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Mitchell River, Victoria : ウィキペディア英語版 | Mitchell River (Victoria)
The Mitchell River is a perennial river of the East Gippsland catchment, located in the Australian state of Victoria. The unregulated river and provides a unique example of riparian ecology, flowing generally south with the catchment area drawing from the steep mountains of the Victorian Alps to enter Lake King, one of the Gippsland Lakes, and then empty into the Bass Strait. ==Course and features== Formed by the confluence of the Wentworth and Wonnangatta rivers and Swamp Creek near Horseshoe Bend, north of the national park that bears its name, the Mitchell River rises in Lake Tabberabbera, drained by runoff from the southern Victorian Alps of the Great Dividing Range. The river flows generally south in a highly meandering course in its upper reaches through the Mitchell River National Park, and then south by east as it spills onto the fertile Gippsland Plain west of . The river then flows generally east towards and empties into Jones Bay, part of Lake King, within the Gippsland Lakes via the silt jetties, a narrow long digitate delta. Within the lake, the Mitchell is joined by the Nicholson and Tambo rivers; and then enters Lake Victoria, where the Mitchell and Latrobe rivers form their confluence, with the Mitchell reaching its mouth in Bass Strait, south of . The river descends over its course; joined by more than thirteen tributaries,〔 many of which are surrounded by dense native forest. At Bairnsdale, the river is traversed by the Princes Highway, west of the highway's junction with the Great Alpine Road. Also at Bairnsdale, the railway line from Melbourne to crossed the river. However, the V/Line rail service now terminates at Bairnsdale railway station, west of the river; with a V/Line, coach bus service now operating east of Bairnsdale. , the former railway crossing of the river has been identified as a potential asset of the East Gippsland Rail Trail, however the current poor condition of the bridge makes it unsafe for use.
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