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Compiled by Sheldon Harvey and Wayne Grubert April 2018 POPULAR BIRDING LOCATIONS in MONTREAL and OTHER REGIONS in the PROVINCE of QUEBEC
Compiled by Sheldon Harvey and Wayne Grubert April 2018 POPULAR BIRDING LOCATIONS IN MONTREAL AND OTHER REGIONS IN THE PROVINCE OF QUEBEC ISLAND OF MONTREAL Mount Royal Cemetery, Montreal https://www.mountroyalcem.com/index.php/en/about-us/birds-of-mount-royal-cemetery.html Parc des Rapides, LaSalle http://ville.montreal.qc.ca/portal/page?_pageid=9217,104017603&_dad=portal&_schema=PORTAL Montreal Botanical Gardens http://espacepourlavie.ca/en/botanical-garden Parc du Mont-Royal/Mount Royal Park https://www.lemontroyal.qc.ca/en Summit Woods, Westmount, QC https://westmount.org/en/summit-woods-and-summit- lookout/?doing_wp_cron=1523388876.6022169589996337890625 Angrignon Park (Verdun) http://ville.montreal.qc.ca/portal/page?_pageid=7377,94551572&_dad=portal&_schema=PORTAL&id=70 Parc René-Levesque (Lachine) http://ville.montreal.qc.ca/portal/page?_pageid=7377,94551572&_dad=portal&_schema=PORTAL&id=84&sc=5 Technoparc Montreal (St-Laurent) https://gooiseaux.ca/technoparc-montreal/ Parc Jean-Drapeau (Ile-Ste-Helene/Ile-Notre-Dame) http://www.parcjeandrapeau.com/en/ Ile-des-Soeurs/Nuns’ Island http://ville.montreal.qc.ca/portal/page?_pageid=2480,2899998&_dad=portal&_schema=PORTAL Parc-nature de l’Ile-de-la-Visitation http://parcs-nature.com/public/ile-de-la-visitation Parc-nature de la-Pointe-aux-Prairies http://parcs-nature.com/public/pointe-aux-prairies Parc-nature du Bois-de-l’Ile-Bizard http://parcs-nature.com/public/bois-de-l-ile-bizard Parc-nature du Bois-de-Liesse http://parcs-nature.com/public/bois-de-liesse Parc-nature du Bois-de-Saraguay -
Ski Resorts (Canada)
SKI RESORTS (CANADA) Resource MAP LINK [email protected] ALBERTA • WinSport's Canada Olympic Park (1988 Winter Olympics • Canmore Nordic Centre (1988 Winter Olympics) • Canyon Ski Area - Red Deer • Castle Mountain Resort - Pincher Creek • Drumheller Valley Ski Club • Eastlink Park - Whitecourt, Alberta • Edmonton Ski Club • Fairview Ski Hill - Fairview • Fortress Mountain Resort - Kananaskis Country, Alberta between Calgary and Banff • Hidden Valley Ski Area - near Medicine Hat, located in the Cypress Hills Interprovincial Park in south-eastern Alberta • Innisfail Ski Hill - in Innisfail • Kinosoo Ridge Ski Resort - Cold Lake • Lake Louise Mountain Resort - Lake Louise in Banff National Park • Little Smokey Ski Area - Falher, Alberta • Marmot Basin - Jasper • Misery Mountain, Alberta - Peace River • Mount Norquay ski resort - Banff • Nakiska (1988 Winter Olympics) • Nitehawk Ski Area - Grande Prairie • Pass Powderkeg - Blairmore • Rabbit Hill Snow Resort - Leduc • Silver Summit - Edson • Snow Valley Ski Club - city of Edmonton • Sunridge Ski Area - city of Edmonton • Sunshine Village - Banff • Tawatinaw Valley Ski Club - Tawatinaw, Alberta • Valley Ski Club - Alliance, Alberta • Vista Ridge - in Fort McMurray • Whispering Pines ski resort - Worsley British Columbia Page 1 of 8 SKI RESORTS (CANADA) Resource MAP LINK [email protected] • HELI SKIING OPERATORS: • Bearpaw Heli • Bella Coola Heli Sports[2] • CMH Heli-Skiing & Summer Adventures[3] • Crescent Spur Heli[4] • Eagle Pass Heli[5] • Great Canadian Heliskiing[6] • James Orr Heliski[7] • Kingfisher Heli[8] • Last Frontier Heliskiing[9] • Mica Heliskiing Guides[10] • Mike Wiegele Helicopter Skiing[11] • Northern Escape Heli-skiing[12] • Powder Mountain Whistler • Purcell Heli[13] • RK Heliski[14] • Selkirk Tangiers Heli[15] • Silvertip Lodge Heli[16] • Skeena Heli[17] • Snowwater Heli[18] • Stellar Heliskiing[19] • Tyax Lodge & Heliskiing [20] • Whistler Heli[21] • White Wilderness Heli[22] • Apex Mountain Resort, Penticton • Bear Mountain Ski Hill, Dawson Creek • Big Bam Ski Hill, Fort St. -
Canadian Mineralogist, 51
785 The Canadian Mineralogist Vol. 51, pp. 785-800 (2013) DOI : 10.3749/canmin.51.5.785 A COMBINED GEOCHEMICAL AND GEOCHRONOLOGICAL INVESTIGATION OF NIOCALITE FROM THE OKA CARBONATITE COMPLEX, CANADA WEI CHEN§, ANTONIO SIMONETTI, AND PETER C. BURNS* Department of Civil & Environmental Engineering & Earth Sciences, 156 Fitzpatrick Hall, University of Notre Dame, Notre Dame IN, 46556 USA ABSTRACT This study is the first to report a detailed geochemical investigation and in situ U-Pb ages for niocalite, which occurs within carbonatite from the Bond Zone area of the Oka Carbonatite Complex (Canada). Niocalite is a Nb-disilicate member of the låvenite−cuspidine group. The major element composition of the niocalite studied here is relatively homogeneous with the average formula of: (Na0.34Fe0.06Mn0.19Mg0.09Ca13.40REE0.15Ti0.02)Σ14.25Nb2.12Ta0.06(Si2O7)4O7.65F2.44. Niocalite is enriched in minor and trace elements [i.e., Ta, Ti, and rare earth elements (REEs) up to 4.35 wt.%], with double- and triple-valenced elements (i.e., Sr, Y, REEs) substituting at different Ca-occupied lattice sites. The chondrite-normalized REE patterns for niocalite are LREE-enriched (~104 times chondrite) and negatively sloped. In addition, niocalite has higher HREE contents compared to those for co-existing apatite from the identical carbonatite sample. This result is expected based on bond valence data because of differing cation sizes. In situ U-Pb ages for niocalite from three carbonatite samples obtained by LA-ICP-MS define a wide range of ages, between ~111 and ~133 Ma. Niocalite from one carbonatite sample yields a bimodal distribution with weighted mean 206Pb/238U ages of 110.1 ± 5.0 Ma and 133.2 ± 6.1 Ma, and overlap those of co-existing apatite for the same sample. -
Adamsite-(Y), a New Sodium–Yttrium Carbonate Mineral
1457 The Canadian Mineralogist Vol. 38, pp. 1457-1466 (2000) ADAMSITE-(Y), A NEW SODIUM–YTTRIUM CARBONATE MINERAL SPECIES FROM MONT SAINT-HILAIRE, QUEBEC JOEL D. GRICE§ and ROBERT A. GAULT Research Division, Canadian Museum of Nature, P.O. Box 3443, Station D, Ottawa, Ontario K1P 6P4, Canada ANDREW C. ROBERTS Geological Survey of Canada, 601 Booth Street, Ottawa, Ontario K1A 0E8, Canada MARK A. COOPER Department of Geological Sciences, University of Manitoba, Winnipeg, Manitoba R3T 2N2, Canada ABSTRACT Adamsite-(Y), ideally NaY(CO3)2•6H2O, is a newly identified mineral from the Poudrette quarry, Mont Saint-Hilaire, Quebec. It occurs as groups of colorless to white and pale pink, rarely pale purple, flat, acicular to fibrous crystals. These crystals are up to 2.5 cm in length and form spherical radiating aggregates. Associated minerals include aegirine, albite, analcime, ancylite-(Ce), calcite, catapleiite, dawsonite, donnayite-(Y), elpidite, epididymite, eudialyte, eudidymite, fluorite, franconite, gaidonnayite, galena, genthelvite, gmelinite, gonnardite, horváthite-(Y), kupletskite, leifite, microcline, molybdenite, narsarsukite, natrolite, nenadkevichite, petersenite-(Ce), polylithionite, pyrochlore, quartz, rhodochrosite, rutile, sabinaite, sérandite, siderite, sphalerite, thomasclarkite-(Y), zircon and an unidentified Na–REE carbonate (UK 91). The transparent to translucent mineral has a vitreous to pearly luster and a white streak. It is soft (Mohs hardness 3) and brittle with perfect {001} and good {100} and {010} cleav- ␣  ␥ ° ° ages. Adamsite-(Y) is biaxial positive, = V 1.480(4), = 1.498(2), = 1.571(4), 2Vmeas. = 53(3) , 2Vcalc. = 55 and is nonpleochroic. Optical orientation: X = [001], Y = b, Z a = 14° (in  obtuse). It is triclinic, space group P1,¯ with unit-cell parameters refined from powder data: a 6.262(2), b 13.047(6), c 13.220(5) Å, ␣ 91.17(4),  103.70(4), ␥ 89.99(4)°, V 1049.1(5) Å3 and Z = 4. -
Modification Des Limites Du Parc National Du Mont-Orford
ASSOCIATION DES PROPRIÉTAIRES RIVERAINS DU LAC BOWKER 20, chemin du Lynx, lac Bowker, ORFORD (QUÉBEC) J1X 6V7 Téléphone et télécopieur: (450) 532-4684 Site Web: www.lacbowker.ca.tc Courriel: [email protected] Mémoire présenté à la commission du Bureau d’audiences publiques sur l’environnement (BAPE), composée de madame Claudette Journault, présidente, et de monsieur Pierre Béland, commissaire Par Jean-Guy Dépôt, président Réjean Fournier, vice-président Exposant nos opinions et préoccupations sur les différents éléments de la consultation publique sur «Les répercussions d’un échange de terrains sur la biodiversité et l’intégrité écologique du Parc national du Mont-Orford» Mardi, le 1er février 2005 à 19h00 Hôtel Chéribourg, 2603, chemin du Parc à Orford ASSOCIATION DES PROPRIÉTAIRES RIVERAINS DU LAC BOWKER Mandat général et domaine d’activités de l’organisme, APRLB : - Regrouper depuis le 3 septembre 1954, les propriétaires riverains du lac Bowker. - Protéger la qualité de l’eau et de l’environnement dans le bassin versant du lac. - Réaliser des activités, visant à améliorer la qualité de vie et de l’eau. - Réaliser des études, afin de mesurer différents paramètres pour s’assurer du suivi de la qualité de l’eau de ce magnifique lac réservoir d’eau potable, desservant les contribuables d’une partie du Canton d’Orford, et des municipalités de Bonsecours, Lawrenceville, Valcourt et Canton Valcourt. - Représenter ses membres auprès des autorités politiques et des organismes oeuvrant dans le même secteur d’activité. - Membre des organismes suivants; Fédération de protection de l’environnement l’Estrie, RAPPEL, Conseil Régional de l’Environnement de l’Estrie, RNCREQ, Coalition EAU Secours, etc. -
Unusual Fibrous Sodian Tainiolite Epitactic on Phlogopite from Marble Xenoliths of Mont Saint-Hilaire, Quebec, Canada
541 The Canadian Mineralogist Vol. 45, pp. 541-549 (2007) DOI : 10.2113/gscanmin.45.3.541 UNUSUAL FIBROUS SODIAN TAINIOLITE EPITACTIC ON PHLOGOPITE FROM MARBLE XENOLITHS OF MONT SAINT-HILAIRE, QUEBEC, CANADA Thomas ARMBRUSTER§ Laboratorium für chemische und mineralogische Kristallographie,Universität Bern, Freiestr. 3, CH–3012 Bern, Switzerland R. Peter RICHARDS National Center for Water Quality Research, Heidelberg College, Tiffi n, Ohio 44883, USA Edwin GNOS, Thomas PETTKE and Marco HERWEGH Institut für Geologie, Universität Bern, Balzerstr. 1, CH–3012 Bern, Switzerland Abstract Samples of marble xenoliths, thermally metamorphosed by the igneous rocks of Mont Saint-Hilaire, Quebec, contain idio- morphic plates of phlogopite. These plates were later overgrown and to some extent topotactically replaced by sodian tainiolite, tapering in fragile fi bers extending parallel to [100]. The fi bers only protrude parallel to [100] of the phlogopite host. Unit-cell parameters of phlogopite and tainiolite, both 1M polytypes (space group C2/m), are so similar that the phases in the phlogo- pite–tainiolite intergrowth could not be distinguished by single-crystal X-ray methods. Phlogopite of composition K1.01(Mg1.96 Fe0.66Li0.20Mn0.03Ti0.03Al0.04)⌺2.92(Si3.28Al0.72)⌺4 O10[(OH)1.14F0.86]⌺2 has the highest Si/Al value of natural samples of phlogopite known to us. The epitactic fi bers of tainiolite, of composition K1.01(Mg2.00Fe0.01Li0.59Na0.38)⌺2.98(Si3.99Al0.01)⌺4O10[F1.79Cl0.01 (OH)0.20]⌺2, represent to our knowledge the fi rst example of an extended solid-solution, established by combined electron-micro- probe and laser-ablation mass-spectrometry analyses, between tainiolite, K(LiMg2)Si4O10F2, and the recently described mineral shirokshinite, K(NaMg2)Si4O10F2. -
Mont-Tremblant
PARC NATIONAL DU MONT-TREMBLANT CAHIER HISTORIQUE 1895 - 2020 1 LA NAISSANCE DU TERRITOIRE Le parc national du Mont-Tremblant, le doyen des parcs nationaux du Québec fête ses 125 ans ! Territoire de grande nature, il se découvre au fil des décennies à travers plusieurs vocations. Chevauchant deux régions administratives, les Laurentides et Lanaudière, ses 1510 km2 se divisent en trois secteurs : La Diable, La Pimbina et L’Assomption. Aujourd’hui, il est un lieu de prédilection pour les amateurs de plein air. L’AIR PUR ET SEC : L’ORIGINE DU PARC NATIONAL DU MONT-TREMBLANT C’est un sanatorium, un établissement spécialisé dans le traitement des maladies pulmonaires, qui est à l’origine de la création du parc national du Mont-Tremblant. À la fin du 19e siècle, le docteur Camille Laviolette croit en la guérison de la tuberculose si l’on s’expose à l’air pur, sec et frais des montagnes. En 1894, voyant en la montagne Tremblante le site idéal, il fait la demande afin d’obtenir une concession des terres. Le gouvernement du Québec retient la suggestion et cède 60 km2 pour la création de ce centre de soins. Le parc de la Montagne-Tremblante naîtra le 12 janvier 1895, il devient ainsi le 3e parc au Canada et le 6e en Amérique du Nord. Il s’inscrit dans l’histoire mondiale des aires protégées aux côtés des parcs de Yellowstone, Yosemite, Séquoia, Banff et Yoho. Le docteur Camille Laviolette FAITS SAILLANTS • La légende du Manitonga Soutana Manitonga Soutana, en français Montagne des Esprits ou du Diable est à l’origine de l’appellation de la montagne Tremblante. -
An Overview of Soils in Québec: Formation, Variability and Challenges
SOIL CLASSIFICATION AN OVERVIEW OF SOILS IN Nine Mineral Orders and one Organic Order – based on the nature of the soil environment and the effects of the dominant soil forming process QUÉBEC: FORMATION, examples Podzols, Brunisols etc VARIABILITY AND CHALLENGES Note that 90% of Canadian soils are unlikely to be cultivated. The Canadian system classifies soils found only in Canada and is not meant to be comprehensive. Caroline. Begg, Ph.D. [email protected] RELATIONSHIP OF CANADIAN SYSTEM TO OTHER SOIL CLASSIFICATION SYSTEMS Canadian USA FAO Regosolic Entisol Fluvisol, Regosol Brunisolic Inceptisol, some Psamments Cambisol Podzolic Spodosol, some Inceptisols Podzol GEOLOGIC EVENTS IN Luvisolic Boralfs & Udalfs Luvisol SOUTHERN QUÉBEC - Gleysolic Aqy-suborders Gleysol, Pansol Chernozemic Boroll, some Vertisols Kastanozem, Chernozem SOURCE OF THE PARENT Solonetzic Mollisol & Alfisol,Natric great group Solonetz Vertisolic Verticals Vertisol MATERIAL Cryosolic Pergelic subgroups Gelic Organic Histosol Histosol METAMORPHIC ROCKS FROM THE GRENVILLE PROVINCE ARE FROM A MOUNTAIN RANGE 3,500 MILLION YEARS TO NEXT MAJOR EVENT 900 MILLION YEARS OLD The limestone beds found on the Montreal Island and Ile Jesus were part of the continental shelf of the “Lapetus” ocean from 600 million years ago when this area was located near the equator Covers a surface area of 600,000 km² in Québec These limestone beds of mud, fossils and sand or “The St Lawrence Platform” were laid down on part of the Grenville province and now Early Precambrian rocks – oldest underlie most of the St Lawrence Lowlands rocks – sediments and volcanic - One of the soil series (Farmington) found on the Mac Campus formed on granite and gneiss and schist top of the St Lawrence platform bedrock There is disagreement about the age of these rocks which underlie (at a 1 km depth) all of Montreal 5 6 STE LAWRENCE PLATFORM TIME LINE OF GEOLOGICAL EVENTS 135 million years to 6.5 million years ago – igneous rock (magma) intrusions cooled under the earth surface. -
Geology and Petrology of the Mont Royal Pluton, Montreal
GEOLOGY AND PETROLOGY OF THE MONT ROYAL PLUTON, MONTREAL NELSON EBY Environmental, Earth and Atmospheric Sciences, University of Massachusetts, Lowell, MA 01854 Sunday, September 13, 2015 Geology of the Northeastern Adirondack Mountains and Champlain–St. Lawrence Lowlands of New York, Vermont and Québec New York State Geological Association, 87th Annual Meeting State University of New York at Plattsburgh, Plattsburgh, NY 12–13 September 2015 GEOLOGY AND PETROLOGY OF THE MONT ROYAL PLUTON, MONTREAL NELSON EBY Environmental, Earth and Atmospheric Sciences, University of Massachusetts, Lowell, MA 01854 INTRODUCTION The Cretaceous Monteregian Hills (MH) petrographic province consists of a group of small alkaline plutons, and associated dikes, extending along a linear trend from approximately 30 km west of Montreal, Canada, to approximately 60 km east of Montreal (Fig. 1). Mont Megantic, located approximately 150 km east of Montreal has been included in the MH province (because of its geographic location), but geologically Mont Megantic belongs to the Younger White Mountain petrographic province of New Hampshire, Maine and Vermont. The MH plutons are largely composed of silica-undersaturated alkaline rocks: carbonatite and other strongly silica-undersaturated lithologies occur at Oka, and nepheline normative gabbros and pyroxenites, nepheline-bearing diorites, and feldspathoidal-bearing syenites and monzonites occur at the other MH plutons. Slightly silica- saturated quartz-bearing syenites are found at Monts Figure 1. Location and geological setting of the Brome and Shefford. Philpotts (1974) and Eby (1987) Monteregian Hills and White Mountain igenous have summarized the geology and petrology of the provinces (modified from Lentz et al., 2006). MH province. The White Mountain (WM) petrographic province (Fig. -
January 2018 More Than Just a Ski Club SNOWPHONE : 613-736-6235
January 2018 www.raski.ca More than just a ski club SNOWPHONE : 613-736-6235 WELCOME TO RA SKI 2018! WEEKLONG TO PANORAMA, BC January 27-February 3 At the time of this writing, the snow conditions are fabulous but the deep freeze temperatures may be making it difficult to enthusiastically Twenty-three RASkiers are heading to Panorama, British Columbia, to rise from our holiday induced food-coma/couch sitting and get out there enjoy nearly 3000 massive acres of terrain across 4000 vertical feet of on the trails! Let’s hope we’ll be off to a better start as January rolls purely Canadian adventure. We’ll be spending 6 days on the trails of along. the Panorama Resort, before departing to experience an evening in Banff, Alberta. Your Club Executive worked hard to plan full programs for your Winter pleasure. We encourage you to reward their efforts by participating, helping out where you can, and letting other people know about us (bring a friend along to check us out). Help us grow our membership – let your friends and co-workers know that we’re a friendly club with year-round activities. Become an ambassador by encouraging new members to join our four-seasons Club. Don’t forget some of the benefits of being a Member: in addition to a wide array of organized programs, your membership offers you discounts at ski hills and sports shops too. Always carry your card and ask if a discount will apply. Check our website for updates that may be added after the deadline for this newsletter. -
Atlas Des Territoires D'intérêt Pour La Conservation Dans Les Basses
Atlas of Sites of Conservation Interest in the St. Lawrence Lowlands – Methodology Report version 2, including Outaouais region June 2019 This report presents the results of the Atlas of sites of conservation interest in the St. Lawrence Lowlands, including analysis results for the Outaouais region. It follows a first version of the Atlas that was made available in October 2018. Other results will be added in the coming months, including the analysis of aquatic ecological units in areas where LIDAR data is not currently available. This document should be cited as follows: Jobin, B., L. Gratton, M.-J. Côté, O. Pfister, D. Lachance, M. Mingelbier, D. Blais, A. Blais et D. Leclair. 2019. Atlas of Sites of Conservation Interest in the St. Lawrence Lowlands – Methodology Report version 2, including Outaouais region. Environment and Climate Change Canada, ministère de l’Environnement et de la Lutte contre les changements climatiques, ministère des Forêts, de la Faune et des Parcs, St. Lawrence Action Plan, Québec, 186 p. Cover photos: © Thinkstockphotos Published by Authority of the Minister of the Environment © Her Majesty the Queen in Right of Canada, 2020 Published by Authority of the Ministre de l’Environnement et de la Lutte contre les changements climatiques du Québec © Government of Quebec, 2020 Cat. No.: En154-124/2020E-PDF ISBN: 978-0-660-36199-4 Aussi disponible en français sous le titre : Atlas des territoires d’intérêt pour la conservation dans les Basses-terres du Saint-Laurent – Rapport méthodologique version 2, incluant la région -
Proquest Dissertations
HISTOIRE DU SZSTEME ROUTIER DES CâlITONS DE L'EST avant 1855 par Frère Jules Martel,, s.c Thèse présentée à la faculté des arts de l'Université d'Ottawa en vue de l'obtention de la maîtrise es arts, option histoire. % 0 LIBRAfMÉS 9 VICTORIAVILIE,., CANADA,, i960 UMI Number: EC56036 INFORMATION TO USERS The quality of this reproduction is dépendent upon the quality of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleed-through, substandard margins, and improper alignment can adversely affect reproduction. In the unlikely event that the author did not send a complète manuscript and there are missing pages, thèse will be noted. Aiso, if unauthorized copyright material had to be removed, a note will indicate the deletion. UMI® UMI Microform EC56036 Copyright 2011 by ProQuest LLC Ail rights reserved. This microform édition is protected against unauthorized copying underTitle 17, United States Code. ProQuest LLC 789 East Eisenhower Parkway P.O. Box 1346 AnnArbor, Ml 48106-1346 RECONNAISSANCE Cette tnèse a été préparée sous la direction du Dr Lucien Brault, professeur d'histoire à l'Université d'Ottawa et éditeur aux Archives nationales. Nous le remercions de ses précieux conseils. Nos remerciements vont aussi à M. Gérard Malcuelosse, à Mgr Maurice O'Bready, P.D., à Mgr Albert Gravel, P.D., à >21s Juliette Bourque, au Dr Valmore Olivier, à il. l'abbé Jean Mercier, à M. l'abbé Conrad Groleau, au R.. Frère. Robert., o.c au R. Frère Antoine-Marie, s.c. et au R. Frère Louis-Victor, s.c, dont la coopération et l'encouragement nous ont souvent été précieux.