(s) | Shire of Ravensthorpe |
Culham Inlet is an inlet located in the Goldfields-Esperance region of Western Australia. The inlet is also referred to as a coastal salt lake or a transient estuary, as the sand bar that prevents it discharging is almost always closed. The wetlands formed by the system are DIWA listed due to their ecological significance. [1]
The inlet is located on the eastern flank of East Mount Barren [2] in the Fitzgerald River National Park and is approximately 7 kilometres (4 mi) west of Hopetoun.
The inlet is a wave dominated estuary with a degraded catchment, that is a result of substantial clearing and a saline run-off. It covers a total area of 11.3 square kilometres (4 sq mi). [3] The lagoon area is shallow with a typical maximum depth of 2 metres (7 ft) with a record depth of 4.5 metres (15 ft) recorded after exceptional rainfall. Two rivers discharge into the inlet, the Phillips and the Steere.
The inlet is separated from the Southern Ocean by a bar of dunes between 30 metres (98 ft) to 40 metres (131 ft) wide. The dunes are breached intermittently, breaking naturally in 1849, 1872, [4] 1919, [4] 1993, 2000, [5] 2016 [6] and 2017, [7] and artificially in 1920, each time for a period of 3 to 4 weeks.
The inlet was a river valley prior to 6,500 years ago when a rise in sea levels caused the valley to flood, it would have remained an open estuary until 3,500 years ago when the sand bar at the entrance built up to such a degree that discharge into the ocean was prevented. Then further dune building occurred so that breaks became less frequent. [8]
The area periodically supports a large array of flora and fauna. It is used as a commercial fishery and supplied large catches of Black Bream. The waters also support populations of smaller endemic species such as Goby and two Hardyheads. A large population of waterbirds is also found in the area with up to 25 species being recorded in the inlet.
The inlet was named by John Septimus Roe, who named the inlet in 1848 after the Toodyay homestead of his son in law, Samuel Pole Phillips. [9]
An estuary is a partially enclosed coastal body of brackish water with one or more rivers or streams flowing into it, and with a free connection to the open sea. Estuaries form a transition zone between river environments and maritime environments and are an example of an ecotone. Estuaries are subject both to marine influences such as tides, waves, and the influx of saline water, and to fluvial influences such as flows of freshwater and sediment. The mixing of seawater and freshwater provides high levels of nutrients both in the water column and in sediment, making estuaries among the most productive natural habitats in the world.
In oceanography, geomorphology, and geoscience, a shoal is a natural submerged ridge, bank, or bar that consists of, or is covered by, sand or other unconsolidated material, and rises from the bed of a body of water close to the surface or above it, which poses a danger to navigation. Shoals are also known as sandbanks, sandbars, or gravelbars. Two or more shoals that are either separated by shared troughs or interconnected by past or present sedimentary and hydrographic processes are referred to as a shoal complex.
Barrier islands are a coastal landform, a type of dune system and sand island, where an area of sand has been formed by wave and tidal action parallel to the mainland coast. They usually occur in chains, consisting of anything from a few islands to more than a dozen. They are subject to change during storms and other action, but absorb energy and protect the coastlines and create areas of protected waters where wetlands may flourish. A barrier chain may extend for hundreds of kilometers, with islands periodically separated by tidal inlets. The largest barrier island in the world is Padre Island of Texas, United States, at 113 miles (182 km) long. Sometimes an important inlet may close permanently, transforming an island into a peninsula, thus creating a barrier peninsula, often including a beach, barrier beach. Though many are long and narrow, the length and width of barriers and overall morphology of barrier coasts are related to parameters including tidal range, wave energy, sediment supply, sea-level trends, and basement controls. The amount of vegetation on the barrier has a large impact on the height and evolution of the island.
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