Mode of flow of Saskatchewan glacier, Alberta, Canada

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Dept. of the Interior , Washington
Glaciers - Al
The Physical Object
Pagination70 p.
ID Numbers
Open LibraryOL22022706M

The U.S. Geological Survey Library has catalogued this publication as follows: Meier, Mark Frederick, Mode of flow of Saskatchewan Glacier, Alberta, Canada. Washington, U.S. Cited by: Alberta Mode of flow of Saskatchewan Glacier, Alberta, Canada,Geological Survey Professional Paper, P [United States Geological Survey.] on *FREE* shipping on qualifying offers.

Mode of flow of Saskatchewan Glacier, Alberta, Canada, Author: United States Geological Survey. Research in on Saskatchewan Glacier was directed toward the measurement of velocity on the surface and at depth, the surface and bedrock topography, ablation, and structures produced by flow.

These field data are used to test current theories of flow and to derive new conclusions about the flow of a valley glacier. Positions in space of 51 velocity stations fixed in the ice were.

Get this from a library. Mode of flow of Saskatchewan Glacier, Alberta, Canada. [Mark Frederick Meier; United States. Department of the Interior.; Geological Survey (U.S.)] -- Measurement and analysis of ice movement, deformation, and structural features of a typical valley glacier.

The Saskatchewan Glacier is located in Banff National Park, Alberta, Canada, approximately km (75 mi) northwest of the town of Banff, and can be accessed from the Icefields chewan Glacier is the largest outflow glacier from the Columbia Icefield, which rests along the Continental glacier is a primary water source for the North Saskatchewan nates: 52°08′19″N °11′36″W.

Saskatchewan Glacier flows eastward out of Columbia Icefield which lies astride the British Columbia-Alberta border in the Rocky Mountains at the boundary between Banff and Jasper national parks (52"08N., " 12 W.).

The Saskatchewan-is a geometrically simple ice stream emerging from the ice. More than 75% of Alberta’s ice is contained in the headwaters of the North Saskatchewan and Athabasca Rivers, where the largest icfields are clustered. Western Canada lost about 11% of its glacier area betweenwith area loss exceeding 20% on the eastern slopes of the Canadian Rockies.

Mode of flow of Saskatchewan Glacier United States Geological Survey Velocity fluctuations and water regime of arctic valley glaciers. Intemational Association of Scien-tific Hydrology Jan • Marvel at the Columbia Icefield’s longest tongue of ice by hiking almost three kilometres along Parker Ridge.

Here, you’ll be rewarded with sweeping views of the Saskatchewan Glacier and the opportunity to stroll through an alpine meadow of rock jasmine and forgetme- nots. The Saskatchewan Glacier is usually seen from above, on Parker's Ridge, but this much quieter trail will give you access to the very base of the glacier.

Though much longer than the famous Parker's Ridge, this trail is easy and meanders through morraines and forest before reaching the toe of the glacier. Bedrock topography: Supplement 2 from "Mode of flow of Saskatchewan Glacier, Alberta, Canada" (Thesis).

Saskatchewan Glacier The Saskatchewan Glacier is located in Banff National Park, Alberta, Canada, approximately km northwest of the town of Banff, and can be accessed from the Icefields Parkway. Saskatchewan Glacier flows eastward out of Columbia Icefield which lies astride the British Columbia-Alberta border in the Rocky Mountains at the boundary between Banff and Jasper national parks (52°O8N., °12W.).

The Saskatchewan is a geometrically simple ice stream emerging from the ice. When this phase is subtracted, the motion fringes can be processed to obtain line-of-sight glacier flow. Then, by assuming a given glacier flow direction, the LOS motion can be projected to the proper flow direction.

We show results obtained from the Saskatchewan Glacier on November 2/3 The measured flows range up to 30 cm/day. Meier, M. R.,Mode of flow of Saskatchewan Glacier, Alberta, Canada, U.S. Geol. Surv., Profess.

Paper70pp.

Details Mode of flow of Saskatchewan glacier, Alberta, Canada FB2

* Athabasca Glacier * Castleguard Glacier * Columbia Glacier * Dome Glacier * Stutfield Glacier * Saskatchewan Glacier Alberta, T0E 1E0 Canada. win the second edition of. The North Saskatchewan River is a glacier-fed river that flows from the Canadian Rockies continental divide east to central Saskatchewan, where it joins with the South Saskatchewan River to make up the Saskatchewan water flows eventually into the Hudson Bay.

The Saskatchewan River system is the largest shared between the Canadian provinces of Alberta and Saskatchewan. This evidence is best seen at Saskatchewan Glacier where in situ stumps and abundant detrital wood have been dated between ± 60 and ± 60 14 C years BP ( ka; Wood and Smith.

Meier, MF () Mode of flow of Saskatchewan Glacier, Alberta, Canada. USGS Prof. Pap., B, B14–B16 Google Scholar Mîndrescu, M and Evans, IS () Cirque form and development in Romania: allometry and the buzzsaw hypothesis. Geomorphology,– CrossRef | Google Scholar. It is also of interest in any consideration of the mechanism of glacial erosion, for clearly a glacier which is stuck fast to its bed will be a less active eroding agent than one which is slipping and carrying with it debris which can scour the bedrock.

() ‘Mode of flow of Saskatchewan Glacier, Alberta, Canada. GLACIERS OF CANADA GLACIERS OF THE CANADIAN ROCKIES By C. SIMON L. OMMANNEY Photograph of the Victoria Glacier, Rocky Mountains, Alberta, in August T ABLE 1. Named glaciers of the Rocky Mountains cited in the chapter Saskatchewan Glacier FIGURE High-angle oblique aerial photograph of Saskatchewan.

Description Mode of flow of Saskatchewan glacier, Alberta, Canada EPUB

The Saskatchewan Glacier is largest of six major glaciers fed by the Columbia Icefield, the largest icefield in the Rocky Mountains. This view of the terminus of the glacier is from Parker Ridge a 7, ft.

(2, m) subarctic mountain ridge at the northern end of Banff National Park. The small glacial lake at the foot of the glacier feeds the headwaters of the Saskatchewan River which flows Views: K.

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This book has been cited by the following publications. An assemblage of lava flow features on Mercury. Journal of Geophysical Research: Planets, Vol. Issue. 6, p. Boulton, G. Processes of glacier erosion on different substrata J.

Glaciology 23 W. Paterson, The Physics of Glaciers (London: Pergamon Press, ); M. Meier, Mode of Flow of Saskatchewan Glacier, Alberta, Canada, Professional Paper   However, foliation does not necessarily lie parallel to a line of maximum incremental shear strain, as the results of principal strain rate measurements on Saskatchewan Glacier, Alberta (Meier, ) and Kaskawulsh Glacier, Yukon (Anderton, ) indicate.

The Athabasca Glacier is a massive glacial toe to the expansive Columbia Icefield that sits on the British Columbia—Alberta border, Canada. It is arguably the most accessible glacier in North America and offers visitors a chance to get up close and personal an earth shaping wonder.

Mode of flow of Saskatchewan Glacier, Alberta, Canada,Professional Paper Geomorphology and forest ecology of a mountain region in the. The final glacier to be studied, the Saskatchewan Glacier, is about 8 miles (13 km) long and some 23 square miles (30 sq. km) in area, making it the largest of the three glaciers.

It declines gradually from east to northeast, without ice falls, to its terminus at 5, ft. (1, m). The Fraser River is the longest river within British Columbia, Canada, rising at Fraser Pass near Blackrock Mountain in the Rocky Mountains and flowing for 1, kilometres ( mi), into the Strait of Georgia at the city of Vancouver.

It is the 11th longest river in Canada. The river's annual discharge at its mouth is cubic kilometres (27 cu mi) or 3, cubic metres per second (,   Since comparable folds and folia- tions have frequently been observed in non-surging glaciers (e.g.

Blue Glacier, Washington, Allen et al. ; Saskatchewan Glacier, Alberta Rockies, Meier ; White Glacier, Axel Heiberg Island, Hambrey & MOiler ) it seems likely they form during the quiesc- ent phase when the processes of flow are most.

This paper describes the structural glaciology of Haut Glacier d'Arolla, a small valley glacier fed by two distinct accumulation basins in the Swiss Alps. A considerable body of field data is presented alongside observations from ground and aerial photographs.

Suites of structures identified in the field and from aerial photographs are first described in nongenetic terms before being assigned.Saskatchewan Glacier Trail, Banff National Park Distance: km round trip, day trip, allow hours.

Access: Finding the trail head is a little tricky because it is no longer marked and the small pull off is hidden under the highway.Alberta, with an area ofkm 2 (, sq mi), is the fourth-largest province after Quebec, Ontario and British Columbia.

Alberta's southern border is the 49th parallel north, which separates it from the U.S. state of Montana; while the 60th parallel north divides it from the Northwest th meridian west separates it from the province of Saskatchewan; while on the.