Lithic Indications of Social and Economic Change at Housepit 7 of the Keatley Creek Site
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Chapter 2 The Coyote People Because native life and culture is so important to understanding archaeological re- mains in North America, we shall take a brief look at what traditional life was like in the Lillooet region before examining the archaeological remains from Keatley Creek in detail. There are three native linguistic groups that converge on the site catchment area of Keatley Creek (Figure 2.1). This is the area around the site that would have been regularly used for obtaining food resources. These linguistic groups are the Stl’atl’imx (or St’at’imc; pronounced Shtla-tlye-mkh, also known as the Fraser River Lillooet Indians), the Nlaka7pamux (pronounced N-le-ka’-p-mkh, also known as the Upper Thompson Indians), and the Secwepemc (pronounced Sha-khwep-makh, also known as the Shuswap Indians).1 All three languages are members of the Interior Sal- ish language family, and all three claim to be descended from a coyote ancestor who is the most prominent figure in their oral traditions (Teit, 1917, p. 12). All three groups also have similar material culture. Therefore, archaeologists have not been able to distinguish these groups from each other prehistorically, and we cannot say for certain which of the three languages was spoken by the prehistoric residents of Keatley Creek. However, because there is an unbroken cultural tradition throughout the Salish-speak- ing part of the Plateau, from middle Prehistoric times (ca. 7000 B.P.) until contact with Eurocanadians in the 1800s, it seems almost certain that the residents of Keatley Creek spoke one of the Interior Salish languages. -
Food Production During the Late
Supervisors: Dr. Nancy J. Turner and Dr. Michael C.R Edgell ABSTRACT This research traces the emergence of wild plant food production during the Late Prehistoric Period (4500 to 200 BP) on the Canadian Plateau. It builds upon ecological-evolutionary perspectives offered by theories of people-plant interactions and models of plant food production. From this, it derives a general model of wild plant food production outlining the components of such systems, the conditions favouring their development, and the consequences and correlates of these activities. This general model is expanded and made specific to the Canadian Plateau through ethnographic, ethnobotanical, ecological and archaeological evidence for root resource use by the Secwepemc (Shuswap) and other Interior Salish peoples. The implications of these findings for reconstructions of Late Prehistoric culture change are discussed. The study has two components. It begins by demonstrating that historically, the Interior Salish peoples were not plant collectors, "adapting to" the environment, but plant food producers who "domesticated" the landscapes of the region. Ethnobotanical evidence indicates the Secwepemc managed, processed and stored a variety of plant resources to increase their productivity and availability. These actions ensured surpluses for ovenvintering, reducing the threat of recurrent seasonal resource stress. Root foods were particulariy important. At least 20 species were regdarly hamested and stored. Practices associated with harvesting were essentially horticultural and acted at the species, population and landscape levels to increase the density and distribution of targeted species. The productivity of root resources was also increased through processing in earth ovens. An experimental reconstruction of an Interior Salish earth oven found pitcooking increased the energy value of balsamroot (Balsarnorhiza sagittata), a former root staple, by 250 percent. -
Lithic Transport Strategies on the Canadian Plateau
University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School 2010 WHY THE XWISTEN CROSSED THE RIVER: LITHIC TRANSPORT STRATEGIES ON THE CANADIAN PLATEAU Michael Todd Wanzenried The University of Montana Follow this and additional works at: https://scholarworks.umt.edu/etd Let us know how access to this document benefits ou.y Recommended Citation Wanzenried, Michael Todd, "WHY THE XWISTEN CROSSED THE RIVER: LITHIC TRANSPORT STRATEGIES ON THE CANADIAN PLATEAU" (2010). Graduate Student Theses, Dissertations, & Professional Papers. 1185. https://scholarworks.umt.edu/etd/1185 This Thesis is brought to you for free and open access by the Graduate School at ScholarWorks at University of Montana. It has been accepted for inclusion in Graduate Student Theses, Dissertations, & Professional Papers by an authorized administrator of ScholarWorks at University of Montana. For more information, please contact [email protected]. WHY THE XWISTEN CROSSED THE RIVER: LITHIC TRANSPORT STRATEGIES ON THE CANADIAN PLATEAU By Michael Todd Wanzenried B.A. Anthropology, University of Montana, Missoula, MT, 2003 Thesis presented in partial fulfillment of the requirements for the degree of Master of Arts in Anthropology, Archaeology The University of Montana Missoula, MT May 2010 Approved by: Perry Brown, Associate Provost for Graduate Education Graduate School Dr. Anna Prentiss, Chair Anthropology Dr. John Douglas Anthropology Dr. Casey Charles English Wanzenried, Michael, M.A., May 2010 Anthropology Abstract Title: Lithic Transport Strategies on the Canadian Plateau Chairperson: Dr. Anna Prentiss As has been the case for thousands of years a single kind of stone material, referred to by different researchers as arrowstone, basalt, vitreous trachydacite, and/or dacite, provided the majority (often more than 75%) of many lithic assemblages in the Mid- Fraser region of south-western British Columbia. -
The Archive of Place 00Front.Qxd 4/27/2007 6:48 AM Page Ii
00front.qxd 4/27/2007 6:48 AM Page i The Archive of Place 00front.qxd 4/27/2007 6:48 AM Page ii The Nature | History | Society series is devoted to the publication of high-quality scholarship in environmental history and allied fields. Its broad compass is signalled by its title: nature because it takes the natural world seriously; history because it aims to foster work that has temporal depth; and society because its essential concern is with the interface between nature and society, broadly conceived. The series is avowedly interdisciplinary and is open to the work of anthropologists, ecologists, historians, geographers, literary scholars, political scientists, sociologists, and others whose interests resonate with its mandate. It offers a timely outlet for lively, innovative, and well-written work on the interaction of people and nature through time in North America. General Editor: Graeme Wynn, University of British Columbia Claire Elizabeth Campbell, Shaped by the West Wind: Nature and History Tina Loo, States of Nature: Conserving Canada’s Wildlife in the Twentieth Century Jamie Benidickson, The Culture of Flushing: A Social and Legal History of Sewage John Sandlos, Hunters at the Margin: Native People and Wildlife Conservation in the Northwest Territories James Murton, Creating a Modern Countryside: Liberalism and Land Resettlement in British Columbia 00front.qxd 4/27/2007 6:48 AM Page iii The Archive of Place Unearthing the Pasts of the Chilcotin Plateau . UBC Press • Vancouver • Toronto 00front.qxd 4/27/2007 6:48 AM Page iv © UBC Press All rights reserved. No part of this publication may be reproduced, stored in a retrieval system, or transmitted, in any form or by any means, without prior written permission of the publisher, or, in Canada, in the case of photocopying or other reprographic copying, a licence from Access Copyright (Canadian Copyright Licensing Agency), www.accesscopyright.ca. -
Bc26 Report.Pdf
BC Envir&hent SOILS OF THE ASHCROFT MAP AREA Report No. 26 British Columbia Soi1 Survey G. Young, M.A. Fenger and H.A. Luttmerding Integrated Management Branch Victoria, British Columbia 1992 Canadian Cataloguing in Publication Data Young, G. (Gavin), 1947- Soils of the Ashcroft map area (MOE technical report, ISSN 0821-0942 ; 23) (British Columbia soi1 survey, ISSN 03755886 ; report no. 26) Includes bibliographical references. ISBN 0-7718-8560-l 1. Soils - British Columbia - Ashcroft Region. 2. Soils - British Columbia - Ashcroft Region - Maps. 1. Fenger, M. A., 1949- . II. Luttmerding, H. A. III. British Columbia. B.C. Environment. IV. Title. V. Series. VI. Series: British Columbia soi1 survey ; report no. 26. 5599.1 .B7Y 68 1992 63 1.4’7’7 1172 C87-092050-2 0 Copyright 1992 B.C. Environment. SOILS OF THE ASHCROFT MAP AREA Acknowledgements Gratitude is expressedto numerous individuals who have contributed to the preparation of this report, particularly to P.N. Sprout, and H.A. Luttmerding who provided soi1 cor-relation services and gave advice for the preparation of the report. Appreciation is also extended to R.J. Williams, who prepared the climate section in the introduction, and to J. van Barneveld, and J. M. Ryder, whose advice regarding forest zonation and surficial geology, respectively, provided the necessary information which helped for-m the basis of the soils report. Thanks are also extended to Dr. A. van Ryswyk, R. Mitchell and Dr. A. McLean in Kamloops for reviewing the report. Thanks is also due to Barb Webb who did the initial Word processing and to Christine Keumper who completed the first draft. -
Determination of Site Use As Inferred from the Lithics Data of the Post
University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School 2004 Determination of Site Use as Inferred From the Lithics Data of the Post Adandonment Occupation of Housepit 7 at the Keatley Creek Site: Comparing Winter Village and Short-term Camp Models AndreÌ? B. Jendresen The University of Montana Follow this and additional works at: https://scholarworks.umt.edu/etd Let us know how access to this document benefits ou.y Recommended Citation Jendresen, AndreÌ? B., "Determination of Site Use as Inferred From the Lithics Data of the Post Adandonment Occupation of Housepit 7 at the Keatley Creek Site: Comparing Winter Village and Short- term Camp Models" (2004). Graduate Student Theses, Dissertations, & Professional Papers. 9339. https://scholarworks.umt.edu/etd/9339 This Thesis is brought to you for free and open access by the Graduate School at ScholarWorks at University of Montana. It has been accepted for inclusion in Graduate Student Theses, Dissertations, & Professional Papers by an authorized administrator of ScholarWorks at University of Montana. For more information, please contact [email protected]. Maureen and Mike MANSFIELD LIBRARY The University of Montana Permission is granted by the author to reproduce this material in its entirety, provided that this material is used for scholarly purposes and is properly cited in published works and reports. **Please check "Yes" or "No" and provide signature** Yes, I grant permission No, I do not grant permission Author’s Signature: Date:_ S/tb/oH_____________ Any copying for commercial purposes or financial gain may be undertaken only with the author’s explicit consent. -
Skwaha Lake Management Plan Final
M ANAGEMENT LAN P November, 1996 Ministry of for Skwaha Lake Environment, Lands and Parks BC Parks Department Ecological Reserve Skwaha Lake Ecological Reserve M ANAGEMENT LAN P Prepared by BC Parks Kamloops Area Pilot Project Team for Thompson River District Kamloops, B.C. Skwaha Lake Ecological Reserve Management Plan Table of Contents Introduction.....................................................................................................................................1 Background Summary ....................................................................................................................1 Role and Long-term Vision..............................................................................................................5 Management Objectives Grazing .................................................................................................................................6 Fencing .................................................................................................................................6 Fire........................................................................................................................................6 Traditional Uses.....................................................................................................................6 Introduced Plant Species........................................................................................................6 Forest Pests and Diseases.......................................................................................................6 -
Xwísten COMMUNITY PROFILE
XWÍSTEN COMMUNITY PROFILE MAY 2013 ISSUE #1 • FEBRUARY 2013 Xwísten The smiling people NXwísten The foamy waters after the rapids II Contents INTRODUCTION . 1. What is Xwísten’s Community Profile? 1 What is the Xwísten Comprehensive Community Plan? 2 OUR PEOPLE AND CULTURE . 5. History 5 Culture and Language 7 Population and Demographics 8 OUR COMMUNITY . 11. Education 11 Health and Wellness 14 Housing 17 Safety and Security 21 Social Development and Elders 23 GOVERNANCE AND ADMINISTRATION . .25 Elected Leadership 25 Band Administration 25 Xwísten Organization 26 OUR ECONOMY . .29 . Employment and Jobs 29 Economic Development Initiatives 30 OUR LAND AND RESOURCES . .33 . Our Lands 33 Land and Resource Management 34 APPENDIX. 37 Additional Details on Educational Programming 37 Xwísten Community Profile III IV Introduction Introduction What is Xwísten’s Community Profile? This Community Profile provides a ‘snap shot’ of current conditions in our community. It is meant to provide a starting point for preparing the Xwísten Comprehensive Community Plan. In addition to looking at what is happening now in our community, this profile provides some direction on areas that we may need to pay special attention to in our Comprehensive Community Plan. Most of all, it is meant to share information with members on how we are doing and to help get discussions going about where we want to go as a community and how. The profile has been organized into five sections: Our People and Culture – History, Culture and Language, Population and Demographics Our Community – Education, Health and Wellness, Housing, Safety and Security, Social Development Our Government – Leadership and Governance, Band Administration, Band Financial Health Our Economy – Employment and Jobs, Economic Development Initiatives Our Land – Our Land and Resources, Land Use Planning In each of these sections, we looked for trends so we can start thinking about how we can build on our strengths (the positive trends) and address our weaknesses (the negative trends). -
The Opening of Keatley Creek: Research Problems and Background Brian Hayden
Chapter 1 V.'.V aw V'v v.'.v v-'.'i aw '.■■!« v.'.V aw •:«; y.w \w awv.w w.'/ vw vwr v.w v«: v.w VvV.W •.'.v.' vjw vav wji aw \wva'. v w *.y •» w •» ’»• w *av <» w \y y.* *.y *.y *.y y.* *.y *.y *.y y.‘ w w y " w •» *.y y.* y.* y ; The Opening of Keatley Creek: Research Problems and Background Brian Hayden a a A A A A »l» Ml HI Ml III Ml . I l l Ml Ml .♦»». i'll (Vi m V •• ••• I M il Ml* — imiiiin mi L S iJ J J Introduction The Fraser River Investigations into Corporate tarian and nomadic, with no more than 25-50 members. Group Archaeology project (FRICGA) began in 1985 In contrast to simpler hunter/gatherers, some of the with a simple question: why unusually large housepits Lillooet communities housed well over 1,000 people occurred in the Lillooet area of the British Columbia living in seasonally sedentary houses with pronounced Interior Plateau. With hindsight, this was an ambitious wealth differences and hierarchies. undertaking, one fraught with massive data collection and many collateral problems. In the 1960's and 70's, The Lillooet region turned out to be an ideal location Amoud Stryd (1973) had pursued the elusive nature for dealing with all the above and many more of prehistoric social organization in the same region, archaeological issues. The Lillooet region is relatively only to be overwhelmed by the magnitude of the simple to model in terms of environments and undertaking. -
The Fraser Valley Milk Producers' Association
THE FRASER VALLEY MILK PRODUCERS' ASSOCIATION: SUCCESSFUL COOPERATIVE by Morag Elizabeth Maclachlan B.Ed, (sec), The University of British Columbia, 1964 A THESIS SUBMITTED IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF ARTS in the Department of History We accept this thesis as conforming to the required standard THE UNIVERSITY OF BRITISH COLUMBIA ••' April , 1972; In presenting this thesis in partial fuIfilment,of . the requirements for an advanced degree at the University of British Columbia, I agree that the Library shall make it freely available for reference and study. I further agree that permission for extensive copying of this thesis for scholarly purposes may be granted by the Head of my Department or by his representatives. It is understood that copying or publication of this thesis for financial gain shall not be allowed without my written permission. Department of The University of British Columbia Vancouver 8, Canada FRASER VALLEY MILK PRODUCERS' ASSOCIATION SUCCESSFUL COOPERATIVE In 1913 thirty dairy farmers formed the Fraser Valley Milk Producers Association, an organization which began operation in 1917 and became one of the most successful cooperatives in North America. The compact nature of the Fraser Valley was a geographic advantage which laid the basis for the success of the Association. The river itself, the railway and the roads which were built slowly and at great cost, provided transportation which unified the Valley. The insatiable Cariboo markets enabled pioneer farmers to become well established. The completion of the Canadian Pacific Railway opened wider markets which dairymen were able to.take advantage of after the creameries became established. -
Quaternary Stratigraphy and Geomorphology of Lower
QUATERNARY STRATIGRAPHY AND GEOMORPHOLOGY OF LOWER BRIDGE RIVER VALLEY, BRITISH COLUMBIA by DON EDWIN HOWES B.A., University of Western Ontario, 1971 A THESIS SUBMITTED IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE in the Department of Geography We accept this thesis as conforming to the required standard THE UNIVERSITY OF BRITISH COLUMBIA April, 1975 In presenting this thesis in partial fulfilment of the requirements for an advanced degree at the University of British Columbia, I agree that the Library shall make it freely available for reference and study. I further agree that permission for extensive copying of this thesis for scholarly purposes may be granted by the Head of my Department or by his representatives. It is understood that copying or publication of this thesis for financial gain shall not be allowed without my written permission. Department of The University of British Columbia Vancouver 8, Canada ii ABSTRACT Bridge River is an east-flowing tributary of Fraser River originating in the Coast Mountains of British Columbia . Its confluence with the Fraser River is near the village of Lillooet. This study encompasses the lower 15 miles (24 km) of Bridge River Valley. The purpose of the study is: (1) to describe and reconstruct the local Quaternary events and relate them to the regional chronology, (2) to produce a surficial geology map, at a scale of 1:50,000. Lacustrine, ice contact fluvio-glacial, fluvio-glacial (lacking ice contact features), glacial, alluvial fan and recent deposits occur here. From their characteristics and stratigraphic relationships, two alternative Quaternary chronologies can be reconstructed: A: Silts and clays deposited in a proglacial lake were subsequently overridden and partly deformed by ice of the last glaciation . -
Chapteir 5 Tectonic Implications"
Ministry of Employment and In vestment CHAPTEIR 5 TECTONIC IMPLICATIONS"- REGIONALCORRELATION AND which extends continuously along the southwestside ofthe SIGNIFICANCE OF MAIN Yalakom fault for 80 kilometres to Chilko Lake (Figure 39). At the southeast end of thisbelt, within theTaseko . Bridge LITHOTECTONIC ASSEMBLAGES River map area, this clastic succession is inferred to have BRIDGE RIVER TERRANE been deposited abovethe Bridge River Complex($e? Chap- ter 2). The Tyaughton basin beltis also bounded onits north- The Bridge River Terrane is represented the West side by sparse exposures ofthe BridgeRiver Complex BridgeRiver Complex, which includes Mississippianto (Riddell eT 1993a,b), indicating that the Bridge River Middle Jurassic chert, pillowed and massive greenstone, Complex probably underlies, in the subsurface, th3 entire limestone, clastic rocks and blueschist. The Taseko - Bridge belt of clastic sedimentary Theexposures at th north- River map area encompasses the northwestern end Of the west end of the belt, east of Chilko Lake, are bounded to the mainoutcrop beltoftheBridgeRiverComplex~A1ougstrike north by fault-bounded panels OfCadwaIlader and p/Iethow to thenorthwest is the main exposure beltJura-Creta-of terranes, and are the exposures of tl,e ceous clastic sedimentary rocksof the Tyaughton basin, Bridge River complex. Figure 39.Map showing the distributionof major tectonostratigraphic elementsof the southeastern Coast Beltin the Pemhrton, Taseko Lakes and Mount Waddington map sheets. BRC=narrow lens of Bridge River Complex east of Chilko Lake. Map is basec on the compilations of Schiarizza et ai. (1994) and Monger and Joumeay (1994). The Bridge River Terranealso includes local exposures cludes Permian limestone containing Tethyan fusilin :ds of clastic sedimentary rocks assignedto the Gun Lake and (Brandon et 41.