Summary Report of the Geological Survey for the Calendar Year 1911
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The Big Chill
THE BIG CHILL Royal Saskatchewan Museum THE BIG CHILL For further information please contact: Public Programs Royal Saskatchewan Museum 2445 Albert Street Regina, Saskatchewan S4P 4W7 Email: [email protected] Website: www.royalsaskmuseum.ca © Royal Saskatchewan Museum 2012 The contents of this resource package may be reproduced for classroom use only. No portion may be duplicated for publication or sale. The following material provides teachers and students with information about the Ice Age in what is now Saskatchewan (remember, there was no such thing as Saskatchewan in those days!): • To describe Saskatchewan’s climate during the Ice Age. • To illustrate the geological effects of glaciation. • To recognize a variety of animals that lived in Saskatchewan during the Ice Age. Vocabulary advance geology climate glacier debris ice age deposit drumlin esker meltwater erratic moraine evaporation fauna retreat flora stagnant flow till fossil Laurentide Ice Sheet knob and kettle Wisconsin Glacial Period Pleistocene Epoch BACKGROUND INFORMATION Ice Ages The Ice Age or Pleistocene Epoch refers to the last two million years of our geological history when there were at least five periods of glaciation in North America. Gradual climate cooling caused huge continental ice sheets to form. Later, gradual warming caused these to melt during the interglacial periods. The last glacier began forming approximately 110,000 years ago, building until it covered all but the Cypress Hills and the Wood Mountain Plateau region of the Province. The last interglacial period started about 17,000 years ago. The ice sheet melted completely from our borders about 10,000 years ago. This last period of glaciation is called the Wisconsin Glacial Period. -
Archeological and Bioarcheological Resources of the Northern Plains Edited by George C
Tri-Services Cultural Resources Research Center USACERL Special Report 97/2 December 1996 U.S. Department of Defense Legacy Resource Management Program U.S. Army Corps of Engineers Construction Engineering Research Laboratory Archeological and Bioarcheological Resources of the Northern Plains edited by George C. Frison and Robert C. Mainfort, with contributions by George C. Frison, Dennis L. Toom, Michael L. Gregg, John Williams, Laura L. Scheiber, George W. Gill, James C. Miller, Julie E. Francis, Robert C. Mainfort, David Schwab, L. Adrien Hannus, Peter Winham, David Walter, David Meyer, Paul R. Picha, and David G. Stanley A Volume in the Central and Northern Plains Archeological Overview Arkansas Archeological Survey Research Series No. 47 1996 Arkansas Archeological Survey Fayetteville, Arkansas 1996 Library of Congress Cataloging-in-Publication Data Archeological and bioarcheological resources of the Northern Plains/ edited by George C. Frison and Robert C. Mainfort; with contributions by George C. Frison [et al.] p. cm. — (Arkansas Archeological Survey research series; no. 47 (USACERL special report; 97/2) “A volume in the Central and Northern Plains archeological overview.” Includes bibliographical references and index. ISBN 1-56349-078-1 (alk. paper) 1. Indians of North America—Great Plains—Antiquities. 2. Indians of North America—Anthropometry—Great Plains. 3. Great Plains—Antiquities. I. Frison, George C. II. Mainfort, Robert C. III. Arkansas Archeological Survey. IV. Series. V. Series: USA-CERL special report: N-97/2. E78.G73A74 1996 96-44361 978’.01—dc21 CIP Abstract The 12,000 years of human occupation in the Northwestern Great Plains states of Montana, Wyoming, North Dakota, and South Dakota is reviewed here. -
The Archaeology of Brabant Lake
THE ARCHAEOLOGY OF BRABANT LAKE A Thesis Submitted to the College of Graduate Studies and Research in Partial Fulfilment of the Requirements for the Degree of Master of Arts in the Department of Anthropology and Archaeology University of Saskatchewan Saskatoon By Sandra Pearl Pentney Fall 2002 © Copyright Sandra Pearl Pentney All rights reserved. PERMISSION TO USE PERMISSION TO USE In presenting this thesis in partial fulfilment of the requirements for a Postgraduate degree from the University of Saskatchewan, I agree that the Libraries of this University may make it freely available for inspection. I further agree that permission for copying of this thesis in any manner, in whole or in part, for scholarly purposes may be granted by the professor or professors who supervised my thesis work or, In their absence, by the Head of the Department or the Dean of the College in which my thesis work was done. It is understood that any copying or publication or use of this thesis or parts thereof for financial gain shall not be allowed without my written permission. It is also understood that due recognition shall be given to me and to the University of Saskatchewan in any scholarly use which may be made of any material in my thesis. Requests for permission to copy or to make other use of material in this thesis in whole or part should be addressed to: Head of the Department of Anthropology and Archaeology University of Saskatchewan Saskatoon, Saskatchewan (S7N 5B 1) ABSTRACT Boreal forest archaeology is costly and difficult because of rugged terrain, the remote nature of much of the boreal areas, and the large expanses of muskeg. -
CONTEXT DOCUMENT on the FUR TRADE of NORTHEASTERN
CONTEXT DOCUMENT on the FUR TRADE OF NORTHEASTERN NORTH DAKOTA (Ecozone #16) 1738-1861 by Lauren W. Ritterbush April 1991 FUR TRADE IN NORTHEASTERN NORTH DAKOTA {ECOZONE #16). 1738-1861 The fur trade was the commercia1l medium through which the earliest Euroamerican intrusions into North America were made. Tl;ns world wide enterprise led to the first encounters between Euroamericar:is and Native Americans. These contacts led to the opening of l1ndian lands to Euroamericans and associated developments. This is especial,ly true for the h,istory of North Dakota. It was a fur trader, Pierre Gaultier de Varennes, Sieur de la Ve--endrye, and his men that were the first Euroamericans to set foot in 1738 on the lar;ids later designated part of the state of North Dakota. Others followed in the latter part of the ,eighteenth and first half of the nineteenth century. The documents these fur traders left behind are the earliest knowr:i written records pertaining to the region. These ,records tell much about the ear,ly commerce of the region that tied it to world markets, about the indigenous popu,lations living in the area at the time, and the environment of the region before major changes caused by overhunting, agriculture, and urban development were made. Trade along the lower Red River, as well as along, the Misso1.:1ri River, was the first organized E uroamerican commerce within the area that became North Dakota. Fortunately, a fair number of written documents pertainir.1g to the fur trade of northeastern North 0akota have been located and preserved for study. -
Paleosols of the Interglacial Climates in Canada
Document generated on 09/28/2021 2:47 p.m. Géographie physique et Quaternaire Paleosols of the Interglacial Climates in Canada Les paléosols du Canada au cours des périodes interglaciaires Paläoböden zur Zeit der Interglaziale in Kanada Charles Tarnocai The Last? Interglaciation in Canada Article abstract Le dernier (?) interglaciaire au Canada Although paleosols are useful indicators of paleoclimates. it is first necessary to Volume 44, Number 3, 1990 establish the relationships between the northern limits of the various contemporary soils and the pertinent climatic parameters. It is then necessary URI: https://id.erudit.org/iderudit/032836ar to determine the age of the various paleosols and, if possible, their northern DOI: https://doi.org/10.7202/032836ar limits. Comparison of the distribution and northern limits of the contemporary soils with the distribution and northern limits of the analogous paleosols then permits the reconstruction of the paleoenvironments. For the purposes of See table of contents comparison the mean annual temperature of the Old Crow area during the Pliocene epoch was also determined (about 4°C) even though this was not an interglacial period. It was found that during the pre-lllinoian interglacial Publisher(s) periods the central Yukon had a mean annual temperature of about 7°C while during the Sangamonian interglacial period it had a mean annual temperature Les Presses de l'Université de Montréal of about - 3°C. During the Holocene epoch, the current interglacial period, the climate has been similar to or only slightly cooler than that existing during the ISSN Sangamonian interglacial period. The fluctuating position of the arctic tree line 0705-7199 (print) (and associated forest soils) during the Holocene epoch, however, indicates 1492-143X (digital) that the climate has also been fluctuating during this time. -
1E'r County Counci 1 Meeting
I ;;>fee.:<"" t�, . R�§l'1e'r County Counci 1 Meeting . c·ounty of Athabas. ca �o. 12 Tuesday, July 24, 1984 Present: Reeve Kostil•<; Councillors Flasha, Bencharsky, Le>�is, Keith (A./1. only), tlatoga, Johnson, Patry and Richards; County Administrator L. l. Gurel; Assistant Secretary-Treasurer H. R. Jodry; Hunictpal Intern 8. Waldowski. Ca II to Order: Reeve r<osti•' called the meeting to order at 10:00 A.M. �li nutes: It was moved by Councillor Richards that the minutes of the regular County Counci1 meeting of Ju11e 28, 1984, be ap�r.oveld as corrected. Hotion carried. Corr.ection on Page 6498 under heading Drainage - Amlsk Lake. Amend motion as follows: "It by the •1as moved Counci IIor Flasha to amend .agreement for Charron Creek from $40,000. to ·$65;000. and .... " It was moved by Counct llor Flasha that the minutes of the regular County Council meeting of July 3, 1984, be approved as corrected. Motion carried. Correction on Page 65DI under heading Family & ·community Support Services. Amend sentence as· fo 110\•IS: .. "Counci Ilor ·Patry reported Aganda: It •1as moved by Counci Ilor Hatoga that the agenda, wl th additions, be accepted by Counci I. Motion carried unanimously. 1•\tnutes : It •<as moved by Counci Ilor Bencharsky that the minutes of the special County Council meeting of July 6, 1984, be approved as corrected. /•lotion carried. Correction under heading \�estern ·rractot· as follo1·1s: "Harranty on elther Grader - 6 months ••." De Iega t ion: R. Keglowitsch, County A.L.S., attended the meeting at this time to . -
Septembre 2016 Utilisation Du Guide Des Points
MARCHANDISES GÉNÉRALES Points de Service Day & Ross Marchandises Générales Septembre 2016 Utilisation du guide des points Les points de parité et le guide des points publiés Tout tarif appliqué à un point associé à un point de parité ou basé sur celui-ci sera le même que le tarif du point de base. Par exemple, Dieppe, au Nouveau-Brunswick, PROV VILLE TERMINAL NOTE 1 NOTE 2 POINT DE BASE dont le terminal de livraison est Moncton (MTN), est associé à Moncton, au Nouveau-Brunswick. NB DIEPPE MTN MONCTON Par conséquent, tous les taux et frais de la grille tarifaire s’appliquant à Moncton, s’appliqueront également à Dieppe. Changements et exceptions Cette application ne peut pas être utilisée lorsque le tarif est publié pour un point autre qu’un point de parité tel que Dieppe. Par conséquent, le point précisé dans le tarif du client aura préséance, que Moncton soit également publié dans ce tarif ou non. Les tarifs des points ultérieurs de Corner Brook à Labrador sont saisonniers. Les tarifs aériens s’appliqueront en hiver si le service est oert, en absence du service de traversier, sinon les expéditions à destination de Labrador ne seront pas acceptées, à moins que le service puisse être assuré par le terminal de Québec. Les tarifs vers certains points du nord-ouest, de Nunavut, du Yukon et du Labrador peuvent changer en hiver et pendant la période de débâcle du printemps à cause des fermetures de route et de l’interruption du service de traversier. Le service aérien sera oert sur demande. Notes La note 1 du guide des points porte sur les jours de service supplémentaires qui pourraient s’avérer nécessaires. -
The Birds of Western Manitoba. [J^'Y
9 20 Seton on the Birds of Western Manitoba. [J^'y April 3, and was abundant until the first of April. A single individual, 22, iSSs- 107. Philohela minor. —A few during March, 1885. *io8. Gallinago delicata. —Not seen in 1884. First seen March 6, 18S5, and last seen April 7. Abundant. *i09. Tetanus solitarius. —A few in April, 1S84, and April, 1S85. no. Actitis macularius.—First seen April, 17, 1SS4, and April 15, 1SS5. Not common. 111. Fulica americana. —One found dead. April 23, 18S4. 112. Branta canadensis. —-One flock, March 3, 1SS5. 113. Anas discors. —Common in April, 1885. 114. Aix sponsa. — One pair, April 4, 1SS5. THE BIRDS OF WESTERN MANITOBA. BY ERNE.ST E. T. SETON. ( Concluded from p. 156.) 130. Trochilus colubris. Ruby-throated Hummingbird. —Not ob- served by me in any part of the Assiniboine Valley, though given a.^ "occasional at Qii'Appelle" ; "specimens seen on Red Deer River, August 16, 1881," and tolerably common along the Red Ri\er. 131. Milvulus forficatus. Scissor-tailed Flycatcher. —Accidental. One found bv Mr. C. W. Nash at Portage la Prairie. October, 1SS4. (See Auk, April, 1S85, p. 2iS.)' 132. Tyrannus tyrannus. Kingbird.—Very abundant summer resi- dent all over. Very common throughout the Winnipegoosis region. Ar- rives May 24; departs August 30. 133. Myiarchus crinitus. Crested Flycatcher. —Very rare summer resident about Winnipeg. Not taken in Assiniboine region, though I believe I have several times heard it near the Big Plain. Taken by Pro- fessor Macoun at Lake Manitoba, June 17, 18S1. 134. Sayornis phcebe. Phcebe. -
113 HITHER and YON DOUGLAS H. WILLIAMSON, Head of Department
113 HITHER AND YON DOUGLAS H. WILLIAMSON, Head of Department of Geology and Sir James Dunn Professor of Geology at MOUNT ALLISON UNIVERSITY for the past twelve years, is leaving at the end of the present academic year to take up a new appointment as Professor and Head of the Department of Geology at LAURENTIAN UNIVERSITY, Sudbury, Ontario. Dr. Williamson intends to continue with his mapping and research work on the Caledonia Mountain Complex in southeastern New Brunswick. DR. H.B. WHITTINGTON of HARVARD UNIVERSITY, Professor of Geology and curator of invertebrate paleontology in the Museum of Comparative Zoology, has been appointed to succeed PROFESSOR O.M.B. BULMAN as Woodwardian Professor of Geology in the UNIVERSITY OF CAMBRIDGE. This chair is the oldest geological endowment in Britain. Professor Whittington has had wide experience of geology in many countries, and has taught at univers- ities in Britain, Burma and China as well as, since 1949, at Harvard. An internationally recognised authority on trilobites, he has been asked by the GEOLOGICAL SURVEY OF CANADA to direct excavations of the Burgess Shale (Middle Cambrian) in British Columbia; he is also involved in paleontological studies in Western Newfoundland. Direction of these studies will presumably continue from Cambridge. (Reported in Nature, 5 March 1966). New members of staff at McMASTER UNIVERSITY, Hamilton, Ontario, are DR. ROBERT HARRISS, a sedimentary geochemist who gained his Ph.D. degree at RICE UNIVERSITY and has just completed a year of postdoctoral work at HARVARD UNIVERSITY with DR. RAYMOND SIEVER. His interests include chemical weathering and the geochemistry of natural waters. -
Detroit River Group in the Michigan Basin
GEOLOGICAL SURVEY CIRCULAR 133 September 1951 DETROIT RIVER GROUP IN THE MICHIGAN BASIN By Kenneth K. Landes UNITED STATES DEPARTMENT OF THE INTERIOR Oscar L. Chapman, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director Washington, D. C. Free on application to the Geological Survey, Washington 25, D. C. CONTENTS Page Page Introduction............................ ^ Amherstburg formation................. 7 Nomenclature of the Detroit River Structural geology...................... 14 group................................ i Geologic history ....................... ^4 Detroit River group..................... 3 Economic geology...................... 19 Lucas formation....................... 3 Reference cited........................ 21 ILLUSTRATIONS Figure 1. Location of wells and cross sections used in the study .......................... ii 2. Correlation chart . ..................................... 2 3. Cross sections A-«kf to 3-G1 inclusive . ......................;.............. 4 4. Facies map of basal part of Dundee formation. ................................. 5 5. Aggregate thickness of salt beds in the Lucas formation. ........................ 8 6. Thickness map of Lucas formation. ........................................... 10 7. Thickness map of Amherstburg formation (including Sylvania sandstone member. 11 8. Lime stone/dolomite facies map of Amherstburg formation ...................... 13 9. Thickness of Sylvania sandstone member of Amherstburg formation.............. 15 10. Boundary of the Bois Blanc formation in southwestern Michigan. -
Canadian Heritage Rivers System Management Plan for the Thelon River, N.W.T
CANADIAN HERITAGE RIVERS SYSTEM MANAGEMENT PLAN FOR THE THELON RIVER, N.W.T. Sector Tourism I 11-40.12 Plans/Strategies I I I - CANADIAN HERITAGE RIVERS SYSTEM MANAGEMENT PLAN FOR THE THELON RIVER, N.W.T. NWT EDT Can The 1990 — CANADIAN HERITAGE RIVERS SYSTEM MANAGEMENT PLAN FOR THE THELON RIVER, N. W.T. Submitted by the Municipality of Baker Lake; the Department of Economic Development and Tourism Government of the Northwest Territories; and the Department of Indian Affairs and Northern Development of Canada 1990 TABLE OF CONTENTS . 1.0 Introduction . 1.1 Thelon Heritage River Nomination . 1 1.2 Regional Setting and River Description . 1 1.3 Canadian Heritage Rivers System . 4 1.4 Purpose of the Management Plan . 4 l.4.1 General Considerations . 4 1.4.2 Objectives of the Thelon River Management Plan. 5 2.0 Background 2.1 History of the Nomination . 6 2.2 Public Support and Consultation . 6 2.3 Present Land Use . 8 2.3. lBaker Lake Inuit Land Use . 8 2.3.2 Land Tenure and Land Claims . 8 2.3.3 Mining and Other Development . 10 3.0 Heritage Values 3.1 Natural Heritage Values . 11 3.2 Human Heritage Values . 12 3.3 Recreational Values . 13 4.0 Planning and Management Program 4.1 Land Use Framework.. ~ . 15 4.1. 1 River Corridor . 15 4.1.2 Areas of Significance . 15 4.1.3 Potential Territorial Parks . 18 4.2 Heritage Management and Protection . 20 4.2.1 Human Heritage . 20 4.2.2 Natural Heritage . 21 4.2. -
Project Description Larder and Raven Hydroelectric Generating Station
Project Description Larder and Raven Hydroelectric Generating Station 1 Distribution: Canadian Environmental Assessment Agency Federal Agencies to be contacted by the Federal Environmental Assessment Coordinator Environment Canada Fisheries and Oceans Canada Health Canada Indian and Northern Affairs Canada Natural Resources Canada Transport Canada Other departments as identified by CEAA Provincial Agencies Ministry of Aboriginal Affairs Ministry of Tourism and Culture Ministry of Energy and Infrastructure Ministry of the Environment Ministry of Municipal Affairs and Housing Ministry of Natural Resources Ministry of Transportation Ministry of Northern Development, Mines and Forestry Ontario Waterpower Association Ontario Parks- Larder Lake Provincial Park Municipal Town of Larder Lake and Township of Larder Lake Town of Englehart Township of McGarry Township of Evanturel Town of Kirkland Lake First Nations Matachewan First Nation Beaverhouse First Nation Métis Nation of Ontario Wabun Tribal Council 2 TABLE OF CONTENTS 1. GENERAL INFORMATION .............................................................................................. 5 1.1 GENERAL ........................................................................................................................ 5 1.1.1 Name and Proposed Location of Project ................................................................ 5 1.1.2 Nature of the Project ................................................................................................ 5 1.1.3 Purpose of the Project .............................................................................................