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Holocene Glacier Fluctuations in the Middle Canadian Rocky Mountains

Published online by Cambridge University Press:  20 January 2017

B. H. Luckman  and
G. D. Osborn
B. H. Luckman
Affiliation:
Department of Geography, University of Western Ontario, London, Ontario N6A 5C2
G. D. Osborn
Affiliation:
Department of Geology, University of Calgary, Calgary, Alberta T2N 1N4 Australia
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Abstract

Holocene glacial advances in the Banff–Jasper–Yoho area of the Canadian Rocky Mountains have been extremely limited in extent. Limiting 14C dates from two sites within 1 km of contemporary glaciers of fresh terminal moraines indicate that the late Wisconsin Ice Sheet and valley glaciers disappeared prior to 9660 yr B.P. Two subsequent glacial advances are recognized. The earlier Crowfoot Advance is represented by moraines and rock-glacier deposits overlain by Mazama ash (6600 yr B.P.) and is therefore early Holocene or possibly late Wisconsin in age. The late Neoglacial Cavell Advance of the last few centuries is dated by dendrochronology and lichenometry. In addition, there is fragmentary, undated evidence of intermediate-age advance(s), mainly from rock-glacier deposits. All these advances were of limited extent (1–2 km beyond present ice margins) and the Cavell Advance was usually the most extensive. Major exceptions to this pattern occur only where rock glaciers or extensive ice-cored moraines developed during the earlier advance(s?). These deposits were not overrun by glaciers during the Cavell Advance because of their relatively greater downvalley extent and the physical barrier they presented to subsequent glacial advances. Earlier work which postulated more extensive early Holocene advances in the Canadian Rocky Mountains is shown to have inadequate dating control: Many of the features previously attributed to older Holocene events are late Wisconsin in age.

Type
Original Articles
Information
Quaternary Research , Volume 11 , Issue 1 , January 1979 , pp. 52 - 77
Copyright
University of Washington

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References

Alley, N.F., 1976. Post-Pleistocene glaciations in the interior of British Columbia. Geological Association of Canada Programme and Abstracts. 6 (Cordilleran Section).Google Scholar
Baranowski, S., Henoch, W.E.S., 1978 Glacier and Landform Features in the Columbia Icefield Area, Banff and Jasper National Parks, Alberta, Canada. Supplementary Report on a Study carried out for Parks Canada by Glaciology Division, Inland Waters Directorate, Environment Canada, March 1978.Google Scholar
Benedict, J.B., 1967. Recent glacial history of an alpine area in the Colorado Front Range U.S.A.: I, Establishing a lichen-growth curve. Journal of Glaciology. 6, 817-832.Google Scholar
Bowyer, A., 1977. The Sunwapta Section: Composition and Development of a Complex Stratigraphic Section from Sunwapta Pass, Jasper National Park. M.Sc. Thesis. University of Western Ontario, London, Ontario, (unpublished).Google Scholar
Bray, J.R., 1964. Chronology of a small glacier in eastern British Columbia, Canada. Science. 144, 287-288.Google Scholar
Bray, J.R., Struik, G.J., 1963. Forest growth and glacial chronology in Eastern British Columbia and their relation to recent climatic trends. Canadian Journal of Botany. 41, 1245-1271.Google Scholar
Brunger, A.G., Nelson, J.G., Ashwell, I.Y., 1967. Recession of Hector and Peyto Glaciers: Further studies in the Drummond Glacier, Red Deer Valley area, Alberta. Canadian Geographer. XI, 35-48.CrossRefGoogle Scholar
Carrara, P.E., Andrews, J.T., 1976. Holocene glacial/periglacial record: Northern San Juan Mountains, southwestern Colorado. Zeitschrift fur Gletscherkunde und Glazialgeologie. XI, 155-174.Google Scholar
Cautley, R.W., Wheeler, A.O., 1924 Report of the Commission Appointed to Delimit the Boundary between the Provinces of Alberta and British Columbia: Part II, 1917 to 1921. Office of the Surveyor General, Ottawa, 162.Google Scholar
Clague, J.J., 1975. Late Quaternary sediments and geomorphic history of the southern Rocky Mountain Trench, British Columbia. Canadian Journal of Earth Sciences. 12, 595-605.Google Scholar
Crockett, K.J., 1975. The Distribution of Rock Glaciers in the Southern Half of Jasper National Park, Alberta, Canada. B.A. Thesis. University of Western Ontario, London, Ontario, (unpublished).Google Scholar
Crockett, K.J., 1977. The complex post-Pleistocene deposits of the Ramparts. British Columbia, Canada. Geography 531. University of Western Ontario, (unpublished).Google Scholar
Denton, G.H., 1975. Glaciers of the Canadian Rocky Mountains. Field, W.O., Mountain Glaciers of the Northern Hemisphere. Vol. 1, C.R.E.E.L, Hanover, N.H, 603-653.Google Scholar
Denton, G.J., Karlén, W., én, 1977. Holocene glacial and tree-line variations in the White River valley and Skolai Pass, Alaska and Yukon Territory. Quaternary Research. 7, 63-111.CrossRefGoogle Scholar
Dingwall, P.R., 1973. Rock glaciers in the Canadian Rocky Mountains (abstract). Papers and Proceedings of the 9th INQUA Conference. Christchurch, New Zealand 80-81.Google Scholar
Duford, J.M., 1976. Late Pleistocene and Holocene Cirque Glaciations in the Shuswap Highland Area, British Columbia. M.Sc. Thesis. University of Calgary, Calgary, Alberta, (1978).Google Scholar
Duford, J.M., Osborn, G.D., 1978. Holocene and latest Pleistocene cirque glaciations in the Shuswap Highland, B.C.. Canadian Journal of Earth Sciences. 15, 865-873.CrossRefGoogle Scholar
Fox, J.C., 1974. Glacial Geomorphology of the Cataract Brook Valley, Yoho National Park, British Columbia. M.Sc. Thesis. University of Alberta, (unpublished).Google Scholar
Gardner, J., 1972. Recent glacier activity and some associated landforms in the Canadian Rocky Mountains. Slaymaker, H.O., McPherson, H.J., Mountain Geomorphology. Tantalus Press, Vancouver, B.C, 55-62.Google Scholar
Gardner, J., 1978. The Wenkchemna Glacier: Ablation complex and rock glacier in the Canadian Rocky Mountains. Canadian Journal of Earth Sciences. 15, 1200-1204.Google Scholar
Harris, S.A., Boydell, A.N., 1972. Glacial history of the Bow River and Red Deer River Areas and the adjacent foothills. Slaymaker, H.O., McPherson, H.J., Mountain Geomorphology. Tantalus Press, Vancouver, B.C, 47-53.Google Scholar
Harris, S.A., Howell, J.A., 1976. The Chateau Lake Louise glacial event in Banff National Park. Proceedings Canadian Association of Geographers Conference, Laval University. 49-52.Google Scholar
Harris, S.A., Howell, J.A., 1977a. Final stillstand stages and climatic conditions during the last retreat of the Rocky Mountain ice in southwest Alberta. Geological Society of America. 730 (Abstracts with Program).Google Scholar
Harris, S.A., Howell, J.A., 1977b. Chateau Lake Louise Moraines—Evidence for a new Holocene glacial event in southwest Alberta. Bulletin of Canadian Petroleum Geology. 25, 3 441-455.Google Scholar
Harrison, J.E., 1976. Dated Organic Material Below Mazama(?) Tephra: Elk Valley, British Columbia. Geological Survey Canada Paper. 76-1C, 169-170.Google Scholar
Heusser, C.J., 1956. Postglacial environments in the Canadian Rocky Mountains. Ecological Monographs. 26, 253-302.Google Scholar
Horberg, L., 1954. Rocky Mountain and continental Pleistocene deposits in the Waterton region, Alberta, Canada. Bulletin of the Geological Society of America. 65, 1093-1156.Google Scholar
Jackson, L.E. Jr., 1976. Quaternary Geology and Terrain Inventory, Kananaskis Lakes (82J) East of the Continental Divide, Alberta. Geological Survey Canada Paper. 76-1C, 209-211.Google Scholar
Kershaw, 177.L., 1977. A Geomorphological Interpretation of the Mount MacCarib Area, Jasper National Park, Alberta, Canada. B.A. Thesis. University of Western Ontario, (unpublished).Google Scholar
Libby, W.F., 1952 Radiocarbon Dating. Univ. of Chicago Press, Chicago. Google Scholar
Luckman, B.H., 1975. Neoglacial moraines and rock glaciers at the Ramparts, Jasper National Park, Alberta. Proceedings Canadian Association of Geographers Conference. Simon Fraser University. 70-73.Google Scholar
Luckman, B.H., 1976 Glacial Geomorphology at Mount Edith Cavell. Report to Parks Canada, Calgary.Google Scholar
Luckman, B.H., 1977. Lichenometric dating of Holocene moraines at Mount Edith Cavell, Jasper, Alberta. Canadian Journal of Earth Sciences. 14, 8 1809-1822.Google Scholar
Luckman, B.H., Crockett, K.J., 1978. Rock glaciers in the southern part of Jasper National Park. Canadian Journal of Earth Sciences. 15, 4 540-550.Google Scholar
Luckman, B.H., Kearney, M.S., 1978 Analysis and Interpretation of a Holocene Deposit from Castleguard Meadows, Banff National Park, Alberta. Report to Environment Canada, Contract KL229-7-2083.Google Scholar
Luckman, B.H., Kearney, M.S., Holland, K., 1977 Holocene Environmental Change in Jasper National Park. Report to Parks Canada.Google Scholar
Luckman, B.H., Osborn, G.D., King, R.H., 1978. Chateau Lake Louise Moraines—evidence for a new Holocene glacial event in southwest Alberta: A discussion. Bulletin of Canadian Petroleum Geology. 26, 398-402.Google Scholar
McPherson, H.J., 1970. Landforms and glacial history of the upper North Saskatchewan valley, Alberta, Canada. Canadian Geographer. XIV, 16-26.Google Scholar
Nelson, J.G., Ashwell, I.Y., Brunger, A.G., 1966. Recession of the Drummond Glacier, Alberta. Canadian Geographer. X, 71-81.Google Scholar
Ommanney, C.S.L., 1976. Canadian Rock Glacier studies. Proceedings, Canadian Association of Geographers Conference, Laval University. 156-157 Unpublished manuscript. Abstract published.Google Scholar
Osborn, G.D., 1975a. Advancing rock glaciers in the Lake Louise District, Banff National Park, Alberta. Canadian Journal of Earth Science. 12, 1060-1062.Google Scholar
Osborn, G.D., 1975b. Neoglacial deposits in the Lake Louise district, Banff National Park, Alberta (abstract). Geological Society of America. 635-636 Rocky Mountain section, 28th Annual Meeting (Abstracts with Program).Google Scholar
Osborn, G.D., Duford, J.M., 1976. An early Holocene advance in the Canadian Rockies. Geological Society of America. 616 Rocky Mountain section, 29th annual meeting (Abstracts with Program).Google Scholar
Osborn, G.D., Taylor, J., 1975. Lichenometry on calcareous substrates in the Canadian Rockies. Quaternary Research. 5, 111-120.CrossRefGoogle Scholar
Papertezian, 178.C., 1973. A Study of Rock Glaciers. B.Sc. Thesis. Queen's University, Kingston, Ontario, (unpublished).Google Scholar
Porter, S.C., 1978. Glacier Peak tephra in the North Cascade Range, Washington; stratigraphy, distribution, and relationship to late-glacial events. Quaternary Research. 10, 30-41.Google Scholar
Potter, N. Jr., 1972. Ice-cored rock glacier, Galena Creek, North Absaroka Mountains, Wyoming. Bulletin of the Geological Society of America. 83, 3025-3058.Google Scholar
Price, R.A., Mountjoy, E.W., 1970. Geological structure of the Canadian Rocky Mountains between the Bow and Athabaska Rivers—a progress report. Geological Association of Canada, Special Paper. 6.Google Scholar
Reeves, B.O.K., 1972 The Prehistory of Pass Creek Valley, Waterton Lakes National Park. National Historic Sites Service, Ottawa, Manuscript Report 61.Google Scholar
Reeves, B.O.K., 1975. Early Holocene (ca. 8000-5500 B.C.) prehistoric land and resource utilization patterns in Waterton Lakes National Park, Alberta. Arctic and Alpine Research. 7, 237-248.Google Scholar
Reeves, B.O.K., Dormaar, J., 1972. A partial Holocene pedological and archaeological record from the southern Alberta Rocky Mountains. Arctic and Alpine Research. 4, 325-336.CrossRefGoogle Scholar
Roed, M.A., 1975. Cordilleran and Laurentide multiple glaciation, west central Alberta. Canadian Journal of Earth Sciences. 12, 1493-1515.Google Scholar
Roed, M.A., Mountjoy, E.W., Rutter, N.W., 1967. The Athabasca Valley Erratics Train, Alberta and Pleistocene ice movements across the Continental Divide. Canadian Journal of Earth Sciences. 4, 4 625-632.Google Scholar
Rothlisberger, F., 1976. Gletscher und Klimaschwankungen in Raum Zermatt, Ferpecle und Arolla. Die Alpen, (3/4 Quartal, 1976). 59-152.Google Scholar
Rutter, N.W., 1972. Geomorphology and Multiple glaciation, Banff area, Alberta. Geological Survey of Canada Bulletin. 206.Google Scholar
Rutter, N.W., 1976. Multiple glaciation in the Canadian Rocky Mountains with special reference to northeastern British Columbia. Mahaney, W.C., Quaternary Stratigraphy of North America. Dowden, Hutchinson, and Ross, Stroudsburg, Pa, 409-440.Google Scholar
Rutter, N.W., 1977. Multiple Glaciation in the Area of Williston Lake, British Columbia. Geological Survey of Canada Bulletin. 273.Google Scholar
Schafer, J.D., 1954. Scott Glacier notes, 1953. Canadian Alpine Journal. 37, 124-126.Google Scholar
Shaw, J., 1972. Pleistocene chronology and geomorphology of the Rocky Mountains in south and central Alberta. Slaymaker, H.O., McPherson, H.J., Quaternary Stratigraphy of North America. Tantalus Press, Vancouver, B.C, 37-46.Google Scholar
Sherzer, W.H., 1907 Glaciers of the Canadian Rockies and Selkirks. Smithsonian Contributions to Knowledge No. 34.Google Scholar
Smith, N.D., 1975. Sedimentary environments and late Quaternary history of a “low energy” mountain delta. Canadian Journal of Earth Sciences. 12, 2004-2013.CrossRefGoogle Scholar
Stalker, A., Mac, S., 1969. A probable late Pinedale terminal moraine in Castle River Valley, Alberta. Bulletin of the Geological Society of America. 80, 2115-2122.CrossRefGoogle Scholar
Wahrhaftig, C., Cox, A., 1959. Rock glaciers in the Alaska Range. Bulletin of the Geological Society of America. 70, 383-436.Google Scholar
Westgate, J.A., 1975. Holocene tephra layers in southwestern Canada: New units and revision of age estimates (abstract). Geological Society of America, North-Central Section, 9th Annual Meeting. 879 (Abstracts with Programs).Google Scholar
Westgate, J.A., 1977a. Identification and significance of late Holocene tephra from Otter Creek, Southern British Columbia. Canadian Journal of Earth Science. 14, 2593-2600.Google Scholar
Westgate, J.A., 1977b. Compositional variability of Glacier Peak and Mazama Tephra in Western North America and its stratigraphic significance. Abstracts, X. INQUA Conference. Birmingham, England 501.Google Scholar
Westgate, J.A., Dreimanis, A., 1967. Volcanic ash layers of recent age at Banff National Park, Alberta, Canada. Canadian Journal of Earth Sciences. 4, 155-161.Google Scholar
Westgate, J.A., Smith, D.G.W., Tomlinson, M., 1970. Late Quaternary tephra layers in southwestern Canada. Smith, R.A., Smith, J.W., Early Man and Environments in Northwest North America. The Students Press, University of Calgary, 13-34.Google Scholar