010

GEOLOGICAL REPORT

on the

QUIHKE LAKE PROPERTY

of

BEIJAST MINES LIMITED

in the

BLIND RIVER AREA. ONTARIO

by

ALBERT HOPKINSB.A.Sc., P. Eng., M.C.I.M., P.G.A.C.

Consulting Rining Geologist

BLIND RIVER, OUT., 1951*

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^3!bi* consists) of fifteen contiguous unpetented joining claims 8*73fjftl to 8.72795 inclusive, comprising an area of

LOCATIOB

IMo property li*e about tvo ailes northwest of tyixke lake, a mile southwest of Little (fedrko lake, and about 27 '^ s^l** northeast of the tom of KLlnA River. Ihe property la north of and contiguous to the fedrke lake property of A.x goa Uraniua Mines Ltd. The south boundary of the Belfast property Iles abouJJ half a vile north of the Algon five-coB^artaentB shaft,vhieh is north of the ierpent Kiver and about tvo miles vest of (fcdrke lake. 5he Belfast property lies in the north-central part of township 150, Blind River Area, Sudbury Mining Division, Ontario*

ACCESSIBILITY

Thlo property aay be readied by driring fro* the Bain Sudbury-800 highway starting about three miles east of Spragge station on the C.P.R. Soo tine, and thence northward about thirty Biles along the newly constructed road to the Algom (feiirke lake shaft area, and thenco 01 foot half a mile to the north. The Bolfast property aoay also be reached by air from Lau-Ooma Airways base at Algona Mills, Out. on the Budbury-Soo highway to Little (^ilrke lake, a flight of 26 miles, and thence by trail for a aile southvesterly.

This report is based on the current geological survey, and on tha following govenment geological reports and napsi-

Geological Survey of Canada - Itenoir 1^3, 1925. "Korth Shore of Lake Huron"and KHLind River" geological aap Bo. 1970, by W.E. Collins.

Ontario Department of Nines - 3^th Antatal Report, part fc, 1925, "The WhiskeyLake Area" by O* Vibert Douglas and L.7. Kindle.

Geological Survey of Canada - Meaolr 160, 1930, "The Disappearance of theHuronian" by Qoirke and Collins.

Geological Survey of Canada - "Canadian Deposits of Uranium abd Thorium"by A.B* Lang, 1952.

Qeologioal Survey of Canada - (Radioactive Division) "Prospecting forUraniUH in Canada", 0952*

Ontario Department of Mines -Annual Report, 1952, part kt "Geology ofBaldwin tvp M by Jstsea X* Thcaaon*

Ontario Depsr^arat of Mines - Freliitinary Repart Ho. 1953-2, "Geology ofLoog and Sprafge twpc., Blind River Area" by B.M* Abraham.

"''

.JT..•f.;--

of ifca contact between theturonian eodlsMnta 4 ' -- '

axteasi* areas of Keewatin. .. . , in turn jugectod fcgr large gabtoro-diortte

intrusive*, related dark basic AS&nan types, and latet by XavMnavan rocks.

edge of 14* north flarifc of a vida synclinal strnctura of aoroni stre&a, extends jrt*4 tooth of th* Belfast property in an aaaVwaat direction. Ita east-weet soda extends about thirty *ile* east sad vest, andlng at ndskey lake st ^he Mist* Tba width ttf t^* aynclinal fraaiy*~tf*iBfrV trough is about idle* at it* (*iirke lake section,

It nay ba asamed that tba- early pvnaartalan ocespoait* structure nsntionedea the Belfast prcyerty'i vlli also generally underlie at

depth the MtMflTirfaf^ synclinal basin, on **t*1'?h la located t^e AlflpB *^*f'Hce lakeBCoa* - , '

dabriv, chieflyoowrlng ofBelfast roj*rty, being ebaractarlatlo of axrh of

batpaosd 1900 tha aaltinB of eattenslretill, vaa deposited wme the tha terrain of Bortharn Ontario.glacial ice fields* After the flooding of auch of the vicinity of Township 150 by the vatera of tha then *Qrea.ter Lake Huron*, certain areas of tha glacial till evidently beeaae subject to vater and vave aorticg action* Ihe result wa that today a mwber of "raised boulder beaches" nay bo encountered in the township, notably on the Belfast Minos Ltd * property* !Hbese localized areas of boulders, Bony of vhleh attain a Isoree Mice, vere aejppad and are shovn on the aoooBOaiTying geological sketch plan*

A preliminary geological survey of the BLif*ct Unes ltd., property ahovs that rcHoants of tibia early Keewatin volcanics, nt* readily identified aa auch, accur broadly scattered. Bovever they do not exist aa s, large proportion of the igneous rocka as a ufaole, except perhaps that variety of volcanics described aa dacitlc and rhyolltic rocks. Certain of these way, en first observation during iMnaning, lie taken aa aplitic dyke rocks.

A largo area of this type of acidic rocka is loentad in ganezal proxladty to the south boundary of the property toward the east side of the central area, between picket linea noe. toOO and 2000*

Kxtenoive batholithie granite invasions of tha ^xirke lake area, as mentioned above, replaced atoet of the presumably thick acciasilationn of Keevatln Tolcanics. iSfcese latter doubtlessly eoqptlaed basalts, and andaaitea aa veil aa daoitea end rhyolite** Mar* ranoanta of the basic types rensin, and certain of these have poaalbly.ttan olajaified during B ipplag vith plutonic rock types, auch aa anphlbolitaa and diorite*, ate* This if due poasibly to tba lack of character istic geological features, auoh aye flew structure* Qve affphlhiflitaa and dlodtaa re often atoovn in aapping o* Kesroenaswm dyjoaa* Sbe granite dykat ara usually

ooyriaiiig ft hcornbJjSoAe-granite, r/ed in colour*

y - -* '. - ' fc "- * - . - j -* i' - v - s - - - . - . ,: \ ''^kA*V*f Jh^a rib*v eb^fe^K •'^a^k* e9^^^waV ' e^^a^^^^^^^h^^ ^^^^^^^^^ ^A- ^t^^^^A^

— ——,Jw^**O*eV V* wOB J3HJL*ejilB*FV SVvVv^TOW^ VeWw •*aMPCpV''SOn*JJJ

^ l*oriibltnd*~*y*nite,-, Igpllta dyk**, afi4 notably larga dykaa of a ; '- w — —-— - -r - |pr - --r ^-r - - - - , t , - -^- —^ . —— ^p — * w - ^ ~ "— - - * ~, *^~ , T* —— - ' - ^^"^ ~"——4^ ——~- W — B* ^ W ^'

1^ latter 1^ aftinly eoaoiwtvsd vlttin the granite are^ of 'th* *aa^oectral^are* of Uxt j^peny c^ bc se^ to have Sttfferad injection by theji^luQBQM^k B jDQsiVVUBNBVDuLj^ JajflR^ftAQaWlaas J - aVlcL * cQf ItCttt vajJDQltftfl jpa^J-fljBPa^flPfc^hCBfBaa^HPyjf A - ^R33rvft1*MP

aotrth the apUtJU) "rhyolite" is travet^Md by peridotite aod a trap dyke (se* the

': ; --- A dlorite^Drpbyryi prest**.bly of Akileyburian age, can be seen in ^,. outcrops at the north end of picket lin* So. WOO. Xcveenavan pJutonlc

,'.-'V:' injsctioo ecBfports^s a large part of the "opei'ty area. Individual dykes attain 'I'X' iridths lu excess of four hundred feet, these may b* seen on examination of the , 4 gaological nap, to tcvpris* several rock phases, Mainly aaphlboUtes, e.g. In the ^U - .sottthyest/'earner vt the property on claim Bo* 8*72783* ' " :' .. -'

- ; ) Peridotite dykes, up to a hundred feet in vidth, aey possibly date froD wither Kevaenavan or earlier tias, They occur as isolated injections, the

, longest of vhioh crosses the bas&line betv*en pleket lines fi^OQ 1 and 3&0', *h*r* it apparently ti'aiws*s the dacite-rbyolite* locally five hundred feet vide, these rocks are also traversed by a diabase dyke.

CHRCfKTLOSICAL

In* gaologloal history and relation of the svreral epochs cited in this report can be BUKmarited in a table vhich is drawn up here in resune briefly as follorst- Fleistooene and Recent

Boulder till (glacial), and angular boulder talus slopes (Beeent)Boulder beeches, dating froa the greater lake Huron, of post-glacial

Beeent tints* Keveenavan j

Trey dykes, gabbro-diorltos, Gabbro, and Diabase. j Balleyburlan i

Diorito (porphyry), and possibly other basic dykes. '

These ssdinents are singularly lacking on the Belfast property* jf

Aophlbolltes, lamprophyre, perldotitfts* ' feldspar-porphyry, Quartfc*feldsper~porphyry

Qyenlte, aplite dykes, hornblende^granlte* Keewatin

Basalts intercalated vith andesite, dacite, and rhyolite.

PSTROLOOY

A descriptioa of the aain rocks encxxmtered on the Belfast property vill be sunnarised here, ranging fron th* earliest to the latest rocks i-

KeevatJin - .Andosltst ails rock vas tentatively recogniaod in outcrops where it was

alternatively ascribed to a diacritic plutonic rock. It is dark groen, fine-to iM&lxav-grained, vith a scarcity of felapathlc constituents. B&csusa the rock vas usually observed ae a Massive typo, its designation as a flov rock say be accepted vith reservation i

Basalt! Darker, very basic exsnples of peridotite and aaphibolit* MQT in

ML ,w* B?*BV t be mor* aocttrately ascribed to basalt* ?t* basaltic phase of tte volcanic.rocks Is dark ,

i?-'; t''

PJ vhere ms^ped as dj*e*|as*-, fcck in appeexa&oe tad usually fine-grained! the rock

Comprising flova, of varying thicknesses* Only a fev evtji^let * recognised on the propei-ty, vhich might be ascribed tentatively to bmoaltlc origin. The basalt show a characteristic lack of feldspar opnstltuenti* . -

TMs group of volcanics, vhere mapped in the southeast and soith- central areas of the property, are aassive and fine-grained. They Vdather to a light pink colour, and tend to shov bending effects in tha hand speeiaen.. Petrologlcelly, hovever, certain of these consist of a rodt that is fine-grained and highly feldspathic, massive, and ponsequontly bearing an epHtlo pltitonle appeftranee* A dacitic semple vas noted aa a porphyritic type vlth feldspar phenocrysts and an aphanitic groundmass. Hence the rock appeare more probably a fine-grained, feldspar-porphyry.

Bhyolltet Kiie Is one of the *ost peoullar rocks encountered on the Belfast property. It If typically siliceous, and in places consists of a flinty chert. This la notably seen at the east and vest boundaries of the property e.g. on picket line Bo. 1*000 in a eeven-ft. vide out crop of the chert, it is found in sharp contact vlth a semi-foliated aetadlorite, The areal extent of its distribution is considerable, over a distance of tvo thousand feet in the south- central section of the property.

AlgomanSornble vle-granlte : Tfci* rock usually has a red colour *nd contains In the typical

massive, medlum-to coarse-grained outcrops about 30^ hornblende, e. only distributed, as veil as About Pft ouartK phenocryst e, the balance being chiefly feldspar pheuocrysts*

Hornblende- Syenite: Thftse syenite* reaenthle the granite, generally, but lack, hovever, the quartv phenocrysts, except in occasional instances vhere they are noticeable, approximating five, per cent of the rock. A medium-grained type of the syenite occurs, containing feldspar pheno crysts. Bonce this particular section can be designated as a syenite porphyry.

Aplite Dykefll Samples of this rock v*re taken in vhich the matrix appears banded.The rock contains email- sited , thinly distributed naflc minerals, and hence la essentially a syenite vith a highly- feldspathic seal-massive matrix. fala pink, massive, fine-grained types of this rock also occur.

Feldspccr-porphyryt These dykes occur as plutonic rocks at distant intervals across the property. Band specimen* show a mediua-grained, massive section in a dark, aphanitic groundmass, the latter sprinkled vlth 20^ of feldspar phenocrysts. One speclnen shew sericitic alteration, and is lightly banded vlth 03jt of mafic minerals present.

rif^vvv:--- l^^-r^M-:

is

occur:as IDjl of the - -^5.'^rs .v.'-..v -.-. •••.•..--.-M r-^r':'*"r~~ -1 "'.ii i\*t^Mfr.pf ^ ,l*]i^ etiMJftix^ of ttMLtstt

'tV/ft* ii''*^ , /'f ~. - ' ,.. " l--s. , - ',' y. "i : ; ' : ,": J.'. "'''f , ," , .-l'*'.. .. j' - - .' . ' '-' .";. -, ' ' i ,

'^•^ " :^ ' ".•^•'•tf* •'^•'*Cr i -'' ' ' i-V - - ' ^ '" -^-- - , " . -.i'''' " . ' -

" * and Oebbro^dioriteB^, de gabbro and related rocks comprise extensive, 1 BZ& iivjiiia&e*:^

i ' i H!/.r VMM T?^ ny jrAy * i* ix'twv 3L*mi^ vjt^o JUU9CLL W7XV(^Ol-^9 a jWX C3CftntDbL6 OdT ^liCk '

'-:- latter ts at plckei line M800'8 Vhere the dyke appears to traversemassive granites^ indicating a post-Algoman age* Pyroxenic (gabbao )

; } types *ere wt necessarily distinguished in mapping frott the diorltss. - i ,^^.j * * l' '' -' H '--' - - ' " - - '

ccirijpltt. V Hoiri9Treff to possibly aM as an indicsto tovard direction of nansive flovsi if such they are In wich of this area, the finwvgradned and usually darkw-tinted ty^ oliutaed as dioritio1 vblle the doleritic, less basic types^ wiually noted as coareft-grained^ are referred to the gabbroa until closer identification beconfts possible*

A fptartft-gabbro type vas noted* It lo ibadlum-to- coarse-exained, and contains 20^ feldspar phenocrysts as veil as a sprinkling of quarts phenocrysts, the latter being a sixteenth bf an inch long.

gabbros and related rocks appear as medium to dark green rocks, possessing approximately equal percentage of feldspars, largely as phenocrysts, and the mafic minerals, pyroxenes, and/or homblendio mafic minerals, ttie above mentioned riner&ls conqprlse sons seventy percent of the rock, the balance consisting of a groundmass of similar minerals, in which, however, might be found the accessories, biotite, ilmenite, and magnetite.

Peridot ite-Anphibolltes i The very basic rocks, typically dark green to blockish in colour, occur as dykes or isolated intrusive masses. The maphlbolites consist of almost vholly hornblendlc mineral aggregates, vith a email percentage of feldspathic crystal constituents* Of the tvo, peridot itoa are a softer-veathering rock, and contain a larger proportion of groundnaas minerals. Microscopic examination would probably shov a small percentage of accessory minerals such as olivine, biotite, etc.

HurxxaituiThese sediments have been eroded from the surface of the Belfast property. Their present northern limit is less than a (juarter of a mile south of Belfast on Algom's Quirks lake property, and taey angle north of vesterly to vithin a few hundred feet of Belfast's Bouthvcot corner.

HaJXeyburianDiorite-porphyryl A dy*.1) of thin rock outcrops at tho north end of line

It contains large palo-green phenocrysts up to half an inch in length and its lithological nature is comparable to that of dykes of Baileyburian age in Eastern Ontario.

KeyecncomnIkabase ( Dolerite) 13als is a gabbroic rock, usually medium-to-coarse-grained,

ill vhlch feldspar constituents occur mainly vith an euhedral, veil- defined, evenly distributed habit* Thusly the diabase is dis-

. tingulehod frooi a gabbro microscopically. A diabase dyke cutting

from tto^ KeveenewanT*rfc exte^miiirplutonica both to the taet

STRUCTURAL OROLOGY

IVwtoalc*

Jbe structural lineation of rolcanic rodsfi on the Belfastaa yell MI that 'bf later intrusive plutonic rocka, follow a general northwest direction. Kridteoce of strike faults in the direction i* evident, nainly in the fbxisx of foliated conditions of a variety of rodu, of vhich several exatqJLea might

At the northvest corner a (rhyolitftt)chcrt contacts a foliated dioritio anddsite (tuffaoeous?) in this direction on line WOO. Further south, on lin* 1*800^ a hornblende granite is faulted across a narrotr fault tone in vhioh oecura a quarts -*-ein half an inch in vidth striking northveet. Anothr case is a gabtaro on lin* 1*800 S vhich is seal-sheared or foliated in a northwesterly direction. '

Tectonic forces resulted also in structural dislocations in a north easterly direction, e* g. a feldspar-porphyry is foliated northeasterly in the out crop Just south of the baseline on line 2000. Similarly an aplitic rock is stressed northeasterly 700 ft., south of baseline on line 2800.

A shatter zone in vhich narrow quartz veins traverse granite vae

noted across a width of forty feet. This is on the outcrop 150 feet north of the Algon boundaries on line 3000.

Transverse fault zones do not appear as a noticeable structural

feature according to explorations to dato,

Pept\of Volcanics

Individual bends of remnant volcanics are a structural feature of f.Vio af*\ rtcrv, *n f"*** *ft H*yf.b *vrob***"i5A!'ty l? cosofs^ncdi In this connection, tbs

oOB^eratxvely narrow dimensions noted are indicative that depths trould be limited,

except for the rhyollte-dacite (cherty eplitet). Here depths of many hundreds of feet are indicated by the coqparativel y vide areas of the rock. Certain of

the basic plutonic rocku aay also present favourable depth conditions, should

valuable discoveries varrant mining.

BCOHQMIC GEOLOGY

Huroniar. strata vere not observed on the Belfast property. Ifceee sediments are the usual favourable host rocks for uradiw occurrence

in the Blind River area.

The Ontario Department of Mine* aerial scintillation survey map of township 150 (coo[piled March 1?^) shovs an 'east-wr't radioactive anooaly

of the Al^om uhaft,

•-.^•i; *tMf •jkM**vv~JKtiyol.itft/ eocqObex of jfooJts^f^|ti;*',^ "

.-"'•'/v^

' ;T V~ -au jcrea

v ' ' , . mjfiim lain mn 'VA W4JU* (HU*xxj wo* gumcay v*yji u**-"tt * WV*UVJUI^XWBBK*J*^

,,, ,.—trmvwrftiiJe north-south line* across the property. Readings chained vere^V^j^ftc^^ ;'.'-,-,;.x

^ ^'ix , ;l .' Ttaui it i* unlikely thf.t uranioa tecora in eeononio deposits on' !* ' ^i' ' ''^''^i'fcij,^ - - -- -' - - - *- ~ ' . . ' '. ' . .

, •V'f'^j '' wTijJB WOT:,i -*- r .-i * T .-fly *^,"

' A variety of sulphides adnewus, wjdnly^^ pyrite, chalcopyrite, and pyrrhotite^ were obaervad, chiefly aa indifiiJaoua Binerals of the rocka aan?ed. Ate rocks range froak eugihlbolitic basia rocks to feldspar-porphyry, and an exaaple of each viil be described. Conoentretloaa of these adnerals have not been thus far discovered.

(*) P^agenAnated pyrite occura in feldspar porphyry, traversed by a 3* quarts vein ibW fi. aoufei of i&o baseline on line 2000. Pyrite vaa also noted in sheared diorite 1000 ft. south of the baseline on line 2^*00.

(b) Chalcopyrite i spotty signs of disseminated chalcopyrite vaa noted, associated vith a quart t-vein breccia. The latter is 20 inches vide, just south of the baseline on line 2000, in sheared feldspar-porphyry. It also occurs as bleba in amphibolite at the north end of line 1200.

(c) Pyrrhotite occurs in andesite near the north end of line 5200, and disseminated in~~fsnphibollte 650 ft. north of baseline on line 3600.

(d) Quart g veins Some of these might possibly carry gold values. Examplesof interest noticed are:

A ouartt vein stockwork forty feet vide in granite vas observed 150 ft. north of the Algom boundary on line 2000. A five-inch and a tvo-inch quarti; vein traverse a quartz- feldspar-porphyry outcrop 600 ft. south of the baseline on line 2000.Tvo four-inch quartz veins cut across hornblende-syenite 100 ft. north of the Algcu boundary on line 600. A one-half inch quartz vein vaa noied rilling a scarp fault line vhich crosses hornblende-granite on a hill 6^0 ft. north of the baseline on line WOO. A five-inch quartz vein vas observed 650 ft. north of the baseline oa line 3600.

OEHE31AL

The structural control vhich has most affected the precambrian rocka underlying the Belfast property has given rise to tvo sots of semi- sheared and foliated linea of structural stress. These, traverse the couple* of volcanics and plutonic dykes in northveaterly and northeasterly directions. It is possible that at one or more places vithin noderate depth below surface

SS5fp!^v?W^^ -.v;.^Ipl^j;'^^^ilV-K ^^^lij^^^ as a result of vhich . '

- ' *jftni^ntw pountial ocwwr*1a\^y valuable deposit* of - ,'X ;:;- n&a* might **i discovered by geophysical wethods. , ,*

fi ^*pff?i\i\fitpeprrf1r)Q ' jir^f gpyi^j^y jfo thft l*tK^4 fV J "'

claaely iswuiciated vith, disturbed, (wed-sheared,tap quartt-rftined xcoe*^ tend*'-'- *--.-.~---.j-i—!.'-.^i.. -^ t * ^ ' -- i-- --V- j™, .*— . * I^K ' ^ A *^ . '.M. —. - ^ A- '- . .

ajrticipotion concerning the possibility of finding'' '''' ''' ' ' '

of Buttwrpus quarts} yelns is favovprabie a* an . iawKiiiaie area sbovv the resuxts or cotiglOeraoie struotctral

dislocation and shattering by tensioaal aa veil as coajiresaive tectonic fbrcea* quartft Yeiii* vvere not noted to contain sulphide generalisation^ but should^;x^ tA" -I

SJ •^•'•!"'3f?''±,^.'^ttoiL* W"itort exi^ pcHlsfiMiiig dlsttnj|icns even two or three tiaes those of observed

^jarts veins, tbcs^ discrtJTeriea vcni^ exploration,;v ;' 1 -"'j;.'."-vv :,,"''''.V - v- - i.".:' ' v'''--''.'.'' . '"i ' ' ' . -

.th* daoitea md rhyolite* of th* Belfast are eonaldered

l*

3.

. fayburabla boat xooka f or baae wetala, as at Roraoda and Volte-Amulet in

!Bxere is little likelihood of any sedimentary deposit of uranium on this property. It Is possible, however, that veinlet* or stringers of pitchblende occur, but none have been discovered to date.

Pyrite, chalcopyrite, pyrrhotite, and quarts veins are noted in eeveral sections of the property. These ocurrences, to gether vith the prominent east-vest structural fault and shear cones suggest the possibility of base and/or precious metal deposits.

Further exploration of the property for metal deposits is varranted.

i

1.

2.

It is recocmended by the writer that J

An electrical geophysical survey be undertaken over the entire Belfast property, using the existing picket line system as a grid control. Ibis should be of the self potential, resistivity, or electromagnetic induction type, carried out by an established reputable contractor.. Its purpose vould be to locate one or more anomalous areas vhich might contain economic concents&tions of oulphide

Diaaand drilling vould be dependant on the results of the a,bove- recoucDended geophysical survey.

All of vhich is respectfully submitted,

111 * ** *

AlbertB.A.So,, P.Eng,, ILC.I.M., F.Q.A.C.

Consulting Mining Bogineer

Blind River, Oat.'

tf\

WORK INFORMATION

"t

*; ' ' i .* L

''V\ ,-.-' ; '~

*:''.' f:. ' ' -- -

oi survey - - ueoa.ogicai ana

Type of Instrument used.- Precision Radiation Instruments . r , Model 111 Scintillator.

; Consulting Geologist-'

Draftsman ~-

Albert Hopkins,1730, 25 King Street West,Toronto, Ontario.

Wm. Menges,31 Ranleigh Avenue,Toronto, Ontario.

Ass't. Field Geologist - L.F.K.Leicester,Algoma Mills, Ontario.

Instrument Man ~-

Assistant --

Calvin Swanson, Chapleau, Ontario.

George Linklater, Chapleau, Ontario.

Line Cutting Contractors and Sub-Contractors --

Chief-Henry Tweedell,Wllowdale, Ontario

Cutter- Ernest P. Rowe,Richmond Hill, Ontario.

Cutter- John F. Clarke, Miraico, Ontario.

Cutter- John Fitz,La Ronge, Sask.

Lines total about 9 miles

Baseline is about l mile long

Line interval - 400 feet

15 claims, nos. S?2771 to S72785 Inclusive.

i^o^&r^.

SCHEDULE

A. HopkinB

W. Menses

K. Leicester

C. Swanson

Q. Linklater

H. Tweedell

B. Rowe

J. Clarke

J. Fitz

PROM. ' - "--

i* Aug. -7 Sept. -

14 A\ig. -

14 Aug. -

14 Aug. -

20 July -

20 July -

20 July -

20 July -

t6i

29 Aug.

13 Sept.

29 Aug.

29 Aug.

29 Aug.

13 Aug.

13 Aug.

13 Aug.

13 Aug.

10 hr? day*

15

7

15

15

15

25

25

25

25

167 10 hr. man-days

167 x 10 houTB - 1670 hours

1670/8 - 208 man-days of 8 hours each

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