GM 07296 REPORT ON MINING PROPERTIES

H. rt. HOGAN J. A. MCCUAIG

G.EOICIGIST MINING ENGINEER

DADSON LAKE CHIBOUGAIy1Aii MINES LIMITED

MINING PROPERTIES

CHIBOUGAMAÏI AND MISTASSINI AREAS

QUEBEC

iliuistère des Richesses Y~»:~3t° 1~K~ ~ ~ ~ i~u`kLi,

cc.. ~,— ~„„_..~„_,~,~-, SERVICE~~ r.) ï. S G:i: ; MINERA'~~ ti No GM_ y).~

July .:i,1: I`J,n. H. R. HUGAN J. A. McCUAIG GEOLOGIST MINING ENGINEER

DADSON LAKE CHIBOUGAMAU MINES LTD. Mining Properties Chibougamau & Mistassini Areas Quebec

INTRODUCTION Dadson Lake Chibougamau Mines Limited owns 13 mining properties; 12 in the Chibougamau area and one in the Mistassini area. Exploration work has been conducted on some groups while others have had only a cursory examination. The total area held '.y the company is 9815 acres approximately. Acreage reported for individual properties is approximate. The writer has not examined any of these properties but has supervised and conducted exploration work on properties adjoining most of the groups, and is familiar with the geolog- ical setting of all the claim groups. Total cost of recommended exploration program is $20,700.00.

H. R. HOGAN J. At McCUAIG

GEGLG GIST MINING ENGINEER

e( GROUP NO. l. Opemisca Towns'oip - 1400 acres Certif no cl. nos Development Expiry licences Date C-96362 L-19199-L-19203 29639 on .Aug . 6/58 C-96363 V L-19194-L-19198. '29638 Gk ~ C-96364 L-19189-L-19193 29637 o k' Aug. 5/58 C-98822 f 1,20710-L-20714 301., f0 Sep. 5/58 1,-20705-L-20709 30106 014: SQp. 5/58 C-98823 -2ô7~9-L-2ô~~9 30107'ok ~ Sep. 5/58 C-98824 L-20720-L-20724. 30108 ol< V Sep. 5/58

LOCATION AND ACCESSTRILITY The claim group is located 29 miles northwest of the Chibougamau township. The easiest means of access is by flying from Cedar bay on Dore lake and landing on the bay where the Chibougamau river enters hichwacho lake. From the bay the property may be reached by a bush trail.

GENERAL GEOLOGY According to the Geological Survey of Canada,.

maps nos. 602A and 623A the property is underlain by easterly trending andes:ites, tuffs, and sedimentary rocks. These formations are locally ,intruded :by altered gabbro and diorite.

SULPHIDE MINERALIZATION Sulphide mineralization is `known to occur on claim 5, C-96363. The sulphides are in, or adjacent H. R. HOGAN J. A. McCUAIG GEOLOGIST 3 MINING ENGINEER

to. qua•i,z stringers as veinlets in weakly sheared diorite or occur disseminated in the diorite. This occurrence has been traced for a length. of 80 feet. It strikes N. 20° W and dips vertically. A grab sample from this occurrence assayed 2.30% copper, 0.01 ounce of gold per ton, and 0.10 ounces cf silver per ton.

WORK COMPLETED An electrical resistivity survey was con- ducted on the property during February 1957. Four zones of possible faulting and five areas of possible sulphide mineralization were indicated from the re- sults of the electrical resistivity survey. The zones of possible sulphide mineralization are designated "A" to "E" inclusive. The "A" zone is the eastern extension of a

mineralized zone on the ad jacent property owned by Pennbec lines Limited. It is believed to consist of a discontinuous band of siliceous tuff mineralized to varying degrees with pyrite, pyrrhotite, and chalco- pyrite. Two diamuad drill holez intersected sulphides in the western part of the zone bu commercial values were lacking. H. R. HOGAN J. A. •IvieCt7AIG

GEOLOGIST MINING ENGINEER

Zones "F3", "C" and "D" lie, for the most part within a diorite-gabbro intrusive. They strike east, and are parallel to sib-parallel. The resis- tivity data indicate that certain points along these zones are mineralized with sulphides. Zone "E" is believed due to a high ;concen- tration of sulphides over a small area.

RECOMMENDATIONS Geochemical and magnetometer surveys should be conducted over zones A to 'E, inclüsive. This . will aid in determining _ the nature of the zones Where diamond drilling is warranted.

ESTIMATED COST Geochemical and magnetometer check `surveys- (including travelling expenses) ' -- $ 2,000.00 .

L' GROUP NO. Roy township 800 acres

KJ Cert No. ~ ! Fapiry Date C-88984=P")d- E-ï9663-L--19667 a/C Aug . 23/58 C-88985 ,: , .2741- 1,-19653-L-19657 or.", ti;i~~~. Aug. ''24/58 c-88986 „ 1.5704-1,-19658-L-19662 ,~~ °A ~9t;r t ~ C-88987 .. ,?c,16:g- •L-19648-L=19652 a;4; ~~' H. R. HOGAN J. A. McCUAIG GEOLOGIST - 5 MINING ENGINEER

LOCATION AND ACCESSIBILITY The property is 12 miles northeast of the Chibougamau townsite in the east-central portion of Roy township. The eastern half of the property covers a portion of Lake Lunaberner, which is suit- able for use a s a landing base for float-equipped aircraft.

GENERAL GEOLOGY The northern half of the claim group is underlain by an easterly trending intrusive layer of serpentine or pyroxenite. The southern half is underlain by volcanic rocks, predominantly andesite, and minor amounts of serpentinite.

WORK COMPLETED No exploration has been conducted on the claim group.

RECOMMENDATIONS Geological Survey of Canada map no. 304A indicates that outcrops are relatively abundant on the property. The writer recommends that the claims be prospected carefully for sulphide mineralization and for any indications of the presence of asbestos.

H. R. HOGAN - J. A. McCUP;IG

GEGIAGIST MINING ENGINEER

ESTIMATED COSTS Prospecting Program - 1,800.00

v~ GROUP NO. 3 - Levy township 200 acres

G-6670 L-42044-L-42048-- Uk December 11/58

LOCATION AND ACCESSISILITY The property is adjacent to that of. Opem- iska Explores Limited and four miles south of the main property df Opemiska Copper Mines Limited. The easiest means of actes,; is from a good gravel road which joins the Opemiske. highway with. Lake Pres guile, The road passes immediately east of the claim group.

GENERAL GEOLOGY According to Geological Survey of Canada Map no; 602A, the property is underlain by recrystallized volcanic rocks. The formations have a general east- erly strike and a vertical to steeply south dip.

H. R. HOGAN J. A. MOCUAI'G' GEGIGGIST MINING ENGINEER

WORK COMPLETED No exploration work has been conducted on the property.-

RECOMMENDATIONS An electromagnetic survey should be con- ducted on the five claims. any additional work will depend on the results of the survey.

ESTIMATED COSTS l,inecutting and Electromagnetic survey =--- 1; 200.00

GROUP NO. McCorkill township 1000 acres

Cert No. Development claim ntaabers Expiry date license

C-1166031/, gl -34563 0K L-38209-L-38213 Feb. 8/59 "-1166J4 ~ ~ .„ 34564 ak L-.38211i--L-38218 11 c-116605 ~""34565 ~. 345 65 G k L-38219..L-38223 c-1166a6 v 34566 >}A L-38224-L-38228. C-116607 t/ v 34567. Ak. L-38229-L-38233.

LOCATION AND AC ESSIBIL:ITY Group No. 4 of the Dadson Lake Chibouga:mau' Mines Limited lies' 23 miles northeast of the Chibotig-

i H. R. HOGAN J. A. MCCl1A16 GEOLOGIST - II MINING ENGINEER

amau townsite. It may be reached by float-aircraft by landing on the small lake immediately east of Lake Nepton.

GENLKAL GEOLOGY Ac,:ording to Quebec Department of Mines Preliminary map No. 882, the claim group is under- lain by anorthosil,ic and gabbrp: c rocks. These rocks are in the northeast extremity of the large anorthos- itic intrusive which extends eastward from Obalski township to McCorkill township.

WORK COMPLETED No work has been conducted on the property.

RECOMMENDATIONS The property should be geologically pros- pected for any indications of sulphide mineralization or for any zones of bleaching or alteration charac- teristic of the anon-thosite host-rock in Obaiski and

McKenzie c,.,:znships..

ESTIMATED COSTS Geological Prospecting ---- .^ 2,500.00 H. R. HOGAN J.A.41cCUMG GEoLowsr 9 MINING ENGINEER •

v, r-GROUP NO. 5 - Roy township 400 acres

G-6671 L-42126—L-42130 OX Dec. 18/58 G-6672 L-42131-L-42135 Il

LOCATION AND ACCESSIBILITY The property lies 12 miles northeast of the Chibougamau townsite and adjoins both Rapid bay and Gunn bay of Lake Chibougamau. The property may be reached by boat on Chibougaman lake or by float- aircraft.

GENEti.AL GEOLOGY° According to Map no. 304A of the Geological Survey of Canada the north third of the property is underlain by detrital sedimentary rocks of the Chi- bougamau series. The southern two thirds of the pro- perty are underlain by rocks of Fre-Chibougamau series age. From south torth the formations are serpentine; altered diorite and altered andesite; the trend of the foi-mations is easterly and the dip vertical. The two series are separated by a northeast trending fnult. H. R. HOGAN J. A. McCUAIG GEOLOGIST - 10 - MINING ENGINEER

WORK COMPLETED No exploration work has been conducted on the property.

RECOMENDATIONS The serpentine band should be prospected for asbestos. The remainder of the property under- lain by the Pre-Chibougamau series should be pros- pected and an electromagnetic survey conducted during the winter months as a large part of the property is covered by a lake.

ESTIMATED COSTS Prospecting $ 1,200.00 Electromagnetic survey $ 1,500.00

Total $ 2,700.00

. ),/ GROUP NO. 6 Barlow township - . 400 acres c-124364.M•35 .2 61' L-39703-L-39707 osk April 5/59 c-124365 3s 6B. " 4159 H. R. HOGAN J, A. McCUAIG GEOLOGIST MINING ENGINEER

,OCATIG, AND ACCESSIBILITY The property lies 11 miles northwest of the Chiboagamau t,own.site and along the south shore of Chihougamau river between Little aush lake and Rush lake. It may be reached by float-bearing aircraft only.

GENERAL GEOLOGY. According to G.S.C. Map no. =+01A the property is underlain by various volcanic formations of Pre-Gpemisca age. A small northwest trending shear zone occurs in the southeast corner of the claim group.

'WORK COMPLETED No work has been conducted on the claim group.

RECOMMENDATIONS Geological prospecting should be conducted especially in the vicinity of the small shear zone.

ESTIMATED COSTS Geological prospecting -- ù11200.00 H. R. HOGAN J. A. MOCUAIG GEOLOGIST ~ 12 - MINING ENGINEER

✓ ~ GROUP NO Ubalski township - 560 acres

Grouo : 7A ~ ; ~ P;,r'-- 35oz, ~ M -)+293,12 . L-39or~1-L=390'~ ~r r` i~az ; h 10/59 .~ 350'+ ~ ~ f°.{ ~-12429~+~= ~`~"~L-39o75-T -390•~~ ; I~~arch 10/59 G-6669 a? L-420-9-L-42050 o:' :ec. 10/58 Grout) 35049 C-124295 =`X.:~:~ L-39161-L-39164 t,;~. March 13/59 The Group no 7 constts of two separate units, 7A is in the extreme northwest corner of the township and 7B is one ` mile southeast of 7A.

LOCATION AND ACCESSIBILITY Group 7A is 4 miles southwest of the Chi- bougamau townsite and 7B is 5 miles south-southwest of the townsite. 7B is adjacent to the railway and 7A may be reached by walking miles northwest from the r aiLva,T.

GENERAL GEOLOGY " According to the Map no. 1091 of the Quebec Dept. Mines, Group 7A is underlain by andesite. Two zones of carbonatization occur within, the andesite. These zones trending east northeast are believed to represent'.zon. s of shearing or faulting. Group ',?B is showl to be underlain by quartz diorite. H. R. HOGAN J. A. Mc:CUAIG .~~ GEOLOGIBT 13 - MINING ENGINEER

WORK COMPLETED No work has been conducted on either group.

RECOI,0`END.A.TIONS Group 7A should be surveyed electromag- netically. No work should be conducted on group 7B.

ESTIMATED 'COSTS'

Linecutting & electromagnetic survey - - $ 2, 200.00

1/' GROUP NO, McCorkill township 1000 acres 35050 C-124305 4' L-3921+5-L-.39249 aK March 19/59 350 5 1 C-12)1 )s29 Y. L-39835—L -39839 dg April. 12/59 ~C-132047 L-42448-L-42452 0 ~ Feb. 26/59 II C-132048 ` N L-42453-L-42451 a J:- C-132049 =~° L-42458-L-42462 ok I I

LOCATION AND . ACCESSIBILITY The property occurs 19 miles East ,Nor tl3east - , oi the Chibougamau town.site and may be reached by float aircraft. The Nepton river flows through the property.

GENERAL GEOLOGY The northwest half of the main group of claims is underlain by anorthositic rocks and the

H. R. HOGAN J. A. McCUAIG GEOLOGIST 14 — MINING ENGINEER

southeast, half by granitic rocks. All of the small group. attached to the northeast corner of. the main group :is underlain by anorthosite..

WORK COMPLETED No work has been conducted on this group of claims.

RECOMMENDATIONS The contact between the anorthositic and granitic rocks on the property should be established and that portion underlain by anorthositic should be geologically prospected.

ESTIMATED COSTS Geological prospecting 2,000.00

GROUP NO. McCo kill township 1200 acres G-71-1-77,"; L-42910-L-4291.4 May 15/59 G-7478,~/ L-42915-L-42919 ~K II : G-7479 L-42920-L-42924 ok II G-7480 ~~.. it fi L --42925-L-42929 ok" fi G-71+81 L-42935-L-42939 o~ G-7482 L-42930-L-42934 vK

H. R. HOGAN J. A. McCUAIG GEOLOGIST 15 MINING ENGINEER

GENERAL GEOLOGY According to Que. Dept. of Mines map no 882 the property is underlain by anorthositic rocks which are part of the main a.northosite mass under- lying Dore and Chibougamau lakes.

CORK COMPLETED. Previous owners, Marvelor Mines Limited and Newlund Mines Limited conducted magnetometer and electromagnetic surveys on the McCork;;.11 ground presently held by Dadson Lake Chibougamau Mine.; Lim- ited. The writer examined these maps several years o and noted several anomalous zones worthy of further investigation. It is possible that these zones were diamond drilled.

RECOMMENDATIONS It should be determined whether or not the anomalous zones were drilled. Recommendations for work to be conducted on the property will depend upon information obtained concerning the possible diamond drilling. H. R. HOGAN J. A. MdCUAIG GEOLOGIST 16- MINING ENGINEER

y~ 41' V GROUP NO. 10 - ; McKenzie township - 400 acres `. Group 10A 35466 i! C-120s 92 e4~i aK L-40290 May 10/59 35466 V O-1244930 G IK L-40292 35466 v C-124494 ► o R L•-40294 35466 V C-129661 L -40295-L-40299 May 11/59 Group 10B 35467 C-12?0192 C-'e alC L-~4029 C May 10/59 35467 C-1211-493 o/:. L-40293 ,I

LOCATION AND ACC ESSTRILITY

Group 1oA lies mile south of the' Chi-- bougama•u townsite and adjoins the northeast end of Lake Souvage; Group 1OB is 1- miles south soutn.e~.st of thé townsite and "adjoiris the south shore of L.!..ke Sauvage.

GENERAL GEOLOGY Detailed geological mapping (scale 1"- 1000t) covering both groups wa>; conducted by the Quebec Dept. of Mines and reproduced on preliminary map no. 945. Group 10A is divided into two parts by a northeast trending fault which follows the long a:six of ja?ce ,5ouvage. The northern part comprising two- thirds of ` the `area, is underlain by metabasalt; the southern part is predominantly metabasalt and meta- andesite. Two easterly trending zones of carbonate H. R. HOGAN J. A. Mc'UAIG GEOLOGIST - 17- MINING ENGINEER

chlorite schist cut through the metabasalt. The formations strike east and dip vertical. A. southeast trending fault subsdiary to the main fault is present in the southern part. Group 10B is shown to be underlain by metabasalt and metaandesite. A small southwest trending shear zone crosses the northwest corner of the property.

RECOMRENDATIONS Group 10A - An electromagnetic survey should be conducted on the portion of the property lying south of the main fault. Group 10B - No work recommended on this group.

ESTIMATED COSTS Linecutting & electromagnetic survey ------$ 900.00

H. R. HOGAN J. A. McCUAIG • GiEOLOGIST 18 MINING ENGINEER .

'. G/. V. ~ - l /' GROUP 1T0. 11 Queylus township 800 acres C-132059 " L--42581-L-42585 aK March 10/5;, C-132060 T.-42586ÿ1-42590 oX tt C-132061 L-42591-L-42595, OK Nlarç'nl :il/59 C332062 L-42516-L-42600 OK

LOCATIOII AND ACCESSIBILITY Group no. Tl lies 17 miles south south- west of the Chibougamau totimsite. The property is in the west central part of Queylus township, immediately north of the east er_d of Lake Caamor . The Chibougamau highway lies 3 miles 'east of the claim group.

GENERAL GEOLOGY The property is underlain by volcanic rocks mainly basalt and andesite. Some tuffs and frag- mental Jolcanies may be present also. The Verneuil granite ' stock outcrops is 12 miles south of the south boundary of the property. The strike of the formations is easterly and the dips are steep both northand ' south.

E,CONOMIC GEOLOGY The area has been the scene of two rather important staking rushes; firstly, in the fall of H. R. HOGAN J. A. McCUAIG GEOLOGIST - 19 - MINING ENGINEER

1949, after the discovery of a mineralized shear zone on the west shore of Calmar lake, by Calmor Mines limited, and secondly, in July 1950, after two prospectors working for New Mosher Longlac Mines Limited uncovered a wide zone of shearing and silicification on the east shore of the small lake south of Dauversieve lake, two and a half miles east of Nemenjiche river. A showing occurs on the Queylus property of Dadson Lake Chibougamau Mines Limited about 900 feet north of the northeast end. of Calmor lake. The main vein, composed of quartz with some tour- maline and a few remnants of partly silicified schist, has been exposed by stripping for about 100 feet. It trends S 65° E and ranges in width from. eighteen inches to three feet. The vein is miner- alized with auriferous pyrite and chalcopyrite mostly concentrated in the vicinity of the tour- maline ana. schist. A second showing occurs about 1000 feet east of the above described showing. The rocks are lavas with subordinate amounts of gabbro and porphyry. The structure is complex; while the dips are nearly always vertical, the strike of the schistosity ranges from north-south to east-west. These variations,

H. R. HOGAN J. A. McCUAII3 GEOLGGFST - 2G MINING ENGINEER

however, seem to follow a regular pattern and the structure is believed to be a continuation of the zone of drag folding observed on the Calmor property. Quartz stringers and lenses up ;o two by six feet occur erratically. Pyrite is présent, not only in the quartz but also 'within "the sheared lavas. (P.E. Im'oaul t, Que. Preliminary Report ivo. 250, PP. 12 & 13, 1951 •)

RECOMMENDATIONS Geological prospecting is required to extend and dei the potentialities of these' mineralized zones, :Prospecting may uncover addit- ional zones.

ESTIMATED COSTS Geological Prospecting - ,200.00

k/ GROUP NO. 12 McKenzie township - 855_ acres C--132032 i~,~,~~ ` L-42367-L-4 2370 oK Feb. 6/59 0-132033 r 1- 42362-L-42366 cK at C-132034 ~ L-42358-L-42361 oK C-132035c4. L-42354-L-42357 c~ k 11 I1 C-13 2036 c,';4 ,. L-42350-L-42353 0 ?~ H. R. HOGAN ,!. A. MCCLAIG GEOLOGIST - 21 - MINING ENGINEER

LOCATION AND ACCESSIBILITY The claim group lies 2 miles northwest of the Chibougamau townsite and adjoins the south shore of Lake Antoinette. A bush road joins Antoinette lake with the Chibougamau highway, also

the lake can be used as a landing base.

GENERAL GEOLOGY The property is underlain by an easterly trending complex of meta-morphic volcanic rocks

and basic to ultra-basic intrusives. The continuity of the formations is disrupted by four faults, of which two are subsidiary to a main southerly trend- ing fault.

10 ORK COMPLETED The writer directed a comprehensive exploration program for the company that owned the property prior to its acquisition by Dadson Lake

Chibougamau Mines Limited. This work consisted of a magnetometer survey over the entire property with electromagnetic and self-potential surveys over the magnetic anomalies. Approximately 3500 feet of diamond drilling was conducted to test the anomalous zones with negative results. H. R. HOGAN J. A. McCUAIG GEOLOGIST - 22-- MINING ENGINEER

RECOMMENDATIONS No work should be conducted on the property.

GROUP N O . 1 ~ Lake Mistassini area 800 acres C-131800L-41552 -L-41556 °k Sept. 3/*8-SçsA C-131801 ~,~ L-4151+771 -41551 C-131802 L-41557L-41561 f° C-131803 L-41542--L-4151+6: ..~G~~Iavo.p INTRODUCTION Information regarding this property was obtained from a report of W.L. Angus, Mining engineer who examined the p_roperty in September 1953 on behalf of Dadson Lake Chibougamau Mines Limited.

LOCATIOTJ AND ACCESSIBILITY The property is situated 15 miles imately northeast of Rupert River inland from Lake Mistassini lying approximately midway between the and 74th longitudes, 20 miles north latitude, some 110 miles north of Chibougamau. The claim group is accessible by a 1- mile trail leading from the north end of Shy lake which H. R. HOGAN J. A. McCUAIG

GEOLOGIST - 23- MINING ENGINEER

is 2- miles long and suitable for aircraft landings.

GENERAL GEOLOGY The area is underlain by folded layered complex of granite paragneisses with feldspar, quartz and mafic-rich bedding. The topography is generally spruce-covered low-rolling hills and swamps with numerous eskers and light overburden, typical of northern shield glaciated terrain.

Trench DO, 1. An exposed width of 15 feet of a flat lying south-dipping meta-anorthosite phase of the granite gneiss carried fine bands of mostly pyrite with lesser amounts of chalcopyrite that would assay approx. 0.255-0.50% copper over a true width of 7 feet. The mineralization is associated with the darker fine biotite bands in thE. quartz-rich metamorphics. Trench no. 2 Several hundred feet north-easterly from Trench 1, Trench 2 opens up structure which strikes N 40° W and dips 80-90° to the south. The mineraliza- tion is associated with beds of anorthositic gneiss with quartz-rich layers lying within the typical pink granite gneiss host rock. Sulphide mineralization occurs parallel to the bedding and consists predominantly of pyrite with light amounts of chalcopyrite and minor magnetite. A width of 25.0' was channel sampled and assayed 0.500 copper and 0.02 oz/ton gold. A more concentrated sulphide core was pres- ent in the centre of the zone which was traced contin- uously on surface along the 50 feet of total rock ex- posure. To the north, several narrower additional mineral_,zed bands were found in the gneiss complex. One drill hole 25 feet deep was undertaken but was collared in the gneiss and drilled with the formation, thus affording no information. A second hole was collared in sulphides to drill into the dip, but the machine broke down completely and the program was terminated. H. R. HOGAN J. A. MGCUAIG GEOLOGIST - 24- MINING ENGINEER

CONCLUSIONS ( W.L. Angus) It is apparent that the mineralization is occurring in bands associated with anorthositic and. quartz-rich phases of the granite gneiss and will have a re-occurring characteristic in parallel struc- tures. Adequate copper grade of the deposits at present prices is not sufficient to consider the property as having possibilities. Also granite gneiss complex has not been found as an economical host rock for base--metals and therefore the chances of finding a mine are further reduced. The cost of operations is very high in the area, necessitating a high grade deposit to be economical.

RECOMMENDATIONS The writer is not in agreement with the conclusions of Y.L. Angus. He has placed more emphasis on the depressed price of metals than on the occurr- ence of copper mineralization. Detailed prospecting and trenching should be conducted in the vicinity of the trenches and general prospecting over the whole property.

ESTIMATED COSTS Detailed and general prospecting 4 3,000.00

Respectfully submitted,

July 11, 1958. Hogan « McCuaig H. R. HOGAN J. A. McCUAIG GEOLOGIST CERTIFICATION MINING ENGINEER

TO ttTrlOm IT MAY CONCERN .

Howard R. Hogan hereby certify:

• that I am a consulting geologist and. my address in Montreal is 455 Craig st. west, suite 307. .that I am a graduate of McGill Univer- sity and have a degree of Doctor of P.zilosophy in Geological Sciences. that I have been a geologist since 1949, and have practised as a mining consultant since 1953. that I have no personal interest, direct or indirect, in the properties or in the securities of Dadson Lake Chibougamau Mines Limited, nor do I expect any interest. that I have not examined the properties described in this report, that the report is based on geological information obtained from government reports and maps, from geologists and engineers reports believed to be accur- ate and trustworthy, and from personal examination and supervision of explor- ation work on properties in the Chi- bougamau area, many of which are adjacent to the properties of Dadson Lake Chi- bougamau Mines Limited and one which is now owned by Dadson Lake _ Chibougamau Mines Limited. ,. that a personal examination of `à%: re- connaissance nature of the properties would not materially change the writerts reDmmendations .

e...„..„.„,..,...., ~ /~ ~~ .- ~ July 11, 1958. Howard R. Hogan.