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Calmar is a town in central Alberta, Canada. It is located in Leduc County , on Highway 39 , 35 kilometres (22 mi) southwest from Edmonton . It was named in 1900 for Kalmar , Sweden, the home town of its first postmaster, C. J. Blomquist.
Norway ceded its long-dormant claim to the Sverdrup Islands to Canada, in exchange for British recognition of Norway's sovereignty over Jan Mayen. Disputes: December 11, 1931 The Statute of Westminster 1931 confirmed Canada's sovereignty from the United Kingdom on legislative and foreign issues. no change to map: March 31, 1949
Berwyn is a village in northwestern Alberta, Canada. It is located approximately 37 km (23 mi) west of the Town of Peace River, 10 km (6.2 mi) southwest of the Town of Grimshaw, and 15 km (9.3 mi) northeast of the Duncan's First Nation reserve. The Municipal District of Peace No. 135's municipal office is located adjacent to Berwyn.
Reno is a hamlet in northern Alberta, Canada, within Northern Sunrise County. It is located 8 kilometres (5.0 mi) east of Highway 2 , approximately 146 kilometres (91 mi) northeast of Grande Prairie .
Busby is a small hamlet in central Alberta, Canada within Westlock County. [2] It is located on Highway 651 , approximately 52 kilometres (32 mi) northwest of Edmonton and 16 kilometres (9.9 mi) west of Highway 2 .
Alberta Environment - Alberta's River Basins; Statistics Canada - Rivers of Canada, Source: Natural Resources Canada, GeoAccess Division. Last modified: 2005-02-02. "Alberta River Basins". Alberta Environment. Government of Alberta.
The Art Gallery of Alberta (AGA) is an art museum in Edmonton, Alberta, Canada. The museum occupies an 8,000 square metres (86,000 sq ft) building at Churchill Square in downtown Edmonton . The museum building was originally designed by Donald G. Bittorf, and B. James Wensley, although portions of that structure were demolished or built over ...
Mount Tecumseh is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks three miles (4.8 km) thick, 50 miles (80 km) wide and 160 miles (260 km) long over younger rock of the cretaceous ...
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