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Forks Of The Credit Provincial Park
Forks of the Credit Provincial Park, located in Caledon, Ontario, Canada, is part of the Ontario Parks system and is part of the Niagara Escarpment biosphere. The park is on the Bruce Trail. The Credit River runs through the park. Other notable features of the park include a kettle lake and talus slope. History In 1968 the Niagara Escarpment Study recommended that a park be established in the Forks of the Credit area; this recommendation was then accepted by the Government of Ontario. It was officially regulated as a provincial park in 1985. Historic mill and dam There has been a mill in the area since 1820. In 1885, John Deagle bought the mill at the top of the falls and converted it into an electrical generating station, damming the river and creating Cataract Lake; he named the enterprise The Cataract Electric Co. Ltd. Later the station was purchased by Ontario Hydro and was eventually shut down in 1947. The dam was later destroyed and the lake drained. The ruins of the mill ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ontario
Ontario ( ; ) is one of the thirteen provinces and territories of Canada.Ontario is located in the geographic eastern half of Canada, but it has historically and politically been considered to be part of Central Canada. Located in Central Canada, it is Canada's most populous province, with 38.3 percent of the country's population, and is the second-largest province by total area (after Quebec). Ontario is Canada's fourth-largest jurisdiction in total area when the territories of the Northwest Territories and Nunavut are included. It is home to the nation's capital city, Ottawa, and the nation's most populous city, Toronto, which is Ontario's provincial capital. Ontario is bordered by the province of Manitoba to the west, Hudson Bay and James Bay to the north, and Quebec to the east and northeast, and to the south by the U.S. states of (from west to east) Minnesota, Michigan, Ohio, Pennsylvania, and New York. Almost all of Ontario's border with the United States f ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Caledon, Ontario
Caledon (; Canada 2021 Census, 2021 population 76,581) is a town in the Regional Municipality of Peel in the Greater Toronto Area of Ontario, Canada. From a shortened form of Caledonia, the Roman name for North Britain; Caledon is a developing urban area, although it remains primarily rural. It consists of an amalgamation of a number of urban areas, villages, and hamlets; its major urban centre is Bolton, Ontario, Bolton on its eastern side adjacent to York Region. Caledon is one of three municipalities of Regional Municipality of Peel, Peel Region. The town is at the northwest border of the city of Brampton. At over , Caledon is the largest municipality, by area, in the Greater Toronto Area. History By 1869, Belfountain was a Village with a population of 100 in the Township of Caledon County Peel. It was established on the Credit River. There were stagecoaches to Erin, Ontario, Erin and Georgetown, Ontario, Georgetown. The average price of land was $20. In 1973, Caledon acquir ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ontario Parks
Ontario Parks is a branch of the Ministry of the Environment, Conservation and Parks in Ontario, Canada, that protects significant natural and cultural resources in a system of parks and protected areas that is sustainable and provides opportunities for inspiration, enjoyment and education. The Ontario Parks system covers over , which is about 10 per cent of the province's surface area or the equivalent of an area approximately equal to Nova Scotia. It falls under the responsibility and mandate of the province's Ministry of the Environment, Conservation and Parks. It was formerly under the mandate of the Ministry of Natural Resources and Forestry. The Ontario Parks system has been used as a model for other parks systems in North America. This can be attributed to its delicate balance of recreation, preservation and conservation. Many parks in Ontario also offer a Natural Heritage Education program. History The Ontario Parks system began its long and rough history in 1893 with ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Niagara Escarpment
The Niagara Escarpment is a long escarpment, or cuesta, in Canada and the United States that runs predominantly east–west from New York through Ontario, Michigan, Wisconsin, and into Illinois. The escarpment is most famous as the cliff over which the Niagara River plunges at Niagara Falls, for which it is named. The escarpment is a UNESCO World Biosphere Reserve. The reserve has the oldest forest ecosystem and trees in eastern North America. The escarpment is not a fault line but the result of unequal erosion. It is composed of an outcrop belt of the Lockport Formation of Silurian age, and is similar to the Onondaga Formation, which runs in a parallel outcrop belt just to the south, through western New York and southern Ontario. The escarpment is the most prominent of several escarpments formed in the bedrock of the Great Lakes Basin. From its easternmost point near Watertown, New York, the escarpment shapes in part the individual basins and landforms of Lake Ontario, Lak ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Biosphere
The biosphere (from Greek βίος ''bíos'' "life" and σφαῖρα ''sphaira'' "sphere"), also known as the ecosphere (from Greek οἶκος ''oîkos'' "environment" and σφαῖρα), is the worldwide sum of all ecosystems. It can also be termed the zone of life on Earth. The biosphere (which is technically a spherical shell) is virtually a closed system with regard to matter, with minimal inputs and outputs. With regard to energy, it is an open system, with photosynthesis capturing solar energy at a rate of around 130 terawatts per year. However it is a self-regulating system close to energetic equilibrium."Biosphere" in ''The Columbia Encyclopedia'', 6th ed. (2004) Columbia University Press. By the most general [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bruce Trail
The Bruce Trail is a hiking trail in southern Ontario, Canada, from the Niagara River to the tip of Tobermory, Ontario. The main trail is more than long and there are over of associated side trails. The trail mostly follows the edge of the Niagara Escarpment, one of the nineteen UNESCO World Biosphere Reserves in Canada. The land the trail traverses is owned by the Government of Ontario, local municipalities, local conservation authorities, private landowners, and the Bruce Trail Conservancy (BTC). The Bruce Trail is the oldest and longest marked hiking trail in Canada. Its name is linked to the Bruce Peninsula and Bruce County, through which the trail runs. The trail is named after the county, which was named after James Bruce, 8th Earl of Elgin who was Governor General of the Province of Canada from 1847 to 1854. History The idea for creating the Bruce Trail came about in 1959 out of a meeting between Ray Lowes and Robert Bateman, of the Federation of Ontario Naturalists. Ra ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Credit River
The Credit River is a river in southern Ontario, which flows from headwaters above the Niagara Escarpment near Orangeville and Caledon East to empty into Lake Ontario at Port Credit, Mississauga. It drains an area of approximately . The total length of the river and its tributary streams is over . Despite urbanization and associated problems with water quality on the lower section of this river, it provides spawning areas for Chinook salmon and rainbow trout. There is a fish ladder on the river at Streetsville. Much of the river can still be travelled by canoe or kayak. The headwaters of the Credit River is home to a native self-sustaining brook trout population and an introduced brown trout population. Credit Valley Conservation, the local watershed management conservation authority, operates several Conservation Areas including Belfountain, Island Lake, and Terra Cotta. Forks of the Credit Provincial Park is located on the upper part of the river between Brampton and Orang ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kettle Lake
A kettle (also known as a kettle lake, kettle hole, or pothole) is a depression/hole in an outwash plain formed by retreating glaciers or draining floodwaters. The kettles are formed as a result of blocks of dead ice left behind by retreating glaciers, which become surrounded by sediment deposited by meltwater streams as there is increased friction. The ice becomes buried in the sediment and when the ice melts, a depression is left called a kettle hole, creating a dimpled appearance on the outwash plain. Lakes often fill these kettles; these are called kettle hole lakes. Another source is the sudden drainage of an ice-dammed lake. When the block melts, the hole it leaves behind is a kettle. As the ice melts, ramparts can form around the edge of the kettle hole. The lakes that fill these holes are seldom more than deep and eventually fill with sediment. In acid conditions, a kettle bog may form but in alkaline conditions, it will be kettle peatland. Overview Kettles are fluviog ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Talus Slope
Scree is a collection of broken rock fragments at the base of a cliff or other steep rocky mass that has accumulated through periodic rockfall. Landforms associated with these materials are often called talus deposits. Talus deposits typically have a concave upwards form, where the maximum inclination corresponds to the angle of repose of the mean debris particle size. The exact definition of scree in the primary literature is somewhat relaxed, and it often overlaps with both ''talus'' and ''colluvium''. The term ''scree'' comes from the Old Norse term for landslide, ''skriða'', while the term ''talus'' is a French word meaning a slope or embankment. In high-altitude arctic and subarctic regions, scree slopes and talus deposits are typically adjacent to hills and river valleys. These steep slopes usually originate from late-Pleistocene periglacial processes. Notable scree sites in Eastern North America include the Ice Caves at White Rocks National Recreation Area in southern V ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Government Of Ontario
The government of Ontario (french: Gouvernement de l'Ontario) is the body responsible for the administration of the Canadian province of Ontario. A constitutional monarchy, the Crown—represented in the province by the lieutenant governor—is the corporation sole, assuming distinct roles: the executive, as the ''Crown-in-Council''; the legislature, as the ''Crown-in-Parliament''; and the courts, as the ''Crown-on-the-Bench''. The functions of the government are exercised on behalf of three institutions—the Executive Council; the Provincial Parliament (Legislative Assembly); and the judiciary, respectively. Its powers and structure are partly set out in the ''Constitution Act, 1867''. The term ''Government of Ontario'' refers specifically to the executive—political ministers of the Crown (the Cabinet/Executive Council), appointed on the advice of the premier, and the non-partisan Ontario Public Service (whom the Executive Council directs), who staff ministries and age ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ontario Hydro
Ontario Hydro, established in 1906 as the Hydro-Electric Power Commission of Ontario, was a publicly owned electricity utility in the Province of Ontario. It was formed to build transmission lines to supply municipal utilities with electricity generated by private companies already operating at Niagara Falls, and soon developed its own generation resources by buying private generation stations and becoming a major designer and builder of new stations. As most of the readily developed hydroelectric sites became exploited, the corporation expanded into building coal-fired generation and then nuclear-powered facilities. Renamed as "Ontario Hydro" in 1974, by the 1990s it had become one of the largest, fully integrated electricity corporations in North America. Origins The notion of generating electric power on the Niagara River was first entertained in 1888, when the Niagara Parks Commission solicited proposals for the construction of an electric scenic railway from Queenston to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Credit Valley Railway
The Credit Valley Railway was a railway located in Ontario, Canada from Toronto to St. Thomas. Chartered in 1871 by Ontario railway magnate George Laidlaw, it operated as an independent company until 1883 when it was leased by the Ontario and Quebec Railway, a Canadian Pacific Railway (CPR) operating company building a network of lines in southern Ontario. The section from Toronto to Woodstock remains in use as the CPR mainline through Ontario, forming portions of what is now the Galt and Windsor Subdivisions. The section from Woodstock to St. Thomas is operated by OSR as a short line railway. The branch to Orangeville is currently operated as the Orangeville Brampton Railway. The Elora branch was abandoned and converted to rail trail use. History Formation Following initial discussions held in Milton and Brampton in 1870, the Credit Valley Railway was incorporated by Act of the Legislative Assembly of Ontario in 1871, authorized to build a railway line from Toronto to Or ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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