Corra Linn Dam Explained

Corra Linn Dam
Dam Crosses:Kootenay River
Res Name:Kootenay Lake
Operator:FortisBC[1]
Dam Height:16m
Opening:1932

Corra Linn Dam is a concrete hydroelectric dam on the Kootenay River between the cities of Castlegar and Nelson, in the West Kootenay region of southern British Columbia.

Rapids

The Corra Linn Rapids, named after the Falls of Clyde upper falls of Cora Linn,[2] preceded the dam at this location.

Neighbourhood

The adjacent former train station and neighbourhood were named after the rapids, but the locality has been frequently misspelled as Corra Lynn.

Dam

For the six-year period after the 1932 opening, the dam was not permitted to raise the level of Kootenay Lake. It operated as a run-of-the-river hydroelectricity plant allowing the spring freshet to pass downstream. After devastating floods to Idaho farmlands in 1938, the International Joint Commission granted two approvals.

The first allowed excavation to the outlet of the lake at Grohman Narrows. In 1939, 334585cuyd of gravel and 17927cuyd of rock were removed, which included rock bluffs on the south side of the river.[3] The narrows was made deeper and wider, allowing for a greater drawdown of the lake during the winter and a greater flow during spring freshet. Even after excavation, Grohman Narrows continued to limit outflow. During the 1961 flood, the level of the lake was 3m (10feet) above the maximum level of the dam, owing to water held back at the narrows.[4] [5] Models indicate the lake would have been almost 2m (07feet) higher without the excavation. Between 2005 and 2010 BC Hydro considered more excavation at the narrows as a potential "Resource Smart" project.[6]

The second approval permitted the dam to be used to raise the level of Kootenay Lake by 2 metres, thus forming a reservoir for flood control and hydro power.[7] [8]

The dam's powerplant has a generating capacity of 51 MW.[1] In 2003, FortisBC bought the dam formerly owned by West Kootenay Power.

Successive dams

After the 1948 Vanport Oregon flood, the 1961 Columbia River Treaty led to the construction of the flood control Duncan Dam in 1967, and Libby Dam in 1975, which regulated water flowing into Kootenay Lake.

Most outflow is diverted 4.5km (02.8miles) past Corra Linn along the Kootenay Canal to the more efficient generating station opened in 1976. Kootenay basin reservoirs provide nearly 7000000acre.ft of storage which constitutes almost half of the 15500000acre.ft stored in Columbia River Treaty reservoirs.[9]

See also

References

49.4667°N -145°W

Notes and References

  1. Web site: Electricity facilities and operations . www.fortisbc.com.
  2. Web site: Nelson Star, 8 Dec 2013 . www.nelsonstar.com. 8 December 2013 .
  3. Web site: Consolidated Mining and Smelting, Annual Report, 31 Dec 1939 . 21. www.library.mcgill.ca.
  4. Web site: Archived copy . 2011-07-10 . 2011-09-27 . https://web.archive.org/web/20110927072920/http://www.ijc.org/rel/boards/Kootenay_Lake/kootenay_060922b.htm . dead .
  5. Web site: Brilliant Dam . www.trailsintime.org.
  6. Web site: Correspondence, 4 Nov 2005. www.bcuc.com.
  7. Web site: Corra Linn Dam. https://web.archive.org/web/20111004041631/http://virtualmuseum.ca/Exhibitions/Hydro/en/dams/?action=corralinn. 2011-10-04.
  8. Web site: Kootenay Lake Board of Control Responsibilities . https://web.archive.org/web/20110927072824/http://www.ijc.org/conseil_board/kootenay_lake/en/kootenay_mandate_mandat.htm . 2011-09-27 .
  9. Web site: The Governments of the United States of America and Canada. Treaty relating to cooperative development of the water resources of the Columbia River Basin (with Annexes). Center for Columbia River History. 17 Jan 1961 . https://web.archive.org/web/20100706215743/http://www.ccrh.org/comm/river/docs/cotreaty.htm. 2010-07-06.