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Trilobites of the Hagastrand Member (Tøyen Formation, Lowermost Arenig) from the Oslo Region, Norway. Part Il: Remaining Non-Asaphid Groups
Trilobites of the Hagastrand Member (Tøyen Formation, lowermost Arenig) from the Oslo Region, Norway. Part Il: Remaining non-asaphid groups OLE A. HOEL Hoel, O. A.: Trilobites of the Hagastrand Member (Tøyen Formation, lowermost Arenig) from the Oslo Region, Norway. Part Il: remaining non-asaphid groups. Norsk Geologisk Tidsskrift, Vol. 79, pp. 259-280. Oslo 1999. ISSN 0029-196X. This is Part Il of a two-part description of the trilobite fauna of the Hagastrand Member (Tøyen Formation) in the Oslo, Eiker Sandsvær, Modum and Mjøsa areas. In this part, the non-asaphid trilobites are described, while the asaphid species have been described previously. The history and status of the Tremadoc-Arenig Boundary problem is also reviewed, and I have found no reason to insert a Hunnebergian Series between the Tremadoc and the Arenig series, as has been suggested by some workers. Descriptions of the localities yielding this special trilobite fauna are provided. Most of the 22 trilobite species found in the Hagastrand Member also occur in Sweden. The 12 non-asaphid trilobites described herein belong to the families Metagnostidae, Shumardiidae, Remopleurididae, Nileidae, Cyclopygidae, Raphiophoridae, Alsataspididae and Pliomeridae. One new species is described; Robergiella tjemviki n. sp. Ole A. Hoel, Paleontologisk Museum, Sars gate l, N-0562 Oslo, Norway. Introduction contemporaneous platform deposits in Sweden are domi nated by a condensed limestone succession. In Norway, the The Tremadoc-Arenig Boundary interval is a crucial point Tøyen Formation is divided into two members: the lower in the evolution of several invertebrate groups, especially among the graptolites and the trilobites. In the graptolites, this change consisted most significantly in the loss of bithekae and a strong increase in diversity. -
Shunda Creek Hostel to Siffleur Falls Ho Coliseum Rn (Shunda Mtn.) Mtn -From the Hostel Ride 3 Km on the Shunda Ck
B ig Mnt. Baldy Shunda Creek Hostel to Siffleur Falls ho Coliseum rn (Shunda Mtn.) Mtn -From the Hostel ride 3 km on the Shunda Ck. Recreation Rd to Hwy 11. 734 Start Km0 -Turn RIGHT on Hwy 11 heading W toward the mtns. 124.4 Shunda Creek 1.9 -Junction with Hwy 734 122.5 Hostel R 8.0 -Goldeye center on the right. 116.4 an Nordegg ge 12.3B -Access to campground on the N side of the Hwy. 112.1 ra Fish (Shunda) z Goldeye e 17.3a -Rest Stop @ Service Station on the Hwy (Fuel, food...etc) 107.1 Lake Lake u R a 17.8 -Crescentn Falls access on the right. g 106.6 e Rest Stop @ 11 734 20.1 -Crossing the Bighorn River 104.3 Service Station 22.8 -Bighorn Dam turnoff on the left 101.6 25.4 -Lake Abraham. The Hwy follows the shore for the next 30km. 99.0 horn River ig F 31.0 B C er -Allstones Creek crossing. 93.4 a wa Riv r e n l e h l tc s s ka 33.2 c s -Rest Stop @ large roadside turnout/viewpt – Mt Michener, elev. 2337m 91.2 e Sa n t h rt 45.5 -Rest Stop @ David Thompson Resort; motel, camping, gas, food 78.9 o N 47.7 -Cline River Crossing 76.7 57.5 -Preacher’s Point. Access for launching boats or canoes 66.9 62.2 -Siffleur Falls trailhead on the LEFT, S side of Hwy. 62.2 734 Rest Stop @ Did You Know That.. -
Banff National Park Offers Many More Helen Katherine Backcountry Opportunities Than Those Lake Lake PARK Trail Shelters Berry River Described Here
BACKCOUNTRY CAMPGROUNDS JASPER CAMPGR OUND TOPO MAP NO . GRID REF . CAMPGR OUND TOPO MAP NO . GRID REF . WHITE GOAT NATIONAL Nigel Ba15 Wildflower Creek 82 N/8 686-003 * Lm20 Mount Costigan 82 0/3 187-783 Pass Bo1c Bow River/canoe 82 0/4 802-771 * Lm22 The Narrows 82 0/6 200-790 PARK * Br9 Big Springs 82 J/14 072-367 Lm31 Ghost Lakes 82 0/6 210-789 Sunwapta WILDERNESS AREA ◊ Br13 Marvel Lake 82 J/13 043-387 ◊ Ml22 Mystic Valley 82 0/5 886-824 Mount Pass Abraham Snowdome Lake Br14 McBride’s Camp 82 J/13 041-396 Mo5 Mosquito Creek 82 N/9 483-240 Mount Br17 Allenby Junction 82 J/13 016-414 * Mo16 Molar Creek 82 N/9 555-154 BIA Athabasca * Bw10 Brewster Creek 82 0/4 944-600 ◊ Mo18 Fish Lakes 82 N/9 556-217 NORTH * Cr6 Cascade Bridge 82 0/5 022-827 * No5 Norman Lake 83 C/2 071-706 * Cr15 Stony Creek 82 0/5 978-896 ◊ Pa8 Paradise Valley 82 N/8 528-898 * Cr31 Flints Park 82 0/5 862-958 * Re6 Lost Horse Creek 82 0/4 784-714 COLUM Glacier 93 Saskatchewan * Cr37 Block Lakes Junction 82 0/5 815-935 Re14 Shadow Lake 82 0/4 743-691 Cs Castleguard 82 C/3 857-703 * Re16 Pharaoh Creek 82 0/4 768-654 ICE FIELD Pinto Lake Mount E5 Healy Creek 82 0/4 825-608 Re21 Ball Pass Junction 82 0/4 723-652 Mount Sunset Coleman ◊ ◊ Sk5 Hidden Lake 82 N/8 626-029 Saskatchewan Pass E13 Egypt Lake 82 0/4 772-619 Ek13 Elk Lake Summit 82 0/5 951-826 ◊ Sk11 Baker Lake 82 N/8 672-049 Cs Fm10 Mount Cockscomb 82 0/4 923-766 ◊ Sk18 Merlin Meadows 82 N/9 635-093 No 5 ◊ SASKATCHEWAN 11 * Fm19 Mystic Junction 82 0/5 897-834 Sk19 Red Deer Lakes 82 N/9 667-098 River * Fm29 Sawback Lake 82 0/5 868-904 Sf Siffleur 82 N/16 441-356 Mount Gl 9 Glacier Lake 82 N/15 114-528 ◊ Sp6 Mount Rundle 82 0/4 030-647 Amery Alexandra He5 Hector Lake 82 N/9 463-144 Sp16 Rink’s Camp 82 0/4 040-555 Mount Jo9 Larry’s Camp 82 0/5 820-830 * Sp23 Eau Claire 82 J/14 067-505 Wilson * Jo18 Johnston Creek 82 0/5 771-882 * Sp35 Mount Fortune 82 J/14 123-425 ◊ Jo19 Luellen Lake 82 0/5 764-882 Su8 Howard Douglas Lake 82 0/4 880-546 Ta6 Taylor Lake 82 N/8 636-832 SASKATCHEWAN RIVER Jo29 Badger Pass Junction 82 0/5 737-932 N. -
Information Package Watercourse
Information Package Watercourse Crossing Management Directive June 2019 Disclaimer The information contained in this information package is provided for general information only and is in no way legal advice. It is not a substitute for knowing the AER requirements contained in the applicable legislation, including directives and manuals and how they apply in your particular situation. You should consider obtaining independent legal and other professional advice to properly understand your options and obligations. Despite the care taken in preparing this information package, the AER makes no warranty, expressed or implied, and does not assume any legal liability or responsibility for the accuracy or completeness of the information provided. For the most up-to-date versions of the documents contained in the appendices, use the links provided throughout this document. Printed versions are uncontrolled. Revision History Name Date Changes Made Jody Foster enter a date. Finalized document. enter a date. enter a date. enter a date. enter a date. Alberta Energy Regulator | Information Package 1 Alberta Energy Regulator Content Watercourse Crossing Remediation Directive ......................................................................................... 4 Overview ................................................................................................................................................. 4 How the Program Works ....................................................................................................................... -
Upper North Saskatchewan River and Abraham Lake Bull Trout Study, 2002 - 2003
Upper North Saskatchewan River and Abraham Lake Bull Trout Study, 2002 - 2003 CONSERVATION REPORT SERIES The Alberta Conservation Association is a Delegated Administrative Organization under Alberta’s Wildlife Act. CCONSERVATIONONSERVATION RREPORTEPORT SSERIESERIES 25% Post Consumer Fibre When separated, both the binding and paper in this document are recyclable Upper North Saskatchewan River and Abraham Lake Bull Trout Study, 2002 – 2003 Marco Fontana1, Kevin Gardiner2 and Mike Rodtka2 1 Alberta Conservation Association 113 ‐ 1 Street Cochrane, Alberta, Canada T4C 1B4 2 Alberta Conservation Association 4919 – 51 Street Rocky Mountain House, Alberta, Canada T4T 1B3 Report Series Editor PETER AKU KELLEY J. KISSNER Alberta Conservation Association 59 Hidden Green NW #101, 9 Chippewa Rd Calgary, AB T3A 5K6 Sherwood Park, AB T8A 6J7 Conservation Report Series Type Data, Technical ISBN printed: 978‐0‐7785‐6573‐4 ISBN online: 978‐0‐7785‐6574‐1 Publication No.: T/165 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: Fontana, M., K. Gardiner, and M. Rodtka. 2006. Upper North Saskatchewan River and Abraham Lake Bull -
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 .................................................................................................................. -
First Record of the Early Sheinwoodian Carbon Isotope Excursion (ESCIE) from the Barrandian Area of Northwestern Peri-Gondwana
Estonian Journal of Earth Sciences, 2015, 64, 1, 42–46 doi: 10.3176/earth.2015.08 First record of the early Sheinwoodian carbon isotope excursion (ESCIE) from the Barrandian area of northwestern peri-Gondwana Jiri Frýdaa,b, Oliver Lehnertc–e and Michael Joachimskic a Faculty of Environmental Sciences, Czech University of Life Sciences Prague, Kamýcká 129, Praha 6 – Suchdol, 165 21, Czech Republic b Czech Geological Survey, Klárov 3/131, 118 21 Prague 1, Czech Republic; [email protected] c GeoZentrum Nordbayern, Universität Erlangen, Schlossgarten 5, D-91054 Erlangen, Germany; [email protected], [email protected] d Department of Geology, Lund University, Sölvegatan 12, 223 62 Lund, Sweden; [email protected] e Institute of Geology at Tallinn University of Technology, Ehitajate tee 5, 19086 Tallinn, Estonia Received 15 July 2014, accepted 21 October 2014 Abstract. The δ13C record from an early Sheinwoodian limestone unit in the Prague Basin suggests its deposition during the time of the early Sheinwoodian carbon isotope excursion (ESCIE). The geochemical data set represents the first evidence for the ESCIE in the Prague Basin which was located in high latitudes on the northwestern peri-Gondwana shelf during early Silurian times. Key words: Silurian, early Sheinwoodian, carbon isotope excursion, northern peri-Gondwana, Barrandian area, Prague Basin, Czech Republic. INTRODUCTION represent, beside coeval diamictites in western peri- Gondwana, an evidence of an early Silurian glaciation. The early Sheinwoodian carbon isotope excursion The expression of this glacial in the Prague Basin has (ESCIE) is known from several palaeocontinents in the already been discussed with respect to the deposition Silurian tropics and subtropics (Lehnert et al. -
Smithsonian Miscellaneous Collections
SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 53, NUMBER 6 CAMBRIAN GEOLOGY AND PALEONTOLOGY No. 6.-0LENELLUS AND OTHER GENERA OF THE MESONACID/E With Twenty-Two Plates CHARLES D. WALCOTT (Publication 1934) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION AUGUST 12, 1910 Zl^i £orb (gaitimovt (pnee BALTIMORE, MD., U. S. A. CAMBRIAN GEOLOGY AND PALEONTOLOGY No. 6.—OLENELLUS AND OTHER GENERA OF THE MESONACID^ By CHARLES D. WALCOTT (With Twenty-Two Plates) CONTENTS PAGE Introduction 233 Future work 234 Acknowledgments 234 Order Opisthoparia Beecher 235 Family Mesonacidas Walcott 236 Observations—Development 236 Cephalon 236 Eye 239 Facial sutures 242 Anterior glabellar lobe 242 Hypostoma 243 Thorax 244 Nevadia stage 244 Mesonacis stage 244 Elliptocephala stage 244 Holmia stage 244 Piedeumias stage 245 Olenellus stage 245 Peachella 245 Olenelloides ; 245 Pygidium 245 Delimitation of genera 246 Nevadia 246 Mesonacis 246 Elliptocephala 247 Callavia 247 Holmia 247 Wanneria 248 P.'edeumias 248 Olenellus 248 Peachella 248 Olenelloides 248 Development of Mesonacidas 249 Mesonacidas and Paradoxinas 250 Stratigraphic position of the genera and species 250 Abrupt appearance of the Mesonacidse 252 Geographic distribution 252 Transition from the Mesonacidse to the Paradoxinse 253 Smithsonian Miscellaneous Collections, Vol. 53, No. 6 232 SMITHSONIAN MISCELLANEOUS COLLECTIONS VOL. 53 Description of genera and species 256 Nevadia, new genus 256 weeksi, new species 257 Mcsonacis Walcott 261 niickwitzi (Schmidt) 262 torelli (Moberg) 264 vermontana -
The Carboniferous Evolution of Nova Scotia
Downloaded from http://sp.lyellcollection.org/ by guest on September 27, 2021 The Carboniferous evolution of Nova Scotia J. H. CALDER Nova Scotia Department of Natural Resources, PO Box 698, Halifax, Nova Scotia, Canada B3J 2T9 Abstract: Nova Scotia during the Carboniferous lay at the heart of palaeoequatorial Euramerica in a broadly intermontane palaeoequatorial setting, the Maritimes-West-European province; to the west rose the orographic barrier imposed by the Appalachian Mountains, and to the south and east the Mauritanide-Hercynide belt. The geological affinity of Nova Scotia to Europe, reflected in elements of the Carboniferous flora and fauna, was mirrored in the evolution of geological thought even before the epochal visits of Sir Charles Lyell. The Maritimes Basin of eastern Canada, born of the Acadian-Caledonian orogeny that witnessed the suture of Iapetus in the Devonian, and shaped thereafter by the inexorable closing of Gondwana and Laurasia, comprises a near complete stratal sequence as great as 12 km thick which spans the Middle Devonian to the Lower Permian. Across the southern Maritimes Basin, in northern Nova Scotia, deep depocentres developed en echelon adjacent to a transform platelet boundary between terranes of Avalon and Gondwanan affinity. The subsequent history of the basins can be summarized as distension and rifting attended by bimodal volcanism waning through the Dinantian, with marked transpression in the Namurian and subsequent persistence of transcurrent movement linking Variscan deformation with Mauritainide-Appalachian convergence and Alleghenian thrusting. This Mid- Carboniferous event is pivotal in the Carboniferous evolution of Nova Scotia. Rapid subsidence adjacent to transcurrent faults in the early Westphalian was succeeded by thermal sag in the later Westphalian and ultimately by basin inversion and unroofing after the early Permian as equatorial Pangaea finally assembled and subsequently rifted again in the Triassic. -
Summits on the Air – ARM for USA - Colorado (WØC)
Summits on the Air – ARM for USA - Colorado (WØC) Summits on the Air USA - Colorado (WØC) Association Reference Manual Document Reference S46.1 Issue number 3.2 Date of issue 15-June-2021 Participation start date 01-May-2010 Authorised Date: 15-June-2021 obo SOTA Management Team Association Manager Matt Schnizer KØMOS 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 11 Document S46.1 V3.2 Summits on the Air – ARM for USA - Colorado (WØC) Change Control Date Version Details 01-May-10 1.0 First formal issue of this document 01-Aug-11 2.0 Updated Version including all qualified CO Peaks, North Dakota, and South Dakota Peaks 01-Dec-11 2.1 Corrections to document for consistency between sections. 31-Mar-14 2.2 Convert WØ to WØC for Colorado only Association. Remove South Dakota and North Dakota Regions. Minor grammatical changes. Clarification of SOTA Rule 3.7.3 “Final Access”. Matt Schnizer K0MOS becomes the new W0C Association Manager. 04/30/16 2.3 Updated Disclaimer Updated 2.0 Program Derivation: Changed prominence from 500 ft to 150m (492 ft) Updated 3.0 General information: Added valid FCC license Corrected conversion factor (ft to m) and recalculated all summits 1-Apr-2017 3.0 Acquired new Summit List from ListsofJohn.com: 64 new summits (37 for P500 ft to P150 m change and 27 new) and 3 deletes due to prom corrections. -
Further Exploration in the Canadian Rocky Mountains Author(S): J
Further Exploration in the Canadian Rocky Mountains Author(s): J. Norman Collie and T. G. Bonney Source: The Geographical Journal, Vol. 21, No. 5 (May, 1903), pp. 485-499 Published by: geographicalj Stable URL: http://www.jstor.org/stable/1775430 Accessed: 26-06-2016 12:56 UTC Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at http://about.jstor.org/terms JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. The Royal Geographical Society (with the Institute of British Geographers), Wiley are collaborating with JSTOR to digitize, preserve and extend access to The Geographical Journal This content downloaded from 137.99.31.134 on Sun, 26 Jun 2016 12:56:46 UTC All use subject to http://about.jstor.org/terms The Geographical Journal. No. 5. MAY, 1903. VOL. XXI. FURTHER EXPLORATION IN THE CANADIAN ROCKY MOUNTAINS.* By J. NORMAN COLLIE, F.R.S. THE exploration of the main range of the Canadian Rocky mountains lying between the sources of the Athabasca river and the Kicking Horse pass has been the subject of two papers read by myself before the Royal Geographical Society. In these two papers I attempted to give a description of some of the great snowfields that exist amongst the Rocky mountains, and also as far as possible to make clear the geo- graphy of a mountain district up till that time but little known. -
Smithsonian Miscellaneous Collections
SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 75. NUMBER 3 CAMBRIAN GEOLOGY AND PALEONTOLOGY V No. 3—CAMBRIAN AND OZARKIAN TRILOBITES (With Plates 15 to 24) BY CHARLES D. WALCOTT es'^ VorbH (Publication 2823) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION JUNE 1, 1925 Z^e. JSorb Q0affttttorc (preee BALTIMORE, MD., U. S. A, . CAMBRIAN GEOLOGY AND PALEONTOLOGY V No. 3.—CAMBRIAN AND OZARKIAN TRILOBITES By CHARLES D. WALCOTT (With Plates 15 to 24) CONTENTS PAGE Introduction 64 Description of genera and species 65 Genus Amecephalus Walcott 65 Amecephalus piochensis (Walcott), Middle Cambrian (Chis- holm) 66 Genus Anoria Walcott 67 Anorta tovtoensis (Walcott), Upper Cambrian 68 Genus Armonia Walcott 69 Armonia pelops Walcott, Upper Cambrian (Conasauga) 69 Genus Beliefontia Ulrich 69 Beliefontia collieana (Raymond) Ulrich, Canadian 72 Belief07itia nonius (Walcott), Ozarkian (Mons) y2 Genus Bowmania, new genus 73 Bonmiania americana (Walcott), Upper Cambrian y^ Subfamily Dikelocephalinae Beecher 74 Genus Briscoia Walcott _. 74 Briscoia sinclairensis Walcott, Ozarkian (Mons) 75 Genus Burnetia Walcott yj Burnetia urania (Walcott), Upper Cambrian yj Genus Bynumia Walcott 78 Bynumia eumus Walcott, Upper Cambrian (Lyell) 78 Genus Cedaria Walcott 78 Cedaria proUUca Walcott, Upper Cambrian (Conasauga) 79 Cedaria tennesseensis, species, .' new Upper Cambrian . 79 Genus Chancia Walcott 80 Chancia ebdome Walcott, Middle Cambrian 80 Chancia evax, new species, Middle Cambrian 81 Genus Corbinia Walcott 81 Corbinia horatio Walcott, Ozarkian (Mons) 81 Corbinia valida, new species, Ozarkian (Mons) 82 Genus Crusoia Walcott 82 Crusoia cebes Walcott, Middle Cambrian 82 Genus Desmetia, new genus 83 Desmetia annectans (Walcott) , Ozarkian (Goodwin) 83 Smithsonian Miscellaneous Collections, Vol. 75, No. 3 61 62 SMITHSONIAN MISCELLANEOUS COLLECTIONS VOL.