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Summary Report of the Geological Survey for the Calendar Year 1911
5 GEORGE V. SESSIONAL PAPER No. 26 A. 1915 SUMMARY REPORT OK THE GEOLOGICAL SURVEY DEPARTMENT OF MINES FOR THE CALENDAR YEAR 1914 PRINTED BY ORDER OF PARLIAMENT. OTTAWA PRTNTKD BY J. i»k L TAOHE, PRINTER TO THE KING'S MOST EXCELLENT IfAJESTS [No. 26—1915] [No , 15031 5 GEORGE V. SESSIONAL PAPER No. 26 A. 1915 To Field Marshal, Hit Hoi/al Highness Prince Arthur William Patrick Albert, Duke of Connaught and of Strath-earn, K.G., K.T., K.P., etc., etc., etc., Governor General and Commander in Chief of the Dominion of Canada. May it Please Youb Royal Highness.,— The undersigned has the honour to lay before Your Royal Highness— in com- pliance with t>-7 Edward YIT, chapter 29, section IS— the Summary Report of the operations of the Geological Survey during the calendar year 1914. LOUIS CODERRK, Minister of Mines. 5 GEORGE V. SESSIONAL PAPER No. 26 A. 1915 To the Hon. Louis Codebrk, M.P., Minister of Mines, Ottawa. Sir,—I have the honour to transmit, herewith, my summary report of the opera- tions of the Geological Survey for the calendar year 1914, which includes the report* of the various officials on the work accomplished by them. I have the honour to be, sir, Your obedient servant, R. G. MrCOXXFI.L, Deputy Minister, Department of Mines. B . SESSIONAL PAPER No. 28 A. 1915 5 GEORGE V. CONTENTS. Paok. 1 DIRECTORS REPORT REPORTS FROM GEOLOGICAL DIVISION Cairncs Yukon : D. D. Exploration in southwestern "" ^ D. MacKenzie '\ Graham island. B.C.: J. M 37 B.C. -
Varve-Related Publications in Alphabetical Order (Version 15 March 2015) Please Report Additional References, Updates, Errors Etc
Varve-Related Publications in Alphabetical Order (version 15 March 2015) Please report additional references, updates, errors etc. to Arndt Schimmelmann ([email protected]) Abril JM, Brunskill GJ (2014) Evidence that excess 210Pb flux varies with sediment accumulation rate and implications for dating recent sediments. Journal of Paleolimnology 52, 121-137. http://dx.doi.org/10.1007/s10933-014-9782-6; statistical analysis of radiometric dating of 10 annually laminated sediment cores from aquatic systems, constant rate of supply (CRS) model. Abu-Jaber NS, Al-Bataina BA, Jawad Ali A (1997) Radiochemistry of sediments from the southern Dead Sea, Jordan. Environmental Geology 32 (4), 281-284. http://dx.doi.org/10.1007/s002540050218; Dimona, Jordan, gamma spectroscopy, lead-210, no anthropogenic contamination, calculated sedimentation rate agrees with varve record. Addison JA, Finney BP, Jaeger JM, Stoner JS, Norris RN, Hangsterfer A (2012) Examining Gulf of Alaska marine paleoclimate at seasonal to decadal timescales. In: (Besonen MR, ed.) Second Workshop of the PAGES Varves Working Group, Program and Abstracts, 17-19 March 2011, Corpus Christi, Texas, USA, 15-21. http://www.pages.unibe.ch/download/docs/working_groups/vwg/2011_2nd_VWG_workshop_programs_and_abstracts.pdf; ca. 60 cm marine sediment core from Deep Inlet in southeast Alaska, CT scan, XRF scanning, suspected varves, 1972 earthquake and tsunami caused turbidite with scouring and erosion. Addison JA, Finney BP, Jaeger JM, Stoner JS, Norris RD, Hangsterfer A (2013) Integrating satellite observations and modern climate measurements with the recent sedimentary record: An example from Southeast Alaska. Journal of Geophysical Research: Oceans 118 (7), 3444-3461. http://dx.doi.org/10.1002/jgrc.20243; Gulf of Alaska, paleoproductivity, scanning XRF, Pacific Decadal Oscillation PDO, fjord, 137Cs, 210Pb, geochronometry, three-dimensional computed tomography, discontinuous event-based marine varve chronology spans AD ∼1940–1981, Br/Cl ratios reflect changes in marine organic matter accumulation. -
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. -
The Cordilleran Ice Sheet 3 4 Derek B
1 2 The cordilleran ice sheet 3 4 Derek B. Booth1, Kathy Goetz Troost1, John J. Clague2 and Richard B. Waitt3 5 6 1 Departments of Civil & Environmental Engineering and Earth & Space Sciences, University of Washington, 7 Box 352700, Seattle, WA 98195, USA (206)543-7923 Fax (206)685-3836. 8 2 Department of Earth Sciences, Simon Fraser University, Burnaby, British Columbia, Canada 9 3 U.S. Geological Survey, Cascade Volcano Observatory, Vancouver, WA, USA 10 11 12 Introduction techniques yield crude but consistent chronologies of local 13 and regional sequences of alternating glacial and nonglacial 14 The Cordilleran ice sheet, the smaller of two great continental deposits. These dates secure correlations of many widely 15 ice sheets that covered North America during Quaternary scattered exposures of lithologically similar deposits and 16 glacial periods, extended from the mountains of coastal south show clear differences among others. 17 and southeast Alaska, along the Coast Mountains of British Besides improvements in geochronology and paleoenvi- 18 Columbia, and into northern Washington and northwestern ronmental reconstruction (i.e. glacial geology), glaciology 19 Montana (Fig. 1). To the west its extent would have been provides quantitative tools for reconstructing and analyzing 20 limited by declining topography and the Pacific Ocean; to the any ice sheet with geologic data to constrain its physical form 21 east, it likely coalesced at times with the western margin of and history. Parts of the Cordilleran ice sheet, especially 22 the Laurentide ice sheet to form a continuous ice sheet over its southwestern margin during the last glaciation, are well 23 4,000 km wide. -
British Columbia Ministry of Natural Resource Operations Regional
T a t s h e n s h in i R i v e r K r e Tutshi Lake l e s v a i ys R ll d iv R r R la e r e k i v G iv e e Swift R L iver Petitot River s r R B a Petitot R l t e Gladys Lake iver if av B A e ic Hall Lake w r h Tagish Lake S R e Teslin Lake w R iv Ri Cro iv e ve i er k e r r w ft Riv e r P S et r re Maxhamish Lake it e o C t Surprise Lake iv er Riv s R R ia u ek iv s her er g re e nc iv n C r y Ra R r illy Peti d A e tot R a e e i l l u k v D v t l c i S e G it B a a r J l R h L d e B G o r h a n ree t r n i a ve it C k y Liard River er a i n k ling iv h R in n m R i R C O l g l iv 'Don e s S e a n K r e r Riv Ts e Atlin Lake er e r k S R e h iver v e nts R i e d k A R e R a i r i n l e s v er V K a h i wig i iv e R C oko a ree R Sl R n k i R i k T M iv a cDame Cre a v e e N k u C ek p r r e y i G o d lu e a ndeb Cr t R ery t T R o i e n ve T s i r r li v w er o e o n od Riv iv u er Gu R r R nda a se R h t i De o R v a e Tuya Lake o Sa Kotcho Lake r i h b I r R v t n e e a b i k v v r n l i i it e e n R R r h R Nahl r in e R iv e l er i iv e R iv v e i r i r T ve i R N r v M ro R u e r t D e e R ud s u i r K e v i r t e e d a l o s r iv le g F o R d o e r K r n a n ive in o e D R d Cr k o v t e u d e e r i r E C n Fort Nelson t e R a ch iv e R o u y v r D o R i e T a i D R v e ek H e a re e k o C n r Cry Lake T l ykl i urn l K h aga iver R la in R t iv u e Nets on S r Cre e S Dease Lake k h e B K Elleh Cre s e utc ek la a h tt o y y Cr R e T C ek r o nta iv Ri e s Creek Fo s r v iv e e lla e r a v e nzi r e R d R r a e e T v g h i i o R -
BC OGC Water Use in Oil and Gas Activities 2012
Water Use in Oil and Gas Activities Quarterly Updates on Short-Term Water Approvals and Use Q2 (April-June 2012) / Q3 (July-September 2012) About Us More Information BC Oil and Gas Commission Contact www.bcogc.ca Table of Contents The BC Oil and Gas Commission (Commission) is The short-term water approvals and usage data is the single-window regulatory agency with responsibilities updated quarterly with new information and statistics. A About the BC Oil and Gas Commission 2 for regulating oil and gas activities in British Columbia, current copy is available on the Commission website at More Information and Contact 2 including exploration, development, pipeline www.bcogc.ca, along with: transportation and reclamation. • Oil and Gas Activities Act and Water Act Update on Short-Term Water Approvals and Use 3 • Short-term Use of Water Application Manual The Commission’s core services include reviewing and • Data files of all Active Section 8 Approvals Water Used in Oil and Gas Activities 3 assessing applications for industry activity, consulting • 2011 Annual Water Report and Quarterly with First Nations, cooperating with partner agencies, Updates (Jan-Mar, Apr-Jun, Jul-Sep) Total Approvals and Reported Use 4 and ensuring industry complies with provincial legislation • 2012 Quarterly Updates Table 2 – Q2 Section 8 Data 6 and all regulatory requirements. The public interest • Northeast Water Tool is protected by ensuring public safety, respecting Table 3 – Q3 Section 8 Data 10 those affected by oil and gas activities, conserving the environment, and ensuring equitable participation in For specific questions or enquiries regarding this data, Appendix A – Water Source Well Production 14 production. -
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. -
Bibliography of PHYSI~AL LIMNOLOGY
STATE OF OHIO DEPARTMENT OF NATURAL RESOURCES DIVISION OF SHORE EROSION DIVISION OF GEOLOGICAL SURVEY REPORT OF INVESTIGATIONS NO. 25 (CONTRIBUTION NO. 4 LAKE ERIE GEOLOGICAL RESEARCH PROGRAM) Bibliography Of PHYSI~AL LIMNOLOGY 1781 ••••1954 COLUMBUS 1955 STATE OF OHIO Frank J. Lausche, Governor DEPAR 1MENT OF NATURAL RESOURCES A. W. Marion, Director NATURAL RESOURCES COMMISSION George Wenger, Chairman John A. Slipher, Bryce Browning, Vice Chairman Secretary C. D. Blubaugh Dr. John L. Rich Dr. C. L. Dow Milton Ronsheim A. W. Marion Dean L. L. Rummell DIVISION OF GEOLOGICAL SURVEY John H. Melvin, Chief DIVIS ION OF SHORE EROSION F . 0 , Kugle , Chief STATE OF OHIO Frank J. Lausche, Governor DEPARTMENT OF NATURAL RESOURCES A. W. Marion, Director DIVISION OF SHORE EROSION F. 0. Kugel, Chief DIVISION OF GEOLOGICAL SURVEY John H. Melvin, Chief REPORT OF INVESTIGATIONS NO. 2 5 (CONTRIBUTION NO. 4 LAKE ERIE GEOLOGICAL RESEARCH PROGRAM) BIBLIOGRAPHY OF PHYSICAL LIMNOLOGY 1781 .... 1954 By James L. Verber This publication is a cooperative project of the Division of Shore Erosion and The Division of Geological Survey. The research upon which the publication is based has been sponsored chiefly by t the Division of Shore Erosion. i COLUMBUS, 1955 I Blank Page t:;ONTENTS Page INTRODUCTION •••••••••• v Organization of the Index • v Suggestions on using the Index vi ABBREVIATIONS • vii BmLIOGRAPHY 1 INDEX and ALPHABETICAL LIST OF LAKES CITED 45 ADDENDUM WITH INDEX . • . 54 iii Blank Page INTBODU~TION The Bibliography of Physical Limnology, 1781- their assistance in preparing the manuscript for publica- 1953, contains both a bibliography and subject index tion. -
The Forest Vegetation of the Driftless Area, Northeast Iowa Richard A
Iowa State University Capstones, Theses and Retrospective Theses and Dissertations Dissertations 1976 The forest vegetation of the driftless area, northeast Iowa Richard A. Cahayla-Wynne Iowa State University Follow this and additional works at: https://lib.dr.iastate.edu/rtd Part of the Botany Commons, Ecology and Evolutionary Biology Commons, Other Forestry and Forest Sciences Commons, and the Plant Pathology Commons Recommended Citation Cahayla-Wynne, Richard A., "The forest vegetation of the driftless area, northeast Iowa" (1976). Retrospective Theses and Dissertations. 16926. https://lib.dr.iastate.edu/rtd/16926 This Thesis is brought to you for free and open access by the Iowa State University Capstones, Theses and Dissertations at Iowa State University Digital Repository. It has been accepted for inclusion in Retrospective Theses and Dissertations by an authorized administrator of Iowa State University Digital Repository. For more information, please contact [email protected]. The forest vegetation of the driftless area, northeast Iowa by Richard A. Cahayla-Wynne A Thesis Submitted to the Graduate Faculty in Partial Fulfillment of The Requirements for the Degree of MASTER OF SCIENCE Department: Botany and Plant Pathology Major: Botany (Ecology) Signatures have been redacted for privacy Iowa State University Ames, Iowa 1976 ii TABLE OF CONTENTS Page INTRODUCTION 1 STUDY AREA 6 METHODS 11 RESULTS 17 DISCUSSION 47 SUMMARY 55 LITERATURE CITED 56 ACKNOWLEDGMENTS 59 APPENDIX A: SPECIES LIST 60 APPENDIX B: SCIENTIFIC AND COMMON NAMES OF TREES 64 APPENDIX C: TREE BASAL AREA 65 1 INTRODUCTION Iowa is generally pictured as a rolling prairie wooded only along the water courses. The driftless area of northeast Iowa is uniquely contrasted to this image; northeast Iowa is generally forested throughout, often with rugged local relief. -
Bildnachweis
Bildnachweis Im Bildnachweis verwendete Abkürzungen: With permission from the Geological Society of Ame- rica l – links; m – Mitte; o – oben; r – rechts; u – unten 4.65; 6.52; 6.183; 8.7 Bilder ohne Nachweisangaben stammen vom Autor. Die Autoren der Bildquellen werden in den Bildunterschriften With permission from the Society for Sedimentary genannt; die bibliographischen Angaben sind in der Literaturlis- Geology (SEPM) te aufgeführt. Viele Autoren/Autorinnen und Verlage/Institutio- 6.2ul; 6.14; 6.16 nen haben ihre Einwilligung zur Reproduktion von Abbildungen gegeben. Dafür sei hier herzlich gedankt. Für die nachfolgend With permission from the American Association for aufgeführten Abbildungen haben ihre Zustimmung gegeben: the Advancement of Science (AAAS) Box Eisbohrkerne Dr; 2.8l; 2.8r; 2.13u; 2.29; 2.38l; Box Die With permission from Elsevier Hockey-Stick-Diskussion B; 4.65l; 4.53; 4.88mr; Box Tuning 2.64; 3.5; 4.6; 4.9; 4.16l; 4.22ol; 4.23; 4.40o; 4.40u; 4.50; E; 5.21l; 5.49; 5.57; 5.58u; 5.61; 5.64l; 5.64r; 5.68; 5.86; 4.70ul; 4.70ur; 4.86; 4.88ul; Box Tuning A; 4.95; 4.96; 4.97; 5.99; 5.100l; 5.100r; 5.118; 5.119; 5.123; 5.125; 5.141; 5.158r; 4.98; 5.12; 5.14r; 5.23ol; 5.24l; 5.24r; 5.25; 5.54r; 5.55; 5.56; 5.167l; 5.167r; 5.177m; 5.177u; 5.180; 6.43r; 6.86; 6.99l; 6.99r; 5.65; 5.67; 5.70; 5.71o; 5.71ul; 5.71um; 5.72; 5.73; 5.77l; 5.79o; 6.144; 6.145; 6.148; 6.149; 6.160; 6.162; 7.18; 7.19u; 7.38; 5.80; 5.82; 5.88; 5.94; 5.94ul; 5.95; 5.108l; 5.111l; 5.116; 5.117; 7.40ur; 8.19; 9.9; 9.16; 9.17; 10.8 5.126; 5.128u; 5.147o; 5.147u; -
88 Reasons to Love Alberta Parks
88 Reasons to Love Alberta Parks 1. Explore the night sky! Head to Miquelon Lake Provincial Park to get lost among the stars in the Beaver Hills Dark Sky Preserve. 2. Experience Cooking Lake-Blackfoot Provincial Recreation Area in the Beaver Hills UNESCO Biosphere Reserve. This unique 1600 square km reserve has natural habitats that support abundant wildlife, alongside agriculture and industry, on the doorstep of the major urban area of Edmonton. 3. Paddle the Red Deer River through the otherworldly shaped cliffs and badlands of Dry Island Buffalo Jump Provincial Park. 4. Wildlife viewing. Our parks are home to many wildlife species. We encourage you to actively discover, explore and experience nature and wildlife safely and respectfully. 5. Vibrant autumn colours paint our protected landscapes in the fall. Feel the crunch of fallen leaves underfoot and inhale the crisp woodland scented air on trails in many provincial parks and recreation areas. 6. Sunsets illuminating wetlands and lakes throughout our provincial parks system, like this one in Pierre Grey’s Lakes Provincial Park. 7. Meet passionate and dedicated Alberta Parks staff in a visitor center, around the campground, or out on the trails. Their enthusiasm and knowledge of our natural world combines adventure with learning to add value to your parks experiences!. 8. Get out in the crisp winter air in Cypress Hills Provincial Park where you can explore on snowshoe, cross-country ski or skating trails, or for those with a need for speed, try out the luge. 9. Devonshire Beach: the natural white sand beach at Lesser Slave Lake Provincial Park is consistently ranked as one of the top beaches in Canada! 10. -
Geomorphic and Sedimentological History of the Central Lake Agassiz Basin
Electronic Capture, 2008 The PDF file from which this document was printed was generated by scanning an original copy of the publication. Because the capture method used was 'Searchable Image (Exact)', it was not possible to proofread the resulting file to remove errors resulting from the capture process. Users should therefore verify critical information in an original copy of the publication. Recommended citation: J.T. Teller, L.H. Thorleifson, G. Matile and W.C. Brisbin, 1996. Sedimentology, Geomorphology and History of the Central Lake Agassiz Basin Field Trip Guidebook B2; Geological Association of CanadalMineralogical Association of Canada Annual Meeting, Winnipeg, Manitoba, May 27-29, 1996. © 1996: This book, orportions ofit, may not be reproduced in any form without written permission ofthe Geological Association ofCanada, Winnipeg Section. Additional copies can be purchased from the Geological Association of Canada, Winnipeg Section. Details are given on the back cover. SEDIMENTOLOGY, GEOMORPHOLOGY, AND HISTORY OF THE CENTRAL LAKE AGASSIZ BASIN TABLE OF CONTENTS The Winnipeg Area 1 General Introduction to Lake Agassiz 4 DAY 1: Winnipeg to Delta Marsh Field Station 6 STOP 1: Delta Marsh Field Station. ...................... .. 10 DAY2: Delta Marsh Field Station to Brandon to Bruxelles, Return En Route to Next Stop 14 STOP 2: Campbell Beach Ridge at Arden 14 En Route to Next Stop 18 STOP 3: Distal Sediments of Assiniboine Fan-Delta 18 En Route to Next Stop 19 STOP 4: Flood Gravels at Head of Assiniboine Fan-Delta 24 En Route to Next Stop 24 STOP 5: Stott Buffalo Jump and Assiniboine Spillway - LUNCH 28 En Route to Next Stop 28 STOP 6: Spruce Woods 29 En Route to Next Stop 31 STOP 7: Bruxelles Glaciotectonic Cut 34 STOP 8: Pembina Spillway View 34 DAY 3: Delta Marsh Field Station to Latimer Gully to Winnipeg En Route to Next Stop 36 STOP 9: Distal Fan Sediment , 36 STOP 10: Valley Fill Sediments (Latimer Gully) 36 STOP 11: Deep Basin Landforms of Lake Agassiz 42 References Cited 49 Appendix "Review of Lake Agassiz history" (L.H.