Big Muddy River The Big Muddy was not covered by the Wisconsin Glacier, about 70,000 to 10,000 years before present. However, during the melting of that glacier, the level of the Mississippi River was much higher. Water backed up into the Big Muddy Basin, forming a lake much like the artificial Rend Lake but covering a larger area. The ancient lake silted in, forming a flat bottom. After the melting of the Wisconsinan glacier, the level of the Mississippi dropped, allowing the lake to drain. A new channel formed within the old lake bed. This channel meandered in the flat bottom of the
King River (Great Southern, Western Australia) The land along the river is estimated as being 83% cleared yet the water quality is generally healthy fresh water. The salinity level of the King River at discharge is 800 mg/L. The main tributary of the King River is Mill Brook which joins the King about north-west of the Upper King Bridge. King River (Great Southern, Western Australia) The King River is a river in the Great Southern region of Western Australia. The river rises east of the town of Redmond and then flows for approximately and along with the Kalgan River drains into Oyster Harbour and finally King