Mitchell Lake | |
---|---|
Location | Kawartha Lakes, Ontario |
Coordinates | 44°34′26″N78°57′01″W / 44.57389°N 78.95028°W [1] Coordinates: 44°34′26″N78°57′01″W / 44.57389°N 78.95028°W [1] |
Type | Lake |
Part of | Great Lakes Basin |
Primary inflows | Trent–Severn Waterway, Grass Creek |
Primary outflows | Trent–Severn Waterway, Grass Creek |
Basin countries | Canada |
Max. length | 3.3 kilometres (2.1 mi) |
Max. width | 2.2 kilometres (1.4 mi) |
Surface elevation | 256 metres (840 ft) |
Mitchell Lake is a small, artificial lake in the Great Lakes Basin and located in the city of Kawartha Lakes in Central Ontario, Canada. [1] [2] [3] [4] The lake was formed sometime in the first decade of the twentieth century alongside the construction of the Kirkfield Lift Lock, which was completed and operational by the end of 1907. [5] It is part of the summit of the Trent–Severn Waterway, the middle of a connection via canals of Balsam Lake on the Gull River system, which flows eventually to Lake Ontario, and the Kirkfield Lift Lock and Canal Lake on the Talbot River system, which flows to Lake Simcoe and eventually to Lake Huron.
Prior to flooding, the Grass River (now Grass Creek) flowed through the centre of marshland above which the current lake sits in Eldon Township, Victoria County. It entered from the south-west, reaching Fennel Road (Kawartha Lakes Road 35) where it now crosses the Trent Canal. From here it turned west and followed the same course as the modern canal to Portage Road (formerly Ontario Highway 48, today Kawartha Lakes Road 48). Passing under the road, it resumed a north-easterly course towards the village of Victoria Road, where it flowed as it continues to today, now controlled by a dam, westward into the Talbot River. [6]
Like many of the lakes of the Kawarthas, Mitchell Lake enjoys use by recreational cottagers. However, most of the lake is relatively shallow (Between 3 and 6 feet deep), swampy, and filled with partially or wholly submerged tree stumps remaining from before the flooding. As such, cottages are sparse outside of the canal zone and south eastern section of the lake. The shallow south-western section of the lake is isolated from the rest by Hartley Road, which crosses the lake by causeway, and is only navigable by canoe.
The former path of the Grass River north of Kawartha Lakes 48 is still visible beneath the shallow and undisturbed waters of the lake. [7]
Mitchell Lake suffers from man-made tides. Essentially reaching high tide for the summer months , and low tide throughout the winter. Each year on thanksgiving weekend the Trent-Severn Waterway is closed, Mitchell lake floodplain drops its water elevation 2ft, and the shoreline recedes up to 20ft. In late May the Trent-Severn Waterway opens up again and the Mitchell Lake floodplain raises its water elevation 2ft, and the shoreline expands up to 20ft. Since this floodplain used to be a forest, decaying underwater biomass raises small islands and releases dissolved methane gas into the water, acidifying the water. The southern portion exposes the ancient tree stumps during low tide. Mitchell Lake floodplain has been completely overrun by invasive Eurasian Milfoil weed (Myriophyllum spicatum). It has decimated the oxygen and natural flora of the water, and begun spreading to other lakes on the Trent-Severn Waterway via boat travel.
The Trent–Severn Waterway is a 386-kilometre-long (240 mi) canal route connecting Lake Ontario at Trenton to Georgian Bay, Lake Huron, at Port Severn. Its major natural waterways include the Trent River, Otonabee River, Kawartha Lakes, Lake Simcoe, Lake Couchiching and Severn River. Its scenic, meandering route has been called "one of the finest interconnected systems of navigation in the world".
Coboconk, often shortened to Coby, is a community in the city of Kawartha Lakes, in the south-central portion of the Canadian province of Ontario. The village lies at the junction of Highway 35 and former Highway 48, on the northern tip of Balsam Lake, the highest point on the Trent–Severn Waterway. Coboconk has a prominent role in the logging, limestone, and tourism industries of the Kawartha Lakes region over the past 150 years.
The City of Kawartha Lakes is a unitary municipality in Central Ontario, Canada. It is a municipality legally structured as a single-tier city; however, Kawartha Lakes is the size of a typical Ontario county and is mostly rural. It is the second largest single-tier municipality in Ontario by land area.
The Otonabee River is a river in Peterborough County in Central Ontario, Canada. The river flows from Katchewanooka Lake, at the north end of the community of Lakefield, through the city of Peterborough to Rice Lake. It is in the Great Lakes Basin and forms part of the Trent-Severn Waterway.
Lake Scugog is an artificially flooded lake in Scugog, Regional Municipality of Durham and the unitary city of Kawartha Lakes in central Ontario, Canada. It lies between the communities of Port Perry and Lindsay. The lake has been raised and lowered several times over its history. Though not technically part of the Kawartha lakes due to its shallow depths, it is often geographically linked to them. Its sole outflow, the Scugog River, connects to Sturgeon Lake. Lake Scugog is in the Great Lakes Basin and forms part of the Trent–Severn Waterway.
The Scugog River is a river in the city of Kawartha Lakes in Central Ontario, Canada. It is in the Kawartha Lakes region, is part of the Great Lakes Basin, and is a branch of the Trent-Severn Waterway.
The Talbot River is a river in the Great Lakes Basin in Central Ontario, Canada which flows from Talbot Lake to Lake Simcoe and forms the border between Ramara township to the north and the Brock township to the south from the river mouth to the edge of their border with the city of Kawartha Lakes at the east.
The Kawartha Lakes (/kə'wɔrθɐ/) are a chain of lakes in south-central Ontario, Canada that form the upper watershed of the Trent River. The lakes are located on the boundary between the Paleozoic limestone regions of the Golden Horseshoe, and the Precambrian granite Canadian Shield of northern and central Ontario.
Balsam Lake is a lake in the City of Kawartha Lakes in Central Ontario, Canada. It is in the Great Lakes Basin, is one of the lakes of the Kawartha Lakes, and is at the summit of the Trent–Severn Waterway.
The Peterborough Lift Lock is a boat lift located on the Trent Canal in the city of Peterborough, Ontario, Canada, and is Lock 21 on the Trent-Severn Waterway.
Jack Lake is a lake and reservoir in the municipalities of Havelock-Belmont-Methuen and North Kawartha, Peterborough County in Central Ontario, Canada, about 100 mi (160 km) directly northeast of Toronto and at the edge of the Canadian Shield in the northeastern portion of the Kawartha lakes region. The lake is in the Great Lakes Basin, and serves as a small headwater pond for the Trent-Severn Waterway. The Dispersed rural community of Jack Lake is on the northwest shore of the lake, reached by Peterborough County Road 52 / Jack Lake Road from the community of Apsley, about 5 kilometres (3.1 mi) to the north on Ontario Highway 28.
Kirkfield is a village located in the city of Kawartha Lakes, in the Canadian province of Ontario. The unincorporated village was named in 1864 after the initial name, Novar, was rejected by the government. A list of 8 possible choices was then offered. The village, being predominantly Scottish at the time, chose Kirkfield, after Kirk' o' Field in Edinburgh. It is home to Lock 36 of the Trent-Severn Waterway, a hydraulic lift lock which connects Canal Lake and the artificially flooded Mitchell Lake. Travellers and commuters pass through Kirkfield regularly while travelling on Highway 48 west towards Highway 12 and east towards Highway 35.
The Kirkfield Lift Lock is a boat lift located in the city of Kawartha Lakes, Ontario, Canada, near the village of Kirkfield. It is designated "Lock 36" of the Trent–Severn Waterway, situated at the highest section of the canal. It is Canada's second lift lock, the other one is the Peterborough Lift Lock, located on the same canal system.
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.
Silver Lake is a small lake in the city of Kawartha Lakes in Central Ontario, Canada. Located near the community of Coboconk, it is the lowest lake on the Gull River, a drainage basin that supplies water at its mouth to Balsam Lake at the top of the Trent-Severn Waterway. Like many other lakes in the Kawarthas, Silver Lake lies in a depression formed between the Precambrian granite to the north, and the Ordovician limestone to the south.
St. Mary's was the site of a planned village within early Victoria County, in the Canadian province of Ontario. The site was laid aside in the surveying of the county in the 1830s, but was later found to be unusable when limestone was discovered two inches below the ground. Today its site marks one end of a man-made canal between Balsam Lake and Lake Simcoe, part of the Trent-Severn Waterway.
Burleigh Falls is both a geological feature and a small community in Peterborough County, Ontario, Canada. The falls form the boundary between the municipality of North Kawartha to the north and the municipality of Selwyn to the south.
Canal Lake is a lake of Ontario, Canada, situated in the City of Kawartha Lakes. The lake is triangular, roughly 8.4 kilometres (5.2 mi) long and 2.6 kilometres (1.6 mi) at its widest point, with an area of 2,136 acres (864 ha). The depth ranges from 4.44 feet (1.35 m) to a max depth of 15 feet (4.6 m). Canal Lake is a medium size lake with a large diversity of fishing spots.
Little Lake is a small lake on the Otonabee River in the city of Peterborough, Ontario, Canada. The lake is in the downtown of the city and is used for fishing, swimming, boating, and for various special events. The lake lies on the water route from Lake Ontario to the Kawartha Lakes. The area around the lake was first settled by Europeans around the start of the 19th century. Steam- and water-powered saw mills were built on the lake and on the river upstream to prepare lumber for shipment overseas. Sawdust and other debris from the mills polluted the lake, killed the fish and clogged up the navigable channels. The smell was so noxious it drove residents near the lake to move. These problems were resolved by the end of the century, when the lake became a hub on the new Trent-Severn Waterway from Lake Ontario to Lake Huron. However, industries attracted by cheap hydroelectric power, such as General Electric used the lake for disposal of industrial chemicals for many years. The pollutants seems to be mostly contained in the sediment, and the lake is now considered safe for recreational use.
The Rosedale River is a river in the City of Kawartha Lakes in Central Ontario, Canada. It is in the Great Lakes Basin and is part of the Trent–Severn Waterway. The river is named after Rosa Dale, the wife of settler John Cameron, who first settled the area of nearby Fenelon Falls.