Noosa River | |
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Location | |
Country | Australia |
State | Queensland |
Physical characteristics | |
Source | |
• location | Como Escarpment |
Mouth | |
• location | Pacific Ocean |
Basin size | 854 km2 (330 sq mi)[1] |
TheNoosa River is ariver situated inSouth East Queensland. The catchment starts in the Como Escarpment near Mount Elliott in the coastalGreat Sandy National Park and meanders south through a lakes district aroundTewantin.[2]
Lakes situated on the river includeLake Cooloola,Lake Como,Lake Cootharaba,Lake Cooroibah andLake Weyba. The catchment is mostly covered bysand dunes and has two major tributaries—Kin Kin Creek and Teewah Creek.[1]
The Noosa River enters theCoral Sea betweenNoosa Heads andNoosa North Shore. Substantial residential development has encroached into areas previously occupied by the changing river path. The river is noted for its populations of migratory birdlife.[3]
The Noosa River was formed sometime during theNeolithic period, as a result of sea level rises. TheGubbi Gubbi tribes occupied the area before European settlement in the early 19th century.[citation needed]
Logging along the river began in 1864. The logs were transported north to a sawmill nearMaryborough until 1870 when a sawmill was built on Lake Cootharaba.[4]
Richard Branson purchasedMakepeace Island on the river in May 2003. Noosa Council scaled down his plans for a luxury resort on the river.[5]
Several kilometres of beach to the north of the mouth were a popular destination for four-wheel driving, until Sunshine Coast Regional Council placed restrictions on them in May 2007.[3]
Chemicalcontamination has been the suspected cause of a fishmutation resulting intwo-headedfish larvae found in the Noosa River.[6] Government investigations into the problem began in 2007. A final scientific report into the cause of the spawning was delayed in 2010 because of the potential to prejudice ongoing civil court proceedings involving the hatchery and a nearbymacadamia nut farm.[7]
Until the 1960s the Noosa beach and river entrance were in a state of dynamic equilibrium. The beach was wide and usable and it recovered quickly from the occasional extreme storm events such as cyclones. From the mid-1960s rapid development on the beachfront including building a rockwall along the beach created instability. The beach became narrow and often non existent at high tide. At this time the river entered the sea at the present day Noosa Woods. In 1978 a training wall was built to relocate the river entrance to the northwest where it is today.[8]
The Noosa Ferry operates along the Noosa River fromNoosa Heads viaNoosaville toTewantin with timetabled regular services and tourist cruises.[9]
Noosa River & Canal Cruises offers tourist cruises on the Noosa River and its canals departing Noosaville and Noosa Heads.[10]
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