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Colonels Mountain (New Brunswick)
Colonels Mountain is a mountain in the Canadian province of New Brunswick. It lies adjacent to Big Bald Mountain, at the headwaters of the Northwest Miramichi River and the Sevogle River. The mountain top has been weathered to generate a series of mushroom-shaped granitic tors. Because the weathering process which forms tors is normally very slow, these features have been interpreted as indicating that part of northern New Brunswick escaped the last, Wisconsinan glaciation.Rampton, V. N., Gauthier, R. C., Thibault, J., and Seaman, A. A. 1984. Quaternary geology of New Brunswick. Geological Survey of Canada. Memoir 416. It has been suggested, however, that the mountain lay near the centre of the ice cap; these erosional remnants thus escaped the scouring action of the glaciers 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 over many years, often centuries. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northumberland County, New Brunswick
Northumberland County is located in northeastern New Brunswick, Canada. Geography Northumberland County is covered by thick forests, whose products stimulate the economy. The highest peaks in the province, including Mount Carleton lie in the northwestern corner of the county. The county is dominated by the Miramichi River, world famous for its salmon fishing. The lower portion of the river is an estuary that widens into Miramichi Bay, a part of the Gulf of St. Lawrence. Services The city of Miramichi is a local service centre for the county and surrounding regions with schools, hospitals and government offices and retail locations. The county has several saw mills in the city of Miramichi and up the Southwest Branch of the Miramichi River. There were formerly two large pulp and paper mills at Miramichi. Chatham was also home to an air force base, CFB Chatham, until 1996. Renous-Quarryville, located along the Southwest Miramichi was also home to an army post - a federal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tors On Colonels Mountain NB Canada
{{disambiguation, surname ...
Tors may refer to: * Tor (rock formation), rock outcrops * Ivan Tors (1916–1983), playwright, screenwriter and film and television producer * TransOral Robotic Surgery, a surgical technique See also * Tor (other) * Ten Tors * Tors Cove, Newfoundland and Labrador Tors Cove is a local service district and designated place in the Canadian province of Newfoundland and Labrador. It is on the east coast of the Avalon Peninsula of the island of Newfoundland, approximately 40 kilometres south of the St. John ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of New Brunswick
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 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 isolated summits, but most occur in mountain ranges. Mountains are formed through 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 slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glaciers
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 over many years, often centuries. It acquires distinguishing features, such as crevasses and 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 latitudes 35°N and 35°S, glaciers occur only ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ice Cap
In glaciology, an ice cap is a mass of ice that covers less than of land area (usually covering a highland area). Larger ice masses covering more than are termed ice sheets. Description Ice caps are not constrained by topographical features (i.e., they will lie over the top of mountains). By contrast, ice masses of similar size that ''are'' constrained by topographical features are known as ice fields. The ''dome'' of an ice cap is usually centred on the highest point of a massif. Ice flows away from this high point (the ice divide) towards the ice cap's periphery. Ice caps have significant effects on the geomorphology of the area that they occupy. Plastic moulding, gouging and other glacial erosional features become present upon the glacier's retreat. Many lakes, such as the Great Lakes in North America, as well as numerous valleys have been formed by glacial action over hundreds of thousands of years. On Earth, there are about of total ice mass. The average temperature ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wisconsinan Glaciation
The Wisconsin Glacial Episode, also called the Wisconsin glaciation, was the most recent glacial period of the North American ice sheet complex. This advance included the Cordilleran Ice Sheet, which nucleated in the northern North American Cordillera; the Innuitian ice sheet, which extended across the Canadian Arctic Archipelago; the Greenland ice sheet; and the massive Laurentide Ice Sheet, which covered the high latitudes of central and eastern North America. This advance was synchronous with global glaciation during the last glacial period, including the North American alpine glacier advance, known as the Pinedale glaciation. The Wisconsin glaciation extended from approximately 75,000 to 11,000 years ago, between the Sangamonian Stage and the current interglacial, the Holocene. The maximum ice extent occurred approximately 25,000–21,000 years ago during the last glacial maximum, also known as the ''Late Wisconsin'' in North America. This glaciation radically altered th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Weathering
Weathering is the deterioration of rocks, soils and minerals as well as wood and artificial materials through contact with water, atmospheric gases, and biological organisms. Weathering occurs ''in situ'' (on site, with little or no movement), and so is distinct from erosion, which involves the transport of rocks and minerals by agents such as water, ice, snow, wind, waves and gravity. Weathering processes are divided into ''physical'' and ''chemical weathering''. Physical weathering involves the breakdown of rocks and soils through the mechanical effects of heat, water, ice, or other agents. Chemical weathering involves the chemical reaction of water, atmospheric gases, and biologically produced chemicals with rocks and soils. Water is the principal agent behind both physical and chemical weathering, though atmospheric oxygen and carbon dioxide and the activities of biological organisms are also important. Chemical weathering by biological action is also known as biological wea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tor (rock Formation)
A tor, which is also known by geomorphologists as either a castle koppie or kopje, is a large, free-standing rock outcrop that rises abruptly from the surrounding smooth and gentle slopes of a rounded hill summit or ridge crest. In the South West of England, the term is commonly also used for the hills themselves – particularly the high points of Dartmoor in Devon and Bodmin Moor in Cornwall.Ehlen, J. (2004) ''Tor'' in Goudie, A., ed., pp. 1054-1056. ''Encyclopedia of Geomorphology.'' Routledge. London, England. Etymology Although English topographical names often have a Celtic etymology, the Oxford English Dictionary lists no cognates to the Old English word in either the Breton or Cornish languages (the Scottish Gaelic ''tòrr'' is thought to derive from the Old English word). It is therefore accepted that the English word ''Tor'' derives from the Old Welsh word ''tẁrr'' or ''twr'', meaning a cluster or heap. Formation Tors are landforms created by the erosion and weath ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sevogle River
The Big Sevogle River is a Canadian river in central New Brunswick. It consists of two branches, the North Sevogle and South Sevogle Rivers. Below the confluence of these rivers at the Square Forks, the river is properly referred to as the Big Sevogle River. This name serves to distinguish it from the "Little Sevogle River", a much smaller tributary to the Northwest Miramichi River. The Mi'kmaq may have referred to the river as ''Sewokulook'', "river of many cliffs", or as ''Elmunakuncheech'', meaning "little beaver hole".Rayburn, A. (1975) Geographical Names of New Brunswick. Toponymy Study 2. Surveys and Mapping Branch, Energy Mines and Resources Canada, Ottawa The river rises in the Big Bald Mountain area of the Miramichi Highlands, a region in north-central Northumberland County. The river flows southeast through heavy forests before joining the Northwest Miramichi River at Big Hole Tract at Indian Reserve 8, several kilometres northeast of Red Bank. The Big Sevogle Riv ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New Brunswick
New Brunswick (french: Nouveau-Brunswick, , locally ) is one of the thirteen provinces and territories of Canada. It is one of the three Maritime provinces and one of the four Atlantic provinces. It is the only province with both English and French as its official languages. New Brunswick is bordered by Quebec to the north, Nova Scotia to the east, the Gulf of Saint Lawrence to the northeast, the Bay of Fundy to the southeast, and the U.S. state of Maine to the west. New Brunswick is about 83% forested and its northern half is occupied by the Appalachians. The province's climate is continental with snowy winters and temperate summers. New Brunswick has a surface area of and 775,610 inhabitants (2021 census). Atypically for Canada, only about half of the population lives in urban areas. New Brunswick's largest cities are Moncton and Saint John, while its capital is Fredericton. In 1969, New Brunswick passed the Official Languages Act which began recognizing French as an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northwest Miramichi River
The Northwest Miramichi River or Elmunokun is a river in New Brunswick, Canada. The Mi'kmaq referred to the river as Elmunokun, possibly meaning "a beaver hole" in reference to a deep pool in the river, just below the mouth of the Big Sevogle River, its second largest tributary, after the Little Southwest Miramichi.Geographical Names of Canada The Northwest Miramichi River has its origins near Big Bald Mountain in the Miramichi Highlands, part of the Appalachian Mountains in Northumberland County. Initially flowing east, the river turns south at the confluence of the Tomogonops River and Portage River. It continues south to Sunny Corner where it becomes tidal, and then flows east. The Northwest Miramichi River joins the Southwest Miramichi River at Newcastle, NB to form the Miramichi River. The river is noted for Atlantic Salmon fishing. The headwaters offer important spawning sites for Atlantic Salmon; thus, much of the upper river is either closed to fishing, or des ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Big Bald Mountain (New Brunswick)
Big Bald Mountain, also known as Bald Mountain, is a prominent peak in the Canadian province of New Brunswick. It lies adjacent to Colonels Mountain, east of the Christmas Mountains The Christmas Mountains are a series of rounded peaks in northern New Brunswick, Canada, at the headwaters of North Pole Stream and the Little Southwest Miramichi River, west of Big Bald Mountain, and south of Mount Carleton. The mountains, in ..., and near the headwaters of the Northwest Miramichi River, the Sevogle River, and the South Branch Nepisiguit River. It is a well-known feature, in part because of its height, but especially because of its bald summit (hence the name).Geographical Names of Canada Before aerial surveillance was extensively used, a hut was maintained on the summit for fire-spotting in the remote north-central part of the province. A very similar hut was maintained on Mount Carleton, the province's highest peak. Triangulation among these huts and other fire towers a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
