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L'évolution Du Lac Proglaciaire Memphrémagog, Sud Du Québec
Document généré le 28 sept. 2021 21:30 Géographie physique et Quaternaire L’évolution du lac proglaciaire Memphrémagog, sud du Québec The Evolution of Proglacial Lake Memphremagog, Southern Québec Die Entwicklung des proglazialen Sees Memphremagog im Süden von Québec Paul Boissonnault et Q. H. J. Gwyn Volume 37, numéro 2, 1983 Résumé de l'article Lors de la déglaciation finale des Appalaches, le lac proglaciaire URI : https://id.erudit.org/iderudit/032514ar Memphremagog a inondé les vallées situées immédiatement à l'est des monts DOI : https://doi.org/10.7202/032514ar Sutton. Le lac a d'abord occupé le nord du Vermont, tout près de la frontière internationale. Il a ensuite envahi, au Québec, les vallées du lac Aller au sommaire du numéro Memphrémagog actuel, de la rivière Missisquoi et, enfin, du Saint-François. Une étude détaillée des dépôts sur le versant est du bassin du Memphrémagog permet de reconstituer l'évolution du lac proglaciaire et, par conséquent, celle Éditeur(s) du retrait glaciaire. Huit phases lacustres se sont succédé entre les altitudes de 365 m et 165 m. L'une d'elles, la phase Va, contribue à redéfinir la position du Les Presses de l'Université de Montréal front associé à la moraine de Cherry-River. Au cours de cette évolution, la déglaciation s'est faite de deux manières. Durant les phases I à Va, la glace, ISSN encore active, formait un lobe appuyé sur le versant est. Par la suite, le front a reculé plus au nord; la glace est devenue stagnante et s'est morcellée, isolant 0705-7199 (imprimé) ainsi de petites calottes dans les vallées du lac Magog et de la rivière 1492-143X (numérique) Massawippi. -
GOLD PLACER DEPOSITS of the EASTERN TOWNSHIPS, PART E PROVINCE of QUEBEC, CANADA Department of Mines and Fisheries Honourable ONESIME GAGNON, Minister L.-A
RASM 1935-E(A) GOLD PLACER DEPOSITS OF THE EASTERN TOWNSHIPS, PART E PROVINCE OF QUEBEC, CANADA Department of Mines and Fisheries Honourable ONESIME GAGNON, Minister L.-A. RICHARD. Deputy-Minister BUREAU OF MINES A.-0. DUFRESNE, Director ANNUAL REPORT of the QUEBEC BUREAU OF MINES for the year 1935 JOHN A. DRESSER, Directing Geologist PART E Gold Placer Deposits of the Eastern Townships by H. W. McGerrigle QUEBEC REDEMPTI PARADIS PRINTER TO HIS MAJESTY THE KING 1936 PROVINCE OF QUEBEC, CANADA Department of Mines and Fisheries Honourable ONESIME GAGNON. Minister L.-A. RICHARD. Deputy-Minister BUREAU OF MINES A.-O. DUFRESNE. Director ANNUAL REPORT of the QUEBEC BUREAU OF MINES for the year 1935 JOHN A. DRESSER, Directing Geologist PART E Gold Placer Deposits of the Eastern Townships by H. W. MeGerrigle QUEBEe RÉDEMPTI PARADIS • PRINTER TO HIS MAJESTY THE KING 1936 GOLD PLACER DEPOSITS OF THE EASTERN TOWNSHIPS by H. W. McGerrigle TABLE OF CONTENTS PAGE INTRODUCTION 5 Scope of report and method of work 5 Acknowledgments 6 Summary 6 Previous work . 7 Bibliography 9 DESCRIPTION OF PLACER LOCALITIES 11 Ascot township 11 Felton brook 12 Grass Island brook . 13 Auckland township. 18 Bury township .. 19 Ditton area . 20 General 20 Summary of topography and geology . 20 Table of formations 21 IIistory of development and production 21 Dudswell township . 23 Hatley township . 23 Horton township. 24 Ireland township. 25 Lamhton township . 26 Leeds township . 29 Magog township . 29 Orford township . 29 Shipton township 31 Moe and adjacent rivers 33 Moe river . 33 Victoria river 36 Stoke Mountain area . -
Lake This By-Law Is Intended to Prevent the Infestation of Lake Memphremagog and the Magog River and Rivière-Aux-Cerises (Cherry River) by Zebra Mussels
By-law concerning nuisances and the prevention of zebra mussel infestation Lake This by-law is intended to prevent the infestation of Lake Memphremagog and the Magog River and Rivière-aux-Cerises (Cherry River) by zebra mussels. Any watercraft (motorized or not) MEMPHREMAGOG must go through a washing station before launching. Any boat owner must be able to present a $100 valid washing certificate or user certificate 22001144 Regulation respecting the protection of waters from pleasure craft discharges This by-law is intended to prevent water pollution by boats on Lake Memphremagog and its tributaries and adjacent bays. Any discharge from a pleasure boat constitutes an infraction; any boat equipped with a fixed or portable toilet must have a water-tight holding tank. Any person who empties or causes to $300 have emptied the holding tank elsewhere than at the emptying station __________________ Discharge is defined as any organic, liquid or solid, but excludes kitchen and laundry waste water ("grey water")* and the wastes from the boat's motor. * NOTE cyanobacteria: Toilet, kitchen and laundry waters contain organic matters and phosphorus that pollute and contribute to the apparition of cyanobacteria blooms (blue green algae). Those blooms are usually colorfully green, turquoise or red. They may look like paint, pea soup Boating safety patrol or scum. Cyanobacteria blooms may be dangerous for users since toxins, invisible to the naked eye, can be released into the water. MRC Memphremagog If you observe a blue green algae bloom, avoid any contact with contaminated water and keep pet away from it. Report the situation as soon as possible to Environment-Emergency 1-866-694-5454. -
Nutrient Loading and Impacts in Lake Champlain – Missisquoi Bay and Lake Memphremagog
Nutrient Loading and Impacts in Lake Champlain – Missisquoi Bay and Lake Memphremagog Missisquoi Bay. IJC Collection Lake Memphremagog. IJC Collection Missisquoi Bay Cyanobacteria. Pierre Leduc Prepared by the International Joint Commission April 21, 2020 Table of Contents I. Synthesis Document ........................................................................................................................ 3 A. Context ........................................................................................................................................ 3 Cyanobacteria .................................................................................................................................. 3 Actions and Consequences of Non-action ........................................................................................ 3 The Governments’ Reference ........................................................................................................... 4 IJC’s Approach to the Reference ...................................................................................................... 5 Workshops to Review Science and Policy on Nutrient Loading ........................................................ 6 Public Meeting and Online Consultation .......................................................................................... 6 B. IJC Analysis of SAG Reports ....................................................................................................... 7 C. Common Basin Recommendations and IJC Recommendations -
Yours to Discover Vale Perkins
Vale Perkins Potton : Yours to discover Nestled between Owl’s Head and Elephantis, not far from the Vale Perkins shores of Lake Memphremagog, is a valley extending to Knowlton Landing. This is Vale Perkins, an area of easy terrain likely used by the Abenakis as a « carrying place » between Lake Memphremagog and the North Missisquoi River, south to Lake Champlain. It is thought that Chemin de Vale Perkins roughly follows an original native portage trail. The original settlements in Potton Township were named by geographic location. This area was then East Potton. From 1867 to 1880 it was called Herbert; however, history is silent as to the reason. In 1880, Herbert became known as Vale Perkins, named after its founding family. The Pioneers In 1793, Loyalist Nicholas Austin arrived to clear a portion of land granted to him, near what is now Perkins Landing on Lake Memphremagog. He miscalculated the location of his grant, however; and was obliged to move north. Austin settled near Gibraltar Point, on the bay now bearing his name. Fred Jersey, Gathering sap Potton Heritage Association P.O. Box 262, Mansonville, (Québec) J0E 1X0 [email protected] ww.pottonheritage.org The Wharf, circa 1920 In 1793, Peter Perkins also arrived in Potton with his family. In 1865, used as a school until 1948, and sold in 1949 to the 1795, his son Samuel followed the Abenaki trail to Austin’s United Church for use as a Church. It was closed in 1964, but original partially cleared lot on the lake. He homesteaded there re-opened in 1982, for seasonal use, and was finally closed in with his three sons. -
"Newport City's Age-Friendly Community Action Plan
2016 Newport City’s Age Friendly Community Action Plan Table of Contents Advisory Council Members and Workgroups………………………………………. page 2 Introduction………………………………………………………………………………………. page 4 Why Newport is Pursuing Age Friendly Community Status…………………. page 6 Newport’s Domains of Age Friendliness……………………………………………… page 8 Domain 1: Town Information……………………………………………. page 9 Domain 2: Outdoor Spaces and Buildings…………………………... page 11 Domain 3: Transportation………………………………………………… page 15 Domain 4: Job Opportunities………………………………………………page 18 Domain 5: Health …………...………………………………………………….page 20 Domain 6: Housing…………………………………………………………….page 22 Domain 7: Caregiving…………………………………………………………page 24 Domain 8: Social Participation……………………………………………page 27 1 | Page Newport’s Age Friendly Community Advisory Council Members Council members include: Kathy Austin, Community National Bank Paul Dreher, Newport City Renaissance Corporation (NCRC) Design Committee, Northeast Kingdom Learning Services (NEKLS) & Dreher Design Harriet Hall, Vermont Association of Blind & Visually Impaired (VABVI) & Community member Eileen Illuzzi, North Country Career Center Trisha Ingalls, RuralEdge Pam Ladds, NCRC Design Committee & Community member Jennifer Leithead, NCRC Design Committee; Fresh Start Community Farm Alison Low, Northeastern Vermont Development Association (NVDA) Mike Marcotte, Vermont State Representative Paul Monette, Newport City Mayor Barbara Morrow, Orleans County Restorative Justice Center (OCRJC) Kelly Stoddard Poor, AARP Vermont Patricia Sears, Chair of Age -
72 Sherbrooke
SHERBROOKE 72 HOURS STARTING FROM $120 Plus taxes and service fees if applicable, does not include meals or lodging DAY 1-2 DESCRIPTION TIME DURATION Montréal Montreal Grand Christmas Market* - - DAY 3 DESCRIPTION TIME DURATION Arrival Sherbrooke and check-in at hotel 4:00 PM - Check-in of choice Dinner and Christmas Shopping - - Activity A Downtown Sherbrooke DAY 4 DESCRIPTION TIME DURATION Activity B Murals Tour 9:00 AM 2 HOURS Orford Express Christmas Train - 2.5 HOURS Activity C *Lunch Outing included in price Activity D Sherbrooke Christmas Market - 1 HOUR Activity E Christmas Tea at Uplands Cultural Centre - 1 HOUR Activity F Musée des beaux-arts de Sherbrooke - 1 HOUR Activity G Dinner Sherbrooke - - DAY 5 DESCRIPTION TIME DURATION Check Out - - - Activity H Saint-Benoît-du-Lac Monastery 9:00 AM 1 HOUR Activity I Merry House - Christmas Activity - 1 HOUR Activity J Lunch in Magog - - Activity K Vanden Eyden Chocolate Factory Tour - 0.5 HOUR - Departure Quebec City - - DAY 6-7 DESCRIPTION TIME DURATION Quebec City German - - Québec City Christmas Market* *for contact info see back QUÉBEC 55 216 143 E 112 R 610 143 I A U T 216 610 N C U SA SHERBROOKE D IN M 12 55 E H TH 10 410 55 C NORD AV. 112 DINNER, SHOPPING 112 AND MUSEUM BOUL. 10 SAINT-FRANÇOIS HOTEL OF ORFORD 216 NORD MONT CHOICE 10 ORFORD MONTREAL NORTH TERRIL 147 BOUL. LAKE MAGOG HATLEY JACQUES-CARTIER NORD MAGOG 108 KING EST 112 (Activities H to K) BOUL MAGOG 143 . PORTLAND 141 KING OUEST 247 410 BELVÉDÈRE SUD MAGOG RIVER GALT OUEST LAKE MASSAWIPPI S WELLINGTONAI SUD LAKE MEMPHREMAGOG NT-FRAN IVERSITÉ Ç 112 N O U I S L. -
TOWNSHIPS ODDITIES and EXTREMES Text and Photography (Except Where Noted): Matthew Farfan
TOWNSHIPS ODDITIES AND EXTREMES Text and photography (except where noted): Matthew Farfan The following tour features fourteen attractions found in the Eastern Townships, each of which is either odd or unique in some way, or else the smallest, largest, longest, shortest, highest, or oldest of its kind. Sites range from a slave burial ground, to the highest village in Quebec, to the largest open-pit asbestos mine in the Western Hemisphere. 1) Slave Burial Ground: “Nigger Rock” & the Black Community of Saint-Armand Strong oral tradition and increasing hard evidence suggest that there was once a substantial slave community in Saint-Armand. According to tradition, a large outcrop of rock near the village, known for generations by the derogatory term “Nigger Rock,” was a burial ground for slaves two centuries ago. The "Rock" is located on what was once the property of Philip Luke, a Loyalist, who settled in the area after the American Revolution, and who, documents show, arrived with slaves he inherited from his mother. Oral tradition surrounding the site is strong among Saint-Armand's older residents, some of whom recall stories from their parents or from their childhood about the old slave burial ground or about the blacks in the area. “Nigger Rock” is believed to be the only known burial ground in Canada for blacks who were born and died in slavery. In 2003, a plaque was presented to the municipality by the Government of Quebec. It reads (in French): “Oral tradition holds that near here, at a place known as Nigger Rock, many black slaves were buried between 1794 and 1833. -
WATERS THAT DRAIN VERMONT the Connecticut River Drains South
WATERS THAT DRAIN VERMONT The Connecticut River drains south. Flowing into it are: Deerfield River, Greenfield, Massachusetts o Green River, Greenfield, Massachusetts o Glastenbury River, Somerset Fall River, Greenfield, Massachusetts Whetstone Brook, Brattleboro, Vermont West River, Brattleboro o Rock River, Newfane o Wardsboro Brook, Jamaica o Winhall River, Londonderry o Utley Brook, Londonderry Saxtons River, Westminster Williams River, Rockingham o Middle Branch Williams River, Chester Black River, Springfield Mill Brook, Windsor Ottauquechee River, Hartland o Barnard Brook, Woodstock o Broad Brook, Bridgewater o North Branch Ottauquechee River, Bridgewater White River, White River Junction o First Branch White River, South Royalton o Second Branch White River, North Royalton o Third Branch White River, Bethel o Tweed River, Stockbridge o West Branch White River, Rochester Ompompanoosuc River, Norwich o West Branch Ompompanoosuc River, Thetford Waits River, Bradford o South Branch Waits River, Bradford Wells River, Wells River Stevens River, Barnet Passumpsic River, Barnet o Joes Brook, Barnet o Sleepers River, St. Johnsbury o Moose River, St. Johnsbury o Miller Run, Lyndonville o Sutton River, West Burke Paul Stream, Brunswick Nulhegan River, Bloomfield Leach Creek, Canaan Halls Stream, Beecher Falls 1 Lake Champlain Lake Champlain drains into the Richelieu River in Québec, thence into the Saint Lawrence River, and into the Gulf of Saint Lawrence. Pike River, Venise-en-Quebec, Québec Rock River, Highgate Missisquoi -
Contribution À L'étude De La Déglaciation Wisconsinienne Dans Le Centre Des Cantons De L'est, Québec
Document generated on 09/26/2021 8:32 p.m. Géographie physique et Quaternaire --> See the erratum for this article Contribution à l’étude de la déglaciation wisconsinienne dans le centre des Cantons de l’Est, Québec Contribution to the study of the Wisconsinan deglaciation of the central area of the Eastern Townships Pierre Clément and Michel Parent Troisième Colloque sur le Quaternaire du Québec : 2e partie Article abstract Volume 31, Number 3-4, 1977 Various geomorphological and sedi-mentological observations, such as southward till fabric orientations, northern slope location and direction of URI: https://id.erudit.org/iderudit/1000274ar frontal glacial features, and orientation and location of interlobate system, DOI: https://doi.org/10.7202/1000274ar indicate that an ice-body flowed southward, east and northeast of Sherbrooke. Westward, this mass probably extended to the Saint Claude eskers north of the See table of contents Stoke Mountains Interlobate Moraine. Its origin cannot be recognized in the studied area, but could be located in the Thet-ford Mines Appalachian plateau. This ice which was conflicting with its western southeastward flowing neighbor had a growing influence in the last déglaciation stages, especially Publisher(s) during the Cherry River readvance which could be extended southeastward Les Presses de l’Université de Montréal beyond the limit proposed by McDONALD (1967). The lack of southwestward continuity and the slope position of the frontal features are explained by the occurence of ice-dammed lakes in the main valleys where the glacier was ISSN afloat. As the presumed east-west trend of ice fronts cuts obliquely the 0705-7199 (print) northeast-southwest topographical axes, spillways generally tended to flow 1492-143X (digital) westward according to the decreasing lake altitudes in this direction. -
The Impact of Railways on Stanstead: 1850 to 1950 J
Document generated on 10/02/2021 2:08 p.m. Histoire Québec The impact of railways on Stanstead: 1850 to 1950 J. Derek Booth Volume 14, Number 3, 2009 URI: https://id.erudit.org/iderudit/11391ac See table of contents Publisher(s) Les Éditions Histoire Québec ISSN 1201-4710 (print) 1923-2101 (digital) Explore this journal Cite this article Booth, J. D. (2009). The impact of railways on Stanstead: 1850 to 1950. Histoire Québec, 14(3), 10–18. Tous droits réservés © Les Éditions Histoire Québec, 2009 This document is protected by copyright law. Use of the services of Érudit (including reproduction) is subject to its terms and conditions, which can be viewed online. https://apropos.erudit.org/en/users/policy-on-use/ This article is disseminated and preserved by Érudit. Érudit is a non-profit inter-university consortium of the Université de Montréal, Université Laval, and the Université du Québec à Montréal. Its mission is to promote and disseminate research. https://www.erudit.org/en/ VOL nin n \ ni i mi The impact of railways on Stanstead: 1850 to 1950 by J. Derek Booth D' J. Derek Booth was educated at McGill and is Professor Emeritus of Geography at Bishop's University. He is the author of several books on the role of railways in Quebec. This article is based on a lecture by Derek Booth on the occasion of the opening of the Stanstead Historical Society's Summer 2005 exhibition, "Arrival and Departure: The Regional Train." Le Dr J. Derek Booth a fait ses études à l'Université M'Gill; il est actuellement professeur émérite de géographie à l'Université Bishop's. -
FLOODING in the MASSAWIPPI BASIN DURING the 20TH CENTURY Norman Jones Bishop's University
107 FLOODING IN THE MASSAWIPPI BASIN DURING THE 20TH CENTURY Norman Jones Bishop's University RESUME L'histoire des inondations dans les Cantons de l'Est quebecois n'a jamais ete etudiee en detail. Cet article relate I'histoire des inondations dans Ie bassin hydrographique de la riviere Massawippi au 2CF siecle d'un point de vue joumalistique, archivistique et physiographique. Les donnees proviennent de plusieurs joumaux locallX, en particulier du Sherbrooke Record, des photos d'archives reunies par fe Centre de recherche des Cantons de l'Est, des mesures faites de fa physiographie du bassin et des donnees climatiques foumies par Environnement Canada. L'analyse de ces divers types de donnees revele qu'il y a eu des inondations dans Ie bassin de la Massawippi a 6S des 100 demieres annees. Ces inondations ont cause des dommages allX infrastructures gouvemementales, des inconvenients et des pertes d'ordre personnel ainsi que des pertes commerdales, particulierement dans Ie secteur agricofe. Certaines preuves indiquent une augmentation possible de fa frequence des inondations vers fa fin du siecle. La partie inferieure du bassin, Lennoxville et Ie sud de fa ville, est Ie secteur qui a ete Ie plus souvent touche. ABSTRACT The history of flooding in the Eastern Townships of Quebec has never been studied in detail. This article describes the history of flooding in the Massawippi Drainage Basin throughout the 20th century, from a newspaper media, archival and physical geographic perspective. The data are derived from a number of local newspapers, particularly the Sherbrooke Record, from archival photographs collected by the Eastern Townships Research Centre, from measurements of the basin's physiography, and from climate data provided by Environment Canada.