An Assessment of Coalbed Methane Exploration Projects in Canada
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2007 Executive Committee Strategies to Successfully Manage
Canadian Publication Mail Contract - 40070050 $3.00 VOLUME 33, ISSUE 11 DECEMBER 2006 ■ 2007 Executive Committee ■ Strategies to Successfully Manage Longevity ■ Potwar of Pakistan – A General Study ■ Uncertainty Assessment in 3D Reservoir Modeling CSPG OFFICE #600, 640 - 8th Avenue SW Calgary,Alberta, Canada T2P 1G7 Tel:403-264-5610 Fax: 403-264-5898 Web: www.cspg.org Office hours: Monday to Friday, 8:30am to 4:00pm Business Manager:Tim Howard CONTENTS Email: [email protected] Communications Manager: Jaimè Croft Larsen Email: [email protected] Conventions Manager: Lori Humphrey-Clements Email: [email protected] Corporate Relations Manager: Kim MacLean Email: [email protected] ARTICLES Membership Services: Sarah Barton Email: [email protected] Reception/Administration:Tanya Santry CONGRATULATIONS: CALGARY BUSINESS HALL OF FAME . .15 Email: [email protected] 2007 EXECUTIVE COMMITTEE . 23 EDITORS/AUTHORS Please submit RESERVOIR articles to the CSPG STRATIGIES TO SUCCESSFULLY MANAGE LONGEVITY . 30 office. Submission deadline is the 23rd day of the month, two months prior to issue date. POTWAR OF PAKISTAN – A GENERAL STUDY . 33 (e.g., January 23 for the March issue). UNCERTAINTY ASSESSMENT IN 3D RESEVOIR MODELING . 38 To publish an article, the CSPG requires digital copies of the document. Text should be in Microsoft Word format and illustrations should CSPG BOOKSTORE – NEW TITLES! NOW AVAILABLE! . 43 be in TIFF format at 300 dpi. For additional information on manuscript preparation, refer to 2007 CSPG CSEG CALL FOR ABSTRACTS . 46 the Guidelines for Authors published in the CSPG Bulletin or contact the editor. COORDINATING EDITOR & OPERATIONS Jaimè Croft Larsen DEPARTMENTS CSPG Tel:403-264-5610, Ext 227 Fax: 403-264-5898 EXECUTIVE COMMENT . -
Coal Studies ELK VALLEY COALFIELD, NORTH HALF (825102, 07, 10, 11) by R
Coal Studies ELK VALLEY COALFIELD, NORTH HALF (825102, 07, 10, 11) By R. J. Morris and D. A. Grieve KEYWORDS: Coalgeology, Elk Valley coalfield, Mount the area is formed by Hmretta andBritt creeks, and is Veits, Mount Tuxford, HenretlaRidge, Bourgeau thrust, coal immediately north of the Fc'rdingRiver operations of Fording rank, Elk River syncline, Alexander Creek syncline. Coal Ltd.(Figure 4-1-1).The northernboundary is the British Columbia - Alberta border. The map area includes INTRODUCTION the upper Elk Valley and a portion of the upper Fording Detailed geological mapping and sampling of the north Valley. half of theElk Valley coalfieldbegan in 1986 and were Most of the area is Crown land and includes three c:od completed in 1987. The end poduct, a preliminary map at a properties. The most southerly comprises the north end ol'tbe scale of 1: IO OOO, will extend available map coverage in the Fording Coal Ltd. Fording River property. Adjacent to the coalfield north from the areas covered by Preliminary Maps north is theElk River property, in which Fording Coal 51 and 60 (Figure 4-l-l),which in turn expanded previous currently holds aSO-per-cent interest. Coal rights to the most coverage in the adjacent Crowsnest coalfield (Preliminary northerly property, formerly known as tlne Vincent option, Maps 24, 27,31 and 42). are reserved to the Crown Work in 1986 (Grieve, 1987) was mainly concentrated in Exploration history of the Weary Ridge - Bleasdell Creek the Weary Ridge ~ Bleasdell Creek area. Themore extensive area was summarized by Grieve (1987). Of the remailing 1987 field program was completed by R.J. -
Sport Fish Distribution and Relative Abundance on the Lower Red Deer River from Dickson Dam to Joffre, Alberta, 2005
Sport Fish Distribution and Relative Abundance on the Lower Red Deer River from Dickson Dam to Joffre, Alberta, 2005 CONSERVATION REPORT SERIES The Alberta Conservation Association is a Delegated Administrative Organization under Alberta’s Wildlife Act. CONSERVATION REPORT SERIES 25% Post Consumer Fibre When separated, both the binding and paper in this document are recyclable Sport Fish Distribution and Relative Abundance on the Lower Red Deer River from Dickson Dam to Joffre, Alberta, 2005 Jason Blackburn Alberta Conservation Association 2nd floor, YPM Place, 530 – 8th Street South Lethbridge, Alberta, Canada T1J 2J8 Report Series Co‐editors PETER AKU KELLEY KISSNER Alberta Conservation Association 50 Tuscany Meadows Cres. NW #101, 9 Chippewa Rd Calgary, AB T3A 5K6 Sherwood Park, AB T8A 6J7 Conservation Report Series Type Data, Technical ISBN printed: 978‐0‐7785‐7731‐7 ISBN online: 978‐0‐7785‐7732‐4 Publication No.: T/199 Disclaimer: This document is an independent report prepared by the Alberta Conservation Association. The authors are solely responsible for the interpretations of data and statements made within this report. Reproduction and Availability: This report and its contents may be reproduced in whole, or in part, provided that this title page is included with such reproduction and/or appropriate acknowledgements are provided to the authors and sponsors of this project. Suggested Citation: Blackburn, J. 2007. Sport fish distribution and relative abundance on the Lower Red Deer River from Dickson Dam to Joffre, Alberta, 2005. -
Water Storage Opportunities in the South Saskatchewan River Basin in Alberta
Water Storage Opportunities in the South Saskatchewan River Basin in Alberta Submitted to: Submitted by: SSRB Water Storage Opportunities AMEC Environment & Infrastructure, Steering Committee a Division of AMEC Americas Limited Lethbridge, Alberta Lethbridge, Alberta 2014 amec.com WATER STORAGE OPPORTUNITIES IN THE SOUTH SASKATCHEWAN RIVER BASIN IN ALBERTA Submitted to: SSRB Water Storage Opportunities Steering Committee Lethbridge, Alberta Submitted by: AMEC Environment & Infrastructure Lethbridge, Alberta July 2014 CW2154 SSRB Water Storage Opportunities Steering Committee Water Storage Opportunities in the South Saskatchewan River Basin Lethbridge, Alberta July 2014 Executive Summary Water supply in the South Saskatchewan River Basin (SSRB) in Alberta is naturally subject to highly variable flows. Capture and controlled release of surface water runoff is critical in the management of the available water supply. In addition to supply constraints, expanding population, accelerating economic growth and climate change impacts add additional challenges to managing our limited water supply. The South Saskatchewan River Basin in Alberta Water Supply Study (AMEC, 2009) identified re-management of existing reservoirs and the development of additional water storage sites as potential solutions to reduce the risk of water shortages for junior license holders and the aquatic environment. Modelling done as part of that study indicated that surplus water may be available and storage development may reduce deficits. This study is a follow up on the major conclusions of the South Saskatchewan River Basin in Alberta Water Supply Study (AMEC, 2009). It addresses the provincial Water for Life goal of “reliable, quality water supplies for a sustainable economy” while respecting interprovincial and international apportionment agreements and other legislative requirements. -
Summits on the Air – ARM for Canada (Alberta – VE6) Summits on the Air
Summits on the Air – ARM for Canada (Alberta – VE6) Summits on the Air Canada (Alberta – VE6/VA6) Association Reference Manual (ARM) Document Reference S87.1 Issue number 2.2 Date of issue 1st August 2016 Participation start date 1st October 2012 Authorised Association Manager Walker McBryde VA6MCB Summits-on-the-Air an original concept by G3WGV and developed with G3CWI Notice “Summits on the Air” SOTA and the SOTA logo are trademarks of the Programme. This document is copyright of the Programme. All other trademarks and copyrights referenced herein are acknowledged Page 1 of 63 Document S87.1 v2.2 Summits on the Air – ARM for Canada (Alberta – VE6) 1 Change Control ............................................................................................................................. 4 2 Association Reference Data ..................................................................................................... 7 2.1 Programme derivation ..................................................................................................................... 8 2.2 General information .......................................................................................................................... 8 2.3 Rights of way and access issues ..................................................................................................... 9 2.4 Maps and navigation .......................................................................................................................... 9 2.5 Safety considerations .................................................................................................................. -
Escape from the Great Plains the Icelanders in North Dakota and Alberta
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Great Plains Quarterly Great Plains Studies, Center for Fall 1983 Escape From The Great Plains The Icelanders In North Dakota And Alberta Howard Palmer University of Calgary Follow this and additional works at: https://digitalcommons.unl.edu/greatplainsquarterly Part of the Other International and Area Studies Commons Palmer, Howard, "Escape From The Great Plains The Icelanders In North Dakota And Alberta" (1983). Great Plains Quarterly. 1695. https://digitalcommons.unl.edu/greatplainsquarterly/1695 This Article is brought to you for free and open access by the Great Plains Studies, Center for at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Great Plains Quarterly by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. ESCAPE FROM THE GREAT PLAINS THE ICELANDERS IN NORTH DAKOTA AND ALBERTA HOWARD PALMER Immigration historians in Canada and the United One important feature of this movement that States are becoming aware of the need to look they do not highlight is the extent to which at immigration history within the larger context it included European immigrants and their of North American history. Canadian immi children who had settled earlier in the United gration patterns have been affected, indirectly, States but decided to move on as new oppor almost as much by American immigration pol tunities opened up in Canada. The Hrst sizable icy as by Canadian policy. Within many ethnic settlements of Hungarians, Slovaks, Lithuan groups in North America, there has been a ians, Czechs, Danes, Finns, Norwegians, Swedes, significant exchange of people and cultural Icelanders, Dutch, Welsh, and Hutterites on patterns between Canada and the United the Canadian prairies did not come directly States. -
High Streamflow Advisory Update River Basins Currently With
High Streamflow Advisory Update Issued at 1:30 PM - June 11, 2010 Issued by River Forecast Centre River Basins Currently with Advisories Hay Peace Information in addition to this advisory may be found at: Athabasca High http://www.environment.alberta.ca/forecasting/forecasterscomments Level http://www.environment.alberta.ca/apps/basins Ft. McMurray High Streamflow Advisory – Stream levels are rising or expected to Peace rise rapidly and no major flooding is expected. Minor flooding in low- River lying areas is possible. Anyone situated close to the streams affected Grande Prairie is advised to be cautious of the rising levels. Beaver Flood Watch – Stream levels are rising and will approach or may Edmonton exceed bank full. Flooding of areas adjacent to these streams may North occur. Anyone situated close to the river is advised to take Saskatchewan appropriate precautionary measures. Red Deer Red Deer Flood Warning – Rising stream levels will result in flooding of areas adjacent to the streams affected. Anyone situated close to the river Calgary South Bow Saskatchewan should take appropriate measures to avoid flood damage. Medicine Hat Lethbridge Oldman Milk Streamflow Advisory Overview for Alberta Advisories apply to streams and their tributaries unless otherwise noted. ♦ Up to 50 mm of precipitation fell, with local amounts of up to 60 mm, in the North Saskatchewan and Red Deer River basins on Wednesday and Thursday. ♦ No significant precipitation is forecast in these areas over the next few days. ♦ Conditions are being monitored – -
Fording River Operations: the Swift Project Description
Fording River Operations: The Swift Project Description Submitted to: BC Environmental Assessment Office 1st Floor 836 Yates Street PO Box 9426 Stn Prov Govt Victoria, BC, V8W 9V1 Pursuant to: British Columbia Environmental Assessment Act Submitted by: Teck Coal Limited – Fording River Operations April 2011 Teck Coal Limited – Fording River Operations: The Swift Project TABLE OF CONTENTS 1 PROPONENT INFORMATION ...................................................................... 1 1.1 Key Proponent Contacts .................................................................................................. 1 2 PROJECT INFORMATION ............................................................................ 2 2.1 Location ........................................................................................................................... 2 2.2 Project History and Overview .......................................................................................... 2 2.3 Deposit Geology and Resource Characterization ........................................................... 6 2.3.1 Stratigraphy ......................................................................................................... 6 2.3.2 Structure .............................................................................................................. 8 2.4 Components and Infrastructure ..................................................................................... 10 2.4.1 Conceptual Mine Plan and Schedule ............................................................... -
Room for the River in the Red Deer River Basin Advice to the Government of Alberta with Addendum
Room for the River in the Red Deer River Basin Advice to the Government of Alberta With Addendum July 23, 2015 Submitted by: Submitted to: P. Kim Sturgess, P.Eng., FCAE Cathy Maniego and Andrew Wilson CEO Resilience and Mitigation Branch WaterSMART Solutions Ltd. Environment and Sustainable Resource Development #200, 3512 - 33 Street NW 205 JG O'Donoghue Building Calgary, Alberta T2L 2A6 7000 - 113 Street Edmonton, Alberta T6H 5T6 Please note: The Room for the River process applied in the Red Deer River Basin and the subsequent Room for the River report are not government policy. The advice in this report will be taken under consideration by the Government of Alberta to help inform sound water management and policy decisions. This was not a public consultation process. The project was carried out with a technical working group, the Red Deer River Watershed Alliance, and the Red Deer River Municipal Users Group to provide advice to the Government of Alberta. It is a step toward developing a comprehensive inventory of flood mitigation projects and all options were put forward for consideration. Options presented in this report reflect concepts suggested by contributors; their inclusion in this report should not be viewed as an endorsement. i Executive Summary In the nearly two years since the 2013 floods in Alberta, many mitigation options for the province’s flood-prone areas have been identified, studied, and implemented by the Government of Alberta (GoA), municipalities, non-government organizations, and others. In the fall of 2014 the GoA announced that it wanted to look more closely at the approach taken by the Netherlands to manage flooding in the Rhine River branches – the Room for the River program. -
Glaciers of the Canadian Rockies
Glaciers of North America— GLACIERS OF CANADA GLACIERS OF THE CANADIAN ROCKIES By C. SIMON L. OMMANNEY SATELLITE IMAGE ATLAS OF GLACIERS OF THE WORLD Edited by RICHARD S. WILLIAMS, Jr., and JANE G. FERRIGNO U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1386–J–1 The Rocky Mountains of Canada include four distinct ranges from the U.S. border to northern British Columbia: Border, Continental, Hart, and Muskwa Ranges. They cover about 170,000 km2, are about 150 km wide, and have an estimated glacierized area of 38,613 km2. Mount Robson, at 3,954 m, is the highest peak. Glaciers range in size from ice fields, with major outlet glaciers, to glacierets. Small mountain-type glaciers in cirques, niches, and ice aprons are scattered throughout the ranges. Ice-cored moraines and rock glaciers are also common CONTENTS Page Abstract ---------------------------------------------------------------------------- J199 Introduction----------------------------------------------------------------------- 199 FIGURE 1. Mountain ranges of the southern Rocky Mountains------------ 201 2. Mountain ranges of the northern Rocky Mountains ------------ 202 3. Oblique aerial photograph of Mount Assiniboine, Banff National Park, Rocky Mountains----------------------------- 203 4. Sketch map showing glaciers of the Canadian Rocky Mountains -------------------------------------------- 204 5. Photograph of the Victoria Glacier, Rocky Mountains, Alberta, in August 1973 -------------------------------------- 209 TABLE 1. Named glaciers of the Rocky Mountains cited in the chapter -
Castle Project Initial Project Description in Accordance with Schedule 1 of the Impact Assessment Act Information and Management of Time Limits Regulations
Castle Project Initial Project Description in accordance with Schedule 1 of the Impact Assessment Act Information and Management of Time Limits Regulations October 2020 Teck Coal Limited Fording River Operations P.O. Box 100 +1 250 865 2271 Tel Elkford, B.C. Canada V0B 1H0 www.teck.com October 9, 2020 Fraser Ross Project Manager Impact Assessment Agency of Canada 210A - 757 West Hastings Street Vancouver, BC, V6C 3M2 Dear Mr. Ross Reference: Fording River Operations Castle Initial Project Description As requested by the Impact Assessment Agency of Canada (IAAC, the Agency), Teck Coal Limited is submitting the attached 2-part document to satisfy the federal requirements of an Initial Project Description (IPD) for the Fording River Operations Castle Project: 1. Provincial IPD published in April 2020 - The provincial IPD was previously submitted to the British Columbia (BC) Environmental Assessment Office in April 2020 and was prepared to satisfy information requirements under the BC Environmental Assessment Act. 1. IPD Addendum – the IPD Addendum focuses on providing supplemental information required by the Agency to satisfy the requirements of an IPD in accordance with Schedule 1 of the Information and Management of Time Limits Regulations under the Impact Assessment Act of Canada. Summaries of the IPD documents noted above, in English and in French, are provided under separate cover. Please contact the undersigned if you have any questions or comments on the enclosed material. Sincerely, David Baines Senior Lead Regulatory Approvals Teck Coal Limited Initial Project Description: Castle Project Teck Coal Limited Fording River Operations April 2020 Initial Project Description: Castle Project Executive Summary Introduction This document is an Initial Project Description (IPD) for the Teck Coal Limited (Teck) Fording River Operations Castle Project (the Castle Project or the Project) under the British Columbia (BC) Environmental Assessment Act (BC EAA) (SBC 2018, c 51). -
The Letters F and T Refer to Figures Or Tables Respectively
INDEX The letters f and t refer to figures or tables respectively "A" Marker, 312f, 313f Amherstberg Formation, 664f, 728f, 733,736f, Ashville Formation, 368f, 397, 400f, 412, 416, Abitibi River, 680,683, 706 741f, 765, 796 685 Acadian Orogeny, 686, 725, 727, 727f, 728, Amica-Bear Rock Formation, 544 Asiak Thrust Belt, 60, 82f 767, 771, 807 Amisk lowlands, 604 Askin Group, 259f Active Formation, 128f, 132f, 133, 139, 140f, ammolite see aragonite Assiniboia valley system, 393 145 Amsden Group, 244 Assiniboine Member, 412, 418 Adam Creek, Ont., 693,705f Amundsen Basin, 60, 69, 70f Assiniboine River, 44, 609, 637 Adam Till, 690f, 691, 6911,693 Amundsen Gulf, 476, 477, 478 Athabasca, Alta., 17,18,20f, 387,442,551,552 Adanac Mines, 339 ancestral North America miogeocline, 259f Athabasca Basin, 70f, 494 Adel Mountains, 415 Ancient Innuitian Margin, 51 Athabasca mobile zone see Athabasca Adel Mountains Volcanics, 455 Ancient Wall Complex, 184 polymetamorphic terrane Adirondack Dome, 714, 765 Anderdon Formation, 736f Athabasca oil sands see also oil and gas fields, Adirondack Inlier, 711 Anderdon Member, 664f 19, 21, 22, 386, 392, 507, 553, 606, 607 Adirondack Mountains, 719, 729,743 Anderson Basin, 50f, 52f, 359f, 360, 374, 381, Athabasca Plain, 617f Aftonian Interglacial, 773 382, 398, 399, 400, 401, 417, 477f, 478 Athabasca polymetamorphic terrane, 70f, Aguathuna Formation, 735f, 738f, 743 Anderson Member, 765 71-72,73 Aida Formation, 84,104, 614 Anderson Plain, 38, 106, 116, 122, 146, 325, Athabasca River, 15, 20f, 35, 43, 273f, 287f, Aklak