The Clearwater River has a total length of. It flows southeastward from its headwaters at Broach Lake and turns to the southwest from Careen Lake to the Alberta/Saskatchewan border. From there it flows westward for a distance of to join the Athabasca River at Fort McMurray. The section of the river in Fort McMurray is affectionately referred to as The Chant. From Broach Lake at an elevation of above sea level, the Clearwater drops about to the confluence at Fort McMurray. Its waters eventually reach the Arctic Ocean via the Athabasca and Mackenzie Rivers. Tributaries of the Clearwater River include Descharme River and McLean River in Saskatchewan and the Christina River in Alberta.
Geology
In its upper reaches, the Clearwater River flows over the Precambrian rocks of the Canadian Shield. That section of the river is rough, characterized by rapids, small waterfalls, and a gorge. The river leaves the Shield near the Alberta border and enters the Interior Plains where it becomes meandering, with numerous sand bars and small islands. There it is flanked by outcrops of the Devonian limestones, dolomite, and shales of the La Loche, Contact Rapids, Keg River, and Waterways Formations, as well as the Cretaceousoil sands of the McMurray Formation. The Clearwater River is an underfit stream; that is, its present flow is insufficient to have carved its broad, steep-sided valley. Instead, its morphology may be the result of a catastrophic paleoflood that originated from Glacial Lake Agassiz during late Pleistocene time and flowed through the Clearwater and Athabasca river valleys on its way to the Arctic Ocean. The channel cut by that flood is known as the Clearwater Spillway. There are several salt springs and saline marshes that discharge into the Clearwater River in northeastern Alberta. The water, which comes from the underlying Devonian rock formations, is effervescent in places and smells of sulfur.
History
Rock-paintings along the upper portion of the river, shapes and symbols on rock surfaces, suggest that the area was already inhabited 5,000 years ago. Before the European colonisation, native groups of Beaver, Chipewyan, and Cree people lived in the Clearwater River area. During European exploration and the fur trade of the 18th century, the lower Clearwater River was part of an important canoe route between Hudson Bay and Montreal in the east, and the District of Athabasca in the west. The rough Precambrian upper portion of the Clearwater River was a barrier to the traders until 1778, when explorer Peter Pond crossed the Methye Portage to bypass it. Methye Portage extended between Lac La Loche and the Clearwater River, forming a overland link on the route from Churchill, Manitoba to Athabasca, Alberta. For almost 40 years, this was the only overland connection for the fur trade in the region, and it continued in use for most of the 19th century.
The province of Saskatchewan has established the Clearwater River Provincial Park, encompassing an area of 865 mi2; or 2240 km2, to protect the river's environment.
The Saskatchewan section was granted Canadian Heritage River status because of its "unspoiled, clear-water river in a pristine" isolated "wilderness setting of spectacular beauty".
Regional Aquatics Monitoring Program (RAMP)
The Regional Aquatics Monitoring Program uses the Clearwater River as a "baseline river system" to provide "information on the variability and characteristics of natural systems". Although natural outcrops of McMurray Formation oil sands are present along the river, the "lack of significant oil sands developments" within its watershed allows it to be used as a baseline.
