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Fossil Mountain (Alberta)
Fossil Mountain is a mountain located south of Skoki Mountain in Banff National Park, Canada. The mountain was named in 1906 by M.P. Bridgland, of the first ascent party, after the numerous fossils that can be found on its slopes. Fossil Mountain is the site of the first known skiing fatality in the Canadian Rockies. On April 7, 1933, Raymond Paley died in a slab avalanche An avalanche is a rapid flow of snow down a slope, such as a hill or mountain. Avalanches can be set off spontaneously, by such factors as increased precipitation or snowpack weakening, or by external means such as humans, animals, and earth ... when he attempted to ski down the mountain after skiing almost to the top. In February 1988, cousins Dan and Wayne Hugo (29 and 27 respectively) were hiking and skiing on Fossil Mountain when an avalanche, which they may have triggered, occurred. They both died. Routes The scrambling route ascends easy scree slopes from Deception Pass. Due to these easy s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Slate Range (Alberta)
The Slate Range is a mountain range of the Canadian Rockies, located in Banff National Park, Canada. The range is named after slate, the primary composition of the mountains in the area. The Lake Louise Ski Resort is on the southern slopes of this range. This range includes the following mountains and peaks: See also * Ranges of the Canadian Rockies The Canadian Rockies are a segment of the North American Rocky Mountains found in the Canadian provinces of Alberta and British Columbia. List of ranges There is no universally accepted hierarchical division of the Canadian Rockies into subranges. ... References {{Canadian Rockies, state=collapsed Ranges of the Canadian Rockies Mountain ranges of Alberta Mountains of Banff National Park ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fossil
A fossil (from Classical Latin , ) is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, objects preserved in amber, hair, petrified wood and DNA remnants. The totality of fossils is known as the ''fossil record''. Paleontology is the study of fossils: their age, method of formation, and evolutionary significance. Specimens are usually considered to be fossils if they are over 10,000 years old. The oldest fossils are around 3.48 billion years old to 4.1 billion years old. Early edition, published online before print. The observation in the 19th century that certain fossils were associated with certain rock strata led to the recognition of a geological timescale and the relative ages of different fossils. The development of radiometric dating techniques in the early 20th century allowed scientists to quantitatively measure the abs ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fossil Mountain Seen From Ptarmigan Lake
A fossil (from Classical Latin , ) is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, objects preserved in amber, hair, petrified wood and DNA remnants. The totality of fossils is known as the ''fossil record''. Paleontology is the study of fossils: their age, method of formation, and evolutionary significance. Specimens are usually considered to be fossils if they are over 10,000 years old. The oldest fossils are around 3.48 billion years old to 4.1 billion years old. Early edition, published online before print. The observation in the 19th century that certain fossils were associated with certain rock strata led to the recognition of a geological timescale and the relative ages of different fossils. The development of radiometric dating techniques in the early 20th century allowed scientists to quantitatively measure the a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scrambles In The Canadian Rockies
''Scrambles'' is the fifth studio album by Bomb the Music Industry!, released digitally and physically on February 15th, 2009. The album was released a year and a half after Get Warmer, making it the longest gap between the release of two chronologically adjacent Bomb the Music Industry! albums. Frontman Jeff Rosenstock aimed to record the album on a limited budget of $50; up to that point, the band had never spent that much money on the recording of an album. In 2019, to celebrate the album's 10th anniversary, a compilation of demos for the album was released by Rosenstock. Recording and composition In November 2007, the band announced they were in the demo and writing phase for their next album; alongside this, they posted a demo of "25" on their Myspace profile. A demo for "Fresh Attitude Young Body" was posted online on March 30, 2008, followed by several others for a limited time. In September 2008, the band played a few East Coast shows with the Riot Before. On October 6, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Deception Pass (Alberta)
Deception Pass is a trail in Banff National Park Alberta, Canada. It is named so because it is deceiving in that it looks small but the end never seems to come into sight. It is used to access the Skoki Valley, The Red Deer Lakes, Skoki Mountain and many beautiful smaller alpine lakes. The pass is a challenge for the guests of the Skoki Ski Lodge The Skoki Ski Lodge National Historic Site of Canada was built in 1930-31 in the Skoki Valley of Canada's Banff National Park. Built by local members of the Ski Club of the Canadian Rockies, the lodge was the first commercial building built spe .... It is located between Fossil Mountain and Ptarmigan Peak. References Banff National Park {{AlbertaRockies-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Avalanche
An avalanche is a rapid flow of snow down a slope, such as a hill or mountain. Avalanches can be set off spontaneously, by such factors as increased precipitation or snowpack weakening, or by external means such as humans, animals, and earthquakes. Primarily composed of flowing snow and air, large avalanches have the capability to capture and move ice, rocks, and trees. Avalanches occur in two general forms, or combinations thereof: slab avalanches made of tightly packed snow, triggered by a collapse of an underlying weak snow layer, and loose snow avalanches made of looser snow. After being set off, avalanches usually accelerate rapidly and grow in mass and volume as they capture more snow. If an avalanche moves fast enough, some of the snow may mix with the air, forming a powder snow avalanche. Though they appear to share similarities, avalanches are distinct from slush flows, Mudflow, mudslides, Landslide#Debris landslide, rock slides, and serac collapses. They are also ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Raymond Paley
Raymond Edward Alan Christopher Paley (7 January 1907 – 7 April 1933) was an English mathematician who made significant contributions to mathematical analysis before dying young in a skiing accident. Life Paley was born in Bournemouth, England, the son of an artillery officer who died of tuberculosis before Paley was born. He was educated at Eton College as a King's Scholar and at Trinity College, Cambridge. He became a wrangler in 1928, and with J. A. Todd, he was one of two winners of the 1930 Smith's Prize examination. He was elected a Research Fellow of Trinity College in 1930, edging out Todd for the position, and continued at Cambridge as a postgraduate student, advised by John Edensor Littlewood. After the 1931 return of G. H. Hardy to Cambridge he participated in weekly joint seminars with the other students of Hardy and Littlewood. He traveled to the US in 1932 to work with Norbert Wiener at the Massachusetts Institute of Technology and with George Pólya at ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canadian Rockies
The Canadian Rockies (french: Rocheuses canadiennes) or Canadian Rocky Mountains, comprising both the Alberta Rockies and the British Columbian Rockies, is the Canadian segment of the North American Rocky Mountains. It is the easternmost part of the Canadian Cordillera, which is the northern segment of the North American Cordillera, the expansive system of interconnected mountain ranges between the Interior Plains and the Pacific Coast that runs northwest–southeast from central Alaska to the Isthmus of Tehuantepec in Mexico. Canada officially defines the Rocky Mountains system as the mountain chains east of the Rocky Mountain Trench extending from the Liard River valley in northern British Columbia to the Albuquerque Basin in New Mexico, not including the Mackenzie, Richardson and British Mountains/ Brooks Range in Yukon and Alaska (which are all included as the "Arctic Rockies" in the United States' definition of the Rocky Mountains system). The Canadian Rockies ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Banff National Park
Banff National Park is Canada's oldest national park, established in 1885 as Rocky Mountains Park. Located in Alberta's Rocky Mountains, west of Calgary, Banff encompasses of mountainous terrain, with many glaciers and ice fields, dense coniferous forest, and alpine landscapes. The Icefields Parkway extends from Lake Louise, connecting to Jasper National Park in the north. Provincial forests and Yoho National Park are neighbours to the west, while Kootenay National Park is located to the south and Kananaskis Country to the southeast. The main commercial centre of the park is the town of Banff, in the Bow River valley. The Canadian Pacific Railway was instrumental in Banff's early years, building the Banff Springs Hotel and Chateau Lake Louise, and attracting tourists through extensive advertising. In the early 20th century, roads were built in Banff, at times by war internees from World War I, and through Great Depression-era public works projects. Since the 1960s, park acc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Richardson (Alberta)
Mount Richardson is the highest mountain of the Slate Range located beside Pika Peak in Banff National Park, Alberta, Canada. The mountain was named in 1859 by James Hector after Sir John Richardson who was the ship's surgeon and naturalist on John Franklin's 1819 and 1825 expeditions into the Arctic. The Lake Louise Mountain Resort is developed on the southern slopes of the Merlin Ridge, which includes Mount Richardson, Ptarmigan Peak, Pika Peak. A campground is located at the foot of the mountain, near Hidden Lake. The first ascent was made in 1911 by L.L. Delafield who was guided by Edward Feuz jr. Routes The scrambling route (rated easy/moderate) begins from Hidden Lake and ascends the southern slopes to the top. The only real challenge on the ascent are a few rubbly gullies just above the lake. A traverse to Pika Peak Pika Peak is a mountain located between Mount Richardson and Ptarmigan Peak in Banff National Park, Alberta, Canada The mountain was named in 192 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Skoki Mountain
Skoki Mountain is a mountain located in Banff National Park in Alberta, Canada. It is situated towards the east of the Skoki Valley, at the head of the Red Deer River, and is part of the Slate Range. At the base of the mountain lies Skoki Lodge, a historic ski lodge constructed in 1931, where several routes up to the peak originate. Skoki Mountain was named by James F. Porter in 1911 after the Indian word for marsh or swamp A swamp is a forested wetland.Keddy, P.A. 2010. Wetland Ecology: Principles and Conservation (2nd edition). Cambridge University Press, Cambridge, UK. 497 p. Swamps are considered to be transition zones because both land and water play a role in .... References Two-thousanders of Alberta Mountains of Banff National Park {{AlbertaRockies-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
