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Silver Lake (Kawartha Lakes)
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. Geography Silver Lake forms a portion of the boundary between the geographic townships of Somerville and Bexley. It is the southernmost lake in a chain of reservoirs feeding the Trent-Severn Waterway at its highest point. The primary inflow is the Gull River arriving at the north from Shadow Lake. There are three unnamed secondary inflows: one at the east, and two at the southwest. The primary outflow, at the southeast, is also the Gull River, which flows to its mouth at Balsam Lake. Balsam Lake flows via the main Kawartha Lakes chain, t ...
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Kawartha Lakes
The City of Kawartha Lakes (2021 population 79,247) 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 (after Greater Sudbury). The main population centres are the communities of Lindsay (population: 22,367), Bobcaygeon (population: 3,576), Fenelon Falls (population: 2,490), Omemee (population: 1,060) and Woodville (population: 718). History The Kawartha Lakes area is situated on the traditional territory of the Anishinaabeg, Huron-Wendat and more recently, the Haudenosaunee peoples. The city's name is from the Kawartha Lakes. ''Kawartha'' is an anglicization of ''Ka-wa-tha'' (from ''Ka-wa-tae-gum-maug'' or ''Gaa-waategamaag''), which was coined in 1895 by Martha Whetung of the Curve Lake First Nations. It meant "land of reflections" in the Anishinaabe ...
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Precambrian
The Precambrian (or Pre-Cambrian, sometimes abbreviated pꞒ, or Cryptozoic) is the earliest part of Earth's history, set before the current Phanerozoic Eon. The Precambrian is so named because it preceded the Cambrian, the first period of the Phanerozoic Eon, which is named after Cambria, the Latinised name for Wales, where rocks from this age were first studied. The Precambrian accounts for 88% of the Earth's geologic time. The Precambrian is an informal unit of geologic time, subdivided into three eons ( Hadean, Archean, Proterozoic) of the geologic time scale. It spans from the formation of Earth about 4.6 billion years ago ( Ga) to the beginning of the Cambrian Period, about million years ago ( Ma), when hard-shelled creatures first appeared in abundance. Overview Relatively little is known about the Precambrian, despite it making up roughly seven-eighths of the Earth's history, and what is known has largely been discovered from the 1960s onwards. The Precambrian fossil ...
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Cuesta
A cuesta (from Spanish ''cuesta'' "slope") is a hill or ridge with a gentle slope on one side, and a steep slope on the other. In geology the term is more specifically applied to a ridge where a harder sedimentary rock overlies a softer layer, the whole being tilted somewhat from the horizontal. This results in a long and gentle backslope called a dip slope that conforms with the dip of resistant strata, called caprock. Where erosion has exposed the frontslope of this, a steep slope or escarpment occurs. The resulting terrain may be called scarpland. Definition In general usage, a cuesta is a hill or ridge with a gentle slope (backslope) on one side, and a steep slope (frontslope) on the other. The word is from Spanish: "flank or slope of a hill; hill, mount, sloping ground". In geology and geomorphology, cuesta refers specifically to an asymmetric ridge with a long and gentle backslope called a dip slope that conforms with the dip of a resistant stratum or strata, called cap ...
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Paleozoic
The Paleozoic (or Palaeozoic) Era is the earliest of three geologic eras of the Phanerozoic Eon. The name ''Paleozoic'' ( ;) was coined by the British geologist Adam Sedgwick in 1838 by combining the Greek words ''palaiós'' (, "old") and ''zōḗ'' (), "life", meaning "ancient life" ). It is the longest of the Phanerozoic eras, lasting from , and is subdivided into six geologic periods (from oldest to youngest): # Cambrian # Ordovician # Silurian # Devonian # Carboniferous # Permian The Paleozoic comes after the Neoproterozoic Era of the Proterozoic Eon and is followed by the Mesozoic Era. The Paleozoic was a time of dramatic geological, climatic, and evolutionary change. The Cambrian witnessed the most rapid and widespread diversification of life in Earth's history, known as the Cambrian explosion, in which most modern phyla first appeared. Arthropods, molluscs, fish, amphibians, reptiles, and synapsids all evolved during the Paleozoic. Life began in the ocean ...
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Canadian Shield
The Canadian Shield (french: Bouclier canadien ), also called the Laurentian Plateau, is a geologic shield, a large area of exposed Precambrian igneous and high-grade metamorphic rocks. It forms the North American Craton (or Laurentia), the ancient geologic core of the North American continent. Glaciation has left the area with only a thin layer of soil, through which exposures of igneous bedrock resulting from its long volcanic history are frequently visible. As a deep, common, joined bedrock region in eastern and central Canada, the Shield stretches north from the Great Lakes to the Arctic Ocean, covering over half of Canada and most of Greenland; it also extends south into the northern reaches of the United States. Geographical extent The Canadian Shield is a physiographic division comprising four smaller physiographic provinces: the Laurentian Upland, Kazan Region, Davis and James. The shield extends into the United States as the Adirondack Mountains (connected by the Fro ...
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Bay Of Quinte
The Bay of Quinte () is a long, narrow bay shaped like the letter "Z" on the northern shore of Lake Ontario in the province of Ontario, Canada. It is just west of the head of the Saint Lawrence River that drains the Great Lakes into the Gulf of Saint Lawrence. It is located about east of Toronto and west of Montreal. The name "Quinte" is derived from "''Kenté''" or Kentio, an Iroquoian village located near the south shore of the Bay. Later on, an early French Catholic mission was built at Kenté, located on the north shore of what is now Prince Edward County, leading to the Bay being named after the Mission. Officially, in the Mohawk language, the community is called "Kenhtè:ke", which means "the place of the bay". The Cayuga name is ''Tayęda:ne:gęˀ or Detgayę:da:negęˀ'', "land of two logs." The Bay, as it is known locally, provides some of the best trophy walleye angling in North America as well as most sport fish common to the great lakes. The bay is subject to al ...
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Trent River (Ontario)
The Trent River is a river in southeastern Ontario which flows from Rice Lake to empty into the Bay of Quinte on Lake Ontario. This river is part of the Trent-Severn Waterway which leads to Georgian Bay. The river is long. The Trent drains a large portion of south-central Ontario, including most of the Kawartha Lakes and their supplying watersheds. The river is host to numerous species of birds, amphibians and fish. Some species of fish in the river include: Smallmouth bass, Largemouth bass, Pike, Walleye, Freshwater drums, Crappie as well as other smaller fish such as Sunfish, Rock Bass and Bluegill. Located in traditional territory of the Mississauga Anishinaabek, Trent River's name in Ojibwe is both "zaagidawijiwanaang", and "Saugechewigewonk", meaning "Strong Rapids Waters". Tributaries of this river include the Crowe River and the Otonabee River, which runs through the city of Peterborough, Ontario. Trent University, located in Peterborough, is named after the region, ...
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Otonabee River
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. Etymology The river is called ''Odoonabii-ziibi'' in the Ojibwe language. Otonabee comes from the words ''ode'' which means "heart" and ''odemgat'' that comes from "boiling water". It translates into "the river that beats like a heart in reference to the bubbling and boiling water of the rapids along the river". Course The river begins at Katchewanooka Lake on the north side of the community of Lakefield in the municipality of Selwyn, and flows south over the Lakefield (Trent-Severn lock 6) dams and locks. After leaving the community to the Peterborough city limits, the river forms the border between Selwyn and the municipality of Douro–Dummer. The river continues south, passing through ...
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Shadow Lake (Kawartha Lakes)
Shadow Lake is a lake in the city of Kawartha Lakes in Central Ontario, Central Ontario, Canada. With an area of and an elevation of , it is the second lake upstream of the mouth of the Gull River (Balsam Lake), Gull River, and is in the Lake Ontario drainage basin. Geography Shadow Lake has an area of and lies at an elevation of . The maximum depth of the lake is . The primary inflow is the Gull River, at the northwest and arriving from the community of Norland, Ontario, Norland, which accounts for 98% of the inflow into the lake. There are three unnamed secondary inflows. The primary outflow, at the south, is also the Gull River, which flows south through two rapids, known locally as "the chute", to Silver Lake.Shadow Lake and Silver Lake Management Plan (2019), p 15. It continues to the mouth of the Gull River at Balsam Lake (Ontario), Balsam Lake, and then via the main Kawartha Lakes (Ontario), Kawartha Lakes chain, the Otonabee River and the Trent River (Ontario), Trent ...
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Bexley Township
The Township of Bexley (Population 1305 c.1996) was a municipality located in the northern half of the former Victoria County, now the city of Kawartha Lakes, in the Canadian province of Ontario. History Bexley's history can be traced back to Indian villages established at the end of the Portage Road, a long historic trail that ended at the site of St. Mary's, on the western shore of Balsam Lake's West Bay. The villages flourished and faded for at least a century prior to the arrival of Samuel de Champlain on his tour with the Hurons. Various tribes used the site up until 1760, when English fur traders established a trading post at the site. Victoria County was opened to settlement in 1821, but Bexley remained unchanged for over a decade due to its northern position within the county, which meant it was surveyed at some point in the early 1830s. The first settler was Admiral Vansittart, who was given a grant of one thousand acres (4 km2) of land on the west shores of Bals ...
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Somerville Township
The Township of Somerville was a municipality located in the north-eastern corner of the former Victoria County, now the city of Kawartha Lakes. Communities * Burnt River *Kinmount * Union Creek * Baddow *Dongola See also *List of townships in Ontario This is a list of townships in the Canadian province of Ontario. Townships are listed by census division. Northern Ontario Northeastern Ontario Algoma District Historical/Geographic Townships *Abbott *Aberdeen Additional *Abigo *Abotossaway * ... Communities in Kawartha Lakes Former township municipalities in Ontario {{Ontario-geo-stub ...
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Township (Canada)
The term township, in Canada, is generally the district or area associated with a town. The specific use of the term to describe political subdivisions has varied by country, usually to describe a local rural or semirural government within the country itself. In Eastern Canada, a township is one form of the subdivision of a county. In Quebec, the term is ''canton'' in French. Maritimes The historic colony of Nova Scotia (present-day Nova Scotia, New Brunswick, and Prince Edward Island) used the term ''township'' as a subdivision of counties and as a means of attracting settlers to the colony. In Prince Edward Island, the colonial survey of 1764 established 67 townships, known as lots, and 3 royalties, which were grouped into parishes and hence into counties; the townships were geographically and politically the same. In New Brunswick, parishes have taken over as the present-day subdivision of counties, and present-day Nova Scotia uses districts as appropriate. Ontario In Ontar ...
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