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La Cloche Mountains
The La Cloche Mountains, also called the La Cloche Range, are a range of mountains in Northern Ontario, Canada, along the northern shore of Lake Huron near Manitoulin Island. The mountains are located in the Canadian Shield, and are composed primarily of white quartzite. They extend roughly from La Cloche Provincial Park, south of Massey, to Killarney Provincial Park, southwest of Sudbury. The communities of West River, Willisville and Whitefish Falls are located directly within the range; the town of Espanola and the municipality of Killarney are located nearby, however they can be seen (from some vantage points) as far away as Manitoulin Island. Ontario Highway 6 is the principal transportation route through the range. Killarney Provincial Park is located in the range and is very popular among tourists. Another feature includes the "Heaven's Gate Trail" which traverses the length of the range from Willisville in the east to Massey in the west. Thought to be an old abo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northern Ontario
Northern Ontario is a primary geographic and quasi-administrative region of the Canadian province of Ontario, the other primary region being Southern Ontario. Most of the core geographic region is located on part of the Superior Geological Province of the Canadian Shield, a vast rocky plateau located mainly north of Lake Huron (including Georgian Bay), the French River, Lake Nipissing, and the Mattawa River. The statistical region extends south of the Mattawa River to include all of the District of Nipissing. The southern section of this district lies on part of the Grenville Geological Province of the Shield which occupies the transitional area between Northern and Southern Ontario. The extended federal and provincial quasi-administrative regions of Northern Ontario have their own boundaries even further south in the transitional area that vary according to their respective government policies and requirements. Ontario government departments and agencies such as the Grow ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quartz
Quartz is a hard, crystalline mineral composed of silica ( silicon dioxide). The atoms are linked in a continuous framework of SiO4 silicon-oxygen tetrahedra, with each oxygen being shared between two tetrahedra, giving an overall chemical formula of SiO2. Quartz is the second most abundant mineral in Earth's continental crust, behind feldspar. Quartz exists in two forms, the normal α-quartz and the high-temperature β-quartz, both of which are chiral. The transformation from α-quartz to β-quartz takes place abruptly at . Since the transformation is accompanied by a significant change in volume, it can easily induce microfracturing of ceramics or rocks passing through this temperature threshold. There are many different varieties of quartz, several of which are classified as gemstones. Since antiquity, varieties of quartz have been the most commonly used minerals in the making of jewelry and hardstone carvings, especially in Eurasia. Quartz is the mineral defini ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Ranges Of Ontario
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited Summit (topography), summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
La Cloche Silhouette Trail
The La Cloche Silhouette Trail is a backpacking (wilderness), backpacking loop across the white quartzite peaks of the La Cloche Mountains, La Cloche mountain range. The trail is situated in Killarney Provincial Park, Ontario, Canada. The trail is named for Group of Seven (artists), Group of Seven painter Franklin Carmichael's painting "La Cloche Silhouette." Wildlife can be seen throughout the trail - black bears, moose, wolverines, mountain lions, lynx, fishers, snakes, porcupines, beavers, river otters, among other animals, can be encountered at various points along the way. The trail itself is divided into five sections, individually listed below. Baie Fine The Baie Fine section runs for 14 kilometres, and is known for its gentle rolling hills, hardwood forests, beaver dams, and pink granite. It begins at the trailhead - a large, informative sign detailing the history of the trail. The forest comprises red and yellow birch, red maple, white pines, and black spruce. The ter ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Charlton Lake Camp
Charlton Lake Camp is a housekeeping cottage resort located in the La Cloche Mountains of northern Ontario, Canada. Dan McGuire and Lisa McGuire are the current owners. History The following is a brief history of Charlton Lake Camp as cited by Peg Forbes in a 1997 document. The first cottage on the site now known as Charlton Lake Camp, was built by Percy Coones (1878-c1978)in 1935 on an acre of land he purchased from the Willis family for $25. The cottage was known as "The Wigisee". When Percy retired from Inco in 1943 he added three more cottages to rent out to fishermen. The fishing was so good, that Percy began building flatbottomed rowboats which were used by vacationers and fishermen in the area for many years. In 1955 Percy built another cabin "up the Howry" and sold the fishing camp to Tom and Liza Kerr. Percy's Howry Creek cottage was later moved to Bill and Norma Starbuck's site on the south shore of Charlton Lake. Percy lived well into his 90s and is still missed by those ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coureur Des Bois
A coureur des bois (; ) or coureur de bois (; plural: coureurs de(s) bois) was an independent entrepreneurial French-Canadian trader who travelled in New France and the interior of North America, usually to trade with First Nations peoples by exchanging various European items for furs. Some learned the trades and practices of the indigenous peoples. These expeditions were part of the beginning of the fur trade in the North American interior. Initially they traded for beaver coats and furs. However, as the market grew, ''coureurs de bois'' were trapping and trading prime beavers whose skins were to be felted in Europe. Evolution While French settlers had lived and traded alongside Indigenous people since the earliest days of New France, coureurs des bois reached their apex during the second half of the 17th century. After 1681, the independent coureur des bois was gradually replaced by state-sponsored voyageurs, who were workers associated with licensed fur traders. They tr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
First Nations In Canada
First Nations (french: Premières Nations) is a term used to identify those Indigenous Canadian peoples who are neither Inuit nor Métis. Traditionally, First Nations in Canada were peoples who lived south of the tree line, and mainly south of the Arctic Circle. There are 634 recognized First Nations governments or bands across Canada. Roughly half are located in the provinces of Ontario and British Columbia. Under Charter jurisprudence, First Nations are a "designated group," along with women, visible minorities, and people with physical or mental disabilities. First Nations are not defined as a visible minority by the criteria of Statistics Canada. North American indigenous peoples have cultures spanning thousands of years. Some of their oral traditions accurately describe historical events, such as the Cascadia earthquake of 1700 and the 18th-century Tseax Cone eruption. Written records began with the arrival of European explorers and colonists during the Age of D ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ontario Highway 637
Secondary Highway 637, commonly referred to as Highway 637 is a Highways in Ontario, provincially maintained secondary highway in the Canada, Canadian province of Ontario. Located entirely within Sudbury District, the highway connects Ontario Highway 69, Highway 69 to the primary townsite of Killarney, Ontario, Killarney, away, as well as providing access to Killarney Provincial Park. The highway was opened in 1962. Prior to its completion, the community of Killarney relied primarily on water transport via Georgian Bay and the North Channel (Ontario), North Channel. The route has remained unchanged since then, aside from a very short extension to meet the realigned Highway 69 (future Ontario Highway 400, Highway 400) interchange (road), interchange. Route description Highway 637 is a long and isolated secondary highway which travels north of Georgian Bay. It begins in the town of Killarney at Channel Street, near the shoreline of the bay. From there it trave ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rocky Mountains
The Rocky Mountains, also known as the Rockies, are a major mountain range and the largest mountain system in North America. The Rocky Mountains stretch in straight-line distance from the northernmost part of western Canada, to New Mexico in the southwestern United States. Depending on differing definitions between Canada and the U.S., its northern terminus is located either in northern British Columbia's Terminal Range south of the Liard River and east of the Trench, or in the northeastern foothills of the Brooks Range/ British Mountains that face the Beaufort Sea coasts between the Canning River and the Firth River across the Alaska-Yukon border. Its southernmost point is near the Albuquerque area adjacent to the Rio Grande rift and north of the Sandia–Manzano Mountain Range. Being the easternmost portion of the North American Cordillera, the Rockies are distinct from the tectonically younger Cascade Range and Sierra Nevada, which both lie farther to its we ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quartzite
Quartzite is a hard, non- foliated metamorphic rock which was originally pure quartz sandstone.Essentials of Geology, 3rd Edition, Stephen Marshak, p 182 Sandstone is converted into quartzite through heating and pressure usually related to tectonic compression within orogenic belts. Pure quartzite is usually white to grey, though quartzites often occur in various shades of pink and red due to varying amounts of hematite. Other colors, such as yellow, green, blue and orange, are due to other minerals. The term ''quartzite'' is also sometimes used for very hard but unmetamorphosed sandstones that are composed of quartz grains thoroughly cemented with additional quartz. Such sedimentary rock has come to be described as orthoquartzite to distinguish it from metamorphic quartzite, which is sometimes called metaquartzite to emphasize its metamorphic origins. Quartzite is very resistant to chemical weathering and often forms ridges and resistant hilltops. The nearly pure silica co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually relate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saunders_Quarry-1.jpg "Click for more on -> Sandstone")