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Stony Mountain Institution is a clustered site, housing maximum, medium and minimum security inmates. There are seven operational units within the clustered facility, offering various levels of supervision, including healing units for Indigenous inmates (named NI-MIIKANA at the medium security site and AANIIKEKANA at the minimum security site).
It was opened on 14 July 1880 as a maximum security penitentiary on a hill overlooking the Memramcook River valley. It is now, having been built three years after Stony Mountain Institution (1877), the second oldest federal corrections facility in Canada still in operation following the closure of Kingston Penitentiary on September 30, 2013.
Rockwood Institution is a federal minimum-security facility located in the community of Stony Mountain, Rural Municipality of Rockwood, Manitoba, about 11 mi (18 km) from Winnipeg It opened in 1962 and can accommodate up to 167 inmates.
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Stony Mountain, MB: Minimum Men Provincial (Manitoba Corrections) Saskatchewan Penitentiary: One kilometre west of Prince Albert, SK: Medium/Maximum Men Federal Saskatoon Correctional Centre: Saskatoon, SK: Remand/Multi-level Men South Mackenzie Correctional Centre: Hay River, NWT: Minimum/Medium Men Territorial (NWT Corrections Service) [10]
Stony Mountain is a small community in Manitoba, Canada approximately 11 kilometres (6.8 mi) north of Winnipeg on Provincial Highway 7. The town is in the Rural Municipality of Rockwood and is the location of Stony Mountain Ski Area. The Stony Mountain Institution and Rockwood Institution prisons are in Stony Mountain. Stony Mountain Institution
Stony Mountain Wildland Provincial Park is a wildland provincial park in Wood Buffalo, northern Alberta, Canada. The park was established on 20 December 2000 [ 3 ] and has an area of 13,974 hectares (34,530 acres). [ 2 ]
Stone Mountain is the centerpiece of Stone Mountain State Park in North Carolina. It is a dome of exposed granite (specifically a quartz diorite to granodiorite) of Devonian age, which has intruded into the gneiss of the Precambrian Alligator Back Formation. [1] It rises sharply over 600 feet (183 m) above the surrounding terrain.
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