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 1 
 
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/; 
 
 / 
 
 OF 
 
 ri 
 
 MONSIEUR A. MICHEL 
 
 GTSOLOGIS r, 
 
 1^ 
 
 ON THE 
 
 GOLD MINES OF THE RIVER CHAUDIERE 
 
 III 
 
 AND ITS TRIBUTARIES. 
 
 OF THE M m\ COLD MINING COIPAH. 
 
 '-»■ ^ ■> » 
 
 t / 
 
 QUEBEC : 
 
 PBINTIB AT THR "MORNING CHRONICtl^" OPPICB, FOOT OP MOUNTAIN HIM. 
 
 1806. 
 
Tt E B» O H T 
 
 OK 
 
 MONSIEUR i. MICHEL, GEOLOGIST, 
 
 ON THK 
 
 GOLD MINES OF THE RIVER OHAUDIERE 
 
 AND ITS TRIBUTARIES. 
 
 To the Directors of the de Lery Gold Mining Company. 
 
 GiNTt»««N,-Tbe valley of the Chaudiere, in Lower Oaaada excites 
 e ada„„»tlonof all thee who visit it. After i couple of honJrdVen 
 
 R.rer, on the conBnes of the Parish of St. Isidore. Then the road, skirtine 
 the nght bank of the river, passes successively through the parUhes o Ste 
 M^: at ;. T'' ^*,/""^"' *"•* '* «««'«•• -«» 'P«- into the State Of 
 
 An nnint! ' '"/ """''^ " '''°'''^''" ''°°» ''"«'' *»>« «»*d t^^es its name- 
 
 An uninterrupted succession of farm houses, cultivated lands, and agrical- 
 
 oral establishments please the eye while animating the scene y; and when 
 
 ™7w;tlT?.' ''IT' '' "*'^ " "'''""""' '^^ touri'st m'eer.t 
 
 r/c: ^h jrpist::^'" ^- ^^--^-^ ^-'-^ •"*-^-^. ^^e 
 
 The farmers of this dist.ict are the proprietors of the soil; hence the 
 are exb.b.ted in its cultivation. They are exclusively French 'oa .dian, 
 
 ^therr th"""'V"**"'.*'* **°«"«'' «"^»°'»'' •»•» "I'«ion of their fore 
 others This population is very sympathetic and hospitable in i.s character 
 
 Irl'ul'r »"^J'"*"«'"''» P°P"I««on; and to the persevering eJ^Jt, J; 
 several A«6./a«s-who became miners after the gold discoveries-are 7«?*i,/ 
 
 z^s:::^^r'- " '- " ^'^^^-^ "^ -h:=o::'^^ 
 
 P.rl'\^t^T^ Of Kiguud-Vaudreuil, which at a later period became the 
 Pa sb of St. Francois, is situated at about 50 miles distance from Zb^o 
 .a the most picturesque portion of this beautiful valley. It h«^H e^'tSj'! 
 »!ong the Ckau,Iure River-which flows through Md divideTittnto tw« 
 
 of the river, and has a general superficies of 84,672 arptnh. 
 
or •''•/'A-«^-e;.„Vb;7«ltr^^^^^ -- tl.e»aintr,bat.,ie. 
 
 W become swollen and tor^tuou. Th7n °''. V""' P'""*^" "^ »»•. 
 /«««. or J,e> Planter Ri.er, on the ri.btLM' ""*"""' ^'»« ^•"^- 
 Ri-er. "Mill" and Z. 5.„, on its left bank "" ''*'"'''""• "<» »»>« 
 
 "•, tb..rt, f„ ,t. „„., ;."t,7,f; ?«'••'. ""^ b". ..a ,h„. crop 
 «ll"lon, ,f ,„„b,, m^i,',,, • """'"' "°'I" l«jcrs or „g,t,bl. mom or 
 
 «!■« Of rn,«^ Honrj W«rn.r T^ "" ""°«*>«lfi-t., «.o.goth.,, 
 
 . , '^epjoie with encouragement. 
 
 ;ero«.:Xrth:rj^trand\rp"^^^ -— theaur.. 
 
 the r..«lt. Obtained since 18C3 r embodu? ''V"' '"''' "^^Wiahed and 
 which I had the honor to addre « to st W ^ ''''''''''''"' '" ^^e report 
 ^.t. It 1. only such of .hoae obs ^v! llanr"' "" *'' '"' *'^^»'"»V 
 Se-gnory of Rlgaud-Vaudreuil tbl "l rn, ""'V"^""'""' "' '«'»'« »<> the 
 page., adding thereto the in L^UoVlZt. V"" "^ '"*''« ^°"«^"g 
 tion, in thi. present month of luJZ ^^^^'"'^ ^^"'^i '^J recent explora- 
 -ce Of .teen days ^ro^^J^T^^lJ^Z JJ^X" ""'^ 
 
 Bonrce in the northern part of tbiMerdtv " r •'''' """ ''''"''" "" "' 
 reunua at Lot 73 in the Concession ScL' u "" •"' '"'^'''"'' '">'«'' 
 from northeast to southweat in the ConcestZs. a ^""?*^ '•"°«'' ^^w. 
 aod In the first range northeast of the So ' .m ^*''* ""^ ^»- O'*"'". 
 other, Which flows down from the Col!^sTon7i '* *"' '"'°"°° ^^ »he' 
 northwest, through the Concession St CbTrle;. ' "" ''*'" ''°"*''««« *o 
 
 tion.tfir::r?g:X:cierr; ''"r-"- -"— «io,p,ora. 
 
 effort, greatl, contrL^d to The Ico; 7 ""r*"*'' ''''°''« enterprising ' 
 
 took the working of the mines with v!' 7.?°'' '" ''''"' Canada,'nder' 
 tily Of gold obtained. Since Mat r ^ Jtisfactorj results as to the quan- 
 
 -rching for the preciotrii; J Te ed tf'r '''' ^^° -"^«7 
 **ter, and they hav-oi , . , °® "**' ^^ the river, at tiai»« o* l«= 
 
le maio tributaries 
 ral ptrloda of th« 
 tins are ihe Gutl- 
 auditre, and the 
 
 itituted of schist 
 f quartz, some of 
 ' locality, while 
 bedsof grarel. 
 
 Silurian forma- 
 
 and there crop 
 
 •table mould or 
 
 fical Survey of 
 ii among others 
 >le information 
 ictir 18 relative 
 ouragement. 
 
 nine the auri- 
 itablished and 
 
 Jn the report 
 It of February 
 " relate to the 
 ^he following 
 cent ezplora- 
 
 to the short 
 Jmy. 
 
 '88 the River 
 '/««/«« has its 
 whes, which 
 branch flows 
 St. Charles, 
 otion of the 
 ioutheast to 
 
 i-al cxpiora- 
 nterprisiog 
 Bda, under- 
 the qasn- 
 constantly 
 Jes of low 
 '«7> 'n pro- 
 
 I devoted several days, in October 1803, to the cxomination of this river, 
 Roiug up its bed between the 'wo Falls, and I was excocainyly well satisfied 
 with the results of the exploration. Recently, I visited that part of the river 
 situated between the Great Fall and the junction of the two branches, and I 
 also explored the southeast branch, aa far up a? two miles above the Fork. 
 
 I found gold everywhere, on digging into the soil, in the bed of the river, 
 and in the high banks. A washing with the " rocker" of about a ton and a 
 half of gravel, made up from different excavations, gave nearly a doUat's 
 worth of gold. I am persuaded that a systematic working of the alluvion of 
 the River i)f,s Platitea would be profitable, and that it would not be either 
 difficult or expensive in the higher parts of the stream ; the sinuous course 
 of this river, and the peculiar configuration of the land on its banks, permit- 
 ting a variety of cuttings and the sinking of canals, for d ainage and to turn 
 aside the river and lay bare its bed. 
 
 A quartz vein crosses the River Des Plantes below the Little Fall, and 
 besides the numerous fragments of this mineral scattered here and there in 
 the bed of the river, I met with very large blocks belonging to a vein— the 
 cropping out of which I could not discover— in the southeast branch, at 
 about a mile and a half above the Fork. Having assayed, mechanically, 
 several pounds weight of this quartz, I found a few particles of gold in the 
 sediment of the washing. 
 
 Some of the habitans, whom I questioned on the subject, assured me that 
 quartz crops out of the soil In divers places in the Gottcessions Frazer and 
 St. Gaspard, and I am of opinion that a special exploration of these Conces- 
 Bioni would result in very interesting discoveries. 
 
 From the River Des Plantes to the residence of Mr. Louis Barbeau, for a 
 distance of several miles, the road crosses a number of small st ■rr-s, which 
 fall into the Chaudiere, and in most of which gold in alluvion hi j already 
 been found. One of these streams, " Marcoux Cieek," on Lot 30 of the first 
 range northeast, is traversed by a quartz lode running from northeast to 
 touihwest, which is known in the neighborhood as the " Rodrigue-Vein." 
 
 My fattention wa^ particularly attracted by those lots, in the first range 
 northeast of the Seignory, which ere washed by the C/iaudiere, at the place 
 called the '• Devil's Rapids." Eere the soil is uneven, ravined, and divided 
 into mounds or bluffs, which fall away to the river in slopes that are often 
 very abrupt. 
 
 Between Lots 4S and 55, on the property of Mr. Louis Barbeau, are 
 visible several elrips of schist and clayey gravel, cropping out in ridges 
 above the soil, and traversed in every direction bv veins and seams of quartz. 
 
 Certain croppingg out of this minsral on Lots 50, 51, 52 and 53, seem to 
 beloiig to lodes ; but the indications in some excavations made here and 
 there on those same lots, lead me to believe in the existence in this locality 
 
trold T u """""i 0/ uis mechanical ads.. "oouea it with care 
 
 oenind the property of Mr. Louig Barbeaa " ''" ^*"»" 
 
 the contete'lnhJt'",^;;';/"^''^^^'^"^ ^^^gi^t after in tbe Caur 
 PTticoIarly at the CrR^Z'^r' '' '""> «o'^ »>«arini.r?a; '";;?' 
 
 Creek" on Lot 59 A of the firsf ,. ^**' °''® <»*' these, called « Rnl ' 
 
Tbn (greatest quantity as well as tho largest nugi{nt8 of Canadian gold, 
 up to the present time, baye been gathered in the ToujTt des Pint or Gilbtft 
 ftlver. Like the River Dtn Planter, the (iitbert River takei ita rise in the 
 north, UowIdk in two branches, which reunite on Lot IG of the GonceBiion 
 St. Oharles. The main branch flows from north to soatb io the Gonceisions 
 De Lerjr and St Charles ; it takes a bend on Lot 7 of the latter CoDceRsioo, 
 and then traverses the first range northeast, directing its course from north- 
 east to southwest. 
 
 It Is the rich products of tho alluvion of the Gilbert River which have 
 principally attracted public attention to the aurifevous deposits of the ChaU' 
 ditrt ; I therefore felt that a special exploration was duo to this portion of the 
 Seignory. 
 
 Notwithstanding the favorable results of the works undertaken by Dr. 
 James Douglas, sixteen years ago, gold in alluvion has not yet been actively 
 sought for in that part of the Gilbert River which waters the first range 
 northeast of the Concession St. Charles. Neveitheless, a mining effort 
 undertaken in the course of last sommer, on Lot 75 of the iirst range north- 
 east, gave satisfactory results, one of which was a nugget weighing six 
 ounces. 
 
 Qold has also been found in the Concession St. Charles ; notably at 
 <« Oaron-Creek," as well as on the Lot 14, where four associated miners took 
 out four ounces in one week. 
 
 Tho alluvions which have produced a considerable qm^ntity of gold, 
 without their richness being yet exhausted, are on Lots 18, 19 and 20, of the 
 Concession de Lory. 
 
 On the occasion of my first visit to the Gilbert River, in October, 1863, 
 Lota 13 and 19 were occupied by about a hnndred miners, whose labors, 
 carried on in the open air, consisted of a series of excavations, sunk one near 
 the other, without method r^r regularity, and constituting on the whole a 
 general working without b . .m or order. 
 
 It is in this deplorable state that the organised companies, up to the pre- 
 sent time, have abandoned the allnvial ^dli diggings to the industry of the 
 habitant ; and these (diggings— often very productive, notwithstanding their 
 irregularity, more or less actively pursued since 1863, even during tb« winter 
 months by means of wells and tunnels— extend at the present time, with like 
 success, on Lots 16 and 17, at the junction of the two branches of the river. 
 
 In all those excavations the gold is found in the gravel' resting on the 
 hard-pan, formed sometimes of schist, sometimes of gravel, often of both 
 these foimatious interstratified : bnt the precious metal is found lodged par- 
 ticularly between the leaves of the schist, and the cracks of the gravel, whern 
 the latter has penetrated and become hardened. 
 
 It is certain that the alluvions of this locality have blready produced 
 much gold, among which were many nuggets varying in valne from f 25 to 
 
8 
 
 *w.l^'SJ;r;,ti!;°.:,t::'. "rr" """■"■ ""-'«' i-m .^. .nu 
 
 •PP'M.MIIr.l,-, ibo ,,„„,;,„ .„. 7."'' ", " '""""' l» eiUm.1,, ,„„ 
 
 '» o«.=..i, .b,i. <,,„„,. b„v„ ., j;„tn ,:;;°;::',;r """■" ■''~ "'■•" 
 
 y 'bid. it eroMe. at Lot i ; s.„ ' ^'""»"'" J" l-m .ud Ob.„„,J, 
 ■">'"-"»"-.«. .0 .oulb "„ b L ' r?'? ""'"■"S"'. '""»>.» from 
 
 jreenlBh gold in .ueaUon, Z piel "wZ I ir^' '''''''''''' ^' ^<> »»>« 
 bat recently detached «id not .!. e^^ammed seemed to Lave been 
 
 «o..o„ .ub „,b„ .on;;b:i:ir.L"::xt" '•- -""^ - ^1° 
 
 The two branches of IheRivor /'./a- # 
 
 which come down to the cwL; '^'''^^^ 
 
 I'erj..8t.0harlea, and St 1 ": nCr^.'^T^' ''' ^-«'«"'0««' ^e 
 northeast to southwest. I slw'ZTJ '' ' '^'" *""''"°° ^eing from 
 
 ;onr feet, a little wa, ubo.e're" 3:^?^ "^•""'^' "'°^ »' - >" 
 Concession do Lcry. "caration which I made on Lot 26 of the 
 
 B«tag ..«.,.d m.ch.„ic.|l° soita „fS^-°* ^''"' '■"""of'b.c.mnt. 
 lion 0. tb. tigbt babk, , c„™m t, .„,v t. ° '"'"'' '"^ "• «»'- 
 lie Mdii>„», of lb, „„»u„g '" """'J--"" "T Ene p.piloi., „r g„u ,„ 
 
 o.3.irsftrrr.":irti7r'''°'-°-'»'*-''-- 
 
 «<««J«, inweb. Dr. f. Stem Hunt ««l7^i,,C f'^'""^'- »"l«'l« 
 »25.e6 pM ton. ^ "'• "''"™'' *» P'odoct to an arwage of 
 
tvta 
 
 On Lot •'•2 of the lirat range northeait » quartz cropplog out of from four 
 to &r» fttt in tbiokneu, known in tlie localitj as the " Loabier-V«In" wai, I 
 am ioformed, subjected to lome asaayi, one of wbloh, made at New Vork, 
 Attributes to the mineral taken from it a production in gold of $15 per ton ; 
 and tbia value was incrensed to Sl06 per ton, hj nnotiier nssaj made bj Mr. 
 ColTln. 
 
 A rnry slight surl'ace working, consistiog of a trench sunk to a depth of 
 from two to three feet, exposed to view on Lot l:) r'' the Concession St. 
 Gbarlts, a bed of quart/ which lias hccn named the " Louivon-Loubier- 
 Vein." The assay of this quart/, by H.*. A. A. Hnyrs assigns it a ralue in 
 gold of $70.9") per ton ; a value which six nssn}?, nia'^o by Dr. T. Slerry 
 Hunt, redneed to an averag*? of f'.'t.Tl per ton. 
 
 Finally, a well has been Bunk on another lude, on liOt Hit uf the first range 
 northeast. 1 assayed mechanically JO lbs of quart/, taken from this, the 
 " Rigg-Vein," and Ibund Bomo particloa of gold in llie sediment of the washing. 
 
 Thus, operations of a suporliuial cbaniclcr, opoiicd at the cruppiogs out 
 of several bods of tiuart/. in tho Sjoignory, have cuablod o)» to establish their 
 existence, to determine the directions in which ihcy run, and to extract from 
 them a certain quantity of mineral,— tho repeated oaaays of which have 
 proved, in the case of some cf tho specimens, u well pronoonced value in 
 gold. But the conditions of regularity or irregularity, the average richness 
 and capacity, and tho continuity of depth, — that ia to say, all the conditions 
 necessary for tho more or less profitable working out of a «iuart/. vein, — must 
 remain in doubt, until a solution is dotcrminou hy operations ot greater 
 magnitude than have been hitherto attempted in tho Ohaudiere gold mines. 
 
 The mines of tbo Soignory of Rigaud-Vaudrcuil, situated on thu lei i bank 
 of the Chaudicre, have not yet been explored. It is known, however, that the 
 alluvions of the Uivcra Le Brat and " Mill'' are gold bearing ; for grains of 
 the precious metal have been found in both these principal streams, as well 
 as in most of the creeks which cither flow into them or fall directly into the 
 Chttudiere. Recently, I went over tl:e Goncessiotis of this section of the 
 Seignory, and I remarked numerous croppingsout of quartz at the River Le 
 Bras, whore tho gravels and clayey schists are intersec'td l)y veins and 
 seams which cross each other and run in every direction. Home of these 
 Teins have a width of several feet, and those arc the ones which appeared to 
 me to be most regular in character. 
 
 The landa watered by " Mill' River, iu the Conccfidions of St. Etienn* 
 and St. Guillaume, are also traversed by largo ridges of quartz, associated 
 
 w.fK a/>Ktof 4(iA ««Fnnnlniv« aii( nf nrViir|t T aato at T.oira Cf VpAnf>'\|.* 4%mA *\*^ 
 
 course of which I followed through the townships of Lampton and Forsyth. 
 Those croppinge out are again met with on the road from Lambtoa to St. 
 Francois, and at Lakes Volet and Rond, in the Seignory of Rigand-Vaudreuil. 
 
10 
 
 The reins which I pointed out on the right bank of the Ckauditrc, aoiodc 
 
 he a,m„ons of the Gilbert River, are discovered in the prolongation or 
 
 these ridges; besides which, I would also mention two other lodes, al^a,"/ 
 
 .nd" 1 T: '*" '"' °'r '"^'^''''^ '^' - '^« boundary l!; Of l1 
 •outh of Mr. de Lery's m.lls on tlio first mnge southwest. 
 
 of a ^!!r T Y"^'^ '"''"^' '" "^''"'^ '^" ""^* f «'^^' ^«'""l'«<i and noted, 
 of a favorable character U the future of the gold bearine lands of thJ 
 
 ^gnory of Rigaud.Vaudreuil. and atfording encourageZVr their deve 
 1 pment But, besides the Btriking local tac.e. which, of themsC already 
 g.ye»a mcontestable vulu« to this extensive proper y, I augur in tsflvor 
 
 "SUd aS' "'^"•r'",^ '--"'ereeent'disc'overieflde ICai: 
 [rvet Witt -K. ^ ^•T'"^''^ g"ld-bear:ng regions of undoubted ch.rac- 
 
 Gilbert Rjvor permit us to make comparisons . 
 
 In Australia and California the later, or contemporary alluvions resting. 
 
 on the EUurian formation, at the level of the earth or witMn a fl^ of 
 
 to surface, naturally «ere those first discovered and turned to aclount for 
 
 the working of this class of aUu.ial mines is that alone possibe to those 
 
 ZZT.T"' "''""' •" '""^ ^''^ «^'^« ^^«'" »l- '"O'nent that fam 
 has pointed them out to the seekors after gold, 
 
 metaf l!!"'"' '""'' '^' "^''"^"^^ «'" '^'°'' <l«P0"t8, in which the precious 
 metal was very capriciously distributed, but which, nevertheless, produc-d 
 immense wealth discoveries have been made of ^ore ancient\nuvions 
 h dden by deposits of later date.-buried so deep, in Australia, that to reaci 
 them necessitated mining through layers of argile, sand ani basalt, to « 
 depth varying from 45 to 400 feet. After some cautious attempts thi k^^d 
 of m mug was perfected, and to-day it has attained a marvellous degree of 
 success and prosperity. ""grce oi 
 
 These enterprises are of that kind which exact considerable time.capital 
 ad perseverance ; yet the profits are generally so great, that a shar; in he 
 
 InZTu * '''" '' ""'" '^ '"''' '"^""^- ^" "''^> '^^ "-^^"^ 0? h 
 ancient a uvions is sometimes so much superior to that of the modern depo- 
 
 ts that the, acsuon has beenasked, "ifthose alluvions are really produced 
 
 '. ?ormrtiororftt" '''■T """'^' ''«^- which pierce through th/sHurSu 
 formaiion, or it there might not be underneath the solid crust of the riobe 
 an immense reservoir from whence this gold comes, aud where no doubt 
 
 adrtirrLr^i^^r "r ^-"^^^ ^^^ «^'«- utt;rance tt; L houg^t 
 adds, with reason that we dare hardly risk hypothesis on this sabjeot. and 
 
 X s wilZirH" rf .'' "•''°"' °^J«^'' «-'"« '^'^^ 'f there 8 ould 
 exist within the bowel, of the earth, real agglomeration., nf nati- -Id th^- 
 must assuredly be at a depth impossible to~reach. ' " *""'"""'' ^^'' 
 
 But whatever may have been the origin of the ancient alluvions does it 
 not seem probable that they may have contributed, in certain locamt to 
 
11 
 
 iiere, aiuoDg 
 lODjfation or 
 des, alreadjr 
 ' line of Lots 
 pentB to the 
 
 1 and noted, 
 ands of the 
 ' their deve- 
 vea, already 
 in its faTor 
 ide in Cali- 
 ted charac- 
 lucts of the 
 
 Dus, resting 
 w yards of 
 Jccunt ; for 
 le to those 
 that fame 
 
 e precious 
 produced 
 alluvions, 
 tt to reach 
 asalt, to u 
 I this kind 
 degree of 
 
 ae, capital 
 are in the 
 ess of the 
 crn depo- 
 prodaced 
 i Silurian 
 the globe 
 no doQbt, 
 I thought 
 jeot, and 
 'e should 
 :o!d, they 
 
 s, does it 
 lities, to 
 
 4 
 
 tbc enriching of the later deposits ; and may not this supposition be admitted 
 ia respect of the deposits so profitably worked out on the Gilbert River ?— 
 ■upposrtion which naturally leads to the belief in the existence of aneient 
 and very rich alluvions in the gold fields of Lower Canada ! 
 
 The incessant washings, by the operation of which nature forms the 
 modern alluTions,— washings which appear insigoifleant when compared 
 with the resistance offered by tbose rocks which enclose gold, — become very 
 effective when the subterranean waters, disturbed by exceptional causesi 
 react upon and upheave the ancient alluvions. 
 
 Such may be the origin of those unusual deposits of gold met in with 
 the modern alluvions, and it is in reliance upon these considerations that i 
 have always believed that the search after the alluvial wealth of Lower 
 Canada, received a strong guarantee from the mining results of the Gilbert 
 River ! 
 
 Moreover, we must not lose sight of the fact, that there exist many sec- 
 tions of modern allavion in the Se . .ry, capable of being advantageously 
 worked out by the Californian methods, which permit the profitable wash- 
 ing of gravelly alluvion when the minimum return in gold reaches only about 
 10 cents per ton. 
 
 The crushing of quartz which does not give a gold value of at least $7 
 per ton, becomes unprofitable in Oalifornia and Australia, owing to the high 
 price of labour ; this would not be the case in Lower Canada, where labour 
 is proverbially cheap. I have pointed out the abundance of quartz bedi 
 already discovered in the lands of the Seignory, as well ad the favourable 
 results ot the assays applied to the mineral extracted from the several veins. 
 Tet, as I have already said in another report, the distribution of gold in 
 quartz is so irregular, it might often be dangerous to receive with too much 
 confidence, (with a view to operating,) the average richness of a bed given 
 by assays of specimens, even when those assays are numerous. 
 
 In conclusion, gentlemen, the certainty of the gold bearing quality, in 
 a very high degree, of several of the quartz beds in the Saignory ia already 
 an important fact ; and everything leads to the belief that the crushing mill 
 in course of erection will soon prove, by its results, that the working out of 
 the quartz of the Seignory of Rigaud-Vaudreuil, as well as of its deposits of 
 allavion, is worthy the attention of tbose interested in gold mining and the 
 confidenca of capitalists. 
 
 I have the honor to be, gentlemen. 
 
 Your very humble and obedient servant, 
 
 A. MICHEL. 
 St, Francois, County of Beauce, 
 August 16tb, 1866.