The Tower (Alberta)
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The Tower (Alberta)
The Tower is the unofficial name for a large prominent peak that sits above Rummel Lake. It is located between Mount Engadine and Mount Galatea of the Kananaskis Range in Alberta, Canada. Geology The Tower is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate Based on the Köppen climate classification, The Tower is located in a subarctic climate The subarctic climate (also called subpolar climate, or boreal climate) is a climate with long, cold (often very cold) winters, and short, warm to cool summers. It is found on large landmasses, often away from the moderating effects of an ocean, ge ... zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. References Three-thousanders of Alberta Alberta's Rockies {{AlbertaRockies-geo-st ...
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Kananaskis Range
The Kananaskis Range is a mountain range west of the Kananaskis River in the Canadian Rockies. Many of the peaks are named after ships and people involved in the Battle of Jutland The Battle of Jutland (german: Skagerrakschlacht, the Battle of the Skagerrak) was a naval battle fought between Britain's Royal Navy Grand Fleet, under Admiral John Jellicoe, 1st Earl Jellicoe, Sir John Jellicoe, and the Imperial German Navy .... Mount Bogart is named after D.B. Dowling. Bogart was his mother's maiden name and his middle name. D.B. Dowling surveyed the area in the early 1900s for the Geographical Society of Canada. Tower was named after Francis George Towers an early homesteader of the region. Mt McDougal another early homesteader Archie McDougal of Carstairs. Mts. Evans Thomas named after Thomas Oldham Evans an early homesteader. Peaks of this range include: References Ranges of the Canadian Rockies Mountain ranges of Alberta {{AlbertaRockies-geo-stub ...
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Mount Bogart
Mount Bogart is a summit located in Kananaskis Country in the Canadian Rockies of Alberta, Canada. Mount Bogart's nearest higher peak is Wind Mountain, to the north. Mount Bogart is situated northwest of Mount Kidd, and both can be seen from Highway 40 near the Kananaskis Village junction. History Mount Bogart was named by Donaldson Bogart Dowling (1858-1925), after his mother, whose maiden name was Bogart. Donaldson Dowling, an engineer with the Geological Survey of Canada, explored the area in 1904. The first ascent of the peak was made in 1930 by Kate Gardiner and Walter Feuz. The duo also made first ascents of Mount Lyautey and Mount Galatea in 1930.Thorington p. 19, 56 The mountain's name was officially adopted in 2006 by the Geographical Names Board of Canada. Geology Mount Bogart is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during th ...
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List Of Mountains Of Alberta
Most of Alberta's mountains are found on the western edge of the province of Alberta, consisting of the eastern slopes of the Canadian Rockies, which run through the province from Alberta's mid-point to its southern border with the United States. Other elevated spots can be found in the Caribou Mountains and the Cypress Hills. The peaks of the Canadian Rockies are majestic, many of them reaching a height of more than three kilometres above sea level. Alberta's southwestern boundary is traced on the Continental Divide, along the high ranges of the Rocky Mountains, and many peaks are located on the Alberta–British Columbia border. The peak of Mount Columbia, within Jasper National Park, is the highest point in Alberta, second highest in the Canadian Rockies and 28th highest in Canada. The Caribou Mountains are located in the northern extremity of Alberta, forming an elevated plateau in the northern plains and wetlands. They reach an altitude of 1,030 m, almost 700&n ...
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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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Alberta
Alberta ( ) is one of the thirteen provinces and territories of Canada. It is part of Western Canada and is one of the three prairie provinces. Alberta is bordered by British Columbia to the west, Saskatchewan to the east, the Northwest Territories (NWT) to the north, and the U.S. state of Montana to the south. It is one of the only two landlocked provinces in Canada (Saskatchewan being the other). The eastern part of the province is occupied by the Great Plains, while the western part borders the Rocky Mountains. The province has a predominantly continental climate but experiences quick temperature changes due to air aridity. Seasonal temperature swings are less pronounced in western Alberta due to occasional Chinook winds. Alberta is the fourth largest province by area at , and the fourth most populous, being home to 4,262,635 people. Alberta's capital is Edmonton, while Calgary is its largest city. The two are Alberta's largest census metropolitan areas. More tha ...
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National Topographic System
The National Topographic System or NTS is the system used by Natural Resources Canada for providing general purpose topographic maps of the country. NTS maps are available in a variety of scales, the standard being 1:50,000 and 1:250,000 scales. The maps provide details on landforms and terrain, lakes and rivers, forested areas, administrative zones, populated areas, roads and railways, as well as other man-made features. These maps are currently used by all levels of government and industry for forest fire and flood control (as well as other environmental issues), depiction of crop areas, right-of-way, real estate planning, development of natural resources and highway planning. To add context, land area outside Canada is depicted on the 1:250,000 maps, but not on the 1:50,000 maps. History Topographic mapping in Canada was originally undertaken by many different agencies, with the Canadian Army’s Intelligence Branch forming a survey division to create a more standardized mappi ...
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Rummel Lake
People Rummel is the surname of: * Elizabeth Rummel (1897-1980), German-Canadian mountaineer and environmentalist *Franz Rummel (1853–1901), German pianist * Henrik Rummel (born 1987), American rower * Joseph Rummel (1876–1964), American Archbishop * Martin Rummel (born 1974), Austrian cellist * R. J. Rummel (1932–2014), American historian and political scientist * Walter Morse Rummel (1887–1953), German-born French pianist Other * Archbishop Rummel High School, Metairie, Louisiana * Bavarian Rummel The Bavarian Rummel (german: Bayrischer Rummel; ) was the term used Euphemism, to downplay (''Rummel'' means 'hustle and bustle') the warlike events in which Bavarian Army, Bavarian troops of Elector Maximilian II Emanuel of Bavaria, Maximilian II ..., the 1703 Bavarian campaign in Tyrol See also * Rummel T {{surname ...
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Mount Engadine
Mount Engadine is a mountain summit located in the Spray River Valley of Kananaskis Country, in the Canadian Rockies of Alberta, Canada. It was named in 1917 after HMS ''Engadine'', a seaplane tender of the Royal Navy present at the Battle of Jutland during World War I. The mountain is located in the Kananaskis Range in Alberta. Geology The mountain is composed of sedimentary rock laid down during the Precambrian to Jurassic periods and was later pushed east and over the top of younger rock during the Laramide orogeny. Climate Based on the Köppen climate classification, Mount Engadine is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. In terms of favorable weather, June through September are the best months to climb. Precipitation runoff from the mountain drains into Smuts Creek and Buller Creek, which empty into Spray Lakes Reservoir. See also * Geology of the Rocky ...
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Mount Galatea
Mount Galatea is the highest peak of the Kananaskis Range, a subrange of the Canadian Rockies in the province of Alberta. It is located in the upper Spray Lakes Valley of the Kananaskis Country system of provincial parks. The mountain was named after the Royal Navy cruiser HMS ''Galatea''. Geology Mount Galatea is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate Based on the Köppen climate classification, Mount Galatea is located in a subarctic climate zone with cold, snowy winters, and mild summers. Winter emperatures can drop below −20 °C with wind chill factors below −30 °C. References External links Fresh-Oxygen- route beta, photos Galatea Galatea is an ancient Greek name meaning "she who is milk-white". Galatea, Galathea or Gallathea may refer to: In mythology * Galatea (Greek myth ...
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Sedimentary Rock
Sedimentary rocks are types of rock that are formed by the accumulation or deposition of mineral or organic particles at Earth's surface, followed by cementation. Sedimentation is the collective name for processes that cause these particles to settle in place. The particles that form a sedimentary rock are called sediment, and may be composed of geological detritus (minerals) or biological detritus (organic matter). The geological detritus originated from weathering and erosion of existing rocks, or from the solidification of molten lava blobs erupted by volcanoes. The geological detritus is transported to the place of deposition by water, wind, ice or mass movement, which are called agents of denudation. Biological detritus was formed by bodies and parts (mainly shells) of dead aquatic organisms, as well as their fecal mass, suspended in water and slowly piling up on the floor of water bodies (marine snow). Sedimentation may also occur as dissolved minerals precipitate from ...
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Precambrian
The Precambrian (or Pre-Cambrian, sometimes abbreviated pꞒ, or Cryptozoic) is the earliest part of Earth's history, set before the current Phanerozoic Eon. The Precambrian is so named because it preceded the Cambrian, the first period of the Phanerozoic Eon, which is named after Cambria, the Latinised name for Wales, where rocks from this age were first studied. The Precambrian accounts for 88% of the Earth's geologic time. The Precambrian is an informal unit of geologic time, subdivided into three eons ( Hadean, Archean, Proterozoic) of the geologic time scale. It spans from the formation of Earth about 4.6 billion years ago ( Ga) to the beginning of the Cambrian Period, about million years ago ( Ma), when hard-shelled creatures first appeared in abundance. Overview Relatively little is known about the Precambrian, despite it making up roughly seven-eighths of the Earth's history, and what is known has largely been discovered from the 1960s onwards. The Precambrian fossil ...
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Jurassic
The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately Mya. The Jurassic constitutes the middle period of the Mesozoic, Mesozoic Era and is named after the Jura Mountains, where limestone strata from the period were first identified. The start of the Jurassic was marked by the major Triassic–Jurassic extinction event, associated with the eruption of the Central Atlantic magmatic province, Central Atlantic Magmatic Province. The beginning of the Toarcian Stage started around 183 million years ago and is marked by an extinction event associated with widespread Anoxic event, oceanic anoxia, ocean acidification, and elevated temperatures likely caused by the eruption of the Karoo-Ferrar, Karoo-Ferrar large igneous provinces. The end of the Jurassic, however, has no clear boundary with the Cretaceous and i ...
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