Eastern Townships of Quebec Connector
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Pioneer English Catholics in the Eastern Townships
CCHA Report, 7 (1939-40), 55-70 Pioneer English Catholics in the Eastern Townships BY THE REV. T. J. WALSH, S.J. Men are forever drifting down the slow stream, and most of their deeds, like themselves, pass into oblivion; it is well while the opportunity is at hand to save as much of the record as possible for posterity. In preparing the present paper any English-speaking man or woman who has in any conspicuous way aided the growth of the Church in the Eastern Townships has been deemed a suitable p erson for these pages. To the heroism and uncomplaining industry of these pioneers who hewed out homes in the wilderness, and little by l i t tle overcame the obstacles of nature, are we indebted now for our thriving Catholicity and to omit a record of their labours and select only for permanent record the deeds of our priests, who came upon the scene when most of the rugged work was done, would be singularly unjust. What is known as the Eastern Townships is, unlike almost all other Quebec regions, a political division rather than a natural one, for it includes all the level land of the St. Lawrence plain, as well as the hilly country of the Appalachians. The name applied to this part of Quebec was to distinguish it from the Western Townships on the North Shore of the St. Lawrence. Twelve counties go to make up this region, whose names tell something of the story of their different origin from the other parts of the Province, Arthabaska, Brome, Compton, Drummond, Megantic, Missisquoi, Richmond, Shefford, Sherbrooke, Stanstead, Wolfe and – an exception, which was carved from Compton within the present century, – Frontenac. -
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. -
Railway Stations
RAILWAY STATIONS OF THE EASTERN TOWNSHIPS Texts and Photography (except where noted) by Matthew Farfan (With special thanks to J. Derek Booth) The 19th century saw a massive railway boom all across the Eastern Townships. Driven by the need to access raw materials, the desire for rapid transit, the growth of industry, and a mania to build more and more branch lines, literally dozens of companies vied for territory and markets. By 1900, a network of local and regional railway lines crisscrossed virtually every corner of the region. The Grand Trunk (later Canadian National), Quebec Central, and Canadian Pacific railways emerged as the dominant players. The presence of a railway line was a major advantage to a small town. The stakes were high, and the good fortune of one town could mean the decline of another. Not surprisingly, local business leaders and politicians were enthusiastic railway boosters. Towns with an early advantage were those situated along the route of the Grand Trunk Railway. This line, completed in 1853, linked Montreal with the ice-free shipping facilities of Portland, Maine. Sherbrooke, Richmond, Acton Vale, and Coaticook were all situated along this route and enjoyed rapid growth as a result. Yet, the heyday of the train was relatively short-lived. With the development of the road network, the mass production of the automobile, and the growth of the trucking industry, railways declined throughout the 20th century, and many branch lines and stations were closed. Passenger service to some towns began to be scaled back or eliminated altogether in the 1950s, with station closures continuing along various lines throughout the 1960s, 1970s, and 1980s. -
Eastern Townships·
CONTRIBUTIONS TO THE HISTOHY I)F THE EASTERN TOWNSHIPS· A WOltK COX'L\IXIX~; AN ,\lTOl'XT OF TIlE EARLY SETTLE)IEXT OF ST ...:\.R~L\.XD, DUNHA~I, SUTTON, BROME, POTTON, AND BOLTON: WITH'\' HISTORY OF THE PRINCIPAL EVENTS TIlAT HAVE TRANSPIRED IN EACH OF THESE TO\\')/ ~IIIPS l:P TO THE PItE~E~'1T TDIE. I.:Y C. THOUA~. ;!\tollt\'Cltl: PRIXTED BY .JOH~ LOVELL, ST. XICIIIIL.\S SnEET. 181~1~. PREFACE. SA YS the poet: " He that writes, Or makes a feast, more certainly invites His judges than his friends j there's not a guest But will find something wanting, or }II drc,t." Conscious that much truth is contained in the above lines, the writer does not present this .work to the public with the expectation that it will meet the approval of all who read; but literary fame not being the object for which it was written, he trusts that he will be in no wise disconcerted by the criti· cisms it may call forth. He would say, however, to the individual inclined to regard the work as one unworthy the attention of the public, that it will be far more becoming in him-considering the want of histories of the Townships-to employ his time and talents in preparing one which/fliTl lIe entitled to PREFACE. respect, than only to indulge in fault-findings with the one HOW issued. In the . (l'paration of this history, it has been the desire of the writer to " give credit to whom credit is due;" yet, he doubts not that there are worthy Hons of worthy sirC':;, living in the townships about which he has writtell, whose names do not appear in these pages; but by the intelligent, the impossibility of noticing all the pioneers and their posterity, in a volume of this size, will at once be seen. -
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 -
People, Landscapes and Buildings of the Eastern Townships by Robert Lemire
6 People, Landscapes and Buildings of The Eastern Townships by Robert Lemire The SSAC holds its Annual Meeting in many different areas of Canada. Each year members anticipate that, perhaps, somewhere within the chosen area the long sought after vernacular structure will be found that is truly Canadian in conception. Someday, we may be foreced to conclude that the tepee and the igloo hold the honours; but, until such time, we will continue to study and analyse our land· scapes and buildings, gaining knowledge and appreciation, while at the same time voicing constructive criticism of what we have done, and, hopefully, learning to adapt to our surroundings without alter· ing them beyond recognition. Alteration of the natural environment was the main preoccupa· tion of people who settled in The Eastern Townships. Settlement began after the American War of Independence when Loyalists cross· ed the border from the United States to remain British subjects. Sur· vival was the first concern of the early settlers. They were confronted by a vast landscape covered with forests, lakes and rivers; but, these gifts of nature offered potential that brought later generations a life of prosperity and comfort. An excellent illustration of how a settler progressed from a shan· ty in the bush to a model farm was promoted in The Eastern Townships, Information for Intending Settlers (1881) (Fig. 1). Dense forests of spruce, pine, cedar and maple were cleared to provide wood for construction, fuel, and products such as pot and pearl ash. An informative description of the hardships and challenges faced by settlers of the region is found in: Charles P. -
Eastern Canada Quebec Heart & Soul Road Trip
EASTERN CANADA QUEBEC HEART & SOUL ROAD TRIP Eastern Canada Quebec Heart & Soul Road Trip Eastern Canada Road Trip 7 Days / 6 Nights Montreal to Montreal Priced at USD $2,408 per person Prices are per person and include all taxes. INTRODUCTION This 7-day Eastern Canada Quebec road trip combines Montreal and the eastern townships of Quebec with two of its most spectacular outdoor destinations. In Quebec City, discover urban highlights as your explore chic streets, historic sites and architectural wonders, then take a helicopter tour before moving on to St. Alexis des Monts and Auberge du Lac-à-l'Eau-Claire. On your return journey to Montreal you'll explore some of the most picturesque countryside that French Canada has to offer, complete with pretty lakes and walking trails. Itinerary at a Glance DAY 1 Montreal to Eastern Townships | 138 km/86 mi DAY 2 Eastern Townships | Exploring DAY 3 Eastern Townships to Quebec City | 251 km/156 mi DAY 4 Quebec Exploring | Helicopter Ride DAY 5 Quebec City to St. Alexis des Monts | 191 km/119 mi DAY 6 Auberge Lac a l’eau Claire | Exploring DAY 7 St. Alexis des Monts to Montreal | 139 km/87 mi Start planning your vacation in Canada by contacting our Canada specialists Call 1 800 217 0973 Monday - Friday 8am - 5pm Saturday 8.30am - 4pm Sunday 9am - 5:30pm (Pacific Standard Time) Email [email protected] Web canadabydesign.com Suite 1200, 675 West Hastings Street, Vancouver, BC, V6B 1N2, Canada 2021/06/14 Page 1 of 4 EASTERN CANADA QUEBEC HEART & SOUL ROAD TRIP MAP DETAILED ITINERARY Day 1 Montreal to Eastern Townships | 138 km/86 mi Today travel east to North Hatley in the Eastern Townships region of Quebec. -
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.