Gull River (Balsam Lake) Explained

Gull River
Map:Gull River watershed.png
Map Size:250px
Pushpin Map:Canada Southern Ontario
Pushpin Map Size:250px
Pushpin Map Caption:Location of the mouth of the Gull River in southern Ontario.
Subdivision Type1:Country
Subdivision Name1:Canada
Subdivision Type2:Province
Subdivision Name2:Ontario
Subdivision Type4:County
Subdivision Name4:Haliburton
Subdivision Type5:Municipalities
Discharge1 Min:12m3/s
Discharge1 Avg:20m3/s
Discharge1 Max:27m3/s
Source1:Longboot Lake
Source1 Location:Southern Algonquin Provincial Park in Dysart et al, Haliburton County
Source1 Coordinates:45.2211°N -78.2667°W
Source1 Elevation:457m (1,499feet)
Mouth:Balsam Lake
Mouth Location:Coboconk, Kawartha Lakes
Mouth Coordinates:44.6411°N -78.8053°W
Mouth Elevation:256.3m (840.9feet)
River System:Great Lakes Basin
Tributaries Right:Boshkung River, Kennisis River, Redstone River

The Gull River is a river in Algonquin Highlands and Dysart et al, Haliburton County and the single-tier municipality of Kawartha Lakes in south-central Ontario, Canada. It is in the Trent River and Lake Ontario drainage basins, and flows from southern Algonquin Provincial Park to Balsam Lake on the Trent–Severn Waterway.

Etymology

While there are no sources as to the naming of the Gull river, one of the possible origins is a translation of the name of the village of Coboconk. The name is translated from the Indigenous (Likely Ojibwa) term, Quash-qua-be-conk, meaning "where the gulls nest."[1] The town of Minden, about 30km (20miles) north, was named Gull River prior to April 1, 1859.[2]

Course

The Gull River begins at Longboot Lake in the geographic township of Bruton in Dysart et al, Haliburton County. This is in the southern arm of Algonquin Provincial Park, and just south of the York River in the Ottawa River drainage basin.[3] The river leaves the lake at the southeast and loops east, south, west and north west to Percy Lake.

History

The Gull River drainage basin is an important reservoir for the Trent–Severn Waterway. The lakes of the system were flooded during the 1800s by man-made cofferdams in order to preserve the flow of the river throughout the year. While the original purpose of this was to aid lumberjacks — who were cutting pine, spruce and hemlock in the area — in sending logs downstream to Trenton after the initial spring flooding had subsided, it would serve a dual purpose when the lock between Balsam Lake and Cameron Lake was completed in 1873, connecting Trenton with Coboconk. Balsam lake was raised 5 metres to provide enough depth for steamboats passing through the lock.[4]

Since that time, the Gull River has been an integral part of the Trent-Severn Waterway. The water levels of the lakes in the drainage basin are closely monitored in order to preserve the reservoir year-round, as well as to protect the cottage lands adjacent to the lakes. Lake levels generally swell during the spring thaw and late fall, and settle back to normal by mid-June. The lowest water levels are in late winter.[5]

Most of the lake front property on the lower sections of the Gull River system was divided into deep narrow lots in the 1830s,[6] unlike the regular-sized concessions in the adjacent land. These properties would in time develop into the many cottages that dot the lakes today.

Geology

The river's lowest and southernmost lake, Silver Lake, lies upon the boundary line between the granite Canadian Shield, and the Limestone sheaths which lie south of it. The lakes and rivers north of Silver Lake twist and wind between the mountains and valleys created by the retreating glaciers at the end of the ice age. The result is the spectacular and pristine wilderness that has earned Highway 35, that passes through the drainage basin, a reputation as one of the most scenic highways of Ontario.[7]

Recreation

An artificial white water course was constructed through Minden and has earned the river a reputation amongst enthusiasts and kayakers.[8]

Tributaries

See also

Sources

External links

Notes and References

  1. Web site: A Phantom Village, Victoria County, Ontario Canada. Canadian Genealogy. 2010-07-28.
  2. Book: Murray, Florence Beatrice. Muskoka and Haliburton 1615-1875: A Collection of Documents. 1963. Publications of the Champlain Society, Ontario series, number 6. Champlain Society for the Government of Ontario. Toronto. 166620505.
  3. Web site: Algonquin Provincial Park and the Haliburton Highlands. McMurtrie. Jeffrey. 2008. Wikimedia Commons. 2010-07-28. dead. https://web.archive.org/web/20110629004354/http://commons.wikimedia.org/wiki/File%3AAlgonquin_Map_2008_-_Version_1.0_-_Smaller_rs.jpg. 2011-06-29.
  4. Book: Angus, James T. A Respectable Ditch. A History of the Trent-Severn Waterway, 1833-1920. 1988. McGill-Queen's University Press. Kingston, Ont. 139–141. 978-0-7735-0597-1. 19519316. 2009-07-07.
  5. Web site: Water Levels. Trent-Severn Waterway National Historic Site of Canada. Parks Canada. 2009-08-09. 2011-05-14. https://web.archive.org/web/20110514024313/http://www.pc.gc.ca/lhn-nhs/on/trentsevern/visit/ne-wl/trent_e.asp. dead.
  6. Web site: Hell's Half Acre, Victoria County, Ontario Canada. Canadian Genealogy. 2010-07-28.
  7. 1993 Ontario Road map which designates "scenic highways".
  8. Web site: The Gull River. Whitewater Ontario. 2009-08-09.