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Canmore

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Series: GSA Field Guide, GSA Field Guide
Published: 01 January 2017
DOI: 10.1130/2017.0048(05)
... of these depositional settings can be observed in the Sulphur Mountain Formation in outcrops in Canmore and Kananaskis. The rocks display a wide variety of sedimentary structures and a suite of body and trace fossils, and provide a valuable window into the subsurface, with the outcropping facies acting as direct...
Journal Article
Published: 01 June 1989
Bulletin of Canadian Petroleum Geology (1989) 37 (2): 198–209.
...Brent B. Waters; Ronald J. Spencer; Robert V. Demicco ABSTRACT Peritidal carbonates of the Middle and Upper Cambrian Waterfowl Formation are 32 m thick near Canmore, Alberta, where they are exposed in a nearly continuous, 5 km long outcrop belt. The formation comprises eight facies here: thin...
Journal Article
Published: 01 June 1984
Bulletin of Canadian Petroleum Geology (1984) 32 (2): 147–161.
...Ian W. Moffat; John H. Spang ABSTRACT A system of transverse faults, oriented at high angles to predominant northwest-southeast trending structures, is contained within the major Rundle and Sulphur Mountain Thrust Sheets of the Canadian Rocky Mountain Front Ranges near Canmore, Alberta...
Journal Article
Published: 20 February 2020
Canadian Journal of Earth Sciences (2020) 57 (5): 662–670.
FIGURES | View All (9)
Journal Article
Published: 01 September 2003
Bulletin de la Société Géologique de France (2003) 174 (5): 453–469.
Journal Article
Published: 01 September 1991
Bulletin of Canadian Petroleum Geology (1991) 39 (3): 260–269.
... Lakes, near Canmore, Alberta, contains large vugs and fossil molds in a dense, dolomite matrix and the outcrop is an analog, with respect to characteristics of the pore system, of the producing zones of some Devonian reservoirs in the subsurface of western Canada. The outcrop was systematically...
Journal Article
Published: 01 October 1981
Canadian Journal of Earth Sciences (1981) 18 (10): 1635–1636.
... also a minimum for the Canmore advance in the Bow Valley, Alberta, and suggests that the Canmore was not related to deposition of the Bighill Creek Formation at Cochrane. Pollen samples from the bog indicate a shrub–herb pioneer assemblage following deglaciation of that portion of the valley. Des...
Series: GSA Special Papers
Published: 01 January 1974
DOI: 10.1130/SPE153-p75
..., and the highest occurs in the Canmore coalfield. The coalification gradient affects the availability of coking coals of most favorable rank, that is, the medium-volatile coals. With a low gradient (and corresponding steep curve), medium-volatile coals occur over a greater stratigraphic interval...
Journal Article
Published: 25 August 1999
Canadian Journal of Earth Sciences (1999) 36 (3): 395–407.
... and glacitectonite fabric shapes with similar sediments elsewhere indicate that the subglacially deformed material that caps some of the sections is immature and has undergone short travel distances. Although the exact age of the readvance is unknown, it probably represents the Canmore Readvance of the Late...
Journal Article
Published: 01 June 1991
Bulletin of Canadian Petroleum Geology (1991) 39 (2): 219.
...N.C. Meijer Drees; D.I. Johnston A 298.5 m thick, composite section of the Palliser near Exshaw includes 5 units. It was sampled for conodonts and correlated with incomplete sections near Canmore and Lake Minnewanka. The basal, dark grey dolostone of unit 1 did not yield conodonts...
Journal Article
Journal: AAPG Bulletin
Published: 01 April 1984
AAPG Bulletin (1984) 68 (4): 490.
... sections were measured near Canmore where the Cairn Formation is a platform sequence of carbonates approximately 50 km (31 mi) from the nearest reef edge. The entire sequence consists of sediments deposited in a subtidal environment. No evidence of intertidal or supratidal deposition was found...
Journal Article
Published: 01 April 1980
Canadian Journal of Earth Sciences (1980) 17 (4): 459–477.
... valley glaciers during retreat is recognized. The glaciolacustrine Midnapore Silts and Clays were deposited due to Laurentide ice damming of Bow River valley while the Canmore and Eisenhower Junction Tills were deposited by valley glaciers. On the basis of land mammal chronology, the two oldest...
Journal Article
Published: 01 June 1979
Bulletin of Canadian Petroleum Geology (1979) 27 (2): 183–208.
... is suggested for the formation on Morrissey Ridge south of Fernie, British Columbia. The Kootenay Group conformably overlies Upper Jurassic strata of the Fernie Formation and in most areas is disconformably overlain by Lower Cretaceous strata of the Blairmore Group. Near Fernie, Highwood Pass and Canmore...
Journal Article
Published: 03 March 2021
Environmental and Engineering Geoscience (2021) 27 (2): 179–194.
... done at a high level of detail. We first apply it in the Canmore area, Alberta, Canada, where 11 debris-flood fans were studied by BGC Engineering ( Holm et al., 2018 ). We then use it along a 30-km-long roadway corridor near Hope, in Southwestern British Columbia, Canada, that has also been studied...
Journal Article
Published: 01 June 1977
Bulletin of Canadian Petroleum Geology (1977) 25 (3): 441–455.
... of the phases here is not surprising. Depression of ELA during the Chateau Lake Louise Event Table 1 shows the results of estimating the ELA (equilibrium line altitudes) for the present-day icefields, the Chateau Lake Louise event, and also the Eisenhower Junction and Canmore advances. The estimates use...
Journal Article
Journal: AAPG Bulletin
Published: 01 February 1946
AAPG Bulletin (1946) 30 (2): 238–248.
..., of the enlarged Montana Morrison, was named and described by G. M. Dawson and Sir William Dawson (1886, p. 2). Fossil plants were collected at five principal localities said to occur within the Kootenay: Anthracite, Canmore, Coal Creek, Crowsnest Pass, and Martin Creek—all in the vicinity of Bow River...
Journal Article
Published: 01 December 1993
Bulletin of Canadian Petroleum Geology (1993) 41 (4): 373–388.
.... 1. Location map showing major structural and depositional ele- ments of the southern Canadian Rocky Mountains. Line of section is for Figure 4. Numbers indicate locations of measured stratigraphic sections of the Arctomys Formation: 1) Mt. Ogden; 2) Noyes Creek; 3) Canmore; 4) Ghost River; 5) Mount...
Image
Outcrop photo of dolostone from the Upper Devonian Cairn Formation at White...
Published: 01 June 2006
Fig. 1. Outcrop photo of dolostone from the Upper Devonian Cairn Formation at Whiteman Gap near Canmore, Alberta. Partial-molds (PM) occur near the centre of hemispherical and other stromatoporoids. Dolomite has replaced both the fine-grained matrix and the peripheral, outer rind of the large
Journal Article
Published: 01 December 1966
Bulletin of Canadian Petroleum Geology (1966) 14 (4): 620–626.
... feet during the maxi - mum extent . The lack of evidence for a terminal moraine for thi s advance in the study-area suggests that the Bow Valley glacier flowe d into the Foothills as a piedmont glacier . Evidence exists for two equilibrium phases, or pauses during deglacia- tion. Near Canmore, ice...
Image
Outcrop photo of dolostone from the Upper Devonian Cairn Formation along th...
Published: 01 June 2006
Fig. 3. Outcrop photo of dolostone from the Upper Devonian Cairn Formation along the Grassi Lakes trail at Whiteman Gap, near Canmore, Alberta. Pitted appearance of near-vertical cliff corresponds to the occurrence of partial-molds near centre of hemispherical and bulbous stromatoporoids