Geology of the Memphremagog Map Area •

Total Page:16

File Type:pdf, Size:1020Kb

Geology of the Memphremagog Map Area • GM 15279 GEOLOGY OF THE MEMPHREMAGOG MAP AREA • C 4 / Jç- I f Ministère des Richesses Neureiles, Québec SERVICE DES GITES MIN Aq, No GM—. 77 \V) C CN`.i:ii;i:T`l'S Chapter 1 Introduction. Chapter II General character o. <.:ty District. Chapter III General'Geology. Chapter IV Structural Geology. .Chapter V Historical Geology. Chapter VI Economic. Geolo gy. Plate I T .7:Tassri;~p~±-- Bunker Brook, - i+'itc:! Bay valley the north. Plate Il Parallel valleys, the second is that of the Tomifobia River and the pronounced valley die:;. is that of Bunker. Brook. • Plate III Looking southeast across Fitch Bay. 77i`.ls o 'Stanstead granodiorite in right background. Plate IV Whetstone Island. The low flat area in the fore•-. ground is underlain by Devonian limestone. hills in the background are of Stanstead diorite. Plate V Looking northwest toward Lake Massaw p i. ground shows .type of topography west of Bunker fault . In the background the ridge east of the .fault can be traced.far to right. .Plate VI Drag `'olds south of Ayer' s Cliff in the Tomifobia • interbedded slates and•limestone. Plate VII Biotite segregation in Stanstead granodior?. Plate VIII Biotite streaks. in Stanstead granodiorite. Plate IX Parallel pegmatite veins in Stanstead granodiorite m' • a _- _•- • . ..- .. --L- ~ Plate X Stanstead Granite Company's quarry at Gran i te-U < i le, showing the excellent sheeting and ideal working conditions. Plate XI Serpentine hill. u~ Figure Index map showing the location of the I:emphre- ma.gog area. Figure. 2. Showing location of diorite areas and points from which specimens were collected. Figure 3. Cross-section of fold, trend of fold IT.800i5. Figure 4. Showing areas of Siluro-Devoniean. Figure 5. Shôwing areal extent of Stanstead granodi or:i.te and associated dikes • Figure 6. Graphical representation of the quantitative mineralogical analyses and classification of specimens of the main mass of the Stanstead granodiorite and an average of these. Figure 7. Graphical representation of the quantitative mineralogical analyses and classification cf specimens of the intrusives associated with the main mass. o f the Stanstead granodiori te , Figure 8. Showing location of dikes. Figure 9. Diagram to show some features of the Pleistcca_L. ,and Recent geology. Figure 10. To show some important structural features. Figure 11. Showing location of quarries. G N A PTeR i• 'f .1"lkod uc t on . Purpose The tareaçlyinF soUi heaSt• of the' upper ût.!1a. ' z.s.0 e _ '(as •ocCupied.. the attention . of geolosiCts.: since- the inception oft`'_Tco ~O iC tl Survey : and has p.resented Problems.. so complex as to have aff -~'ry ef:. :rounds fo"' over sixty years. Tiloû,rt much.'Or.{~ h~;,~ beer for bitter ControvE'rsy - ,, C'`+~ done throu_ bout the area it has been for the most oarT, promiscuous or in ~y ~-. the nature of large area reconnaissance.l~onSegUeritly sat' sfa,.;t:3L=, knowledge - of the general geol64- or solution of ma:Y.y of the major Ob-- .lems has never :Peen- .gained. For .sO.iTe .ti.(Re a detailed revision of the. 'geology O'° southern Quebec ha:: been contemplated and it was tF'i'}- _ .`ié;4d to beTinriil.l,, th`i S- that the present jFTork iYrJ. trie C.M1Ï?flleiA2,ï,o .(: undertaken. This area was selected because it was thought to a:.. .,.-.__ • ; ^5,st - opportuni tiAS for • Obtc`l.iniri ; a cOïilnrehenSivv kIlo Ÿrle dEs of the ` tr«•'..- ..... ti , i~raphy And because of the presef.C2 of granite masses. of considerable economic importance. Location and size of :dap Area. .The Me_mp rrema.,.=,o- area .as herein. r3efined co.aori ses that part the ; 5 by 30 .minute :1et tpC2re:îa,`;og sheet which ll.es east o- 'y G iLi- ?hrei` Og. It is situated in .southeastern Qu2bvC on t h e international Ç l•. ' -. ' ' . , t t . ~v't•:y .. . i ~Y .~ boU-i1d?ry iY the county of Sta'ristead, and includes the township• of Stan- f % / Stë?dq parts of Magog, ?atley ti - Tt is an area . i r 12 miles- wide- and. .t7 miles 1011~ , apnroximately ?vJ square -Males. P'_n_ysi . ? .~:r %'+.ÇJriiCally . i't represents the transition from - the relatively flat coun- try of .;outhern•~.~-.~,uebec to the ::7'.:,rë rugged ,`toun'tainOUs areas of northern Vermont•'=iild New Hampshire . • Fieldld W.ni r l.. The .Jeological field work unon ',hi ch the renort is based was done during. the. summer'. of 1923. The base : map' used is that of the Depart- ment of ,`il.itia 'and ' Defence published on a. scale of one mile + with 25-foot contours, Lbcations were made mainly 'uÿ pace and com,=ss traverses And comnass trian;ula.tion: 7 , dyre-c-tioht. Lake -,ias5awippi 1 tong „narrow• lake occupying a crook in the valley, has an elevation of 523 -feet. The 'depth of the lake was not as- certained but, appearances would lead one to believe that it ea -,; exceeds 30 feet - and 1-1117 • • siderably. more. 0outh of • iake massawippi there is a id. • upward to .an elevation of 775 feet, then a long gradual descent to an -• elevation of. 683 feet at Fitch Bay. .This part of the valley is o,r-,baby filled to a conSiderable depth with superficial material., Near/_,a',rp, Massawippi wells drilled to a depth of 60 feet are entirely in so--called. gravel. Fitch gay near Magoon Point is reported to be from 40 to 60 feet deep. The narrowness of the valley here clearly indicates that its rock floor is considerably higher than at Zake JAssawippi. In general the rock floor, H.7preL,kent-:.ba6tom, and the land and water surface show an V P/ increaseleelevation from north to south within the map area. The vaLey is unsymmetrical, with a high ridge of abrupt slope on its western side and on the eastern a ridge several hundred feet lower with a gradual slope. The northwestern of the two sections into which, the fl,rr--, is divided . by the-great valley . just described is almost a penirula. is bounded on the west byf;Lake Lilemohremagog and on the east by • 1. , and z_e masi,awippl. In general it constitutes an asyimmetrical " 1 ride with a gradual slope to the west and an abrupt one to the east. The axis lies within a mile or two of thef boundary Valley. Along, the . 1 .-- shore of Lake Mem-ohremarLo is a well-defined low ridge of klIrp-Dey2:--Iian IlimeStone% Between this and the too of the main ridge there are _.,.,n-,.., '0',})/(AsW01( 41 'e0; minor undulationswhich'haver not-very definiteTorm. The hill north of .,:iagoon int assumes such prominence as to dwarf the main ride, which in this section falls away rather rapidly. Farther north Loverina.2:e.1 . sprawls out in a lAcge,' irregular,- though probably shallow, depression on the western slope. ItS'outlet-stream flowin1 south • takes advantage of a break in the ridge and enters Fitch /JJay.. :Northwest of _Lake Idassawi3- -pi. broad depression with-a.horthwestsoutheast'trendand-another-to-t•,... ine-' • . 'Ç rIe south with an eaStweSt-trend destroy this section of the area.: n thesoutheasternseCtion of t e.maP 4area there is in . • A.Yi7«led`j T_'_leTi't S . The writer wishes, to express his appreciation for the infor- mation given him by the quarry operators and many other local residents. He is indebted to the faculty of the Department of ^eology of the Univer- sity of Chicago for laboratory facilities, advice and as::istaIr.•r-, • ciallykto Dr.Albert Johannsen whose continued interest and he:L_r: source of much encouragement. Assistance in the field was r e'r:+d, : e:.i >~?' J.W.trrei; for six weeks aÏiCt. by C W.Wal.lis fOr.the greater.,the part _ ~ season. writer is also indebted to s wife Helen Kerr whose con- . C.,51.0 ~',•~~,: tinued assis ance in .the preparation . of the;~manuscript\~:ade its .H1 ' a; tion possible \znder the pres ure of much otï?ei:, ?i3Ori, \. Previous Work. To. outline completely the;` Ÿ ork done in southern Quebec would --- ~h require more. space and time than the benefits accruing from such a r°e:s le.;'' would warrant. • The. proximity of this section of the country to the o-' - g inal headquarters of the Canadian. *Survey at Montreal. led the earl,, ers to turn their attention to it. Some of-the problems found the .: _.,.c_. became subjects of .controversy, and the "Taconic Question" developed i.h'=o a :,torm center in the geological literature of the period. ~e .CO «;t.N: • - around Lake Champlain and other sections along the:ooun^ ary becaTie Aï'taiît hunting g?"ounds for palrkontolO-;lsts and geologists from across t~c •border. Many articles apneared dealing with the fauna, stra.tigraoliy, is_neous .roC :Cs-, and to a lesser degree .the structure. In the latter part of •the nineteenth cen.turz, revisedd and completed the mapping of the entire southern part of the province - task viich had rten begun' by Sir., William Lo;)-an and carried on by r l ~ colleagues. Since,• „ that time much•wor'; has, been •dOne on small sccitte•r'e ~ areas, faunas, intrusives, mineral deposits, and so on, ._,ut of it tool the form of sys'tematiC areal mapping. •.Of. all. this. work and the literature resulting from it the most outstanding feature is the achievement of .'_,ojan. Though he did. s?o ^o-11.7 ete the mapping of the southern :OaT't of , Que'toec it is quite apparent . that-he was .a.ble 't,o•7oerCeive to a: remarkable' degree.
Recommended publications
  • 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.
    [Show full text]
  • 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 .
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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
    [Show full text]
  • Newport News
    Newport News Author: MK Bateman, March 2nd, 2014 Like Share 3 Tweet 1 1 1 Share Share Apple Maps Newport, Vermont is going through quite a renaissance. What was once a sleepy town on the Quebec border is quickly becoming a boomtown, thanks to nearby Jay Peak Resort and an unprecedented investment of money from both the public and private sectors. Newport is situated in Vermont’s Northeast Kingdom on Lake Memphremagog, a scenic glacial lake roughly 30 miles in length; with one end in Vermont the other in Quebec. Local folklore even mentions that it has its own lake monster, called Memphre. During the winter the lake is a frozen giant, perfect for ice fishing and skating. While in the summer, it has a wonderful assortment of outdoor activities (which I’ll be writing about in the coming months!). The fact that Newport is just 30 minutes from Jay Peak makes it the perfect spot to mix up your ski trip with a little shopping getaway. I recently had the opportunity to spend a day with Patricia Sears, the Executive Director of the Newport City Renaissance, a not-for-profit tasked with advancing and enhancing Newport’s economic environment, developing a cohesive and welcoming City design, and promoting the City as a tourism and investment destination. An enthusiastic lover of her city, she led me on a tour around the downtown, saying hello to all the people she knew, while describing the many things that Newport has done and continues to do to make it such a vibrant destination.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • STIRRINGS in the EASTERN TOWNSHIPS – by Carl Riff
    STIRRINGS IN THE EASTERN TOWNSHIPS – by Carl Riff The first means of transportation in Canada was by water, so it is not surprising that the first railways built in British North America usually performed a portage function by providing a link between navigable waterways. The first public railway in Canada, the Champlain & St. Lawrence Railroad, was opened in July 1836, and is a classic example of a portage railway. It connected Laprairie (opposite Montreal) on the St. Lawrence with St. John’s on the Richelieu River. From there, steamers transported freight and passengers up the Richelieu, through Lake Champlain, into the Hudson River to New York. The only other railroads built in the next decade or so were another short portage line between Montreal and Lachine, Que, eight miles long, to avoid the Lachine Rapids of the St. Lawrence (in 1847); and another that connected Joliette, Que. to the St. Lawrence (in 1849). At the dawn of the 1850s, Canada was about to embark on its first railroad mania. The original role of railways was but a small cog in a water transportation system, but events soon started to stir in Portland, Me., Montreal, Que., and an area in what is now called the “Eastern Townships” of Quebec. The history of the Eastern Townships developed from the practice under the French regime of bestowing lands in seigniorial tenure, and when this was abandoned by the British authorities in Quebec at the beginning of the 19th century, the then underdeveloped territory lying between the St. Lawrence River on the north, the American border on the south, and the Chaudière and Richelieu Rivers on the east and west respectively, was surveyed and divided into townships of 5,400 to 6,000 acres each and designated as the Eastern Townships, however without any statutory significance.
    [Show full text]
  • Inside the Kingdom
    INSIDE THE KINGDOM January 24, 2018 the Chronicle Section B – 16 Pages Condos, Zuckerman break for coffee in Coventry by Elizabeth Trail COVENTRY — If there’s one thing Coventry can do, it’s throw a party. On Saturday afternoon, most of the town’s officials, paid and elected, joined Secretary of State Jim Condos and Lieutenant Governor David Zuckerman in Coventry’s community center gym for a voter information shindig planned by the town’s recreation director Martha Sylvester. “I had a lot of help from Deb and Amanda,” Ms. Sylvester said, referring to Town Clerk Deb Tanguay and administrator Amanda Carlson. “It was a team effort.” Whoever planned each detail, the freshly renovated community center gleamed. There were coffee and tea and cocoa, huge trays of doughnuts, and plates of home-baked cookies. Guests who wanted a place to sit could pull up a chair at a table, but most grabbed refreshments and mingled with the state and local politicians who were there ready to talk. Besides Mr. Condos, Mr. Zuckerman, and town officials, Vermont Senator Bobby Starr and Representative Gary Viens turned out to shake Vermont Secretary of State Jim Condos (center) entertained Coventry residents and officials on Sunday hands and answer questions. And of course afternoon at a political information coffee planned by the town’s new recreation director Martha Sylvester. From left to right are select board member Scott Morley, board Chair and state Representative Mike Marcotte, Mr. Representative Mike Marcotte, who is also chair Condos, delinquent tax collector Kate Fletcher, and Sheila Morley. Photos by Elizabeth Trail of the select board, was there.
    [Show full text]