The Barwon River, New South Wales : a study of basin fill by low gradient stream in a semi-arid climate.
The Barwon River, northern New South Wales, flows through semi-arid alluvial plains with a gradient of 5 x 10⁻⁵ . Its discharges are highly variable and irregular, varying between 0 to 1,500 m³s⁻¹ . The system is essentially anabranching with a series of highly sinuous, deep and narrow trunk streams. The Barwon and its tributaries (the Namoi, Gwydir, Castlereagh and Macquarie Rivers) in their lower reaches all carry around 80 percent of their load in suspension. The rivers are at...[Show more]
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