on a small tributary called Woolshed Creek. The Mitchell River was an important location to the Gunai/Kurnai nation, especially Brabuwooloong and the Brayakuloong people of central Gippsland. The upper reaches of the Wonnangatta and Dargo rivers were mapped in 1850. From the 1860s, Bairnsdale developed as a port with the Mitchell River navigable for several kilometres upstream of Bairnsdale. The Gippsland Lakes provided access to steamers via Lakes Entrance for transport of livestock, timber, wool, skins and hides to market in Melbourne. The Mitchell River is prone to flooding, sometimes cutting off towns such as Wy Yung and Lucknow from Bairnsdale and causing extensive damage to property, farmland and infrastructure. Most notable recent floods were those of April 1990 and June 2007. These floods are usually caused by severe weather systems in the Gippsland region that also flood other nearby rivers such as the Thomson and Avon rivers in the West Gippsland catchment. The tributary rivers have a very large population of Australian grayling, which is listed as a vulnerable species by the Department of Sustainability and Environment, and has a very high conservation value. River delta geology The Mitchell River delta is a classic form of digitate delta and ranks as one of the world’s finest examples of this type of landform. The river sweeps near the western shore of Lake King before hitting Eagle Point Bluff and heading east into the lake. Where the river meets the lake a river delta alluvial deposition of sediment has formed, known locally as silt jetties, which extend more than 8 kilometres east into the lake. Silt deposited by this process forms into long narrow banks which run many kilometres. The silt was deposited over the past 10,000 or so years - since the end of the last glaciation and the rise in sea levels that flooded the Gippsland Lakes - to form silt banks or islets as the speed of the river slows. The silt jetties have been nominated by geologists as a site of international significance, second in size to those of the Mississippi River at the Gulf of Mexico. The Mitchell River silt jetties are subject to erosion caused by a salinity increase in the lakes which is slowly killing off the vegetation. The creation and maintenance of the channel at Lakes Entrance in 1889, harvesting of catchment water and decreased rainfall during drought has increased salinity in the