MAY 2014 VOLUME 41, ISSUE 05 Canadian Publication Mail Contract – 40070050 MORE THAN MAPPING WANT to LIFT YOUR PETREL® WORKFLOWS to NEW HEIGHTS?

Total Page:16

File Type:pdf, Size:1020Kb

MAY 2014 VOLUME 41, ISSUE 05 Canadian Publication Mail Contract – 40070050 MORE THAN MAPPING WANT to LIFT YOUR PETREL® WORKFLOWS to NEW HEIGHTS? 20 Fossils Hunting for Provinces 28 Go Take a Hike 34 GeoConvention 2014: Focus 36 Bringing the Cretaceous Sea to Mount Royal University: A Proposal to Fund the East Gate Entrance Fossil Display $10.00 MAY 2014 VOLUME 41, ISSUE 05 Canadian Publication Mail Contract – 40070050 MORE THAN MAPPING WANT TO LIFT YOUR PETREL® WORKFLOWS TO NEW HEIGHTS? Seamlessly bring more data into the fold. Dynamically present your insight like never before. SOFTWARE SERVICES CONNECTIVITY DATA MANAGEMENT The Petrosys Plug-in for Petrel® gives you access to powerful Petrosys mapping, surface modeling and data exchange from right where you need it – inside Petrel. Now you have the power to effortlessly and meticulously bring your critical knowledge together on one potent mapping canvas. Work intuitively with your Petrel knowledge and, should you so require, simultaneously aggregate, map and model data direct from multiple other sources – OpenWorks®, ArcSDE®, IHS™ Kingdom®, PPDM™ and more. Refine, enhance and then present your results in beautiful, compelling detail. The result? Decision-making is accelerated through consistent mapping and surface modeling as focus moves from regional overview through to the field and reservoir scale. To learn more go to www.petrosys.com.au/petrel. Petrel is a registered trademark of Schlumberger Limited and/or its affiliates. OpenWorks is a registered trademark of Halliburton. ESRI trademarks provided under license from ESRI. IHS and Kingdom are trademarks or registered trademarks of IHS, Inc. PPDM is a trademark of the Professional Petroleum Data Management (PPDM) Association. MAY 2014 – VOLUME 41, ISSUE 05 ARTICLES Fossils Hunting for Provinces ..................................................................................................... 20 CSPG OFFICE Tools to Tackle the Riddle of the Sands ................................................................................ 27 #110, 333 – 5th Avenue SW Calgary, Alberta, Canada T2P 3B6 Go Take A Hike ............................................................................................................................. 28 Tel: 403-264-5610 Web: www.cspg.org 2013 Stanley Slipper Gold Medal ............................................................................................... 31 Office hours: Monday to Friday, 8:30am to 4:00pm 2013 H.M. Hunter Award ........................................................................................................... 32 Executive Director: Lis Bjeld Tel: 403-513-1235, Email: [email protected] Event Coordinator: Kristy Casebeer 2013 Tracks Award ....................................................................................................................... 33 Tel: 403-513-1226, Email: [email protected] Member Services: GeoConvention 2014: Focus ....................................................................................................... 34 Tel: 403-264-5610, Email: [email protected] Publications and Website: Emma MacPherson 2014 Canadian Playmaker Forum ............................................................................................. 35 Email: [email protected], Tel: 403-513-1230 Educational Trust Fund/Outreach Coordinator: Kasandra Amaro Bringing the Cretaceous Sea to Mount Royal University: A Proposal to Fund the Tel: 403-513-1226, Email: [email protected] Technical Programs: Biljana Popovic East Gate Entrance Fossil Display ............................................................................................ 36 Tel: 403-513-1225, Email: [email protected] Corporate Sponsorship: Lis Bjeld Tel: 403-513-1235, Email: [email protected] DEPARTMENTS Controller: Eric Tang Executive Comment .................................................................................................................. 5 Tel: 403-513-1232, Email: [email protected] EDITORS/AUTHORS Technical Luncheons ................................................................................................................. 8 Please submit RESERVOIR articles to the CSPG office. Submission deadline is the 23rd day of the month, two months prior Division Talks ........................................................................................................................... 12 to issue date. (e.g., January 23 for the March issue). Rock Shop .................................................................................................... 11, 12, 15, 25, 34 To publish an article, the CSPG requires digital copies of the document. Text should be in Microsoft Word format and illustrations should be in TIFF format at 300 dpi., at final size. For additional information on manuscript preparation, refer to the Guidelines for Authors published in the CSPG Bulletin or contact the editor. Technical Editors Hugh S. Mosher Colin Yeo (Assistant Tech. Editor) Nunaga Resources Ltd. Encana Corporation M.: 403-809-9997 Tel: 403-645-7724 Email: [email protected] Email: [email protected] Coordinating Editor Emma MacPherson, Publications Coordinator, CSPG Tel: 403-513-1230, [email protected], ADVERTISING Advertising inquiries should be directed to Emma MacPherson, Tel: 403-513-1230 email: [email protected]. The deadline to reserve advertising space is the 23rd day of the month, two months prior to issue date. The RESERVOIR is published 11 times per year by the Canadian Society of Petroleum Geologists. This includes a combined issue for the months of July and August. The purpose of the RESERVOIR is to publicize the Society’s many activities and to promote the geosciences. We look for both technical and non-technical material to publish. Additional information on the RESERVOIR’s submission guidelines can be found at http://www.cspg. org/publications/pubs-reservoir-submissions.cfm. The contents of this publication may not be reproduced either in part or in full without the consent of the publisher. Additional copies of the RESERVOIR are available at the CSPG office. No official endorsement or sponsorship by the CSPG is implied for any advertisement, insert, or article that appears in the Reservoir unless otherwise noted. All submitted materials are reviewed by the editor. We reserve the right to edit all submissions, including letters to the Editor. Submissions must include your name, address, and membership number (if applicable). The material contained in this publication is intended for informational use only. While reasonable care has been taken, authors and the CSPG make no guarantees that any of the equations, schematics, or devices discussed will perform as expected or that they will give the desired results. Some information contained herein may be inaccurate or may vary from standard measurements. FRONT COVER The CSPG expressly disclaims any and all liability for the acts, omissions, or conduct of any third-party user Carboniferous Distal Fan deposits of the Ross Formation at Ballybunnion, of information contained in this publication. Under no circumstances shall the CSPG and its officers, directors, County Kerry, Ireland. Broad wave cut platforms exposed at low tide are backed by employees, and agents be liable for any injury, loss, damage, or expense arising in any manner whatsoever from the acts, omissions, or conduct of any third-party user. steep, unstable cliffs that reveal the transition between the Ross Sandstone Formation Designed and Printed by The Data Group of Companies, Calgary, Alberta. and the underlying Clare Shales. Photo by Dave Hills. RESERVOIR ISSUE 05 • MAY 2014 3 PETROLEUM INDUSTRY COURSES technology • seismic • rocks • maps • formations • land • sediments • history • sea • fossils • environment OVERVIEW OF THE OIL & GAS INDUSTRY IN WESTERN CANADA Date: April 30th and May 1st, 2014 Cost: $1050 (includes GST) Instructor: Bill Ayrton Effective for personnel just joining the oil patch, or for financial, accounting, and information systems personnel. • Learn about the many facets of the industry. • Oil finding, land acquisition, drilling, seismic, well completion, jargon and terminology. GEOLOGY FOR NON-GEOLOGISTS GEOLOGY FOR Date: June 4th and 5th, 2014 NON-GEOLOGISTS Cost: $1050 (includes GST) Old Geologists never die, they just Instructor: Bill Ayrton simply petrify! Effective for geological technicians or administrative Photo by: Bill Ayrton staff, or for those who just want a better understanding of geology to appreciate the world around us. • Learn about earth structure, geologic time-scale and Pr esented by: WHO SHOULD ATTEND processes, Western Canada geology, and interesting W.G. (Bill) Ayrton nearby locations. New geologists, engineers, geophysicists and • Participate in a rock identification exercise, landmen, as well as summer students entering cross-section project and a mini-field trip in the industry for the first time will find the downtown Calgary. courses a very beneficial introduction to the petroleum industry. These courses will be extremely useful to nonprofessional and support staff in the oil and gas industry, as well as GEOLOGY OF THE WESTERN accountants, lawyers, brokerage and financial CANADIAN SEDIMENTARY BASIN personnel working primarily alongside the oil Date: June 10th, 11th, and 12th, 2014 and gas industry. Cost: $1575 (includes GST) Instructor: Bill Ayrton TO REGISTER Ideal for those who wish to improve their geological To register or to obtain additional information understanding of where and how we look for oil and gas fields in Western Canada. regarding in-house and upcoming courses, please contact: • To visualize
Recommended publications
  • A Passion for Palaeontology September 22, 2012-March 17, 2013
    BACK COVER PAGE COVER PAGE Bearing Witness Inside the ROM Governors A dark chapter in ROM NEWSLETTER OF THE Cambodia’s history ROM GOVERNORS The Institute for Contemporary FALL/WINTER 2 012 Summer at the ROM has been a whirlwind of activity. Culture (ICC) presents Observance Exciting new initiatives such as Friday Night Live and our and Memorial: Photographs from family weekend programming have been extremely popular S-21, Cambodia, featuring over 100 and we have seen many new visitors and partners come photographs developed from original through our doors. Also hugely successful has been our negatives abandoned by the Khmer Special thanks to Susan Crocker and INSIDER groundbreaking exhibition Ultimate Dinosaurs: Giants from Rouge in January 1979, at the S-21 secret John Hunkin, Ron Graham, the Gondwana, which pioneers the use of Augmented Reality prison in Phnom Penh, Cambodia. Honourable William C. Graham and and includes the largest dinosaur ever mounted in Canada. Curated by Photo Archive Group, and Cathy Graham, Deanna Horton, Dr. Carla Shapiro from the Munk School Richard W. Ivey, and Sarah and Tom This month, it is a great pleasure to welcome Robert Pierce of Global Affairs, University of Toronto, Milroy for their generous support of this as the new chairman of the Board of Governors. As a this exhibition calls attention to the exhibition. For information on how you long-time volunteer, Board member for more than 12 years, atrocities in Cambodia in the 1970s can support Observance and Memorial and supporter of the ROM, Rob has served in a leadership or to make a donation to the ICC, BIG and human rights issues.
    [Show full text]
  • The Dinosaur Park - Bearpaw Formation Transition in the Cypress Hills Region of Southwestern Saskatchewan, Canada Meagan M
    The Dinosaur Park - Bearpaw Formation Transition in the Cypress Hills Region of Southwestern Saskatchewan, Canada Meagan M. Gilbert Department of Geological Sciences, University of Saskatchewan; [email protected] Summary The Upper Cretaceous Dinosaur Park Formation (DPF) is a south- and eastward-thinning fluvial to marginal marine clastic-wedge in the Western Canadian Sedimentary Basin. The DPF is overlain by the Bearpaw Formation (BF), a fully marine clastic succession representing the final major transgression of the epicontinental Western Interior Seaway (WIS) across western North America. In southwestern Saskatchewan, the DPF is comprised of marginal marine coal, carbonaceous shale, and heterolithic siltstone and sandstone grading vertically into marine sandstone and shale of the Bearpaw Formation. Due to Saskatchewan’s proximity to the paleocoastline, 5th order transgressive cycles resulted in the deposition of multiple coal seams (Lethbridge Coal Zone; LCZ) in the upper two-thirds of the DPF in the study area. The estimated total volume of coal is 48109 m3, with a gas potential of 46109 m3 (Frank, 2005). The focus of this study is to characterize the facies and facies associations of the DPF, the newly erected Manâtakâw Member, and the lower BF in the Cypress Hills region of southwestern Saskatchewan utilizing core, outcrop, and geophysical well log data. This study provides a comprehensive sequence stratigraphic overview of the DPF-BF transition in Saskatchewan and the potential for coalbed methane exploration. Introduction The Dinosaur Park and Bearpaw Formations in Alberta, and its equivalents in Montana, have been the focus of several sedimentologic and stratigraphic studies due to exceptional outcrop exposure and extensive subsurface data (e.g., McLean, 1971; Wood, 1985, 1989; Eberth and Hamblin, 1993; Tsujita, 1995; Catuneanu et al., 1997; Hamblin, 1997; Rogers et al., 2016).
    [Show full text]
  • Late Carboniferous Tropical Dryland Ecosystem, Joggins, Nova Scotia1
    Report of Activities 2002 181 Late Carboniferous Tropical Dryland Ecosystem, 1 Joggins, Nova Scotia H. J. Falcon-Lang and J. H. Calder Museum dioramas usually depict the Late Carboniferous tropical zone as being covered by humid rainforests composed of densely spaced tree-sized lycopsids. However, new evidence from the Langsettian fossil cliffs of Joggins, Nova Scotia suggests that this may only be half the story. At this classic site, grey coal-bearing units deposited in humid wetland coastal plain environments and containing 'normal' lycopsid-dominated rainforest vegetation are interbedded with red bed units. The red bed units, which are the focus of this paper, were deposited in seasonal dryland alluvial environment and contain an unusual floral and faunal assemblage. Depauperate floral remains in the deposits of anastomosing river channels, crevasse splays, and overbank muds are dominated by cordaite gymnosperms (Cordaites leaves, Artisia pith casts, and woody Dadoxylon trunks and branches; >80% of specimens). Present in subordinate numbers are pteridosperms (Eusphenopteris), sphenopsids (Calamites) and lycopsids (Sigillaria). A high proportion of this plant material has been charred in wildfires. Faunal remains associated with waterhole deposits in seasonally dry channels include land snails (Dendropupa), giant freshwater clams (Asterodonta) and the pelvic girdle and jaw of loxomatid reptiles. These data indicate that Late Carboniferous dryland tropical environments supported low diversity, fire-prone gymnospermous vegetation consisting mostly of shrubs or small trees inhabited by a unique fauna. At Joggins, gymnospermous dryland ecosystems repeatedly alternated with lycopsid wetland ecosystems, perhaps in response to glacial-interglacial climate rhythms. 16th European Palaeobotany and Palynology Conference, Athens, Greece; in Abstracts with Programs, p.
    [Show full text]
  • TGI Strat Column 2009.Cdr
    STRATIGRAPHIC CORRELATION CHART TGI II: Williston Basin Architecture and Hydrocarbon Potential in Eastern Saskatchewan and Western Manitoba EASTERN MANITOBA PERIOD MANITOBA SUBSURFACE SASKATCHEWAN OUTCROP ERA glacial drift glacial drift glacial drift Quaternary Wood Mountain Formation Peace Garden Peace Garden Member Tertiary Member Ravenscrag Formation CENOZOIC Formation Goodlands Member Formation Goodlands Member Turtle Mountain Turtle Mountain Turtle Frenchman Formation Whitemud Formation Boissevain Formation Boissevain Formation Eastend Formation Coulter Member Coulter Member Bearpaw Formation Odanah Member Belly River “marker” Odanah Member Belly River Formation “lower” Odanah Member Millwood Member Lea Park Formation Millwood Member MONTANA GROUP Pembina Member Pembina Member Pierre Shale Pierre Shale Milk River Formation Gammon Ferruginous Member Gammon Ferruginous Member Niobrara Formation Chalky Unit Boyne Member Boyne Member Boyne Calcareous Shale Unit Member Carlile Morden Member Carlile upper Formation Morden Member Formation Morden Member Carlile Formation Assiniboine Marco Calcarenite Assiniboine Member Member CRETACEOUS Second White Specks Laurier Limestone Beds Favel Favel Keld Keld Member Member Formation Formation Belle Fourche Formation Belle Fourche Member MESOZOIC COLORADO GROUP Belle Fourche Member upper Fish Scale Formation Fish Scale Zone upper Base of Fish Scale marker Base of Fish Scale marker Westgate Formation Westgate Member lower Westgate Member Newcastle Formation Newcastle Member lower Viking Sandstone
    [Show full text]
  • Dilemmas of Brazilian Grand Strategy
    STRATEGIC STUDIES INSTITUTE The Strategic Studies Institute (SSI) is part of the U.S. Army War College and is the strategic level study agent for issues related to national security and military strategy with emphasis on geostrate- gic analysis. The mission of SSI is to use independent analysis to conduct strategic studies that develop policy recommendations on: • Strategy, planning and policy for joint and combined employment of military forces; • Regional strategic appraisals; • The nature of land warfare; • Matters affecting the Army’s future; • The concepts, philosophy, and theory of strategy; and • Other issues of importance to the leadership of the Army. Studies produced by civilian and military analysts concern topics having strategic implications for the Army, the Department of De- fense, and the larger national security community. In addition to its studies, SSI publishes special reports on topics of special or immediate interest. These include edited proceedings of conferences and topically-oriented roundtables, expanded trip re- ports, and quick reaction responses to senior Army leaders. The Institute provides a valuable analytical capability within the Army to address strategic and other issues in support of Army par- ticipation in national security policy formulation. Strategic Studies Institute Monograph DILEMMAS OF BRAZILIAN GRAND STRATEGY Hal Brands August 2010 Visit our website for other free publication downloads http://www.StrategicStudiesInstitute.army.mil/ To rate this publication click here. The views expressed in this report are those of the author and do not necessarily reflect the official policy or position of the Depart- ment of the Army, the Department of Defense, or the U.S.
    [Show full text]
  • Alberta Basin. See Western Canada Foreland Basin. Alexander Terrane
    — ♦ — Index — ♦ — Alberta basin. See Western Canada foreland basin. Cardium Formation, 33, 35, 201, 202, 265, 302 Alexander terrane, 85 Cardium reservoir unit, 177, 178 Andean-type continental margin magmatic arc, Cascade basin, 273, 274 subduction along, 10 Cascade terrane, 85 Arctic Alaska plate, 376 Cassiar terrane, 85 Arctic National Wildlife Refuge (ANWR), 363 Charlie Lake Formation, 296 Arkoma basin, 436, 437, 443 Chinook Member, 36 Asmari reservoir, 331-332 Chugach terrane, 85, 116 Chungo Member, 33, 36 Bangestan/Qamchuqa reservoir, 332-333 Clearwater Formation, 27 Barrow arch, 375 Coastal belt terrane, 116, 118 Basal Colorado Sand reservoir unit, 170, 171 Coast plutonic complex, 11, 83 Bearpaw sandstones, 236 Colony Formation, 28 Beattie Peaks Formation, 18 Colorado Assemblage, 192,196-197, 199-201, 210-212, Belloy Formation, 297 224-226 Belly River Formation, 38, 117, 272 Colorado Group, 281-286, 300-303 Belly River reservoir unit, 181, 182 Colorado Group oils, 300 Belly River sandstones, 236 Colorado Shale, 284, 286 Belt Supergroup, 275 Crescent terrane, 116 Black Warrior basin, 431, 435, 436 Cummings Member, 24 Bluesky Formation, 22, 25 Cypress Hills/Hand Hills Assemblage, 192-193, 196-197, Boulder Batholith, 238 202-203 Bow Island Formation, 31, 32 Cypress Hills Formation, 42 Bowser basin, 85 Brazeau Formation, 39 Dakota sandstone, 414 Bridge River terrane, 85 Deep basin, Rock-Eval pyrolysis and TOC data, 283 Brookian sequence, 369-370, 370-374 Deformed belt, 84, 268-269 Dezful embayment. See Zagros foreland basin. Cache Creek
    [Show full text]
  • The Earliest Bioturbators As Ecosystem Engineers
    Downloaded from http://sp.lyellcollection.org/ by guest on September 27, 2021 Engineering the Cambrian explosion: the earliest bioturbators as ecosystem engineers LIAM G. HERRINGSHAW1,2*, RICHARD H. T. CALLOW1,3 & DUNCAN MCILROY1 1Department of Earth Sciences, Memorial University of Newfoundland, Prince Philip Drive, St John’s, NL, A1B 3X5, Canada 2Geology, School of Environmental Sciences, University of Hull, Cottingham Road, Hull HU6 7RX, UK 3Statoil ASA, Stavanger 4035, Norway *Correspondence: [email protected] Abstract: By applying modern biological criteria to trace fossil types and assessing burrow mor- phology, complexity, depth, potential burrow function and the likelihood of bioirrigation, we assign ecosystem engineering impact (EEI) values to the key ichnotaxa in the lowermost Cambrian (Fortunian). Surface traces such as Monomorphichnus have minimal impact on sediment properties and have very low EEI values; quasi-infaunal traces of organisms that were surficial modifiers or biodiffusors, such as Planolites, have moderate EEI values; and deeper infaunal, gallery biodiffu- sive or upward-conveying/downward-conveying traces, such as Teichichnus and Gyrolithes, have the highest EEI values. The key Cambrian ichnotaxon Treptichnus pedum has a moderate to high EEI value, depending on its functional interpretation. Most of the major functional groups of mod- ern bioturbators are found to have evolved during the earliest Cambrian, including burrow types that are highly likely to have been bioirrigated. In fine-grained (or microbially bound) sedimentary environments, trace-makers of bioirrigated burrows would have had a particularly significant impact, generating advective fluid flow within the sediment for the first time, in marked contrast with the otherwise diffusive porewater systems of the Proterozoic.
    [Show full text]
  • Porosity Permeability Volume and Lifespan Gabriel Wimmerth
    POROSITY PERMEABILITY VOLUME AND LIFESPAN GABRIEL WIMMERTH 1 THE POROSITY OF A RESERVOIR DETERMINES THE QUANTITY OF OIL AND GAS. THE MORE PORES A RESERVOIR CONTAINS THE MORE QUANTITY, VOLUME OF OIL AND GAS IS PRESENT IN A RESERVOIR. BY GABRIEL KEAFAS KUKU PLAYER WIMMERTH DISSERTATION PRESENTED FOR THE DEGREE OF DOCTORATE IN PETROLEUM ENGINEERING In the Department of Engineering and Science at the Atlantic International University, Hawaii, Honolulu, UNITED STATES OF AMERICA Promoter: Dr. Franklin Valcin President/Academic Dean at Atlantic International University October 2015 2 DECLARATION I declare by submitting this thesis, dissertation electronically that that the comprehensive, detailed and the entire piece of work is my own, original work that I am the sole owner of the copyright thereof(unless to the extent otherwise stated) and that I have not previously submitted any part of the work in obtaining any other qualification. Signature: Date: 10 October 2015 Copyright@2015 Atlantic International University All rights reserved 3 DEDICATION This work is dedicated to my wife Edla Kaiyo Wimmerth for assisting, encouraging, motivating and being a strong pillar over the years as I was completing this dissertation. It has been quite a tremendous journey, hard work and commitment for me and I would not have completed this enormous work, dissertation without her weighty, profound assistance. 4 ABSTRACT The oil and gas industry, petroleum engineering, exploration, drilling, reservoir and production engineering have taken an enormous toll since the early forties and sixties and it has predominantly reached the peak in the early eighties and nineties. The number of oil and gas companies have been using the vertical drilling approach and successfully managed to pinch the reservoir with productive oil or gas.
    [Show full text]
  • Brazil's Oil Discoveries Bring New
    Brazil’s Oil Discoveries Brazil’s discovery of large offshore oil reserves holds the possibility of raising the country’s profile in the international Bring New energy market and bringing an influx of wealth to the country. Safeguard- ing the nation’s economy against the Challenges downside of newfound resource wealth is among its leaders’ concerns. 22 EconSouth First Quarter 2011 While deepwater drilling permits in the United States were Brazil: Oil Production and Consumption, 1995–2012 being withheld because of concerns about safety and the envi- ronment, Brazil is moving at full speed to develop its massive Production deepwater reserves. In fact, Petrobras, the country’s state-run Forecast Consumption oil company, has already committed to investing $224 billion 3 through 2014 in its plan to develop deepwater fields off the country’s coast. day per The Brazilians have much to be optimistic about. The dis- 2 covery of the Tupi oil field in October 2006—the largest oil field barrels found in the Western Hemisphere in 30 years—signified Brazil’s of emergence as a global oil power. During the inaugural extrac- Millions 1 tion from the Tupi super-field, former president Luis Inacio Lula da Silva described the country’s newfound oil riches as a “second independence for Brazil.” (In December 2010, the Tupi 0 field was renamed “Lula.”) Although the oil finds present an 1995 1997 1999 2001 2003 2005 2007 2009 2011 enormous opportunity for Brazil, the logistical and political Source: EIA Short-term Energy Outlook, January 2011 challenges involved in developing the fields leave much of the future unmapped, however.
    [Show full text]
  • The Hell Creek Formation, Montana: a Stratigraphic Review and Revision Based on a Sequence Stratigraphic Approach
    Review The Hell Creek Formation, Montana: A Stratigraphic Review and Revision Based on a Sequence Stratigraphic Approach Denver Fowler 1,2 1 Badlands Dinosaur Museum, Dickinson Museum Center, Dickinson, ND 58601, USA; [email protected] 2 Museum of the Rockies, Montana State University, Bozeman, MT 59717, USA Received: 12 September 2020; Accepted: 30 October 2020; Published: date Supporting Information 1. Methods: Lithofacies Descriptions Facies descriptions follow methodology laid out in Miall (1985). Descriptions mostly follow those of Flight (2004) for the Bearpaw Shale and Fox Hills Sandstone. Additional lithofacies are described for the Colgate sandstone, ?Battle Formation, an undivided Hell Creek Formation, and the lowermost 5–10 m of the Fort Union Formation. It was desirable to stay as close to Flight's (2004) definitions as possible in order to facilitate cross comparison between measured sections and interpretation; however I have also chosen to remain true to the intentions of Brown (1906) in keeping the Basal Sandstone (and associated basal scour) as the first unit of the Hell Creek Formation, rather than the tidal flats identified by Flight (2004). This analysis is not as concerned with the nature of the basal contacts as much as internal stratigraphy within the Hell Creek Formation itself, hence some of the stratal and facies relationships described by Flight (2004) were not directly observed by myself, but I have included them here to ease comparisons. 1.1. Bearpaw Shale The Bearpaw Shale is the basalmost formation considered in this study; as such only the uppermost 10–20 m have been observed in outcrop. In this upper 20 m or so, the Bearpaw Shale generally coarsens upwards, predominantly comprising shale with occasional interbedded sandstone.
    [Show full text]
  • The Canadian Experience by Rebecca Kennedy
    World Heritage nominations – the Canadian experience February 2020 Killarney, Ireland 1 • The World Heritage Convention in Canada • Canadian Tentative List process • Heart’s Content Cable Station, Newfoundland • Lessons learned in development of Canadian nominations • Transboundary and serial nominations • Looking ahead 2 Rebecca Kennedy, “focal point” for World Heritage programme in Canada Who is this person?! 3 Why is Parks Canada Our national involved in Canada’s World office Heritage? Parks Canada has many responsibilities that extend beyond management of National Historic Sites and National Parks 4 Why is Parks Canada involved in Canada’s World Heritage? Given its expertise in cultural and natural heritage, Parks Canada was designated as the lead for World Heritage on behalf of the Government of Canada in 1976 • In 1978, Nahanni National Park and L’Anse aux Meadows National Historic Site were in the first group of 11 sites put on the World Heritage List 5 Canada and World Heritage • Canada is well respected for its expertise and credibility in our work on World Heritage • Elected member of the World Heritage Committee from 1976 to 1978, from 1985 to 1991, from 1995 to 2001 and from 2005 to 2009 • Committee meeting host in 1990 (Banff) and 2008 (Québec City) 6 Canada and World Heritage As the Government of Canada’s representative for the Convention, Parks Canada… • leads the Canadian delegation at Committee meetings • manages Canada’s official participation in relevant international workshops and provides policy input as requested
    [Show full text]
  • The Joggins Fossil Cliffs UNESCO World Heritage Site: a Review of Recent Research
    The Joggins Fossil Cliffs UNESCO World Heritage site: a review of recent research Melissa Grey¹,²* and Zoe V. Finkel² 1. Joggins Fossil Institute, 100 Main St. Joggins, Nova Scotia B0L 1A0, Canada 2. Environmental Science Program, Mount Allison University, Sackville, New Brunswick E4L 1G7, Canada *Corresponding author: <[email protected]> Date received: 28 July 2010 ¶ Date accepted 25 May 2011 ABSTRACT The Joggins Fossil Cliffs UNESCO World Heritage Site is a Carboniferous coastal section along the shores of the Cumberland Basin, an extension of Chignecto Bay, itself an arm of the Bay of Fundy, with excellent preservation of biota preserved in their environmental context. The Cliffs provide insight into the Late Carboniferous (Pennsylvanian) world, the most important interval in Earth’s past for the formation of coal. The site has had a long history of scientific research and, while there have been well over 100 publications in over 150 years of research at the Cliffs, discoveries continue and critical questions remain. Recent research (post-1950) falls under one of three categories: general geol- ogy; paleobiology; and paleoenvironmental reconstruction, and provides a context for future work at the site. While recent research has made large strides in our understanding of the Late Carboniferous, many questions remain to be studied and resolved, and interest in addressing these issues is clearly not waning. Within the World Heritage Site, we suggest that the uppermost formations (Springhill Mines and Ragged Reef), paleosols, floral and trace fossil tax- onomy, and microevolutionary patterns are among the most promising areas for future study. RÉSUMÉ Le site du patrimoine mondial de l’UNESCO des falaises fossilifères de Joggins est situé sur une partie du littoral qui date du Carbonifère, sur les rives du bassin de Cumberland, qui est une prolongation de la baie de Chignecto, elle-même un bras de la baie de Fundy.
    [Show full text]