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Concept
Route 2 (Saskatchewan)
Résumé
Highway 2 is a provincial highway in the Canadian province of Saskatchewan. It is the longest highway in Saskatchewan at 809 km (503 mi). The highway has a few divided sections but is mostly undivided. However, only about near Moose Jaw, near Chamberlain, and near Prince Albert are divided highway. Highway 2 is a major north-south route beginning at the Canada–US border at the Port of West Poplar River and Opheim, Montana customs checkpoints. Montana Highway 24 continues south. It passes through the major cities of Moose Jaw in the south and Prince Albert in the north. Highway 2 overlaps Highway 11 between the towns of Chamberlain and Findlater. This section of road is a wrong-way concurrency. The highway ends at La Ronge, where it becomes Highway 102.
The highway started as a graded road in the 1920s which followed the grid lines of the early survey system and was maintained by early homesteaders of each rural municipality. Paving projects of the 1950s created all weather roads. Technological advances have paved the way for cost-effective methods of improvements to highway surfaces to meet the wear and tear of increased tourist and commercial highway traffic. The stretch of Highway 2 from Moose Jaw to Prince Albert was designated in 2005 as Veterans Memorial Highway. The designation coincided with Veterans Week 2005. The CanAm Highway comprises Saskatchewan Highways 35, 39, 6, 3, and 2.
Saskatchewan Highway 2 departs the Canada–United States border in a northerly direction. Montana Highway 24 continues in a southerly direction in the United States. The United States border crossing is in Opheim, Montana and the Canadian is at West Poplar River.
Nearby there are campgrounds available, and a point of information regarding the crossing of Poplar River. The area is rich in history, this is the Big Muddy Badlands area which featured the hideouts of outlaws and rum runners of the nineteenth and early twentieth century. This area remained above the Quaternary age ice sheets, being pushed and folded by the glacier movement resulting in glaciotectonic hills.
Source officielle
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