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Strange, Ontario
Strange is an unincorporated community west of King City in King Township, Ontario, Canada. It is directly north of Laskay to the west of Highway 400, and is a sparsely populated agricultural area. Strange was founded as ''Williamstown'' in 1841, founded by William Wells who opened a general store. He abandoned his plans to expand the community into a town in 1853 when the Toronto, Simcoe & Lake Huron railway was built through the community of Springhill (now King City) instead of Williamstown. In 1854, the community's first post office closed, but another opened on 1 March 1880 through the efforts of Frederick William Strange, for whom the post office and the community were renamed. Today, only a few residential buildings remain, and only the Presbyterian Church and two graveyards provide links to its past. Geology The Strange Till Plain is a flat ground moraine with underlying glacial till. It was formed by the Ontario ice lobe during the Port Huron Stadial. It is believed ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Country
A country is a distinct part of the world, such as a state, nation, or other political entity. It may be a sovereign state or make up one part of a larger state. For example, the country of Japan is an independent, sovereign state, while the country of Wales is a component of a multi-part sovereign state, the United Kingdom. A country may be a historically sovereign area (such as Korea), a currently sovereign territory with a unified government (such as Senegal), or a non-sovereign geographic region associated with certain distinct political, ethnic, or cultural characteristics (such as the Basque Country). The definition and usage of the word "country" is flexible and has changed over time. ''The Economist'' wrote in 2010 that "any attempt to find a clear definition of a country soon runs into a thicket of exceptions and anomalies." Most sovereign states, but not all countries, are members of the United Nations. The largest country by area is Russia, while the smallest is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Area Codes 905 And 289
Area codes 905, 289, 365, and 742 are telephone area codes in the North American Numbering Plan (NANP) for the Golden Horseshoe region that surrounds Lake Ontario in Southern Ontario, Canada. The numbering plan area (NPA) comprises (clockwise) the Niagara Peninsula, the city of Hamilton, the regional municipalities of Halton, Peel, York, Durham, and parts of Northumberland County, but excludes the City of Toronto. The area codes form an overlay plan for the same geographic region, where area code 905 was established in October 1993 in an area code split from area code 416. When 289 was overlaid on June 9, 2001, all local calls required ten-digit dialing. On April 13, 2010, the Canadian Radio-television and Telecommunications Commission (CRTC) introduced another overlay code, area code 365, which became operational on March 25, 2013. The numbering plan area surrounds the city of Toronto (area codes 416/647/437), leading locals to refer to the primarily suburban cities surrou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sediment
Sediment is a naturally occurring material that is broken down by processes of weathering and erosion, and is subsequently transported by the action of wind, water, or ice or by the force of gravity acting on the particles. For example, sand and silt can be carried in suspension in river water and on reaching the sea bed deposited by sedimentation; if buried, they may eventually become sandstone and siltstone (sedimentary rocks) through lithification. Sediments are most often transported by water (fluvial processes), but also wind (aeolian processes) and glaciers. Beach sands and river channel deposits are examples of fluvial transport and deposition, though sediment also often settles out of slow-moving or standing water in lakes and oceans. Desert sand dunes and loess are examples of aeolian transport and deposition. Glacial moraine deposits and till are ice-transported sediments. Classification Sediment can be classified based on its grain size, grain shape, and c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Erosion
Erosion is the action of surface processes (such as water flow or wind) that removes soil, rock, or dissolved material from one location on the Earth's crust, and then transports it to another location where it is deposited. Erosion is distinct from weathering which involves no movement. Removal of rock or soil as clastic sediment is referred to as ''physical'' or ''mechanical'' erosion; this contrasts with ''chemical'' erosion, where soil or rock material is removed from an area by dissolution. Eroded sediment or solutes may be transported just a few millimetres, or for thousands of kilometres. Agents of erosion include rainfall; bedrock wear in rivers; coastal erosion by the sea and waves; glacial plucking, abrasion, and scour; areal flooding; wind abrasion; groundwater processes; and mass movement processes in steep landscapes like landslides and debris flows. The rates at which such processes act control how fast a surface is eroded. Typically, physical erosion procee ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Till
image:Geschiebemergel.JPG, Closeup of glacial till. Note that the larger grains (pebbles and gravel) in the till are completely surrounded by the matrix of finer material (silt and sand), and this characteristic, known as ''matrix support'', is diagnostic of till. image:Glacial till exposed in roadcut-750px.jpg, Glacial till with tufts of grass Till or glacial till is unsorted glacier, glacial sediment. Till is derived from the erosion and entrainment of material by the moving ice of a glacier. It is deposited some distance down-ice to form terminal, lateral, medial and ground moraines. Till is classified into primary deposits, laid down directly by glaciers, and secondary deposits, reworked by fluvial transport and other processes. Description Till is a form of '' glacial drift'', which is rock material transported by a glacier and deposited directly from the ice or from running water emerging from the ice. It is distinguished from other forms of drift in that it is depos ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacier
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its Ablation#Glaciology, ablation over many years, often Century, centuries. It acquires distinguishing features, such as Crevasse, crevasses and Serac, seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between lati ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moraine
A moraine is any accumulation of unconsolidated debris (regolith and rock), sometimes referred to as glacial till, that occurs in both currently and formerly glaciated regions, and that has been previously carried along by a glacier or ice sheet. It may consist of partly rounded particles ranging in size from boulders (in which case it is often referred to as boulder clay) down to gravel and sand, in a groundmass of finely-divided clayey material sometimes called glacial flour. Lateral moraines are those formed at the side of the ice flow, and terminal moraines were formed at the foot, marking the maximum advance of the glacier. Other types of moraine include ground moraines (till-covered areas forming sheets on flat or irregular topography) and medial moraines (moraines formed where two glaciers meet). Etymology The word ''moraine'' is borrowed from French , which in turn is derived from the Savoyard Italian ("mound of earth"). ''Morena'' in this case was derived from ProvenĂ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Frederick William Strange
Frederick William Strange (September 9, 1844 – June 5, 1897) was an English-born physician, surgeon and political figure in Ontario, Canada. He represented York North in the House of Commons of Canada from 1878 to 1882 as a Liberal-Conservative member. He was the son of Thomas Strange of Berkshire and studied medicine at Liverpool and University College in London. Strange came to Ontario in 1869. A long-time militia medical officer, he served as a deputy surgeon general for the Canadian militia from 1893 to 1896 and was coroner for York County. Strange was an unsuccessful candidate for a seat in the House of Commons in 1896. He died a year later at the age of 52. The community of Strange Strange may refer to: Fiction * Strange (comic book), a comic book limited series by Marvel Comics * Strange (Marvel Comics), one of a pair of Marvel Comics characters known as The Strangers * Adam Strange, a DC Comics superhero * The title char ... was named in his honour after he secur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northern Railway Of Canada
The Northern Railway of Canada was a railway in the province of Ontario, Canada. It was the first steam railway to enter service in what was then known as Upper Canada. It was eventually acquired by the Grand Trunk Railway, and is therefore a predecessor to the modern Canadian National Railway (CNR). Several sections of the line are still used by CNR and GO Transit. First known as the Toronto, Simcoe and Huron Railway, and then the Ontario, Simcoe and Huron Railway, the aim was to provide a portage route from the upper Great Lakes at Collingwood to Toronto. The plan for the railway was largely executed by Frederick Chase Capreol who was fired as manager of the company the day before the ground broke. Financial difficulties and a government bailout led to a reorganization of the company as the Northern Railway of Canada in 1859. The line saw three major expansions; North Grey Railway extended the original mainline to Meaford, the North Simcoe Railway ran to the port town of Pe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ontario Highway 400
King's Highway 400, commonly referred to as Highway400, historically as the Toronto–Barrie Highway, and colloquially as the400, is a 400-series highway The 400-series highways are a network of controlled-access highways throughout the southern portion of the Canadian province of Ontario, forming a special subset of the provincial highway system. They are analogous to the Interstate Highway ... in the Provinces and territories of Canada, Canadian province of Ontario linking the city of Toronto in the Southern Ontario, urban and agricultural south of the province with the scenic and sparsely populated Central Ontario, central and Northern Ontario, northern regions. The portion of the highway between Toronto and Lake Simcoe roughly traces the route of the Toronto Carrying-Place Trail, a historic trail between the Lower and Upper Great Lakes. North of Ontario Highway 12, Highway 12, in combination with Ontario Highway 69, Highway 69, it forms a branch of the Trans-Canada ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Laskay, Ontario
Laskay is an unincorporated rural community in King Township, York Regional Municipality, Ontario, Canada. It is west of King City and Highway 400, and south of the King Road—Weston Road intersection. The settlement was named by Joseph Baldwin, and was named after his hometown Loskie in Yorkshire, England. The community has also been known as "Bulltown", a nickname it acquired after a fall fair in which a bull broke loose from its enclosure and charged the patrons. Several of the original buildings in the community have been moved to other locations. The Laskay Emporium, built in 1856, was moved to Black Creek Pioneer Village Black Creek Pioneer Village, previously Dalziel Pioneer Park, is an open-air heritage museum in Toronto, Ontario, Canada. The village is located in the North York district of Toronto, just west of York University and southeast of the Jane and ... on 19 February 1960. In August 2017, Laskay Hall was moved from its original site to the grounds of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
King City, Ontario
King City is an unincorporated Canadian community in the township of King, Ontario, located north of Toronto. It is the largest community in King township, with 2,730 dwellings and a population of 8,396 as of the 2021 Canadian census. History In 1836, a settlement styled ''Springhill'' was established in King. With the arrival of the Ontario, Simcoe and Huron railway in 1853, the settlement began to expand. In 1890, the reeve of King township (James Whiting Crossley) incorporated King City by merging the hamlets of Springhill, Kinghorn, Laskay, and Eversley. Geography King City is characterized by rolling hills and clustered temperate forests in the Eastern Great Lakes lowland forests ecoregion. Numerous kettle lakes and ponds dot the area. Creeks and streams from King City, the surrounding area, and as far west as Bolton and as far east as Stouffville are the origin for the East Humber River. Situated entirely on the southern slope of the central portion of the Oak Ridges ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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