42A14SE0038 W MANN

Transcription

1 42A14SE0038 W MANN 010 DIAMOND DRILL PROGRAM SEPT/OCT 1995 PHELPS DODGE CORPORATION OF CANADA LIMITED LITTLE DUFF PROJECT - DUFF/MANN/LITTLE TWPS PORCUPINE MINING DIVISION 42A/14 PROPERTIES: LD - 5, LD - 6, LD - 7, LD - 11/19, LD - 15 ;UL l FCF.CUPiNi 'v'-wo DIVISION l ^ -i..jlw - * ' DAVE GAMBLE DAVE GAMBLE GEOSERVICES INC. DECEMBER, 1995

2 1 TABLE OF CONTENTS 42A14SE0038 W "MANN"' 010C I II III IV V VI VII VIII IX x INTRODUCTION LOCATION AND ACCESS CLAIM STATUS REGIONAL GEOLOGY PROPERTY GEOLOGY PREVIOUS WORK DRILL PROGRAM 1995 DISCUSSION OF DRILL RESULTS CONCLUSIONS RECOMMENDATIONS page LIST OF ILLUSTRATIONS FIG l - LOCATION MAP FIG 2 - GRID LOCATION MAP FIG 3 - DIAMOND DRILL HOLE SECTION DDH FIG 4 - DIAMOND DRILL HOLE SECTION DDH FIG 5 - DIAMOND DRILL HOLE SECTION DDH FIG 6 - DIAMOND DRILL HOLE SECTION DDH FIG 7 - DIAMOND DRILL HOLE SECTION DDH FIG 8 - JENSEN CATION PLOT TABLES TABLE l - UTM COORDINATES OF NORTHEAST GRID/CLAIM CORNER TABLE 2 - CLAIMS INFORMATION LITTLE DUFF PROJECT TABLE 3 - DDH LOCATION RELATIVE TO NE CLAIM CORNER TABLE 4 - DRILL HOLE SUMMARY TABLE 5 - WHOLE ROCK SAMPLE DESCRIPTIONS APPENDIX A - DIAMOND DRILL HOLE LOGS l to B - SWASTIKA LAB REPORT GOLD ASSAY RESULTS C - XRAL LAB REPORT WHOLE ROCK ANALYSIS

3 I INTRODUCTION During the period from September 18, 1995 through to October 14, 1995 a five (5) hole diamond drill program totaling 1014 metres (3327 feet) was completed on five (5) separate properties on the Little-Duff Project in the Porcupine Mining Division northeast of Timmins, Ontario. The properties held under option by Phelps Dodge Corporation of Canada Limited and are located in the townships of Duff, Little/Tully, and Mann, and are numbered LD - 5, LD - 6, LD - 7, LD - 11/19, and LD The purpose of the drill program was to test a number of selected horizontal loop electromagnetic (H.L.E.M.) and transient domain electromagnetic (T.E.M.) conductors identified from ground surveys previously carried out by Phelps Dodge during a winter linecutting and geophysical program from November 1994 to April Dave Gamble, of Dave Gamble Geoservices Inc. managed and supervised the drilling project, and this report describes the results obtained from this drill program.

4 II LOCATION AND ACCESS The project area is located approximately 40 km north-northeast of Timmins, Ontario, N.T.S. 42A/14, in the District of Cochrane, Porcupine Mining Division (Figure 1). The general project area can be reached using forest access roads that lead from two Provincial Highways numbered Hwy 11, and Hwy 101. A more detailed location map (Figure 2) shows the location of the grids within the project area. Three properties located in Duff Township LD - 5, LD - 6, and LD - 7, and one property located in Mann Township LD -15 are road accessible from Cochrane, Ontario. Road access is gained by proceeding southwest of Cochrane on the Con 11/111 Lamarche Township road that leads from Hwy #11 to the municipal garbage dump in Fournier Township. Continue south beyond the dump and follow the forest management access road that leads south through both Fournier and Reaume Townships and into the east central part of Duff Township. The forest management access road in Duff Township leads along the east side of Crawfish Lake and lies approximately 500m from the east end of LD - 5 grid area. An old logging road/trail leads onto the property around the north end of Crawfish Lake providing further access. The Duff Township forest management access road continues southward from LD - 5 and passes through the west edge of the LD - 6 grid area. This road continues southward and also crosses the northeast part of the LD - 7 grid area. Several old logging roads (now ATV accessible) provide further access onto the properties LD - 6 and -7. Another logging road (now ATV accessible) leading easterly and then southerly from the Duff Township forest management access road near the north end of LD -6 grid area provides access to LD - 15 grid area in Mann Township. Old logging activity in this area also provides further access onto the LD -15 grid. The LD -11/19 property located mostly in Little Township and a small part in Tully Township is road accessible by proceeding east from Timmins, Ontario along Hwy 101 to Hwy 610 that leads north just east of

5 85" 80 HUDSON BAY MANITOBA o Big Trout Lake o Weagamow Lake ONTARIO Pickle Lake Fort Albany Moosonee osovont Lake Timmins o Kirklond Lake Parry Sound OTTAWA SOOmiles 5OOkms IS pfle/ps dadqs, CorponiiontJol Cladi UmHed Province:. ONTARIO Twp./Araa: Timmins Areo N.T.S.: a, 2 A Compiled by; F. L. J. Drawn byr R T. M REVISION DATE BY LITTLE DUF F PROJECT Timmins Ar ea, Ontario LOCATI ON MAP so 0 DATE ntema. Mor. 95 PROJ. Ho. 210 SCALE a 3 shown FIGURE 1

6 Beck s vr eau me Reaume Hanna 5 km 3 Lucas LD3 LD5 LD6 Mann Newmarket LD8 LD LD 14 Prosser LDM/19 Litriel* phelps dadqe CorpontnaLiol Cftvdt L'miled Province: ONTARIO Twp./Area: Timmins Areo N.T.S.: 42 A Compited by: F. L. J. Drawn bv: R. T. M. REVISION DATE BY LITTLE DUFF PROJECT Timmins Area, Ontario GRID LOCATIONS LD 21 Dun dona LD22 DAT^ Mor95 flleno. PROJ. No. 240 SCALE at s hown FIGURE 2 Evelyn Frec/ericA Mouse Lake

7 Falconbridge's Hoyle metallurgical site. Proceed 6 km northeast along Hwy 610 to the Ice Chisel Lake forest management road turnoff. Proceed north along the Ice Chisel Lake road through Evelyn Township and into Little Township to where a logging road leads westerly between Sawmill Lake to the south and Lecce Lake to the north near the Con IV/V boundary. This winter logging road provides direct access and leads through the southern part of the LD - 11/19 grid area. The location using UTM coordinates for the northeast corner of each claim gridded area is listed in Table I. TABLE I UTM COORDINATES OF NORTHEAST GRID l CLAIM CORNER GRID LD-5 LD-6 LD-7 LD- 11 LD- 19 LD- 15 NORTHING mn mn mn mn mn mn EASTING me me me me me me

8 Ill CLAIM STATUS The claims covered by the diamond drill program were acquired by option in September 1994 and are currently held under option by Phelps Dodge Corporation of Canada Limited. All claims lie in the Porcupine Mining Division, NTS 42 A as listed in Table II. TABLE II CLAIMS INFORMATION - LITTLE-DUFF PROJECT GRID LD-5 LD-6 LD-7 LD -11/19 LD- 15 TOWNSHIP 1 PLAN # DUFF G-3234 DUFF G-3234 DUFF G-3234 LITTLE G-3241 TULLY G-3985 MANN G-3537 CLAIM # P P P P P P P UNITS REC. DATE Nov. 22, 1993 Nov. 22, 1993 Nov. 22, 1993 July 22, 1994 Nov. 22, 1993 July 22, 1994 Nov. 22, 1993 The drill hole collar locations relative to the northeast corner on the following gridded mining claims are listed in Table III: TABLE III DDH LOCATION RELATIVE TO NORTHEAST CLAIM CORNER DDH # GRID # LD 11/ LD LD LD LD - 5 CLAIM # P P P P P TWP LITTLE MANN DUFF DUFF DUFF LOCATION FROM NE CORNER 510 m S and 1030 m W 480 m S " 150 m W 450 m S " 440 m W 190 m S " 490 m W 485 m S " 415 m W

9 IV REGIONAL GEOLOGY The regional geological setting of the Little Duff Project area is within the western portion of the Archean Abitibi greenstone belt. A major calcalkaline belt of felsic volcanics lying to the north of the Porcupine-Destor fault are known as the Kidd-Munro and Duff-Coulson-Rand rhyolite assemblages. These felsic volcanic assemblages have been complexly folded into regional syn and anticlinal structures. In addition several regional north-northwest trending faults transect the area. Mineralization within or proximal to the Kidd Creek rhyolite assemblage, and along regional north - northwest rending fault structures, is well known at the Kidd Creek Mine some 24 kilometres to the southwest. Flanking these felsic assemblages to the north and south are mafic, ultramafic and sedimentary rocks. Deep overburden has presented a challenge to exploration in the region as a whole. The lack of adequate bedrock exposure due to the heavy overburden in this part of the west Abitibi greenstone belt, has provided the potential for deposit hideability. The commodities and type of deposits sought for on the Little Duff properties are volcanogenic polymetallic massive sulphide mineralization (Cu-Zn-Au-Ag) and/or structurally related gold mineralization. O.G.S. maps 2484 and 2205 are the best available public compilations of regional geology of the area. V PROPERTY GEOLOGY Bedrock exposures in the immediate area of the properties LD - 5, LD - 6, LD - 7, LD - 11/19 are unknown. A small cluster of outcrops identified as andesite-basalt flows are indicated on OGS Map No P at the junction of Tully, Little, Duff and Mann Townships at the southwest corner of property LD Overburden cover appears to be substantial over most of the area near the remaining Little Duff Project properties.

10 VI PREVIOUS WORK Geological interpretation also relies heavily on previous drill hole and geophysical information in the area. The properties have no known recorded drill hole information in areas where the current drilling was undertaken. On the LD - 11/19 claims three drill holes were drilled by Massval Mines in 1964 as reported in Assessment Report T-867. The holes are reported to be located some 1200 metres north of the current drilling of DDH 240 -l and to the north of Lecce Lake. The logs from the old drill holes #2, #3, and #4, reported 228, 244, 194 feet of overburden with total depths of 502, 409, and 459 feet respectively. The three holes are reported to have been entirely in rhyolite agglomeratic sequences with pyrite and sercitic alteration in hole #2. Based on this sparse knowledge the property is likely to be underlain by mafic and/or felsic volcanics, and sediments. Drill holes within the region have returned various volcanic rock types including ultramafics, dacite to rhyolite sequences, and metasediments. Two airborne geophysical surveys were utilized that cover the project area; a 1984 helicopter-borne INPUT MarkVI EM and MAG survey and a 1988 fixed-wing GEOTEM EM and MAG survey. Reported work includes the following; in 1977 Shell Resources Canada conducted a ground magnetic survey over parts of LD - 7; in 1984/85 Selco Division of BP Resources Canada Limited conducted ground magnetic and electromagnetic surveys over parts of LD - 5, LD - 6, LD - 7, LD - 11/19, and LD - 15; and in 1994/95 Phelps Dodge Corporation Canada Limited conducted ground magnetic and electromagnetic surveys over all Little Duff Project grids.

11 8 VII DRILL PROGRAM 1995 During the period from September 18, 1995 through to October 14, 1995, a diamond drill program consisting of five holes totaling 1014 metres (3327 feet) was completed for the purpose of testing horizontal loop electromagnetic HLEM and transient domain electromagnetic TEM conductors. The drilling was contracted out to Bradley Bros. Limited from their Timmins, Ontario operation. The drill statistics and results obtained from this drilling program are listed in Table IV. TABLE IV DRILL HOLE SUMMARY GRID 1 DDH # f 11/ Collar Coordinates Line me Stn ms Line me Stn mn Line me Stn ms Line mw Stn mn Line me Stn ms Attitude Azimuth/Dip Total Depth m m m m m Anomaly Source graphitic sediments fault - open seam hematitic fault zones limonitic fault zone hematized Se pyritic mafic dyke

12 VIII DISCUSSION OF DRILL RESULTS Accompanying this report are the following; five (5) detail diamond drill hole logs (in Appendix A); diamond drill hole sections for each hole Figs 3-8 (in text) that illustrate the drill hole geology, conductor axis and source; and gold assay Swastika Lab report (in Appendix B), and XRAL Lab whole rock analytical report (in Appendix C). A total of 35 core samples numbered were split and submitted to Swastika Laboratories for assaying for gold. All assay results are entered on the diamond drill hole logs. In addition a total of 17 core samples numbered were also split and submitted to XRAL Laboratories for whole rock determinations. The sample numbers are also entered on the diamond drill logs. DDH 240-1: After 58.6 metres of overburden the hole intersected a sequence intermediate dacite tuff and breccia volcaniclastics with an andesite flow or dyke near the top of the hole. Thinly bedded, black carbonaceous (stongly graphitic and conductive) sedimentary intervals were intersected at metres down the hole. Thirty (30) samples were split from this hole and assayed for gold. The assay results were insignificant ranging from a low of nil to a high of 185 ppb Au. DDH : After 64.0 metres of overburden the hole intersected a sequence of mafic to intermediate volcanics consisting of andesitic flows, volcaniclastic breccias, intruded by several mafic and andesitic feldspar porphyritic dykes. A 1.0 metre ground or open seam was intersected at metres and may represent the conductor source. One (1) sample was split and assayed yielding only an insignificant result of 3 ppb gold. DDH 240-3: After 83.0 metres of overburden the hole encountered a short interval of andesite pillowed flow with inter-pillow sedimentary infilling indicating from graded bedding that tops are probably downhole. From metres to the end of the hole at 200 metres a sequence of andesite - dacite volcaniclastic breccia containing yellow felsic fragments

13 COLLAR DDH AZIMUTH D -45 L4*OOmE;3*25mS S S 030' S 2 4- DOS l +50S HLEM/TEM CONDUCTOR AXIS overburden o O c? o D dacite tuff - breccia l sediment andesite l dacite flow dacite tuff/or grey sediment o l dacite tuff - breccia l sediment carbonaceous sediment dacite tuff - breccia + minor carbonaceous sediment O 25m ^S!!^1 SC/^E: 1: m dacite tuff - breccia l sediment PHELPS DODGE CORP of CANADA DDH SECTION GRID LD 11/19 L4*OOmE73*25mS MINING CLAIM NO: P l LITTLE TWP Dal* December Sca" l : 1000 N.T.S. 42 A/ 14 5 t 3 FIG. 3

14 m S l + 50 m S i m S HLEM /TEM CONDUCTOR AXIS O H- 50 m S COLLAR DOH AZIMUTH D m N 0 Q o o O ^ 0O Q 0 Q o mafic dyke f-q'?*t M andesite breccia andesite flow andesite breccia andesite feldspar porphyry dyke andesite breccia andesite feldspar porphyry dyke andesite breccia mafic dyke andesite breccia PHELPS DODGE CORP of CANADA DDH SECTION GRID LO 15 L7-K)OmE70*25mN MINING CLAIM NO: P l MANN TWP EOH 224 m SCALE : 1:1000 Dot* Decembw seal* l : looo N.I.S. 4 2 A/14 Drawn/Bel* renc* S. G. FIG. 4

15 m S m S HLEM l T EM CONDUCTOR AXIS m S m S COLLAR DDH AZIMUTH 220; -45 LS + OOmE/1 *OOmS l+ooms cloy overburden sand a o 0 a O Q O O andesite flow (pillowed) tops downhole from interflow/pillow sediment grain gradation intermediate andestie-dacite volcaniclastic breccia o l C; O.3 m hematite gouge fault zone.5 m hematite gouge fault zone O 25m EOH 200 m 50 m PHELPS DODGE CORP of CANADA DDH SECTION GRIOLD6 L 5+00 m E/1+00 m S MINING CLAIM NO: P DUFF TWP SCALE : l: 1000 Dot* December, 1995 Scale l : 1000 N.T.S. 42 A/14 Drawn/Reference S.S. FIG. 5

16 m N COLLAR DDH AZIMUTH 030 ; -45 HLEM; TEM CONDUCTOR AXIS heavily fractured limonitic fault zone degrees T.CA l andesite breccia O 25m ^z^-r SCALE : 1: m PHELPS DODGE CORP of CANADA DDH SECTION GRID LO 7 L 7* 00 m VW 2 * 37 m N MINING CLAIM NO: P DUFF TWP Dale December Scal* l : 1000 N.r.s. 42 A/14 Drawn/tifcrcne* S. G. FIG. li

17 m S 3 + OOmS mS 2+00 m S COLLAR DDH AZIMUTH 220 / -45 L 5 * 00 m E 7 1 * 75 m S HLEM; TEM CONDUCTOR AXIS overburden O o O o O O o Q O andesite breccia andesite flow andestie-dacite breccia mafic dyke andestie-dacite breccia o l o hematized mafic dyke 2 0Xo pyrite mafic dyke andestie-dacite breccia EOH 230 m 25m SCALE: 1: m PHELPS DODGE CORP of CANADA DDH SECTION GRIDLD5 L 5* 00 m E/1 * 75 m S MINING CLAIM NO: P l DUFF TWP Dot* December 1995 Seal* : 1000 N.T.S. 42 A/14 S. G. FIG. 7

18 10 gouge most likely represents the conductor. One (1) sample was split and returned an insignificant assay of nil ppb Au. DDH 240-4: After m of overburden the hole intersected a mafic volcanic andesitic breccia unit that is extensively fractured, faulted and limonitic from 108 to 132 metres. An 2.0 metre open seam was also encountered from 117 to 119 metres. This fault zone represents the conductor in this hole. No samples for gold assay were submitted from this hole. DDH 240-5: After 85.0 metres of overburden the hole encountered a sequence of andesite flow and volcaniclastic breccia with some grey and yellow felsic looking fragments. This sequence is cut by several narrow mafic andesitic dykes and one such dyke intersected at to metres is hematized and contains 2 07o finely disseminated pyrite. It is suggested that where this altered part of the dyke subcrops a muddy weathered profile may exist and this being the source of the conductor. Three samples were split and assayed for gold returning insignificant values ranging from a low of 7 ppb to a high of 158 ppb Au. WHOLE ROCK ANALYSIS A total of 17 core samples were submitted to XRAL Lab for whole rock determinations. The raw data XRAL Lab report is found in Appendix C and a brief description of each sample is listed in Table V. The results show a lack of any major hydrothermal alteration as reflected in the Ishikawa Alteration Index that ranges from a low of to a high of (see Table V). The Zr/Y ratios of 6.4 to 10.5 corresponds to volcanic rocks with a calcalkaline affinity (see Table V). The Jensen cation plots for samples taken from each hole are illustrated in Fig. 8, Jensen Cation Plot Graph l. The results show a cluster of 8 samples lying in the High magnesium tholeiitic basalt field and a scatter of 9 samples lying in the calc-alkalic field from basalt to rhyolite in composition.

19 X-RAY ASSAY LABORATOHIES 22~Dec-95 JENSEN CATION PLOT GRAPH l FE203+7I02+MNO AL203 FIG. 8

20 I-RAI ASSAI LABORATORIES JUSU CAT10I PLOT HTH GRUHSKI HODIMCATlOI CIAPB l 22-Dec-95 SAMPLE SIHBOL CODE AL203 MGD ' " ? 960! , j J i 7 1 i) BT KT AT BT ST BC KT KT AC AC BC BC BC KT RC AC UT , , ,90 44, ,78 44, II ? 28,90 30, , ,00 25,75 24, , , U OK - FT - AT - RT - AC - RC - tt - CODE I trmice - JESSES CATIOI PLOT ULTRAMAFIC KOKATHTf IROI RICi 1ASALT TiOLiiiric mum THQLEIITIC RBIOLITE CALC-ALKALIBI A1DKITE CALC-ALKALIIE RBlOLlTE m D ENIED 11- Bf - UT - BT- JC - DC - BASALTIC KOMTIITE BIBB lagiisibi BASALT TBOLEJITIC DACITE TBOLE1ITIC IASALT CALC-AUALlIt BASALT CALC-ALULIIE DACITE L. S. (1976): A IE? CATIOli PLOT NK SUBALKALIC VOLCAIIC IOCK. ORTAKIO DI7ISIOI Of XIU5, KISC. FAFER 66. E, C. GR1UU (191!): Al ALCORITIX FOR TIE CLASS- IFICATIOI OF SUBALKALIC VOLCAIIC ROCKS 851BG TIE JllSEt CATlfll PLOT. SIHRllI OF HUD BOH. OITAglO Air. or nw,-nic,-run m, Tt

21 DDK #240-1: 3 Samples 9601 High Magnesium tholeiitic basalt (flow) 9602 High Magnesium tholeiitic basalt (tuff-breccia) 9603 Tholeiitic andesite to calc-alkalic basalt (tuff-breccia) DDK #240-2: 4 Samples 9604 High Magnesium tholeiitic basalt (flow) 9605 High Magnesium tholeiitic basalt (andesite breccia) 9606 Calc-Alkalic basalt (andesite breccia) 9607 High Magnesium tholeiitic basalt (andesite breccia) DDK #240-3: 4 samples 9608 High Magnesium tholeiitic basalt (pillow flow) 9609 Calc-alkalic andesite (breccia) 9610 Calc-alkalic andesite (breccia) 9611 Calc-alkalic basalt (breccia) 11 DDK # 240-4: 2 samples 9612 Calc-alkalic andesite (breccia) 9613 Calc-alkalic andesite (breccia) DDH# 240-5: 4 samples 9614 High Magnesium tholeiitic basalt (flow) 9615 Calc-alkalic rhyolite (fragment only) 9616 Calc-alkalic andesite (fragments plus matrix) 9617 High Magnesium tholeiitic basalt (small fragments plus matrix) The samples that are clearly mafic flow rocks returned a chemical affinity signature in the high magnesium tholeiitic basalt field. The volcaniclastic breccia samples containing a felsic breccia clastic component with varying sericite concentrations returned a chemical affinity in the calc-alkalic field. The end member represented in sample # 9615, a carefully segregated yellow rhyolite breccia clast returned a chemical affinity signature of a calc-alkalic rhyolite. The volcanic regime, especially in the areas of the mafic flows and mafic fragmentals, appears to be predominantly in the high magnesium tholeiitic basalt field. However, as the felsic volcanic coarse fragmental component is

22 12 increased and apparently mixed into the tholeiitic andesite-basalt finer tuffaceous matrix, there is a noticeable shift from the high magnesium tholeiitic basalt field into the calc-alkaline field from basalt to rhyolite in composition. This apparent mixing of the two distinct chemical affinities, i.e. high magnesium tholeiitic and calc-alkalic populations, suggests the volcanic material is possibly derived either from two separate volcanic sources and/or possibly from a single evolving volcanic center. In either event, the existence of the calc-alkalic rhyolite breccia clasts is significant in that it clearly identifies a felsic volcanic component is present in the volcanic section. The potential for further development and thickening of a felsic calc-alkalic volcanic assemblage with a probable source nearby should not be underestimated

23 13 Sample # DDH # Metre Depth TABLE V WHOLE ROCK ANALYSIS Rock Type 1 Description Andesite flow; f.g. med green white fsp porphyritic Dacite tuff breccia; yellow sericite altered Dacite tuff breccia; pale-med. green fragments in andesite matrix Andesite flow; pyroxene porphyritic Andesite breccia; dark mafic fragments in med. green tuff matrix Andesite breccia; carbonate "eyes" Andesite breccia; Andesite flow; pillowed with 1mm black crystals Andesite-dacite breccia; yellow sericitized breccia fragments Andesite dacite breccia; yellow sericitized breccia fragments Andesite breccia; Andesite breccia; yellow sericitized breccia fragments Andesite breccia; yellow sericitized breccia fragments Andesite flow; mafic crystals (chlorite?) One yellow sericitized breccia fragments from andesite dacite breccia Andesite dacite breccia; yellow felsic breccia fragments in andesite tuff matrix Andesite dacite breccia; small yellow felsic breccia fragments Ishikawa Altn Index Zr/Y ratio Chein. Affinity High Mg Thol Bs High Mg Thol Bs Thol And -Gale Alk Basalt High Mg Thol Bs High Mg Thol Bs Calc Alk Basalt High Mg Thol Bs High Mg Thol Bs Calc Alk Andesite Calc Alk Andesite Calc Alk Basalt Calc Alk Basalt Calc Alk Basalt High Mg Thol Bs Calc Alk Rhyolite Calc Alk Andesite High Mg Thol Bs

24 14 IX CONCLUSIONS The 1014 metre drill program identified the target source of the H.L.E.M. and T.E.M. conductors in five holes tested. In all cases the anomaly source was interpreted to have been intersected and the cause of the conductors is attributed to carbonaceous fine grained sedimentary strata in DDK l, and to fault zones in DDK 240-2, -3, -4 and -5. All holes encountered moderate to deep overburden from a minimum downhole length of 58.6 metres in DDK l to a maximum of 108 metres in DDK No significant gold or silver values were detected in any of the samples submitted. X RECOMMENDATIONS From the 1995 drill program the prime geophysical H.L.E.M and T.E.M. targets indicated to date on Little Duff properties LD - 5, - 6, - 7, - 11/19, and -15 have been tested and the anomalous sources adequately explained. No further work is warranted on the tested conductive horizons at this time. Respectively submitted Dave Gamble Dave Gamble Geoservices Inc

25 15 APPENDIX A - DIAMOND DRILL HOLE LOGS DDK #'s 240-l,-2,-3,-4,-5. B - SWASTIKA LAB GOLD ASSAY REPORT C - XRAL WHOLE ROCK ANALYSIS REPORT

26 16 APPENDIX A DIAMOND DRILL HOLE LOGS DDH#240-lto240-5

27 17 APPENDIX B SWASTIKA GOLD ASSAY REPORT

28 240LOG1.doc /O First Street, Kirkland Lake, Ontario, P2N 1N3, Tel: , Fax: Project: Little- Duff 240 Property : LD 11/LD 19 Twp/Claim: P LITTLE 1 TULLY TWP Hole No: LD Purpose of Hole: To test HLEM and TEM Conductor C 11/19 A Azimuth: 030 degrees Dip:- 45 degrees Location: L 4+OOmE/ L3*25mS Total Depth: 190m DRILL RECORD Started: Sept. 18, 1995 Completed: Sept. 21, 1995 Core Size: BQ Drilled By: Bradley Bros. Ltd. Logged For Phelps Dodge Corp. of Canada ^ Logged By: Dave Gamble,J^^^ra^r " ^^y^ Tests: TD: 0 Dip:~45 degrees(az: 030 TD: 1 00m Dip:-50 degrees Az: Remarks / Results: -graphite sedimentary interval in altered Dacite Volcaniclastic Breccia - sedimentary sequence \ - quartz eyes and chips near bottom of interval in sericite breccia fragments Metres From: Metres To: Description DDH Sample Number: From: To: Length Au (ppb) OVERBURDEN (Casing Pulled - lost 13m NW, 21m BW) DACITE TUFF BRECCIA 1 SEDIMENT - to grey siliceous sediment, - medium to light grey to buff cream yellow in colour. - fine grained siliceous matrix, no carbonate, with dark grey thread like" fracture fillings of carbonaceous and chlorite material both in the matrix and crossing through fragments. -The unit is chaotic looking with bleached buff yellow patches and what appears to be lapilli and breccia fragments up to 7 cm in size with clear fragment boundaries, -The unit is hard and dense and contains flecks of vibrant green fuchsite especially in areas where the buff coloration is strongest. - Also where the yellowish cream buff discoloration is strongest, weak sericite is developed along the weak fabric and along the small shears; - Weak foliation 45 degrees t.c.a. - Some 20 degrees t.c.a. - trace pyrite locally - could be a carbonaceous fracture filled siliceous clastic sediment unit to Dacite Breccia - fragments tend to have irregular boundaries but are sharp, vary in composition from dacite buff yellow "felsic" to grey-green and grey andesitic material. - cut by white quartz stringers and veinlets throughout - Lower contact sharp and at 40 degrees t.c.a Nil 7 3 Nil Nil Nil Nil 3 3 Nil Nil

29 Metres From: Metres To: Description DDH Sample Number: From: To: Length Au (PPb) ANDESITE TO DACITE FLOW OR DYKE - medium grey green fine grained ground mass with 1 to 2 mm sausseritized feldspar phenocrysts giving weak porphyritic texture, - no carbonate, no magnetite, no pyrite, occasional quartz stringer, generally lacks the black " thread like" fracture fillings of the preceding unit, - Lower contact at 82.5m, sharp wavy, and at 35 degrees t.c.a. W DACITE TUFF 1 O R GREY SEDIMENT - generally fine grained, medium grey mottled, with black carbonaceous "thread like" fracture fillings, weak foliation at 40 degrees t.c.a. - Lower contact sharp slip contact at 30 degrees t.c.a DACITE TUFF - BRECCIA 1 SEDIMENT as previous grading finer down hole to tuff sediment, plus minor intercalated black carbonaceous fracture filling and disrupted lamellae, - bleached buff yellow patches ( weakly sericitic) lapilli and fragments that tend to be irregular in shape with strongly defined clast boundaries. From approximately 109 m, the unit is light grey green, occasional fragments appear as 'in situ' type slump brecciation of a dacite tuff or sediment - still contains green flecks of fuchsite and trace pyrite -weakly sericitic foliation fabric at 50 degrees t.c.a. - "thread like" black carbonaceous fracture fillings and several narrow horizons of intercalated carbonaceous sediment at , , , m within grey - green dacitic tuff/sed - broken core at m, fractured zone - The dacite breccia unit looks fragmental as well as looking like a fractured unit that has had minor contemporaneous carbonaceous black material infilling fractures and as well developing narrow seams or beds of carbonaceous material strong chloritic slips at 20 degrees t.c.a m -becoming increasingly finer grained tuff-sediment and pale yellowish cream to very light yellowish green, locally section contains intercalated carbonaceous component as thread like stringers or fracture fillings, and as well as disrupted carbonaceous patches and possible fragments, - ie contemporaneous dacite tuff - breccia and sedimentation with slumping and minor carbonaceous infilling the voids and fractures and carbonaceous sedimentary layering Nil Nil Nil Nil

30 Metres From: Metres To: Description DDH Sample Number: From: To: Length Au (PPb) - increases carbonaceous component from m. - clean homogeneous buff yellow sericitic interval m - carbonaceous rich section and broken ground m - minor quartz stringers 1 cm and less, trace pyrite - sharp abrupt contact at m at 45 degrees t.c.a. - strong foliation above contact and also at 45 degrees t.c.a. - fuchsite flecks, quartz stringers, trace pyrite, weak sericitic W CARBONACEOUS SEDIMENT (Conductor) graphitic - finely laminated at 40 degrees t.c.a. near contact, progressing to disrupted layering containing white siliceous irregular to ellipsoidal shaped clasts 1-4 cm in size in a dark black fine grained carbonaceous matrix - graphitic also contains 0.5 cm to 2 cm pyrite nodules -slips and black muddy gouge m - finely disseminated pyrite locally, pyrite lamellae and thin pyrite seams locally - Lower contact sharp at 50 degrees t.c.a , DACITE TUFF BRECCIA/SEDIMENT as previous - gray - yellowish cream, -stretch fragments and foliation at 45 degrees t.c.a. - fine thread like stringers ( fractures) and some of the matrix component is fine black carbonaceous sediment within a fine grained to coarse clastic dacite tuff breccia/ sedimentary sequence. - some fragments up to 6 cm, sericitic, grey volcanic and grey green volcanic, subrounded breccia fragments, - minor carbonaceous intervals at the following: broken sheared to crushed carbonaceous intercalated layer sheared to crushed carbonaceous intercalated layer graphitic, pyrite nodules, broken recovery, sheared to crushed, minor qtz veinlet upper contact hematite slip and lower contact graphite 50 degrees t.c.a upper contact 40 degrees t.c.a. - broken crushed zone, sheared, poor recovery. graphitic, lower contact broken mixed black carbonaceous matrix and grey matrix, with mafic volcanic breccia fragments or boulders 1 pebbles, occasional pyrite nodule,

31 Metres From: Metres To: Description DDH Sample Number: From: To: Length Au - chaotic mixture of grey tuff/sediment and fragments of same plus other types, including grey green mafic volcanic, grey sericitic altered felsic, in a grey carbonaceous "graphitic" matrix plus grey tuff/sediment - grades sharply into less carbonaceous component at m - little to no carbonaceous component at 168m to EOH EOH DACITE TUFF BRECCIA/SEDIMENT grey yellowish mudstone brecciated - slump breccia brecciated and with breccia clasts occasional fragments with "qtz eyes" and quartz chips that are pale yellow siliceous with sericitic matrix in the fragments sericitic in the overall unit, imparting a weak buff yellow coloration ( possibly reworked dacite/ breccia sequence with slump brecciation that has resettled with a carbonaceous sedimentary infilling component - minor layering at 30 degrees t.c.a., foliation at 30 degrees t.c.a. W

32 240LOG2.doc 70 First Street, Kirkland Lake, Ontario, P2N 1N3, Tel: , Fax: DRILL RECORD Project: Little- Duff 240 Azimuth: 210 degrees Started: Sept. 22, 1995 Property: LD 15 Dip:- 45 degrees Completed: Sept. 25, 1995 Twp/Claim: P MANN Location: L 7+OOmE/ LO*25mN Core Size: BQ Hole No: LD Total Depth: 224 m Drilled By: Bradley Bros. Ltd. Purpose of Hole: To test HLEM and TEM Conductor C 15 A - 1 Logged For: Phelps Dodge Corp. of Canada,,, Logged By: Dave Gamble s@ftzsaz-*4fr4f Tests: TD: 100 Dip:- 50 degvees Az: TD: 224m Dip:- 45 degrees Az: Remarks 1 Results: Andesite Flow (porphyritic) and breccia sequence Conductor -(possible) 1m open seam at 116 m Metres From: Metres To: Description DDH Sample Number: From: To: Length Au (ppb) l OVERBURDEN (casing pulled) ANDESITE FLOW (PYROXENE, PLAGIOCLASE PORPHYRITIC) massive, uniform flow, - medium grey green, fine grained ground mass, with dark green mafic pyroxene ( stubby prismatic) of 2-3mm in size, and white Omm white plagioclase feldspar crystals, plus epidote; lacy network of epidote and minor quartz filled fractures quartz epidote vein - white quartz, vuggy, trace carbonate, barren, no sulphides, - minor interstitial carbonate above the quartz vein, moderate interstitial carbonate - minor epidote - thread like stringers and weak patchy epidote, - minor white carbonate stringers, fracture filling internal flow contact at 70 degrees t.c.a., sharp - fine grained equivalent - similar to above (Sample at 77.5 for lithogeochem.) -minor pyroxene porphyritic lower contact, sharp but irregular at epidote seam - minor quartz at 50 degrees t.c.a. -carbonate epidote thread like stringers - moderate interstitial carbonate throughout the unit - stringers at 50 degrees t.c.a. with several stringers of carbonate at 5 degrees t.c.a as previous flow, pyroxene porphyritic larger pyroxene crystals to 5mm trace - -\ 0/* pyrite at 84.3m, 84.7, 86.0, 86.9, 87.9, 88.1, 88.6, disseminated pyrite associated with patches of stronger interstitial carbonate W

33 Metres From: Metres To: Description DDH Sample Number: From: To: Length Au trace to 17o pyrite locally associated with greater interstitial carbonate and veinlets carbonate stringers, bleached, with pyrite at 20 degrees t.c.a. - interstitial carbonate weak mottled texture suggesting a flow breccia - medium to pale green to medium green, colour contrast represents a flow cooling feature - stubby pyroxene and/or feldspar start to show carbonate replacement locally at pink carbonate stringers and veinlets ( to 2cm in width) also at , 112.5, , 113.5, at 55 degrees t.c.a weak mottled texture as above suggesting a flow breccia, weak autobrecciated flow - mottled to pervasive epidote locally broken core No Core Recovery- Mud, Ground Seam (Possible Conductor) pink carbonate vein at 65 degrees t.c.a less pyroxene porphyritic, still plagioclase porphyritic, - interstitial carbonate weak to moderate throughout, no magnetite 0.0-0,1 cgs mag susceptibility throughout entire unit lower contact 30 degrees t.c.a., sharp, bleached contact zone, minor carbonate veining along contact, ANDESITE BRECCIA - pale to medium grey green matrix. -pale green to medium green, porphyritic clasts of similar composition to previous flow, some clasts with white carbonate filled variolites, generally angular to subrounded to rounded, equidimensional in shape, less than 1 cm and up to 10 cm in size, fragment are not flattened or stretched -trace pyrite locally, disseminated -trace chalcopyrite on carbonate filled fracture at 131.8m - darker breccia fragments are darker green on borders and lighter green in the center of the fragments, - interstitial carbonate moderate and occasional white calcite stringer plus 1 cm and less veinlets a noticeable clast type contains numerous carbonate "eyes" MAFIC DYKE - upper contact at 35 degrees t.c.a. - fine grained, medium green, containing 1mm white plagioclase crystals and dark mafic crystals, generally fine grained massive, homogenous throughout, - lower contact irregular at approximately 80 degrees t.c.a., contains several zenoliths of W m

34 Metres From: Metres To: Description DDH Sample Number: From: To: Length Au andesite breccia near lower contact, - interstitial carbonate moderate ANDESITE BRECCIA - as previous W ANDESITE (FLOW) OR DYKE - grey green - flow contact layering and chill margin layered at 75 degrees t.c.a. ( bedding) over 15 cm -1-3 mm cream white to yellowish green plagioclase crystals imparting a porphyritic texture, plus mafic crystals -cut by thread like stringers and veinlets of carbonate and quartz - several strong epidote altered zones 5cm in width associated with quartz and carbonate veinlets -becoming finer grained medium green near lower contact from 184 to lower contact sharp at 70 degrees t.c.a ANDESITE BRECCIA - as previous but starting to contain occasional light to medium grey dacite fragments it becomes progressively more fine grained which indicates possible ' fining" down hole becomes tuffaceous - lower contact sharp at 75 degrees t.c.a FELDSPAR PORPHYRY DYKE - ANDESITIC - upper contact fine grained, medium grey green, similar in colour to preceding andesite, - occasional remnant phenocrysts quartz vein, white barren, at 50 degrees t.c.a begin to see 1-3 mm cream white porphyritic plagioclase phenocrysts in a grey - grey green ground mass slight pinkish tinge to the ground mass, weak hematite dusting. - unit is slightly magnetic from ranging from 0.7 to 1.7 cgs on the magnetic susceptibility meter. - becomes finer grained at to lower contact at lower contact sharp at 75 degrees t.c.a. - locally cut by white calcite stringers, plus quartz and carbonate and epidote stringers -no pyrite present in the dyke - weak to moderate interstitial carbonate

35 Metres From: Metres To: Description DDH Sample Number: From: To: Length Au ANDESITE BRECCIA - as previous, coarse grained, fragments FELDSPAR PORPHYRY DYKE - ANDESITIC - as previous - pinkish hue, weak interstitial carbonate - up to 1.7 cgs on the magnetic susceptibility meter ( weakly magnetic) - chloritized contact from 1-3 cm - occasional creamy white feldspar and irregular - ddh tends to parallel the contact giving a scalloped nature to the contact - upper and lower contact at 40 degrees t.c.a ANDESITE BRECCIA (as previous) lower contact at 30 degrees t.c.a FINE GRAINED MAFIC DYKE - dark green mafic, fine grained, massive, interstitial carbonate, - lower contact at 50 t.c.a EOH ANDESITE BRECCIA ( as previous) - matrix becomes lighter grey from 215 to EOH - fragments vary from 1-5 cm in size - some light grey dacite breccia fragments as well as a number of angular dark green andesitic volcanic breccia fragments in the 2 cm range - moderate interstitial carbonate throughout W

36 240LOG3.doc 70 First Street, Kirkland Lake, Ontario, P2N 1N3, Tel: , Fax: Project: Little- Duff 240 Azimuth: 220 degrees Property: LD 6 Dip:- 45 degrees Twp/Claim: P DUFF TOWNSHIP Location: L 5+OOmE/ Ll+OOmS Hole No: LD Total Depth: 200 m Purpose of Hole: To test HLEM and TEM Conductor C 6 A DRILL RECORD Started: Sept. 26, 1995 Completed: Oct Core Size: BQ Drilled By: Bradley Bros. Ltd. Logged For: Phelps Dodge Corp. of Canada, ^ Logged By: Dave Gamble n-j7 i**i :fcfttf-f Tests: TD: 0 DipMS degrees Az: TD: 1 04m Dip:-50 degrees Az: Remarks 1 Results: Intermediate Flow and Volcanic Breccia Sequence Conductor intersected as two hematitic fault zones Metres From: Metres To: Description DDH Sample Number: From: To: Length Au (PPb) OVERBURDEN ( Casing Pulled) ANDESITE FLOW - PILLOWED - pillowed, fine grained, medium grey green mosaic with 1 mm to 2mm and less plagioclase cream white crystals mm black stubby crystals ( pyroxene and /or chlorite) giving pepper like texture - Broken core over first several meters - Selvage to the pillows are generally dark green, fine grained chloritic in the narrow 1-2cm range, several larger selvages to 10 cm containing white interstitial carbonate - One selvage at m or inter pillow interval is composed of finely laminated "cherty" looking interflow sediments that are finely bedded with grain gradation down hole, and bedding at 30 degrees t.c.a. - Occasional minor quartz and epidote 1 cm and less veinlets at degrees t.c.a. and at 90 degrees t.c.a. - No sulphides, no magnetite, no interstitial carbonate in pillows -Lower contact sharp but irregular varying from degrees t.c.a., averaging 70 degrees W INTERMEDIATE VOLCANICLASTIC BRECCIA (Andesite -Dacite Volcaniclastic Breccia) - medium green, fine grained tuff matrix containing angular to subrounded tuff-breccia fragments from 1cm to 5cm in size. -The composition of the fragments ranges from green mafic volcanic to pale green

37 Metres From: Metres To: Description DDH Sample Number: From: To: Length Au (ppb) intermediate to buff cream yellowish felsic ( sericitic), aphanitic to feldspar porphyritic ( 1 mm plagioclase crystals) volcanic fragments - locally lacy interstitial carbonate and occasional 1-2cm quartz and epidote barren veinlets at 45 degrees t.c.a.. - trace hematite lined fractures from m - High percentage of fragments to matrix, to the point where locally the unit is partially clast supported -Hematite lined fractures at degrees t.c.a. at 110.7, 115.0, 115.4, 128.1, 129.0, 131.3m - Weak white interstitial carbonate tends to form around fragments locally and not throughout the matrix, - Occasional large breccia clast to 30 cm in size EOH - fewer but still present yellowish felsic breccia fragments, more andesitic in composition, still occasional felsic angular chips and clast throughout strong hematitic muddy red gouge fault zone at 55 t.c.a. Below this fault zone, core seems to be slightly more fractures and locally stringers of quartz and carbonate m Fractured zone, minorquartz stringers, barren Hematized Fault Zone with 10 cm epidote altered wall rocks - Fault is characterized by strong red hematite preserved in competent core as well as in muddy gouge broken ground. Several white low angle ( 0 to 1 0 degrees t.c.a.) carbonate veinlets and stringers on either side of the fault zone at and m W 9609 W W Nil EOH 200.0m

38 240LOG4.doc 70 First Street, Kirkland Lake, Ontario, P2N 1N3, Tel: , Fax: DRILL RECORD Project: Little- Duff 240 Azimuth: 030 degrees Started: Oct. 1, 1995 Property: LD 7 Dip:- 45 degrees Completed: Oct. 6, 1995 Twp/Claim: P DUFF TOWNSHIP Location: L 7+OOmW/ L2*37mN Core Size: BQ Hole No: LD Total Depth: 170 m Drilled By: Bradley Bros. Ltd. Purpose of Hole: To test HLEM and TEM Conductor C 7 A Logged For: Phelps Dodge Corp. of Canada ^, Logged By: Dave Gamble x^*^b^z±^t^' Tests: TD: 0 Dip:-45 degrees Az:030 TD: 113m Dip:-50 degrees Az: Remarks 1 Results: Mafic to Intermediate Volcaniclastic Breccia Conductor intersected as limonitic extensively fractured fault zone Metres From: Metres To: Description DDH Sample Number: From: To: Length Au EOH OVERBURDEN (Casing pulled - Lost 28m NW) ANDESITE BRECCIA ; VOLCANICLASTIC 1 FAULT ZONE - extremely broken fractured to rubbly core from to m - dirty olive green, limonitic weathered fracture/fault zone, No foliation, brittle fracturing - No carbonate, interstitial or stringers - No magnetite, mag susceptibility 0.0 cgs - No sulphides - On less oxidized material, medium green, tuffaceous matrix with breccia fragments from 0.5 cm to 3.0 cm, occasionally to 10 cm, fragments consist primarily of a green andesitic and to a less extent light grey dacitic volcanic breccia fragments -Also minor constituent of pink felsic fragments, either a hematized volcanic or granitic material -Breccia fragments are angular to subrounded, generally matrix supports clasts, -Occasional short intervals where larger fragments are in contact with each other, only weak clast supported locally - interval is well fractured and contains clay to muddy gouge along some of the fractures and in rubble recovery -Fractures are predominantly at degrees t.c.a m Ground 2m, no recovery, seam or gouge zone m Local minor barren 1-2mm quartz stringers at 70 t.c.a.

39 Metres From: Metres To: Description DDH Sample Number: From: To: Length Au EOH Less limoniticto nil below m only locally fractured and broken below 132.0m, becoming more competent below m - Minor weak pervasive epidote alteration on some fragments from m - Weak interstitial carbonate from m Occasional carbonate stringers and veinlets less than 1 cm and several minor 1 cm quartz plus carbonate veinlets at degrees t.c.a. - barren -Several breccia blocks in the 20 cm size range, also some show porphyritic textures with stubby mafic pyroxene crystals, 1-3mm in crystal size generally in a fine grained volcanic ground mass, breccia fragments are not flattened or stretched. - Most fragments are andesite flow fragments and not fragments of clastic material W W

40 240LOG5.doc SJJTC?. 70 First Street, Kirkland Lake, Ontario, P2N 1N3, Tel: , Fax: Project: Little- Duff 240 Property: LD 5 Twp/Claim: P DUFF TOWNSHIP Hole No: LD Purpose of Hole: To test HLEM and TEM Conductor C 5 Azimuth: 220 degrees Dip:- 45 degrees Location: L 5+OOmE/ L1*75mS Total Depth: 230 m DRILL RECORD Started: Oct. 10, 1995 Completed: Oct. 14, 1995 Core Size: BQ Drilled By: Bradley Bros. Ltd. Logged For: Phelps Dodge Corp. of Cana^r ^ Logged By: Dave Gamble.X^^^5^5*"^ Tests: TD: 98 Dip:-52 decrees Az: TD: 221 Dip:-45 degrees Az: Remarks l Results: Intermediate Flow and Volcaniclastic Breccia Sequence With Increasing Felsic Fragments Down Hole Probable conductor intersected are Hematite rich mafic dykes at and at m that are most likely deeply weathered and muddy at the subcrop surface (fault?). Metres From: Metres To: Description DDH Sample Number: From: To: Length Au (ppb) OVERBURDEN (casing pulled) ANDESITE BRECCIA - Medium green matrix, Tine grained tuff with 1-2cm clasts and occasional 5cm clasts and up to 1 5 cm breccia clasts - No interstitial carbonate or sulphides or magnetite, ( low magnetic susceptibility readings cgs) - Clastic component consists mainly of green andesitic volcanic clasts and to a lesser degree grey to buff pink dacite volcanic clasts with greenish chlorite wisps and 2mm crystals chlorite after amphiboles or pyroxenes. - clasts are subrounded to angular in shape, not flattened and show little strain or stretching - local carbonate stringers and several quartz and epidote veins at at 65 degrees t. c. a. plus several other narrow stringers cm wide at 40 degrees t.c.a at 40 degrees t.c.a at 40 degrees t.c.a at 55 degrees t.c.a carbonate at 50 degrees t.c.a carbonate at 40 degrees t.c.a. All of the above veins and stringers have no sulphides present - Fractured and broken over the first several meters

41 Metres From: Metres To: Description DDH Sample Number: From: To: Length Au (Ppb) Over the lasts meters from 104 to 109 m predominantly dark green - med green matrix with fewer fragments than previous, possibly part of a flow breccia from next flow unit, lower contact defined as irregular, sharp, and by disappearance of the fragment population ANDESITE FLOW - upper contact sharp but irregular at 60 degrees t.c.a. - lower contact is a shear slip surface at 30 degrees t.c.a. - unit is medium green, massive uniform flow - small 1-2mm stubby black to dark green mafic remnant crystals, chlorite after amphiboles or pyroxenes - weak epidote patchy alteration - minor carbonate stringers and minor quartz plus epidote veinlets - several quartz white plus or minus pink carbonate veins at 110.8m at 30 degrees t.c.a. 8cm wide 112.2m at 40 degrees t.c.a. 2cm wide m at 30 degrees t.c.a. 3 cm wide -Occasional minor internal flow features, some narrow areas of darker green, possible chill zones and internal contacts W ANDESITE (DACITE) BRECCIA upper contact shears slip at 30 degrees t.c.a. ( 10 cm), dark green for first 0.5 m with ghost like fragments in the dark matrix - At m clearly an intermediate breccia with good fragment to matrix definition - Medium green matrix similar in colour to preceding flow unit, also contains mafic crystals and/or chips (pyroxenes) in matrix as well as in breccia fragments, - Matrix is generally fine grained enveloping both darker and lighter green andesitic volcanic fragments, buff pink and medium to light grey dacitic fragments, and epidote altered yellowish green fragments, - the grey and buff pink fragments contain interstitial carbonate whereas the green volcanic breccia fragments contain no carbonate - At 127 to 134.6m ( on the down hole side of the mafic dyke, a noticeable increase in buff cream to pale yellow breccia fragments, the largest up to 12 cm in size, - the majority of fragments are in the 1-3cm size range. These breccia clasts are similar in texture to the intermediate clasts, ie porphyritic with mafic remnant crystals and could represent a more advanced alteration of a similar unit - Samples for whole rock analysis at " felsic" breccia fragments, and at breccia unit - From noticeable foliation with weak to moderate fragment stretching at 50 degrees t.c.a. W 9615 W

42 Metres From: Metres To: Description DDH Sample Number: From: To: Length Au (Ppb) - Sharp lower intrusive jagged contact at 20 degrees t.c.a MAFIC DYKE - Upper contact cross cuts weak foliation fabric at 20 degrees t.c.a. and almost normal to fabric clearly indicating an intrusive unit -Dark green, fine grained, no carbonate weakly magnetic up to 0.7 cgs magnetic susceptibility (averaging ) in contrast to for the breccia sequence - Lower contact sharp and undulating and cross cutting breccia fragments, contact approximately 30 to 40 degrees t.c.a ANDESITE ( DACITE) BRECCIA (as previous) From fewer " felsic" breccia fragments, plus a higher percentage of green and grey green fine grained ( plus or minus porphyritic) mafic crystals that are similar to the preceding flow m. - Minor carbonate stringers and occasional hematite lined fractures at m at 20 degrees t.c.a., with pink carbonate vein at 134.4m 3cm at 70 degrees t.c.a "Xo quartz veins and stringers at 80 degrees t.c.a. epidote plus quartz, barren Also quartz veins at : 3cm at at 75 degrees t.c.a. 15 cm at upper contact at 50 degrees t.c.a. lower contact at 70 degrees t.c.a. 3cm at at 60 degrees t.c.a. 5 cm at at 40 degrees t.c.a cm carbonate stringers at parallel t.c.a. for 20 cm, plus possible tourmaline, and hematite lining contact, no sulphides - Occasional weak patchy carbonate, very minor, local - increase percentage of " felsic " fragments plus dacite as previous from ALTERED REDDISH HEMATIZED MAFIC DYKE upper contact broken, possibly at 55 degrees t.c.a. pinkish grey, fine grained, with occasional reddish pink 1 mm feldspar crystals, weak interstitial carbonate, - trace - 2Vo finely disseminated pyrite throughout the overall pinkish hue as a result of hematite dusting throughout lower contact shear, black, sharp at 15 degrees t.c.a. - remnant mafic 1-2mm stubby crystals in a fine grained pinkish mosaic occasional 1 mm - 4 mm white calcite stringers - no magnetite ( 0.0 cgs mag susceptibility)

43 Metres From: Metres To: Description DDH Sample Number From: To: Length Au (PRb) MAFIC DYKE - ANDESITIC - Very similar in texture to above pinkish dyke, may be the same unit but not altered or mineralized with pyrite - weak interstitial carbonate but no hematite - lower contact sharp but ragged at 20 to 60 degrees t.c.a. and appears to cross out both weak underlying foliation and fragments of the next unit down hole - no magnetite in this unit ( magnetic susceptibility 0.0 cgs) ANDESITE (DACITE) BRECCIA - as previous - some breccia fragments, square to 8 sided euhedral black green mafic crystals - pyroxene carbonate quartz vein at 60 degrees t.c.a. barren - more mafic to intermediate breccia fragments with pyroxene porphyritic andesite flow fragments and less buff yellow felsic clasts Red hematized irregular mafic dykelets irregular and sharp contacts, slight darker red contact discoloration at margins of each dykelet, weak interstitial carbonate in all dykelets occur at irregular embayed contacts irregular embayed contacts at 60 degrees t.c.a irregular embayed contacts at 60 degrees t.c.a irregular embayed contacts at 60 degrees t.c.a upper and lower contact at 40 degrees t.c.a. sharp cm white carbonate stringers cut all dykelets - These dykelets are similar to the reddened dyke at mafic crystals have been chloritized - trace, speck of pyrite, stringers are white calcite and carbonate vein W EOH

44 18 APPENDIX C XRAL WHOLE ROCK ANALYIS REPORT

45 ' ;,i,ih :.:TIKA LABS SOO :45PM l : l J B l Swastika Laboratories A Division nf TS(,/A^xaycrs Inc. established 1928 Assaying - Consulting - Rcprcsentaf ion Page l of 2 Geochemical Analysis Certificate 5 W-4553-RG1 comply: PHELPS DODGE CORP OF CANADA LTD D.HC; DEC PLO..PCI: 240 Aim: D.Gamble W2 hereby cenijy the following Geochemical Analysis of 35 Core samples submitted NOV by. Samp 1 e Number , ? Au PPB 3 10 Nil 7 3 Nil Nil Nil' 3 3 Nil Nil Ni 1 Nil Ni Nil Nil Au Check PPB. Nil Certified by P.O. Box 10, Swastika, Ontario POK 1TO Telephone (705) FAX (705)

46 n-jh&tikh Li-iB S? Oi:46PH [81] B2 Swastika Laboratories A Division of T.SI./Assaycrji I nc. Established 1928 Assaying - Consulting. Representation Page 2 of 2 Geochemical Analysis Certificate 5W-4553-RG1 Company: PHELPS DODGE CORP OF CANADA LTD Daic DEC Project: 240 Aim: D.Gamble We hereby certify the following Geochemical Analysis of 35 Core samples submitted NOV by. Sample Au Au Check Number PPB PPB 9531 " Certified by P.O. Box 10, Swastika, Ontario POK 1TO Telephone (705) F AX ( 705)642-^:500

47 16 APPENDIX C XRAL WHOLE ROCK ANALYIS REPORT

48 i K E ;:R-HL NO F n:; ; t: i f r D4 4 D F'. L) l XRAL LES LABORATOIRES XRAL LABORATORIES UNE DIVISION DE f A DIVSION OF SGS CANADA INC 129 AVE. Rf AL CAOUETTE - C.P ROUYN-NORANDA - QUEBEC J9X 5A9 TEL (819) FAX (f(19) 76^,o.ir irl: PROJECT 240 our ret- h36(vr643v T D'ANALY^L/Ab-SAY CLRT1I ; K'ATL PHELPS DODGE CORP. LTD C/O DAVE GAMBLE 120, ADELAIDE STOEET WEST TOKONTXD, ONTARIO M5H!TI ATTENTION: MR. PAUL CHAMOIS Nmcmlicr 2X. No ol p;i'.'o^: 2 ELEMENTS WRMAJ 'v WRMIN PPM B A PPM METTIOD VVR/XRF WR/XRK U R/XRF DETECTION LIMIT lil Ccrlil'ic p. ir/cc ri i fic d t'\ J. J. I anders/miiiuvict Membra du Groups S GS ( Soci6t6 G6n6rale de Surveillance)

49 H L F H:: XBAL JUAtiORATOli1K9 13-D. ao-9s AMPLJ2 * O y b D SAMPLE OC 9607?oe ) SAMPLE NA3O V XRP-F DO S S 3.12 mo v XRF-F Q. 16 O O.OS O. OS SUM * XRF-F 0.1 MC30 * XRF-F Q e.19 FK203 * XRF-F Si 6.65 S V B - 9O RKPORT AL203 V XRF- P O RB evn XRF-F clo clo clo <io clo clo clo clo 4236 GIO2 \ XBF-F CI SQ R PPM XRF- F O WORKOHDER 6366 P205 V XRF-F C y PPM XRF-F K2O * XRF- P S 1.S ZB PPM XRF-F S ? 7* CAO * XRF-F O.O NB PFM XRF-F 10 ^10 ^LQ clo clo clo 0.0 do clo ClO ClO clo Cl0 clo ClO clo clo clo clo ClO PJK3E 1 TI02 f XRF-F Bft. PPM XRF-F S S C! CR2O3 t XRF-P O Q.07 O LOI * XRF-F IS S O ) OO OO.O OO.O

50 eau me L. Hanna Lucas LD3 LD5 X D uff LD7 IM d Mann x- \ Newmarket LD8 LDI LD 14 Prosser LDI1/I9 Little LDI6 McCart opprox. DDH location and number iild22 X:':-: : :l phelps aaaae CvpontioaUot Cmth UmHed Provfnce: ONTARIO Twp^Arwi: Timmins Area N.T.S.: 4 a A Comgltodby: F. L. J. Drawn by: R. T. M. REVISION DATE odd DON Oct. 96 BY R. T. M. LITTLE DUF F PROJECT Timmins Ar 93, Ontario GRID LO( CATIONS Jk s LD21 Durjdorvakd DATE RLE No. Mar.9S pnoj. NO. 240 SCALE as s hown FIGURE 2 Evelyn Frederick House Late

51 Ontario Ministry of Northern Development and Mines Report of Work Conducted After Recording Claim Mining Act Transaction Number Personal information collected on this form is obtained under the authority of the Mining Act. This information will be used for correspondence. Questions about this collection should be directed to the Provincial Manager, Mining Lands, Ministry of Northern Development and Mines, Fourth Floor, 159 Cedar Street, Sudbury, Ontario, P3E 6A5, telephone (705) Instructions: - Please type or print and submit in duplicat0 - Refer to the Mining Act and Regulations ' Recorder. - A separate copy of this form must be cor - Technical reports and maps must accomf - A sketch, showing the claims the work is ' EUU" 42A14SE0038 W o-oo456 MANN --~ 90Q Ftecorded Holder(s) Address 9/2- f*6 St- W-, oa/ M5H lil of Client No. Telephone No. Mining Divtoion TowViship/Area M or G Plan No. Dates Work Performed From: Work Performed ( Check One Work Group Only) Work Group Geotechnical Survey Type Physical Work, Including Drilling Rehabilitation Other Authorized ^ Work "- Assays Assignment from Reserve JVi'l/fiU) (GdJk/ifirf*) J f ECTION 18 ONLY Total Assessment Work Claimed on the Attached Statement of Costs /O /t Jr- '? Z. Note: The Minister may reject for assessment work credit all or part of the assessment work submitted if holder cannot verify expenditures claimed in the statement of costs within 30 days of a request for Persons and Survey Company Who Performed the Work (Give Name and Address of Author of Report) Driue (MtidUl Name Address 70 fiat St ti'rkfoxj lafa. M ft*/ /A/ 3 f ^ the recorded verification. RECORDED (attach a schedule if necessary) Certification of Beneficial Interest * See Note No. 1 on reverse side l certify that at the time the work was performed, the claims covered in this work report were recorded in the current holder's name or held under a beneficial interest by the current recorded holder. Date MM 9, /t 1QQR JUi. l 330 Receipt ^.^ Recortfe3 Holder or Agent (Signature) Certification of Work Report l certify that l have a personal knowledge of the facts set forth in this Work report, having performed the work or witnessed same during and/or after its completion and annexed report is true. Name and Address of Person Certifying Telepone No. Date 'J.,.... r Certified By For Office Use Only Total Value Cr. Recorded Date Recorded Deemed Approval Date Mining Recorder i m l" "' JUL 84 Date Notice for 'Serif 0241

52 Ontario Ministry of Northern Development and Mines Ministere du Developpement du Nord et des mines Statement of Costs for Assessment Credit Etat des couts aux fins du credit devaluation Transaction No./N 0 de transaction Mining Act/Loi sur les mines Personal information collected on this form is obtained under the authority of the Mining Act. This information will be used to maintain a record and ongoing status of the mining claim(s). Questions about this collection should be directed to the Provincial Manager, Minings Lands, Ministry of Northern Development and Mines, 4th Floor, 159 Cedar Street, Sudbury, Ontario P3E 6A5, telephone (705) Les renseignements personnels contenus dans la presente formule sont recueillis en vertu de la Loi sur les mines et serviront a tenir a jour un registre des concessions minieres. Adresser toute quesiton sur la collece de ces renseignements au chef provincial des terrains miniers, ministere du Developpement du Nord et des Mines, 159, rue Cedar, 4e etage, Sudbury (Ontario) P3E 6A5, telephone (705) Direct Costs/Couts directs Type Wages Salaires Contractor's and Consultant's Fees Droits de I'entrepreneur et de I'expertconseil Supplies Used Fournitures utilisees Equipment Rental Location de materiel Description Labour Main-d'oeuvre Field Supervision Supervision sur le terrain Type MM feotp ' Type Type Amount Montant iltfb IHM- 3?? Total Direct Costs Total des couts directs Totals Total global /J,67/ 8ft 9lto t*9. 9ti 2. Indirect Costs/Couts indirects * * Note: When claiming Rehabilitation work Indirect costs are not allowable as assessment work. Pour le remboursement des travaux de rehabilitation, les couts indirects ne sont pas admissibles en tant que travaux d'evaluation. Type Transportation Transport Food and Lodging Nourriture et hebergement Mobilization and Demobilization Mobilisation et demobilisation Description Type tfucv*4(!3 (J faafc Amount Montant tf*28 /3t Sub Total of Indirect Costs Total partiel des couts indirects Amount Allowable (not greater than 20Vt of Direct Costs) Montant admissible (n'excedant pas 20 "ft des couts directs) Total Value of Assessment Credit Valeur totale du credit Total of Direct and Allowable d'evaluation indirect costs) ftotal des couts directs et Indirects admlssibles Totals Total global Y, f 2-8 /3(p W( V ' /67.tf2 Note: The recorded holder will be required to verify expendijures claimed in this statement of costs within 30 days of a request for verification. If verification is not made, the Minister may reject for assessment work all or part of the assessment work submitted. Note : Le titulaire enregistre sera tenu de verifier les defenses demandees dans le present etat des couts dans les 30 jours suivant une demande a cet effet. Si la verification n'est pas effectuee, le ministre peut rejeter tout ou une partie des travaux devaluation presented. Filing Discounts 1. Work filed within two years of completion is claimed at o of the above Total Value of Assessment Credit. 2. Work filed three, four or five years after completion is claimed at 50 0Xo of the above Total Value of Assessment Credit. See calculations below: Total Value of Assessment Credit Total Assessment Claimed x 0.50 = Remises pour depot 1. Les travaux deposes dans les deux ans suivant leur achievement sont rembourses a o de la valeur totale susmentionnee du credit d'evaluation. 2. Les travaux deposes trois, quatre ou cinq ans apres leur achievement sont rembourses a 50 "/o de la valeur totale du credit d'evaluation susmentionne. Voir les calculs ci-dessous. Valeur totale du credit d'evaluation y-' :-i ;!) Certification Verifying Statement of Costs l hereby certify: that the amounts shown are as accurate as possible and these costs were incurred while conducting assessment work on the lands shown on the accompanying Report of Work form. Attestation de l 'etat des couts J'atteste par la presente : que les montants indiques ces depenses ont ete engagees pour effecfuwle's~travab*-*^ vakw tion sur les terrains indiqu6s dans la formule de rapport de travail ci-joint. that as (Recorded Holder, Agent, Position in ' ipany) l am authorized Et qu'a litre de. je suis autoris6 (titulaire enregistre, representant, poste occup6 dans la compagnie) to make this certification a faire cette attestation (04/91) Nota : Dans cette formule, lorsqu'il designe des personnes, le masculin est utilise au sens neutre.

53 1511 Q S. c 3 3 W O" 8 O S D 73 II (B 3 JSS" CO c 2 nfo g w" 3" "* gf o E. 3 C. O (D X) 0 O Claim on this Work Done Assessment Value of O S- Q o-o g: (B (t Q. 3 S' g S O Ul 32. (O 3 fi a. i: 3 ^s 3 ^ Si Credits you are claiming in this report may be cut back. In order to minimize the adverse effects of such deletions, please indicate from which claims you wish to priorize the deletion of credits. Please mark (^) one of the following: 1. D Credits are to be cut back starting with the claim listed last, working backwards Credits are to be cut back equally over all claims contained in this report of work. 3. D Credits are to be cut back as priorized on the attached appendix. In the event that you have not specified your choice of priority, option one will be implemented. Note 1: Examples of beneficial interest are unrecorded transfers, option agreements, memorandum of agreements, etc., with respect to the mining claims. Note 2 : I f work has been performed on patented or leased land, please complete the following: l certify that the recorded holder had a beneficial interest in the patented or leased land at the time the work was performed. Signature Date

54 t. FROM DISPOSITION w., 01 l O iw.r.o. MINING RIGHTS ONLY " S.R.O. -- SURFACE RKHTS ONLY M.-I S. -- MINIW AND SURFACE r.jqhts OMcriptien Order No. Dtt* Distortion FiU W iif/jii I*** vml fi 11 W.O. 87 / S7 UNUER ste iron ae of Tie man ACT ( OCTOBCH 19.18ST ) M. B. B94B53. SURFACE WO MMMO RIGHTS RE-OPENED TO PROSPECTING. STAKM8 OUT. SALE OR LEASE UNDER SECTION 36 OF THE MMM8 ACT IU.O. IMO EFFECTIVE SO-SEP-O8 AT 7AM EJ.T ORDER NO. 0-P 4/SO NR DATED 9O-AUG-2Z. 890*30* 890B9O N I20O9? I20O927 eeeot- 11^) j K UNITS) l. l HM'76 l [5^^, ^1 l (8 UNITS) VI C l H"" OA-s TRM;-s, *!D ftlutl No ruhvi RDLINkS TOVNSHMC. GASf LIN-: ~. 6TC!OrS. MINING CLA. -IS...- -'S. ETC LO' LINES P--\RCfL MINING' RAILWAY/r O RICH OF WAIT UTILITV LINES NON PtRcNulAL S'l I.EAM FLOODING CM F l.o' '-.ivg fllcmts SUBDIVISION OR COWPf-JITt PLAN RESERVATIONS ORIGINAL SHORELINE MARSH OR MUSKEG MINES RAVERSE MONUMENT *-"*l IE * NOTE* PI PLOTTED IN ERF f - S /B PI k P ypw " I2009I P ^ ~ ~ ~ ~" ' IIITllia k -- m^*a^fc " "~^^^^^^.jl^x nmvu f -utuoa (8 UNITS) I20O906 lgoq9q DISPOSITION OF CROWN LANi TYPE OF DOCUMENT PATENT. SUHFACE ft MINING RIGHTS. ". SURFACE RIGHTS ONLY.... MINING RIGHTS ONLY..... LEASE. SURTACE 4 MINING RIG *TS. ".SURFACE RIGHTS ONLY MINING RiwMTS ONLY.... iff w/"* 'IT'1 IDA r i Si M ei! - l p rttteet l20ltob QI ORDER IN COUNCU. RESERVATION... CANCELLED..._ SANP ft GRAVEL..^...,....._... LAND USE PERMIT- - - NOTE: MINING RIGHTS IN PARCELS F*TENTED fhio 'i T, VESTED IN ORIGINAL PATENTLF 8 V - *. LANDS ACT. R.S.O. 197O. CHAT MO. SEC. (J. SUB;.H C " e r e l Lae (12 UNITS) L.U.P. sou 10 M^fcaf jfc j*^ HI*LIUV l I30I&07 (16 UINITS) UNITS) ^ipiit * r 3 v m m H O M li /J SO* O SNOWMOBILE TRAIL ( LAND USE PERMIT ) NOTICE RECEIVED 92-DEC-09 SCALE 1:20 OOO f " 98-e^ft *as8m-! (2 UNITS), ^Jb i lil CO "D ! 44' otl (4 UNITS) IN) j\5 44*090 II 4H67I (16 l ^ITS) nice.i 01 OJ Oi l o THE INFORMATION THAT APPEARS ON THIS MAP HAS BEEN COMPILED FROM VARIOUS SOURCES, AND ACCURACY IS NOT GUARANTEED. THOSE WISHING TO STAKE MIN ING CLAIMS SHOULD CON SULT WITH THE MINING RECORDER, MINISTRY OF NORTHERN DEVELOP MENT AND MINES. FOR AD DITIONAL INFORMATION ON THE STATUS OF T*'E LANDS SHOWN HEREON. TOWNSHIP W4W ' s UNITS H98SCI H UNITS noag*)o e UNIT TOWNSHIP MANN M.N.R. ADMINISTRATIVE DISTRICT COCHRANE MINING DIVISION PORCUPINE f AND TITLFS/ REGISTRY DIV 31' V COCHRANE Ontario o* t Ministry of Natural Ministry of Northern and Mine., G i.-y 42A14SE0038 W S6 MANN 200

55 REFERENCES AREAS WITHDRAWN FROM DISPOSITION M.R.O. - MINING RIGHTS ONLY S.R.O. - SURFACE RIGHTS ONLY M MINING AND SURFACE RIGHTS DMCriptlon Order No. Dart Dtaporition Fit* SEC. 8*X*0 W. 1/80 8/8/SO M * S. nut* a 8u*f*ec memo WITHMMWN unotn ^01*8*1 ac REOPENED FEBRUARY VB89 ORDER NO. O-J" 2/8*1* f BA44 jm~. l REAUME TP. HIGHWAY AND ROUTE No. OTHER ROADS TRAILS LEGEND SURVEYED LINES: TOWNSHIPS, BASE LINES, ETC. LOTS, MINING CLAIMS, PARCELS, ETC. UNSURVEYED LINES: LOT LINES PARCEL BOUNDARY - - MINING CLAIMS ETC. RAILWAY AND RIGHT OF WAY -* UTILITY LINES -1 NON-PERENNIAL STREAM FLOODING OR FLOODING RIGHTS t SUBDIVISION OR COMPOSITE PLAN RESERVATIONS ORIGINAL SHORELINE MARSH OR MUSKEG MINES TRAVERSE MONUMENT r/r/s////?/?////////////. K Subdivision of this township into lots and concessions was annulled May 10,1963. (O < o J*" ~*. fc - -v ~. ^t -^ ^P* ^f ip ^P TP 'IftpfMT^ft tf**mj*m*l.mkttaiuik. I^WV***/ T4* IIVC^^^^V^ l IV/KiVlfW^ l l t ^^^^i^h*h \iwvn-w iiw l\Jb^^wtf^Jj*4 "** ***J^"*^J "P GL : 4- DISPOSITION OF CROWN LANDS TYPE OF DOCUMENT SYMBOL PATENT. SURFACE 81 MINING RIGHTS-_.... * ".SURFACE RIGHTS ONLY._.... O ".MINING RIGHTS ONLY..... O LEASE. SURFACE ft MINING RIGHTS B ".SURFACE RIGHTS ONLY._ B ".MINING RIGHTS ONLY..._._ B LICENCE OF OCCUPATION T ORDER-IN-COUNCIL... _. OC RESERVATION _..._. (J) CANCELLED......, SAND 8. GRAVEL......_._... (J) LAND USE PERMIT. : ^f J*5HLM! NINGLRJS.HTS I N P ARCELS PATENTED PRIOR TO MAY c. *r^^r"^gtsrvts^id~iktbff^inat"^a'tkeftel BY THE PUBLIC LANDS ACT. R.S.O CHAP. 3BO. *fc. 63, 8UBSEC t. REMOTE TOURIST snr ^. 4BP SCALE: 1 INCH ~ 40 CHAINS FEET O SAND ond GRAVEL QUARK Y PCRKUT ifmigim- i lamflh^-^^liauk lotwfl^p* 'i^ cwm i V ~~ ~t ~ ~-\z- fcr^409ilia^ i(o3ifk)4 jfowsocy l j "Se i - \,s~"'- I******i. -A^ - ~ - ^^ ** -*^ ^ vaji*. i. l * JHWwaft*-/ J Tinea. ^- O 200 METRES 1000 (1 KM) 2000 (2 KM) ra*' TOWNSHIP THE INFORMATION THAT APPEAM 01 TM(8 MAP HAS BEEN COMPILED AMD ACCUIWCY * NOT GUARANTEED. THOSE WISHIHa TO STAKE Ml**- ING ajjm*shqutp CON SULT WtTH trtfrjgnins RGQOAOfen, MBNIfflWY OF NORTHERN Df ON LANOS 8MOWN HCRtOR BUNTrt) -'leneff 'l P j- p '.(12 UNITS) l '219219, ^mt 4ltt1M j (16 i IIWWVKA^ l W* W*. W W l J L 1-- r, ID IP ^if-iirx jwiiki 10*** man mtant - ^- \ I T... N^,.^g. ^^^.^^. j-^fc^* ^ l^cwm^* ^BlBf4BT^^AAft4'^r* ^Wov^V'^W9PV9l ""J*'*-" 'L ' "T'-^ ' L jv r.^--4 v*-.^.. h---- V I iujui^liy^.y i^t'^^r***84* l X'i j (9 UNITSl - ^ l t ^ l BK ^l^fc\ l TULLY TP. V X \. \ S. E. CORNER CO-ORDINATES "^ (Aaorox.) (Approx.) LAT. 48" 47' 50" DEP. 81" 04' 28" DUFF M;N.R. ADMINISTRATIVE DISTRICT COCHRANE MINING DIVISION PORCUPINE LAND TITLES/ REGISTRY DIVISION COCHRANE Ontario Dit* MARCH, 1985 Ministryof Land Natural Management Resources Branch G A14SE003B W MANN 210. f * -g