Fluvial Sediment Supply to the North-East Queensland Coast,Australia

Rivers play a dominant role in supplying sediment to the mainly siliceous sandy north-east Queensland coast. The interaction of geology and the seasonally wet tropical climate in the coastal catchments results under natural conditions in a high, but seasonally variable river discharge and sediment yield. These are examined in the sample catchments of the Barron, Mulgrave-Russell and Burdekin Rivers Peak sediment delivery occurs with major river floods produced by tropical cyclones. The initial erosive impact of these floods and subsequent constructional effects are examined along the Burdekin and Barron delta coasts. Human interference in the coastal catchments has caused increased sediment yield especially with extensive clearance of tropical rainforest and with some agricultural practices; but when dams and weirs trap sediment and sand is extracted from river beds a decrease occurs.