Beaver Valley (Ontario)
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Beaver Valley (Ontario)
The Beaver Valley is a valley in southern Ontario, Canada, at the southern tip of Georgian Bay. The Beaver River flows north through the valley, emptying into Georgian Bay in the town of Thornbury. It is a productive agricultural area, producing a significant portion of Canada's apple crop. It also contains one of Ontario's best-preserved hardwood swamp ecosystems. The Bruce Trail follows the perimeter of the valley passing several natural landmarks including Old Baldy, the Duncan Crevice Caves, and Eugenia Falls. The main towns in the valley are Flesherton at the south end, Kimberley, and Thornbury. Geology The Beaver Valley formed over a period of many thousands of years as the Beaver River cut into the Niagara Escarpment. Today, the river continues to cut southward into the bedrock at Eugenia Falls. Gradual erosive processes have created a wedge-shaped valley with a width ranging from 30 meters (90 feet) at the south end to 13 kilometers (8 miles) at the north end. Ecolo ...
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Canada
Canada is a country in North America. Its ten provinces and three territories extend from the Atlantic Ocean to the Pacific Ocean and northward into the Arctic Ocean, covering over , making it the world's second-largest country by total area. Its southern and western border with the United States, stretching , is the world's longest binational land border. Canada's capital is Ottawa, and its three largest metropolitan areas are Toronto, Montreal, and Vancouver. Indigenous peoples have continuously inhabited what is now Canada for thousands of years. Beginning in the 16th century, British and French expeditions explored and later settled along the Atlantic coast. As a consequence of various armed conflicts, France ceded nearly all of its colonies in North America in 1763. In 1867, with the union of three British North American colonies through Confederation, Canada was formed as a federal dominion of four provinces. This began an accretion of provinces an ...
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Flesherton, Ontario
Flesherton (population 584) is a community in the Municipality of Grey Highlands, in Grey County, Ontario, Canada, located at the junction of Highway 10 and Grey County Road 4 (formerly Highway 4). Although the area initially showed a high rate of growth in the 1850s and its founder believed that it would become an important centre of economic activity, growth stagnated when an all-important rail link bypassed it, and the community never grew larger than a small village. The self-proclaimed "Gateway to the Beaver Valley" recently lost its autonomy as a village when it was amalgamated with the surrounding Artemesia Township. History Prehistory A paleolithic quartzite arrowhead that had been quarried north of the Great Lakes was discovered near Flesherton in 1974. Whether it was carried south to the Flesherton area around the east side of Georgian Bay, or dates back to a time when a land bridge existed between the Bruce Peninsula and Manitoulin Island, the arrowhead does point ...
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River Valleys Of Canada
A river is a natural flowing watercourse, usually freshwater, flowing towards an ocean, sea, lake or another river. In some cases, a river flows into the ground and becomes dry at the end of its course without reaching another body of water. Small rivers can be referred to using names such as creek, brook, rivulet, and rill. There are no official definitions for the generic term river as applied to geographic features, although in some countries or communities a stream is defined by its size. Many names for small rivers are specific to geographic location; examples are "run" in some parts of the United States, "burn" in Scotland and northeast England, and "beck" in northern England. Sometimes a river is defined as being larger than a creek, but not always: the language is vague. Rivers are part of the water cycle. Water generally collects in a river from precipitation through a drainage basin from surface runoff and other sources such as groundwater recharge, springs, a ...
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Beaver Valley Ski Club
Beaver Valley Ski Club is a private skiing and snowboarding club located in Beaver Valley, Ontario, Canada. It is situated on a steep sided section of the Niagara Escarpment adjacent to the Bruce Trail. It features some of the steepest runs and most diverse terrain in the region. The Club has 28 trails, five snowparks including a championship snowboard/ski cross course, national level mogul and slopestyle runs, glade skiing and a steep, groomed ski bowl. Its Playground snow park is one of the longest full featured snow park runs in Ontario. The Club has six lifts, two lodges and a ski and snowboard shop with rentals. The Club hosts various national and international series snowboard and freestyle ski events: annual Beaver Valley Banked Slalom (part of the World Snowboard Banked Slalom Tour), annual Mogulmania (ski and snowboard), Beaver Valley Park Brawl (snowboard park), 2016 Canadian Junior Freestyle Ski Championship featuring slopestyle, moguls, big air and aerials events, 20 ...
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Asplenium Scolopendrium
''Asplenium scolopendrium'', commonly known as the hart's-tongue fern, is an evergreen fern in the genus ''Asplenium'' native to the Northern Hemisphere. Description The most striking and unusual feature of the fern is its simple, undivided fronds. The leaves' supposed resemblance to the tongue of a hart (an archaic term for a male red deer) gave rise to the common name "hart's-tongue fern". Taxonomy Linnaeus first gave the hart's-tongue fern the binomial ''Asplenium scolopendrium'' in his '' Species Plantarum'' of 1753. The Latin specific epithet ''scolopendrium'' is derived from the Greek ''skolopendra'', meaning a centipede or millipede; this is due to the sori pattern being reminiscent of a myriapod's legs. A global phylogeny of ''Asplenium'' published in 2020 divided the genus into eleven clades, which were given informal names pending further taxonomic study. ''A. scolopendrium'' belongs to the "''Phyllitis'' subclade" of the "''Phyllitis'' clade". Members of the ''Phyll ...
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Species
In biology, a species is the basic unit of classification and a taxonomic rank of an organism, as well as a unit of biodiversity. A species is often defined as the largest group of organisms in which any two individuals of the appropriate sexes or mating types can produce fertile offspring, typically by sexual reproduction. Other ways of defining species include their karyotype, DNA sequence, morphology, behaviour or ecological niche. In addition, paleontologists use the concept of the chronospecies since fossil reproduction cannot be examined. The most recent rigorous estimate for the total number of species of eukaryotes is between 8 and 8.7 million. However, only about 14% of these had been described by 2011. All species (except viruses) are given a two-part name, a "binomial". The first part of a binomial is the genus to which the species belongs. The second part is called the specific name or the specific epithet (in botanical nomenclature, also sometimes i ...
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Habitat
In ecology, the term habitat summarises the array of resources, physical and biotic factors that are present in an area, such as to support the survival and reproduction of a particular species. A species habitat can be seen as the physical manifestation of its ecological niche. Thus "habitat" is a species-specific term, fundamentally different from concepts such as environment or vegetation assemblages, for which the term "habitat-type" is more appropriate. The physical factors may include (for example): soil, moisture, range of temperature, and light intensity. Biotic factors will include the availability of food and the presence or absence of predators. Every species has particular habitat requirements, with habitat generalist species able to thrive in a wide array of environmental conditions while habitat specialist species requiring a very limited set of factors to survive. The habitat of a species is not necessarily found in a geographical area, it can be the interior ...
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Tillage
Tillage is the agricultural preparation of soil by mechanical agitation of various types, such as digging, stirring, and overturning. Examples of human-powered tilling methods using hand tools include shoveling, picking, mattock work, hoeing, and raking. Examples of draft-animal-powered or mechanized work include ploughing (overturning with moldboards or chiseling with chisel shanks), rototilling, rolling with cultipackers or other rollers, harrowing, and cultivating with cultivator shanks (teeth). Tillage that is deeper and more thorough is classified as primary, and tillage that is shallower and sometimes more selective of location is secondary. Primary tillage such as ploughing tends to produce a rough surface finish, whereas secondary tillage tends to produce a smoother surface finish, such as that required to make a good seedbed for many crops. Harrowing and rototilling often combine primary and secondary tillage into one operation. "Tillage" can also mean the lan ...
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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 ...
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Bedrock
In geology, bedrock is solid Rock (geology), rock that lies under loose material (regolith) within the crust (geology), crust of Earth or another terrestrial planet. Definition Bedrock is the solid rock that underlies looser surface material. An exposed portion of bedrock is often called an outcrop. The various kinds of broken and weathered rock material, such as soil and subsoil, that may overlie the bedrock are known as regolith. Engineering geology The surface of the bedrock beneath the soil cover (regolith) is also known as ''rockhead'' in engineering geology, and its identification by digging, drilling or geophysics, geophysical methods is an important task in most civil engineering projects. Superficial deposition (geology), deposits can be very thick, such that the bedrock lies hundreds of meters below the surface. Weathering of bedrock Exposed bedrock experiences weathering, which may be physical or chemical, and which alters the structure of the rock to leave ...
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