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🌊 Peace River: Through the Rockies

Follow the Peace from its drowned headwaters through the Rockies, northern Alberta, and a delta where the water can run backward.

4
lessons
~20 min
to learn
🗺️ Geography
subject
Adults
level
Start the course →

What you’ll learn

  1. The River Crosses the RockiesExplain how the Peace begins west of the Rockies and crosses the range into Alberta.The Peace's unusual course is a geographic exception made visible by its gap through the Rockies.
  2. The River Is EngineeredTrace how dams transformed the Peace's upper forks and regulated its power.Williston, Peace Canyon, and Site C turn one river into a sequence of reservoirs and generating stations.
  3. People Follow the RiverConnect the river's valley to agriculture, Indigenous history, trade, and settlement.The river is a route, a meeting place, and a climate corridor before it becomes a northern delivery system.
  4. The Delta Runs BackwardExplain how high water reverses channels and sustains the Peace-Athabasca Delta.The delta depends on floods, and its channels can run backward when the Peace rises above Lake Athabasca.

Questions this course answers

What makes the Peace River unusual?

The Peace begins in British Columbia and crosses the Rocky Mountains eastward into Alberta.

What happened to the old Finlay Forks?

The W.A.C. Bennett Dam flooded the former junction of the Finlay, Parsnip, and upper Peace into Williston Lake.

Why is the Peace valley important for farming?

The Peace River Lowland combines a mountain gap with long summer daylight and a distinctive precipitation pattern.

When can water flow back into the Peace-Athabasca Delta?

Parks Canada explains that high Peace levels, often during ice jams or floods, can reverse normally northward channels.

Grounded in trusted sources

  • Encyclopaedia Britannica, Peace River — total course from the head of the Finlay 1,195 miles (1,923 km); named for Peace Point, Alberta, where the Cree and Beaver (Dane-zaa) made peace; Finlay and Parsnip headstreams in the Canadian Rockies of British Columbia; flows northeast across Alberta
  • The Canadian Encyclopedia, Peace River (David W. Leonard; last edited 19 Apr 2018) — 1,923 km; one of the principal tributaries of the Mackenzie; name refers to a settlement between Cree and Dane-zaa around 1781 at Peace Point; Dane-zaa word unchaga, 'big river'; formerly formed by the Finlay from the north and the Parsnip from the south; late 1960s the forks were dammed and the water swelled into Williston Lake; the Peace flows from the east arm of the lake, cuts through the Rocky Mountains, and is joined by the Halfway and Beatton from the north and the Pine from the south; cuts a deep gash, up to 11 km wide, across the northwestern Alberta prairie; near the town of Peace River it is joined by the Smoky and swings north; valley is the northernmost commercially important agricultural region of North America
  • The Canadian Encyclopedia, Peace River Lowland — Pacific air masses can cross over with less modification, resulting in about 350 to 600 mm of annual precipitation, more than in east-central Alberta at the same latitude
  • The Canadian Encyclopedia, Dane-zaa (Beaver) — Dene-speaking people of the Peace River area of British Columbia and Alberta; Alexander Mackenzie passed through Dane-zaa territory in 1793; by 1794 the North West Company established a fur-trading post near present Fort St. John
  • The Canadian Encyclopedia, Historic Dunvegan — provincial historic site on the Peace River, 26 km south of Fairview, Alberta
  • Parks Canada, Fort Dunvegan National Historic Site — established in 1805 for the North West Company by Archibald Norman McLeod; closed as a trading post in 1918
  • Parks Canada, Hydrology, Wood Buffalo National Park (modified 2 Feb 2023) — Peace-Athabasca Delta formed by the Peace, Athabasca and Birch rivers at the western end of Lake Athabasca; many waterways can flow in two directions; three channels (Rivière des Rochers, Revillon Coupé, Chenal des Quatre Fourches) normally flow north, but can reverse when the Peace stands higher than Lake Athabasca; perched basins replenished only by overland flooding, about once per decade; when filled they contribute an estimated 19,000 km of additional shoreline; flow regulation on the Peace plus climatic drying have reduced the frequency of major spring floods
  • Parks Canada, Flooding in the Peace-Athabasca Delta (modified 3 May 2024) — one of the world's largest freshwater deltas; RAMSAR Wetland of International Importance; a main feature of Wood Buffalo National Park as a World Heritage Site; 2020 summer flood created by high Peace flows obstructing outflow and reverse flows into the delta at the same time as high Athabasca flows

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