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Lake Diefenbaker

Lake in Saskatchewan, Canada

  • 5 min read
  • 6 chapters

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Through Reservoir, Coast and Erosion

Lake Diefenbaker provides water for domestic irrigation, drinking, and industrial uses. An extensive aqueduct (canal) system was built from the Gardiner Dam called the South Saskatchewan River Project. From the east-side of Gardiner Dam, the aqueduct system heads in a generally north-easterly direction ending at Dellwood Reservoir north-east of Little Manitou Lake in the RM of Usborne No. 310. Reservoirs along the course of the canal include Broderick Reservoir, Brightwater Reservoir, Indi Lake, Blackstrap Lake, Bradwell Reservoir, and Zelma Reservoir.

Along the lake's shores, there are several parks, protected areas, and communities.

Description

Lake Diefenbaker was created with the construction of the Gardiner Dam along the South Saskatchewan River and the Qu'Appelle Dam along the Qu'Appelle River. The lake filled the South Saskatchewan River Valley with the two dams hemming it in. The South Saskatchewan River is the primary inflow and it enters at the west end. Most of the length of the lake runs east–west following the valley. At the lake's east end, near Elbow, it branches off into two arms — the northward Thomson Arm and the southward Gordon McKenzie Arm. Gardiner Dam is at the end of the Thomson Arm and the Qu'Appelle Dam is at the end of the Gordon McKenzie Arm. The outward flow of the two rivers is now regulated with a considerable portion of the South Saskatchewan diverted into the Qu'Appelle. Prior to the dams' construction, high water levels in the South Saskatchewan would frequently cause dangerous ice conditions downstream in Saskatoon while the Qu'Appelle would frequently dry up in the summer months.

Lake Diefenbaker is 225 kilometres (140 mi) long with approximately 800 kilometres (500 mi) of shoreline. It has a maximum depth of 66 metres (217 ft), while the water levels regularly fluctuate 3–9 metres (9–27 feet) each year.

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