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Alberta’s Lower Athabasca Basin: Archaeology and Palaeoenvironments PDF

565 Pages·2017·12.237 MB·English
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Alberta’s Lower Athabasca Basin Alberta’s Lower Athabasca Basin Archaeology and Palaeo environments EditEd by brian M. ronaghan Copyright © 2016 Brian Ronaghan Published by AU Press, Athabasca University 1200, 10011 – 109 Street, Edmonton, AB T5J 3S8 ISBN 978-1-926836-90-4 (print) 978-1-926836-91-1 (PDF) 978-1-926836-92-8 (epub) doi: 10.15215/aupress/9781926836904.01 Cover and interior design by Marvin Harder, marvinharder.com. Printed and bound in Canada by Friesens. Library and Archives Canada Cataloguing in Publication Alberta’s lower Athabasca basin : archaeology and palaeoenvironments / edited by Brian M. Ronaghan. (Recovering the past : studies in archaeology, ISSN 2291-6784) Includes bibliographical references and index. Issued in print and electronic formats. 1. Athabasca Basin (Sask. and Alta.)—Antiquities. 2. Athabasca Tar Sands (Alta.)—Antiquities. 3. Paleontology—Athabasca Basin (Sask. and Alta.). 4. Paleontology—Alberta—Athabasca Tar Sands. I. Ronaghan, Brian M., editor of compilation II. Series: Recovering the past (Edmonton, Alta.) QE748.A4A43 2016 560.9712’32 C2012-901896-1 C2012-901897-X We acknowledge the financial support of the Government of Canada through the Canada Book Fund (CBF) for our publishing activities. Assistance provided by the Government of Alberta, Alberta Media Fund. This publication is licensed under a Creative Commons Licence, Attribution–Noncommercial–No Derivative Works 4.0 International: see www.creativecommons.org. The text may be reproduced for non-commercial purposes, provided that credit is given to the original author. To obtain permission for uses beyond those outlined in the Creative Commons licence, please contact AU Press, Athabasca University, at [email protected]. Contents IntroductIon The Archaeological Heritage of Alberta’s Lower Athabasca Basin Brian M. Ronaghan | 3 Part One Postglacial Environments 1 | A Tale of Two Floods How the End of the Ice Age Enhanced Oil Sands Recovery—and Decimated the Fossil Record James A. Burns and Robert R. Young | 25 2 | Glacial Geology and Land-Forming Events in the Fort McMurray Region Timothy G. Fisher and Thomas V. Lowell | 45 3 | Raised Landforms in the East-Central Oil Sands Region Origin, Age, and Archaeological Implications Robin J. Woywitka, Duane G. Froese, and Stephen A. Wolfe | 69 4 | Kearl Lake A Palynological Study and Postglacial Palaeoenvironmental Reconstruction of Alberta’s Oil Sands Region Luc Bouchet and Alwynne B. Beaudoin | 83 Part Two Human History 5 | The Early Prehistoric Use of a Flood-Scoured Landscape in Northeastern Alberta Grant M. Clarke, Brian M. Ronaghan, and Luc Bouchet | 115 6 | A Chronological Outline for the Athabasca Lowlands and Adjacent Areas Brian O. K. Reeves, Janet Blakey, and Murray Lobb | 161 7 | Lower Athabasca Archaeology A View from the Fort Hills Robin J. Woywitka | 243 8 | The Early Human History of the Birch Mountains Uplands John W. Ives | 285 Part Three Lithic Resource Use 9 | Beaver River Sandstone Characteristics and Use, with Results of Heat Treatment Experiments Eugene M. Gryba | 333 10 | The Organization of Lithic Technology at the Quarry of the Ancestors Nancy Saxberg and Elizabeth C. Robertson | 359 11 | Microblade Technology in the Oil Sands Region Distinctive Features and Possible Cultural Associations Angela M. Younie, Raymond J. Le Blanc, and Robin J. Woywitka | 401 Part Four Archaeological Methods 12 | Quarries Investigative Approaches in the Athabasca Oil Sands Gloria J. Fedirchuk, Jennifer C. Tischer, and Laura Roskowski | 437 13 | Cumulative Effects Assessment Evaluating the Long-Term Impact of Oil Sands Development on Archaeological Resources Brian M. Ronaghan | 479 List of Contributors | 541 Index of Sites | 549 General Index | 551 vi Alberta’s Lower Athabasca Basin Introduction | The Archaeological Heritage of Alberta’s Lower Athabasca Basin brian M. ronaghan From its headwaters in Jasper National Park, Alberta’s Athabasca River travels some 1,500 miles northeastward across the province, its waters ultimately flow- ing into Lake Athabasca. The river drains a vast region—roughly 159,000 square kilometres—along the southern margin of Canada’s Boreal Plains ecozone, which encompasses much of central and northern Alberta. In contrast to the grasslands further south, the Boreal Plains ecozone is heavily forested, forming part of Canada’s more broadly defined boreal forest.1 The Lower Athabasca basin lies wholly within the Boreal Plains ecozone, and, although some notable uplands occur, the area consists for the most part of glacial lake bed or till plain on which large tracts of muskeg and fen have developed between areas of modest elevation. Major fish-bearing lakes—Lake Athabasca and Lac La Biche— are situated along its northern and southwestern margins, respectively, and smaller lakes and ponds are scattered throughout the area. As with similar regions across the northern hemisphere, food resources are relatively meagre and widely distributed, traditionally supporting only comparatively small popu- lations of hunter-gatherers. With the exception of the access afforded by the river, travel throughout the region is difficult. Although the Lower Athabasca basin features a broad spectrum of natural resources, two classes of resource have proved to be of major commercial inter- est to outsiders. In 1778, explorer and trader Peter Pond arrived in the Athabasca region and established a fur trade post, thereby inaugurating an activity that would serve as the basis of the region’s commercial economy for a century and a doi: 10.15215/aupress/9781926836904.01 33 half. Pond noted the occurrence of a fluid tar-like substance (Stringham 2012, 21), which explorer and trader Alexander Mackenzie described in his journal a decade later, in 1788: At about 24 miles from the fork [of the Athabasca and Clearwater Rivers] are some bituminous fountains into which a pole of 20 feet long may be inserted without the least resistance. The bitumen is in a fluid state and when mixed with gum, the resinous substance collected from the spruce fir, it serves to gum the Indians’ canoes. In its heated state it emits a smell like that of sea coal. (Mackenzie 1970, 129) As Mackenzie noted, the Athabasca River and some of its tributaries had cut down through the surrounding bedrock, exposing bitumen along river banks in various locations to the north of modern Fort McMurray. Aboriginal people had known of these bitumen deposits for millennia. Long before Pond arrived in the oil sands area, a Cree chief, known in historical rec- ords as “the Swan,” had brought them to the attention of the Hudson’s Bay Company traders. In 1715, the Swan visited York Factory, where he described the Athabasca region, telling of a river on whose banks could be found “Gum or pitch.” Four years later, the Swan returned to York Factory, bearing a sample of “that Gum or pitch that flows out of the Banks of that River,” which he presented to HBC governor Henry Kelsey.2 Other resources in the region were, however, of greater value to the indigenous inhabitants. As the chapters in this volume dem- onstrate, a conjunction of natural and human factors has resulted in an unusually rich record of landscape development and human use that makes the Lower Athabasca basin exceptionally valuable for understanding the early history of Canada’s north. The archaeological record currently being revealed represents perhaps the most intense pattern of prehistoric human landscape use yet identi- fied in Canada’s boreal forest region.3 Investigation into the character, extent, and value of Alberta’s bitumen resour- ces began in the 1890s. Early in the twentieth century, in an account of an exped- ition to the Mackenzie basin in connection with Treaty 8 (signed in 1899), Charles Mair wrote: “The tar, whatever it may be otherwise, is a fuel, and burned in our camp-fires like coal. That this region is stored with a substance of great economic value is beyond all doubt, and, when the hour of development comes, it will, I believe, prove to be one of the wonders of Northern Canada” (1908, 121). Mair’s instinct would prove to be correct. Research was accelerated by the demand for fuel during both world wars, and in the early 1960s a commercially viable process 4 Introduction doi: 10.15215/aupress/9781926836904.01

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