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Peel Inlet : ウィキペディア英語版
Peel-Harvey Estuary

The Peel Harvey Estuary is a natural estuary which 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 estuary 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 estuary covers an area of approximately 136 km2 in total with an average water depth of about 2 m.
The Harvey River discharges into the extreme southern end of the elongated Harvey Estuary, which has an area of about 56 km2. 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 75 km2. The Serpentine River and Murray Rivers discharge into the eastern edges of Peel Inlet also.
A 5 km long channel which passes through the town of Mandurah, then runs into the ocean.
After several decades of severe algal blooms in the estuary caused by discharge of nutrients from agricultural land and piggeries along the rivers, a man-made channel was constructed and opened in 1994 as the Dawesville Channel. The channel had the effect of allowing saline sea-water to regularly ''flush'' the estuary using tidal flows. Whilst the ecology of the estuary has changed markedly due to the flushing process, water quality generally has improved.
The catchment area to the east is largely flat coastal plain with about 75% cleared of native vegetation and used for dryland, dairy and beef grazing. Clearing was done in the early days of settlement to allow agricultural expansion. Drainage systems into the three main rivers have been constructed in much of the catchment to remove excess water quickly.
Lake Preston, Lake Clifton and the Leschenault Estuary are farther south.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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