Peace River, Alberta - Geography

Geography

Physiographically, the Town of Peace River lies within the Peace River Formation, a stratigraphical unit of middle Albian age in the Western Canadian Sedimentary Basin. The area developed on sediments of the former lake bottom of Glacial Lake Peace, which covered most of the areas in the region that were below 610 m in elevation.

The specific landform in which the town is situated is the Peace River Lowland which was incised by the Peace River and its tributaries right through the area's former glacial lake sediments and into the Cretaceous bedrock. The Peace River Lowlands is flanked by the Buffalo Head Hills to the east and the Whitemud and Clear Hills to the west.

The general area is categorized ecologically as the aspen parkland with mixedwood stands understory. There is a variety of wetland habitats in the area with several being quite marshy with shallow water, soft bottoms, and abundant aquatic vegetation. Some of the lakes and sloughs are used by various both migrating and resident waterfowls for nesting. The parkland also supports a host of terrestrial and aquatic animals. It is also Canada's most northerly agricultural region.

The Greene Valley Provincial Park lies just east of the town in the Northern Sunrise County and the Peace River Wildland Provincial Park is to the south on the east bank of the Peace River. These parks and the rest of the river valley, including some river islands, provide habitat for wildlife such as moose, deer, bear, coyotes, bats, reptiles, birds and numerous fish species. Maintaining natural areas in the river valley and limiting use to suitable recreational use has minimized impacts to wildlife habitat.

Historically, the town has been the subject of flooding. However, the town has developed a continuous dyke system to prevent flood damage from to 1:100 year flood events and protect against ice-jam floods. As a result, the risk of flooding has been significantly reduced and no longer poses the same threat to the town.

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