Du Lièvre River

The Le Lièvre River (Rivière du Lièvre in French; French pronunciation: ​[ʁivjɛʁ dy ljɛvʁ]) is a river in western Quebec which flows south from the Mitchinamécus reservoir and empties into the Ottawa River at Masson-Angers. The river is 330 kilometres (210 mi) long and drains an area of 10,400 square kilometres (4,000 sq mi). The river's name comes from the French word for hare. The 1908 landslide at Notre-Dame-de-la-Salette and the earlier 1903 clay landslide at Leda both occurred on this river.

Du Lièvre River

The Le Lièvre River (Rivière du Lièvre in French; French pronunciation: ​[ʁivjɛʁ dy ljɛvʁ]) is a river in western Quebec which flows south from the Mitchinamécus reservoir and empties into the Ottawa River at Masson-Angers. The river is 330 kilometres (210 mi) long and drains an area of 10,400 square kilometres (4,000 sq mi). The river's name comes from the French word for hare. The 1908 landslide at Notre-Dame-de-la-Salette and the earlier 1903 clay landslide at Leda both occurred on this river.