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Garrison Golf and Curling Club

1961 establishments in OntarioCurling clubs in OntarioGolf clubs and courses in OntarioSports venues in Kingston, Ontario

Garrison Golf & Curling Club is a golf and curling club, located within CFB Kingston in Kingston, Ontario, Canada. Garrison is a private club, primarily for the use of Canadian Forces personnel and Canadian Department of National Defence employees, although civilians are also eligible to join. The Curling Club was established in 1961 with four sheets of ice, which it has operated since that time. The Golf Club began in 1971 with the first nine holes, designed by Richard H. Green, the longtime professional at Cataraqui Golf and Country Club, and Johnny Marsh. The second nine holes of golf were opened in 1985, and were based on a design by Tom McBroom, who has since become one of Canada's leading golf course architects. The golf course has been a frequent host of Ontario and Canadian championships for the Canadian Forces, as well as local, regional, and provincial events. Matt McQuillan, now a member of the Canadian Professional Golf Tour and a tour winner, learned the game at Garrison as a junior player in the 1990s. McQuillan earned 2011 PGA Tour playing privileges in December, 2010.

Excerpt from the Wikipedia article Garrison Golf and Curling Club (License: CC BY-SA 3.0, Authors).

Garrison Golf and Curling Club
Grenadier Drive, Kingston

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N 44.251 ° E -76.449 °
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Garrison Golf Course

Grenadier Drive
K7L 0C3 Kingston
Ontario, Canada
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ggcc.on.ca

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Cataraqui River
Cataraqui River

The Cataraqui River ( KAT-ə-ROK-way) forms the lower portion of the Rideau Canal and drains into Lake Ontario at Kingston, Ontario. The name is taken from the original name for Kingston, Ontario; its exact meaning, however, is undetermined. Early maps showed several name variations including the Great Cataraqui River and Grand River Cataraquay. The river was once called Riviere de Frontenac, or Frontenac River. The alternate spelling "Cadaraqui" also appears in some historic texts.Prior to the Rideau Canal being built (1826 – 1832), the Cataraqui River had its headwaters in Dog and Loughborough lakes. It was a meandering creek, a 1795 map (by surveyor Lewis Grant) noted "a great number of rapids and Carrying Places on this creek." This changed with the building of the Rideau Canal. The Superintending Engineer of the project, Lt. Colonel John By, used a slackwater construction technique, building dams to drown rapids. In the area of the Cataraqui Creek from Upper Brewers to Kingston Mills he had the forests cut down to form a straight channel (this work is visible in the Burrowes paintings of Brewer's Lower Mill shown below). The area was then flooded in late 1831/early 1832 with the completion of canal dams at Kingston Mills, Lower Brewers and Upper Brewers. Today the watershed of the Cataraqui River includes lakes south of the watershed divide at Newboro, such as Sand, Opinicon, Clear and Newboro. However, in the pre-canal era, water from those lakes flowed into the White Fish River which drained to the Gananoque River rather than the Cataraqui River. The section between those two rivers was the Cranberry Flood Plain; the only water contribution from the White Fish River to the Cataraqui was in times of spring flood. This changed in the early 1800s with the building of a mill dam by Lemuel Haskins at White Fish Falls, near today's village of Morton. That dam retarded the outflow of the White Fish River to the Gananoque, backed it up over the Cranberry Flood Plain, sending water south to the Cataraqui River. To stop the escape of his mill water down Cataraqui Creek, Haskins built a second dam at the Round Tail (just north of Upper Brewers) which blocked the channel of the creek. These two dams made the Cataraqui Flood Plain navigable for the first time. When the Rideau Canal was built, Haskins' dam at Morton was enlarged and a new dam was built at Upper Brewers. Those two dams (managed today by Parks Canada) created Whitefish Lake, Little Cranberry Lake and much expanded Cranberry and Dog lakes. Most of the flow from what was previously the White Fish River watershed now flows down the Cataraqui River. The Cataraqui Region Conservation Authority administers water management concerns within the Cataraqui River watershed.

Cathcart Tower
Cathcart Tower

Cathcart Tower is a Martello tower located on Cedar Island in the St. Lawrence River, off the eastern shore of Fort Henry in Kingston, Ontario, Canada. It is one of four such towers built in the 1840s to protect Kingston's harbour and the entrance to the Rideau Canal. The other towers are: Fort Frederick, Shoal Tower, and Murney Tower. Alexander Mackenzie was a foreman on the construction of the Carthcart Tower and later went on to become Canada's second prime minister 1873–1878. It was his work crew whose boat capsized while returning from Cedar Island, drowning 17 men. Hamilton Cove was subsequently renamed Deadman's Bay. Built in 1848, this limestone tower is 11 m high and 16.5 m in diameter. It is surrounded by a shallow ditch and by a glacis extending to the shorelines on three sides. The guns of Cathcart Tower covered the eastern approaches of Kingston Harbour. The towers' construction was prompted by a dispute between Great Britain and the United States over the boundary between British Columbia and Oregon that threatened to lead to war (see Oregon crisis). When war was averted, Cathcart Tower was used for a time as a barracks for soldiers garrisoned at nearby Fort Henry. Eventually it was abandoned. The tower is now part of the Rideau Canal and Kingston Fortifications National Historic Site, the Rideau Canal and Kingston Fortifications UNESCO World Heritage Site, and is within the boundaries of Thousand Islands National Park (formerly St. Lawrence Islands National Park).The tower is reached by small water craft with a dock located on the north side of Cedar Island.