Coulonge River | |
Pushpin Map: | Quebec South |
Subdivision Type1: | Country |
Subdivision Name1: | Canada |
Subdivision Type2: | State |
Subdivision Name2: | Quebec |
Subdivision Type3: | Region |
Subdivision Name3: | Outaouais |
Length: | 240km (150miles) |
Discharge1 Min: | 25.1m3/s |
Discharge1 Avg: | 74.1m3/s |
Discharge1 Max: | 195m3/s |
Source1: | Lac au Barrage |
Source1 Location: | Lac-Pythonga, Quebec |
Source1 Coordinates: | 47.2083°N -76.8917°W |
Mouth: | Ottawa River |
Mouth Location: | Fort-Coulonge, Quebec |
Mouth Coordinates: | 45.8622°N -76.765°W |
River System: | Ottawa River drainage basin |
Basin Size: | 5060km2 |
Tributaries Left: | East Coulonge River |
The Coulonge River (;[1] in French kulɔ̃ʒ/) is a predominantly wilderness river in western Quebec, Canada.
A popular river for whitewater canoeing enthusiasts, it is often grouped together with the Dumoine and Noire Rivers as three of a kind. The three rivers share the same watershed, and have similar whitewater characteristics.[2] All three empty into the Ottawa River within a distance of 105km (65miles) from one another.
One of a dozen or so significant tributaries of the Ottawa River, the Coulonge River has a length of and a drainage area of,[3] and runs in a general south-eastern direction from its headwaters in Lac au Barrage (situated in La Vérendrye Wildlife Reserve) to the Ottawa River at Fort-Coulonge. Over that distance, it drops approximately 260m (850feet). The massive Grandes or Coulonge Chutes, with a height of 48m (157feet), is approximately 15km (09miles) upstream of the confluence with the Ottawa River.
The historic Félix-Gabriel-Marchand Bridge crosses the Coulonge River near Fort-Coulonge. Constructed in 1898, this long bridge is the longest covered bridge in Quebec.[4] [5]
Over the period 1926 to 1993, the Coulonge River had a mean flow of 74.1m3/s. Mean minimal flow was 25.1m3/s and mean maximum flow was 195m3/s. Record maximum flow was 410m3/s in May 1947, while record minimum flow was 9.58m3/s in October 1948.[6]
The Coulonge River is named after Nicholas d'Ailleboust de Manthet (1663–1709), Sieur de Coulonge, a French explorer who spent the winter of 1694–95 at the nearby Allumettes Island.
The Coulonge was used as a waterway by native North Americans and, later, by the coureurs des bois plying their independent trade in furs. In 1784, the North West Company built a fort at the mouth of the river, named Fort Coulonge, which passed into the hands of the Hudson's Bay Company when the two companies merged in 1821.
In 1835, Scottish-born lumber baron George Bryson acquired timber rights to thousands of acres of forest in the area, including the 200acres immediately surrounding the Grandes Chutes. In 1843, Bryson built a sawmill near the mouth of the river, which led to permanent settlement and the formation of the village of Fort-Coulonge. To transport the squared timber safely past the falls and the 750m (2,460feet) gorge below, Bryson built a 915m (3,002feet)-long timber slide (a wooden chute flowing with water diverted from the head of the falls), which was replaced by a concrete chute in 1923.[7]
For almost 150 years, the forests around the Coulonge were logged throughout the winter months until spring breakup permitted the massive log drives which, along with similar operations throughout the Ottawa River watershed, fueled the economy of the Ottawa Valley region from the early 19th century through the middle of the 20th.[2]
The last spring log drive in Canada took place on the Coulonge River in 1982.[8] Since then, the timber from smaller-scale logging operations has been hauled out by trucks over a network of dirt roads which meander throughout the Coulonge River valley.
In 1994, a hydro-electric dam and power station was built at the head of the Grandes Chutes, leaving the Dumoine River as the last major free-flowing tributary of the Ottawa River.
In August 2020, 2 persons drowned in the Coulonge River in separate incidents: the body of a woman was found just north of Fort Coulonge;[9] and a man was swept away by strong rapids while swimming about upstream.[10]