wagg mineral exploration and consulting inc. · 2017-01-17 · to values strongly anomalous in gold...

52F05SE2001 2.18206 ROWAN LAKE 010

Report of Mechanized Strippingat the

Fairservice Option Cameron-Otterskin Lakes Area

Kenora Mining DivisionNTS 52 F/4, F/5

Prepared for Nuinsco Resources Limited

WAGG Mineral Explorationand Consulting Inc.

November?* 1997.

52F05SE2001 2.18206 ROWAN LAKE o A flp

TABLE OF CONTENTSPage

Introduction......................................................................................................... 1

Location and Access........................................................................................... 1

Geology............................................................................................................... 2

Stripping Program............................................................................................... 3

Sampling Program.............................................................................................. 5

Discussion.......................................................................................................... 5

Recommendations.............................................................................................. 7

References.......................................................................................................... 8

Certificate of Qualifications................................................................................ 9

LIST OF MAPS

Map 1. Plan of Sampling Peripheral to Stripping, Fairservice Option............. back pocket

Map 2. Plan of Sampling at Stripped Gold Showing, Fairservice Option........ back pocket

APPENDICES

Appendix 1. Sample Locations and Descriptions............................................... 10

Appendix 2. Assay Certificates.......................................................................... 13

Appendix 3. Summary of Expenditures............................................................. 25

Introduction

A program of overburden stripping was recently completed by Nuinsco Resources Limited, at a gold occurrence rediscovered by Bob Fairservice, a Kenora based prospector, on claims staked and recorded in his name, located about 8 km southeast of Nuinsco's partially developed Cameron Lake gold deposit. Following an initial inspection of the gold showing by Laird Tomalty, a Nuinsco employee entrusted with care and maintenance of the Cameron Lake facilities, the Fairservice property was subsequently acquired under option by Nuinsco.

Initial examination of the showing by Mr. Tomalty in the Spring of 1997 revealed reasonably strong and pervasive iron carbonate alteration throughout an area of limited bedrock exposure, with local quartz- carbonate veining and stringer development which exhibits minor disseminated pyrite within and alongside the veined areas. As well, small to large blocks of broken vein material were noted along the course of a debris filled, northerly trending, bedrock trench, which leads into a water-filled blasted pit measuring approximately 2.5 m square. The pit, which is situated at the northern limit of the area later stripped, appears to have been excavated certainly prior to 1970, and perhaps as early as the 1930's. The results from about a dozen samples collected by Mr. Tomalty during the period of due diligence ranged from trace levels, to values strongly anomalous in gold (< 0 1 oz./ton; < 3 g/t).

In early October, the author was contracted to oversee a program of overburden stripping and bedrock sampling in the vicinity of the gold occurrence, in order to ascertain:

1. The significance and extent of the gold mineralisation present, and whether or not it is structurally controlled.

2. The relationship of the showing to local geological features; i.e. is the mineralisation confined to a particular lithological unit, or may it occupy a zone which crosscuts bedding within the metavolcanic stratigraphy?

Location and Access

The property is situated in the Kenora Mining Division of Ontario, approximately midway between the towns of Fort Frances and Kenora. It is comprised of the following contiguous mining claims: 1178315, 1178328, 1178329, and 1178330, totalling 50 individual claim units, for an approximate contained area of 800 ha (2000 ac.). The claimgroup is roughly square and lies along the southern boundary of National Topographic System map sheet 52 F/5, with three units of claim 1178315 extending into the extreme northern portion of map sheet 52 F/4. The boundary between the two NTS sheets coincides with the boundary between the applicable claim maps for the area, Rowan Lake (G-2639) to the north, and Brooks Lake (G-2670) to the south.

The property is road accessible via the Cameron Lake Road, which departs easterly from Provincial Highway #71, a short distance south of the community of Sioux Narrows. The road is privately owned by Nuinsco Resources for the first 24 km of its length, at which point the Cameron Lake facilities are reached. A further distance of 13 km of road travel is necessary in order to reach the recently stripped area, which requires the permission of a local logging contractor, Mr. Dave Burt of Sioux Narrows. A short spur road branching southerly (to the right), at about the 12.2 km mark beyond the minesite leads to within a few hundred metres of the stripped area, beyond which the access trail to the area is suitable only for heavy equipment or ATV travel.

At Nuinsco's request, Mr. Burt supplied equipment and personnel in order to construct a portion of the spur road, clear the access trail, and undertake preliminary work at the showing .which included the removal of forest cover and the bulldozing of overburden, to depths of up to two to three metres in places, in areas where bedrock topography was such so as to make this type of work practical.

As the focus of the present program was primarily to strip and sample the vicinity of the known gold mineralization, no systematic examination of the geology of the remainder of the property was undertaken. However, it is evident from brief examination of outcrops along the spur road leading to the stripped area, that a number of differing metavolcanic lithologies are present in the general area.

Geological mapping as well as ground magnetometer and VLF-EM surveying was completed over part of the present property in 1984, for Golden Transit Resources Inc. A copy of assessment work filed at that time was made available to the author by Bob Fairservice.

The geology map produced in 1984 shows at least four significantly different rock types occurring in the vicinity of the area stripped during the present program. They are pyroclastic (tuff-breccia?) and amygdaloidal andesites, massive and tuffaceous dacites, and massive and tuffaceous rhyolites. As well, all noted exposures of sericite schist were mapped and interpreted as altered rhyolitic rock. Observations made in the vicinity of the showing, by the author of this report, conflict markedly with those presented on the geology map produced in 1984 by L.J. Nelson for Golden Transit Resources. Additionally, many sizeable natural outcrops in the vicinity of the showing have been misidentified, or simply do not appear on the map. This is despite the fact that low concentrations of gold are mentioned to occur in veins and wallrocks around the trench and pit, and presumably the area would have been investigated in some detail.

It was noted during the present work program that rock units of probable tuffaceous origin appear to be transitional between andesite and dacite, differing only subtly from andesitic flow rocks, with the primary difference being a tendency for the tuffs (my dacite tuff) to weather more whitish on the outcrop surface, be it either exposed or shallowly covered. Also, at a few locations along the spur road to the showing, but well removed from it, it could not be determined whether or not poorly exposed rocks of intermediate composition were extrusive rocks, or rather, fine grained dykes. Contacts were not exposed, and time- consuming manual stripping in order to produce a better exposure was deemed not to be worthwhile.

Observations made along the spur road about 400 metres to the north of the showing reveal a sequence of pillowed mafic flows, with pillow flattening oriented 090 to 100 degrees and dipping subvertically to 60 S. Pillowed units are separated by amygdaloidal flows of similar composition, mafic lapilli tuffs, tuff-breccias containing intermediate to felsic fragments, and occasional intermediate tuffs. Units other than the broadly andesitic pillowed and amygdaloidal flows are often only one to two metres thick in the area studied, however, the orientation of geological contacts appears to be fairly consistent, ranging from around 085 degrees to about 110 degrees. Similar strikes and dips were measured at well exposed contacts far removed from the stripped area as well, on single traverses made both to the east and to the west of the showing. Foliation measurements also varied from place to place, but commonly dipped subvertically with strikes falling within the 085 to 110 degree range.

One gabbro dyke oriented 350/70 SE was encountered, well to the west of the showing, but it might well be occupying a crosscutting fault or fracture trend. Overall it seems probable that rock units trend east- westerly throughout the area, although lithological contacts may be somewhat undulatory, and upright tight to isoclinal folding may be responsible for the steep north to steep south dips recorded from place to place. It appears that foliation closely parallels bedding.

It would also appear that there is a great deal of complexity present within the part of the property examined to date-lithological if not structural-and that outcrop density in the area is insufficient to provide an adequately clear picture of the distribution of individual flows/units, which is necessary for an accurate interpretation of the local geology.

Outcrops in the area surrounding the stripped showing, and samples collected peripheral to the known gold bearing zone appear on Map 1, at the back of the report. The few samples collected elsewhere from the property are listed in table form in Appendix 1, which provides a brief description of each sample collected

during the program, and gives their locations in either local grid coordinates, or in GPS coordinates for those which do not plot on the maps.

Stripping Program

As mentioned, the initial stripping around the area of known gold mineralization was accomplished by means of a D7 bulldozer. This phase of the program totalled 53 hours, at an hourly rate of $ 85.00 including the operator's wages, and concluded October 8th, the day of the author's arrival on the property From October 9th through to October 27th, a much smaller bulldozer owned and operated by Laird Tomalty of Nestor Falls (John Deere 350C with a rear mounted backhoe) was employed for a total of 1 00 hours at an hourly rate of $ 55.00 including the operator's wages, plus $600.00 in transportation charges, for moving the machine by lowbed to and from Nuinsco's Richardson Township property, located 55km, as the crow flies, to the southwest. This machine was particularly well suited to the bedrock topography since it could fit into the depressions between shallowly covered bedrock "subcrops" exposed by the larger D7. The approximate 50 cm bucket width of the backhoe was also useful because of the uneven to jagged surface of much of the deeply buried bedrock surface. The backhoe succeeded in removing most of the debris from within the trench extending southward from the pit, leaving it reasonably clean. For the duration of the program, from October 7th to October 29th, the author was provided with accommodations at the Cameron Lake minesite, with the exception of two days spent elsewhere on an unrelated property evaluation.

Due to the uneven nature of much of the bedrock surface, considerable shovel work was required in places in order to prepare parts of the area for proper mapping and sampling. Although it would have been of tremendous assistance to have had a properly washed weathered surface to examine in order to determine rock type, no outcrop washing was undertaken on the showing due to the lateness of the season, with temperatures rarely rising above freezing subsequent to October 15th.

An area measuring about 105 metres in length north-south, by 15 metres to 35 metres in width was substantially cleared of overburden. This area is shown in detail on Map 2 (following the report). A smaller area measuring about 15 metres in diameter (which appears on Map 1), referred to as the Eastern Stripped Area, was also cleared, but was in part quickly covered by water due to heavy rainfall the first few days of the program.

Stripping at the main area revealed widespread intense iron carbonate alteration of amygdaloidal andesite flow rocks. Foliation within the unit is about 085 degrees with dips from subvertical to 70 degrees to the north. Two major east-westerly trending shear zones are presently reasonably well exposed, however, since they form recessive topographic features, they are partially mud and water covered. A large number of minor (strong, but narrow) shears were also revealed. Most are parallel to subparallel to the major shears, but a few are oriented at about 065 to 075 degrees or at about 355 degrees, both orientations which are parallel to prominent fracture sets present within the stripped area.

The shears are fissile, deeply weathered zones, exhibiting moderate to strong sericite and chlorite alteration, but which appear to contain only trace to 1% fine disseminated pyrite on average. Fabric measurements are variable from place to place within the two major shears, with both strikes and dips displaying a range of about 20 degrees. Average measurements are about 085/80 N and 095/60 N for the northern and southern shear zones respectively. Alongside both zones on the footwall side, strong pervasive carbonatization can be seen across several metres, but with little evidence of shearing or mineralisation. The intervening andesite between the two zones, and indeed the entire stripped area, exhibits moderate calcite alteration.

Veining is concentrated within three discrete areas. Within the southern shear zone, it appears that a sizeable shear-parallel vein, about 30 cm in width, ran most of the length of the north facing outcrop edge. Although bulldozer and backhoe work removed much of it that occurred above the present waterline, many slab-like blocks up to a metre in diameter can be observed in rubble piles towards its western end. A possibly sub-horizontal vein occurs in the central part of the broad exposure of this shear zone, where

sample 23943 contained about 80% vein material. Shear parallel and crosscutting stringers, from 5 mm to 20 mm wide occur in places within the zone, as noted in samples 23940, 23949, and 23951. The many interconnected stringers present in these samples suggest a recemented shattered rock, which for lack of a better term will be referred to as a quartz stringer breccia.

These veins, and those described in the following paragraphs, consist mainly of white medium grained quartz, with at least a few percent, and often up to 10-15%, fine to medium grained whitish to brownish crystalline iron carbonate minerals, and generally about 1% scattered small pyrite crystals, with only very rare traces of chalcopyrite or malachite. A feature common to the veins is the presence of narrow laminae to a few millimetres wide composed of sericite, chlorite, +/- talc. The laminae are relatively planar, and appear to parallel vein contacts. They may occur singly or as closely spaced parallel seams. It seems unlikely that they are altered inclusions of wallrock, and more likely that they are shear planes or fractures along which alteration minerals have been introduced. Within some samples exhibiting elevated pyrite content, sulphide mineralization is noticeably concentrated along these features. In rare instances, such as sample 23950, narrow seams of pyrite occur in a similar fashion.

The second area of substantial veining is found along the eastern edge of the most southerly large outcrop in the area. Much of the vein material occurs off the outcrop to the east and is partially obscured by mud and rubble. A few vein-like bodies run in a general east west direction with steep, but irregular dips. Most veining, however, occurs as pods or lenses, perhaps occupying dilation zones resulting from the strong shearing and fracturing in the surrounding rocks. Pyrite was observed at levels up to 5% as fine to medium grained crystals in wallrock immediately adjacent to vein material (sample 23932). At the northeastern tip of this large outcrop, at about 0+83 S, BL, a quartz breccia occurs along the southern edge of the southerly major shear zone. Here the host rock has essentially been replaced by fine grained carbonate, then apparently shattered and resealed by an irregular mass of quartz measuring 3 m to 4m in length, and 1.5 m to 2 m in width. Pyrite levels reach 5%-7% within both vein and hostrock material, and there is a possibility that this may be a pipe-like structure, probably plunging steeply to the northeast.

The third and final area of substantial veining runs from the pit, at the northern limit of the stripping, southward to the point where it meets the northerly of the two major shear zones. A single vein which pinches and swells somewhat extends over much of this 30 m length. It ranges from 10 cm to 15 cm in width at its narrow points, up to 50 cm to 60 cm in width at its widest point. Its predominant orientation is 034 degrees, dipping 75 degrees southeasterly. At the lip of the pit, veining occurs as several parallel veinlets, each about 10 cm wide, within well sheared, but competent rock. One veinlet displays a tight fold nose of surprisingly regular and uniform thickness. At one point about twenty-two metres further south, the vein is pinched off and offset a few metres along a fault trending 357 degrees, with an apparent near vertical dip.

Net left-lateral movement is evident along the fault structure, however, it could not be traced with any certainty across the remainder of the stripped area. Here, and at most points along the vein's hangingwall contact, a 10 cm to 20 cm wide zone of "talc-rich, fault-gouge mush" is conspicuous. The material is a very whitish mud-like substance below a depth of a few centimetres, contains small quartz granules and larger angular pieces of quartz to about a centimetre in diameter, and dries to form a soapy, powdery residue on the hands. The presence of this material implies movement subsequent to the formation of the vein, and suggests that the vein may occupy a structure initially opened by a brittle failure of the hostrock.

A shear fabric or deflection of foliation is evident in wallrocks along both sides of the vein. The feature swings to the right as it approaches the trench lip on the far side of the vein from the viewer implying left- lateral displacement along the length of the vein. The fold nose mentioned earlier, and the vein offset along the fault striking 357 degrees confirm this sense of motion. As well, where the southern end of the vein meets the northerly major shear zone, the vein can be seen to be folded to the left and boudinaged, suggesting left lateral movement within the shear zone, and perhaps that the vein predates or was coeval with development of the shear.

Sampling Program

A total of 115 rock samples were collected from the Fairservice Option property over the course of the stripping program. All samples are briefly described in Appendix 1. Of the 113 sample total, 78 were collected from within the boundaries of the stripped area, or immediately adjacent to it, and are plotted on Map 2. A further 24 samples were collected from the area surrounding the stripping, and are plotted on Map 1, including 7 samples from the small eastern stripped area. The remaining 11 samples were obtained from areas well removed from the stripped sites.

Eight samples were submitted for wholerock and trace element geochemical analyses in order to help properly identify rock type, or in order to characterize the nature and degree of alteration to which the sample had been subject. Two particularly well mineralised samples numbered 71412, and 71419 were submitted for 32 element analyses by ICP methods. They contained up to about 10% sulphide mineralisation, presumed to be pyrite, but exhibited dodecahedral crystal outlines (12-sided). Although this crystal form is not extremely rare for pyrite, it is fairly uncommon, however, it seems unlikely to be of particular significance with respect to the presence or absence of gold values in the area.

The remaining samples were analysed for gold only utilizing traditional fire assay methods with an atomic absorption (AA) finish, with all of the analyses conducted by Chemex Labs of North Vancouver, British Columbia.

Sample types collected in the field were standard and selected best grab samples, and representative composite or chip samples. Standard grabs were typically one or more pieces of rock obtained from a small area measuring about 15 cm3, while selected best grabs, rather than being high-graded for mineralization by means of collecting a number of small chips, were similar to standard grabs, but were obtained from an area selected because it exhibited elevated levels of mineralization. Representative chip samples were typically collected by means of hammer and chisel, and were as closely as possible a continuous section taken so as to mimic that which would be obtained in a sawn channel sample. Composite grab samples are similar to chip samples in that they attempt to represent an average grade of the material being sampled, where chip sampling is impractical. Composite samples were often collected from loose blocks of vein material, or at several points along the length of a small veinlet.

The bulk of the samples collected duing the stripping and sampling program returned gold values below the detection limit of 5 ppb Au, and many of the remainder returned only weakly anomalous values of less than or equal to 50 ppb Au (0.05 g/t Au). 16 samples returned strongly anomalous gold values, and of those 4 returned values in excess of > 1000 ppb Au (1 g/t Au). Samples which have returned gold values deemed strongly anomalous (>300 ppb Au) appear in bold type on the two accompanying maps, and within Appendix 1.

Discussion

An examination of assay results clearly reveals that strongly anomalous gold values are present in places within the boundaries of the stripped area, and elsewhere on the property. Anomalous levels of gold mineralisation are clustered in the following areas within the area stripped (from south to north): within veins and mineralized wallrocks at the extreme southern end of the stripped area near 1+05 S, 0+05 W; at the exposure of "quartz breccia" near 0+87 S, 0+01W; at the western limit of the exposed portion of the southern E-W shear zone near 0+88 S, 0+25 W; and at several locations along the length of the trenched N- S vein, including blocks of in situ vein material which lay, prior to stripping, a few metres to the north of the blasted pit. The two best assay results of 3000 and 4440 ppb Au, from samples 23961 and 23963 respectively, were obtained from about the midpoint of the north-south trending trenched vein, about one metre apart. The vein is relatively narrow at this point, but contains subequal amounts of pyrite and chalcopyrite at levels of 2-3% apeice, distributed mostly near and along its hangingwall contact. Samples

from other areas of this vein where chalcopyrite was noted did generally not return elevated gold values, implying that the apparent association is coincidental.

A few general conclusions can be drawn, based upon which samples among those collected returned anomalous values. For one, vein material does on occasion return gold values somewhat erratic in nature, with the presence of increased levels of pyrite not necessarily indicating a greater likelihood of correspondingly elevated gold values. This may suggest the presence of native gold within the system of veining. For another, within the strongly altered well sheared material sampled, elevated gold values seem more common within the southern shear zone, and it appears that with increased pyrite concentration, gold content will be proportionally increased from one sample to the next. Therefore, depth of weathering within zones of fissile shearing may give misleadingly high or possibly low gold values from surface samples, unless fresh material is obtained. However, this also suggests the possibility that any chargeability highs detected by an induced polarization (IP) survey might represent bodies of potentially economic gold bearing mineralisation.

With regard to gold values obtained along the length of the north-south trending vein. It would appear that even the best values obtained from the comprehensive sampling completed are only marginally economic, particularly in view of the apparent narrowness and limited known strike length of the body. Nonetheless, the structure appears to have been "long-lived" and affected by several periods of deformation. As such it may be persistent to depth, and offset across its strike by shear zones striking about perpendicular to its trend. As well, if it is viewed more as an indicator of whether or not gold mineralisation is present in the vicinity, rather than as a potential low tonnage orebody, its presence must be viewed as encouraging.

Of the anomalous results obtained elsewhere from the property, a few merit mention. They include a value of 1720 ppb Au returned by sample 71415, collected 40 m to 50 m to the west of the stripped area, roughly along the strike of the southern E-W shear zone, and at about 10 m lower elevation. A 30cm block of loose vein quartz containing 3%-4% fine disseminated pyrite was broken in order to obtain the sample. The block contained chloritic internal slips, and showed chloritized mafic rock along two sides. Several smaller pieces of vein material were noted along the trend of a narrow? shear in mafic rocks, or possibly tuff-breccia. Exposure is poor in the vicinity, and it appeared that there might once have been an east-west trending trench dug in the overburden at the sample site. Also of note is the value of 585 ppb Au returned from sample 487003, taken from a poor exposure about 25 m beyond the westerly limit of stripping, apparently from the same shear structure. The rock at this site also appeared to be a tuff-breccia, moderately chloritized and iron carbonate altered, with pyrite present only locally alongside a few shear-parallel stringers.

Although the vein material at sample site 71415 lacks iron carbonate and exhibits only minor sericite, it is probably related one way or another to the veining and mineralization exposed by stripping. It appears possible that the southern major shear zone may be confined to a poorly exposed unit of tuff breccia, altered beyond recognition (and also oxidized and deeply weathered) within the boundaries of the stripped area. The geology depicted on Map 2 certainly suggests that this may be the case.

A second individual sample deserving of mention is numbered 23928, which was collected from a roadside bedrock exposure reached by travelling about 400 m south along a branch road, from the junction on the main Cameron Lake road prior to the turn which leads to the stripped area. Comments recorded in field notes can be summarized as follows. A narrow carbonate altered shear zone trending 037/65-70 SE occurs along the contact between coarse grained massive mafic volcanics and a fine grained gabbro. Sample 23927 is representative of the best altered and mineralised portion of the zone. It contained 1% fine disseminated pyrite, several narrow quartz stringers, and a 5 cm to 7 cm wide veinlet which seemed to persist for some distance. As well, the sample contained traces of a silver-coloured, acicular to bladed metallic mineral, within a stringer and in the bleached wallrock alongside. The mineral might be rutile or some type of antimony or bismuth mineral. Sample 23927 returned a value of only 80 ppb Au. Sample 23928 was a grab from an 8 cm wide less attractive quartz vein, which contained minor clusters of chlorite and calcite and traces of pyrite, occurring along the footwatl of the shear zone.

The zone itself seems to hold little economic potential due to its apparent small size, however, it is readily accessible and could easily be stripped along strike to the southwest. More importantly, it is some evidence that the margins of gabbroic intrusives may hold potential for gold mineralisation hosted by zones of shearing and alteration.

It would therefore appear that the remainder of the Fairservice Option property is prospective for shear- hosted gold mineralisation similar in nature to that exposed by the stripping program.

Recommendations

1. Further stripping, outcrop washing, and perhaps limited bedrock trenching should be undertaken at the known gold occurrence on claim 1178315, in order to confirm or broaden the understanding of the geology of the immediate area.

2. An induced polarization survey, or at the least several closely spaced lines of VLF readings should be completed over the area of the gold occurrence. A second set of geophysical survey lines in an east-westerly orientation should be given consideration.

3. Should mapping and prospecting across the remainder of the property be undertaken, it is essential that grid lines be cut in order to facilitate crew movement from place to place, and in order to provide some control on the positioning of outcrops and sample locations on maps.

REFERENCES

Nelson, L.J., 1984. Report on the Geology of the Property of Golden Transit Resources Inc., Area of Nolan-Otterskin Lakes, Kenora Mining Division, NTS 52 F/5, 4p., 1 map: 1 inch:200 feet.

CERTIFICATION

I, Christopher A. Wagg, residing at R.R. #1, in the village of Denbigh, Ontario KOH ILO, do hereby certify that:

1. I hold a Bachelor of Science Degree in Honours Geology, conferred in May of 1989, at the University of Western Ontario, in London, Ontario, Canada.

2. I have been self-employed as a geological consultant since 1987, have been practicing my profession continuously as a consulting project geologist since 1989, and have operated my business as a private Ontario Corporation since November of 1991.

3. My Report on the Fairservice Option property is based upon a personalexamination of the area described, over the course of about 19 days of fieldwork completed between October 8th and October 29th, 1997.

4. My report on the Fairservice Option property has been written in all respects as an independent consultant.

5. I presently hold 2 900 shares of Nuinsco Resources Limited within a SDRRSP account, purchased for their medium to long term appreciation potential, but have no direct interest in the Fairservice Option property itself, or in any other properties in close proximity.

Dated this 7th of November, 1996, at Emo, Ontario. Christopher A. Wagg^RSc.

Ion and Consulting Inc.

APPENDIX 1

Sample # Description Pyrite Content Location(lengths in cm) (vein and stringer measurements are widths) (GPS:E,N or local grid)

23903239042390523906239072390823909239102391123912239132391423915239162391723918239192392023921239222392323924239252392623927239282392923930239312393223933239342393523936239372393823939239402394123942239432394423945

G St. carb alt'd, well fol'd maf-int mvolc rubble. TrG Sim. to prev., int. alt. int tuff. 1-2% qtz str (qs). TrG Similar to previous. 30cm to N. TrG Similar to previous. ImtoW. Tr-1%G Wk min. maf tuff at SW corner, last turn to stripping 2-3%G 1m diam. slabs moved for creek cross, fill. Chl,ser,qs 2%CH175 E stripping. Felsic? V. well sh'd, st. carb alt. Fissile TrCH175 Adjoins prev. to NW. V.sim, but likely some ser. TrCH170 Same as prev. Starts 1.5m SW. 50cm pure carb lens Tr-1%CH170 adjoins prev. to NW. 65cm of same folded carb lens Tr-1%G E stripping. Int. carb alt'd + sh'd. 2.5m W of 23909 1-2%G E stripping. Saprolitic shear, 7-8m ESE of 23909 Tr ?CH45 Block of vein mat'l, SW corner of pit. Prior to stripp. 1%SB Same as prev. From ser-chl rich margins, tr cp, py fg 3%

453863, 5455809453863,5455814453863, 5455814453862,5455814

GVein slab 25-30cm thick. Up to 20% carb-ser slips 3-4%, tr ma

4-5%5%, l-2%cp1%

1-2%

Comp Same as prev. Rep. of remainder of slab. 5% fe-carb Tr-1%G Pit "dump". W.rock w wk-mod chl-carb. 15% qc str's<l%G Same as 23919, but fewer stringers, less sulphide TrComp Muckpile. Chl-carb-ser+/-talc to 2-3% in sample 1%, 5% fe-carbG Muckpile. Sil. w.rock +/or diss. chl-amph in fg qtz Tr, 15-20% carb 0+00G Muckpile. Bx'd vein w 20-25% carb str's, tr ser slips TrG "Hostrock". Unmin. wk'ly sh'd, mod'ly carb alt'd Nil-TrG(l 5cm) Mod-st chl-ser alt., anastomosing q-c str's to 3-5cmSB Chl-ser slip surf, w py, cp, ma. Vein has little min.G(25cm) Narrow sh/frac zone. St fe-carb w qs. 037/65-70SEGSame loc. as 23927. Qv to 8cm along f.wall. Vuggy Tr-1%CH60 Main stripping. Sm. sh in carb alt'd maf mvolcCH230 Oblique. 2m t.w. Qtx Bx, S dip? Most min. at NWCH120 Along strike of sm. qtz lens oriented 45 deg to 23930 < 1 %GFist-size. All qtz-carb repl. zone, minor chl-ser slips 5-7%GGGCH100CH100CH300GGCH200CH175CH125CH175CH200

1 st of 3 from series of 2-1 Ocm wide folded-boudin?veinlets with mod-st. chl-carb alt. and wk. ser alt.3 of 3. Here poss. N-S str's. Zone -115/sv to 70NNarrow st. shear. Fissile. 092/sv to 75 NProb. same shear as in 23936, 10m to EAcross main qtz bx o/c + into w.rocks either sideLoose mafic mvolc w wk calc alt. "assay blank"Loose mat'l from under water. Sh'd-ser-talc, wk chl !-2%,35%qc strW'ern end South E-W shear. 5-10% qc str's to 2cm 2-3%N margin of shear. T.w. ~80cm due to slope of o/cOblique 150cm. Adjoins 23942. 115cm length of qvOffset 125cm from prev. Q-c str's, 1 veinlet to 10cm 1-2%Samples gap betw. 943-944. Sm. ovlap poss. w 944 1-3%, 50% qv

-453875, 5455950 no GPS 453657, 5455240 0+3 4S, 0+64E 0+32S, 0+63E 0+3IS, 0+61E 0+30S, 0+59E 0+34S, 0+62E 0+33S, 0+70E 0+02S, 0+00 0+02S, 0+00

0+0IN, 0+02E0+0 IN, 0+02E 0+03N, 0+03E 0+03N, 0+03E 0+00 , 0+03W

0+03W0+00 ,0+03W 0+07S, 0+06W 0+03N, 0+0IE 0+03N, 0+01E Roadside,no GPS

400m S of Cam. Rd1 -2%, <3% qs 0+98S, 0+11W

1+04S, 0+04W 1+02S, 0+03W

1+03S, 0+4.5W0+99S, 0+8.5W 0+98.5S,0+08W 0+98S, 0+7.5W 0+98S, 0+05W 0+98S, 0+00 0+83 S, 0+01W 0+87S, 0+13W

Tr-1%, <5% qvTr2-3%Nil-tr

0+79S, 0+13W 0+83 S, 0+27W

2%,(to 5-7% loc.)0+82S, 0+25W2-3%, 5%carb 0+83 S, 0+23W

0+87S, 0+23W 0+85S, 0+21W

10

APPENDIX 1 cont'd

Sample # Description Pyrite Content Location(lengths in cm) 23946 G(20cm) 10- 12cm wide veinlet w contorted ser-chl-py margin 2-3% 23947 CH200 Midpoint of S sh. 1 m qv w carb, py, 1 m fissile sh 2% 23948 G Fissile, rotten shear w mod-st. fe-carb alt. <!-!% 23949 G V.pale green to beige, qs bx w carb repl'd w.rock 1-2%

(GPS:E,Norloca 0+86S, 0 0+85 S, 0 0+83S, 0 0+82S, 0

23950 G S end of N-S vein. Qv w py to 2mm filling fractures 2%23951 Comp Slabs of vein mat'l-b.hoe work. V. sim. to 2394023952 G Trench NE of pit. 3-5cm veinlet w abund. fe-carb23953 Comp Strong narrow shear across 10-15cm adj. to vein23954 G Sim to 23952, but 20cm wide. 25% fe-carb23955 G Loose qtz along strike of >lm wide sh, some chl-ser23956 Comp Carb-ser alt'd shear beneath fallen tree.23957 Comp Sim to shears at showing. Top of N facing scarp23958 G Loose rock sim to 23957, qs X-cut shear fabric23959 WR Dacite found south of a gabbro. Trav. to W23960 WR Banded Rhy. flow w Gabbro to N, amyg And. to S23961 SB N-S vein. Py + cp diss. and along fractures23962 G(10cm) Sh'd w.rock along h.w. + qs to 2cm Tr-1%23963 GLoose qtz w abund. py along slips +/or f.w. contact 3-4%23964 G E'ern stripping. Sh'd + frac'd carb-ser schist w Rhy23965 CH125 Along well sh'd h.w. w.rock adj. to N-S vein Tr23966 WR 1.5m E of N-S vein. Bleached? Dacitic? white weath23967 WR St'ly carb alt'd unsh'd amyg. Andesite23968 WR Mod'ly calc alt'd mass to amyg Andesite23969 WR Mod'ly carb alt'd Andesite w mod strength fract.23970 Comp Talc-ser mush. From along trenched qv23971 G Pocket of talc-ser mush. Horiz. within vein?23972 G(l 5cm) South end of fault offset. Qtz + talc on both sides23973 CH30 Poorly exp. sh to S of N main sh. 2 sm. q-c veinlets23974 CH160 Adj. to 23973. Massive carb alt. And. w abund. amygTr23975 CH175 Same as prev. no veinlets. 1 qs Tr, tr cp23976 CH200 Same as prev., but tension crack swarms present,x-cutting fabric

at 90 deg. as shear is approached. Minor chl-carb-ser <l%,tr cp23977 CH125 Less frac. than 976. More sh'd, carb-ser+ q-c sir's Tr23978 CH100 Same as prev. Tr23979 G Best section of sample 23976, 1m to E Tr-1%23980 G Best section of sample 23977, 1m to E. 3% str's Tr

0+27S, 0+06WTr-1% 0+79S, 0+13W Tr 0+25N, 0+33E Tr-1% 0+24N, 0+3 5E Tr 0+24N, 0+34E Tr 0+33N, 0+50E Tr 0+3 5N, 0+52E Tr-1% 0+48N, 0+6IE Tr-1% 0+54N, 0+6IE nil lOOmN of post #4-1178315 nil 750m W+50m S of #4-1178315 3%,2-3%cp 0+13 S, 0+05W

0+15S, 0+06W 0+14S, 0+07W

<!-!% 0+26S, 0+65E 0+18S, 0+05W

0+12S, 0+01W 0+4IS, 0+05W 0+55S, 0+10W 0+60S, 0+14W 0+19StoO+25S 0+20S, 0+06W 0+24S, 0+04W 0+43S, 0+02W 0+42S, 0+02W

nilnilnilnilnil?nil?Tr-1%Tr

0+4IS, 0+03W

0+39S, 0+03W 0+3 7S, 0+05W 0+36S, 0+06W 0+37S, 0+03W 0+3 5 S, 0+04W

71401 Comp Random Grabs of fissile shear from water cov. area Tr-1% 71402G Massive amygdaloidal Andesite. No sulphides nil71403 CH100 75% well fol'd, 25% sheared. No sig. qv/qs Tr71404 G White coarse qtz boudin,-20% rotten carb nil-tr71405 GSouthern end of N-S vein. 20cm wide 1-2%71406 G Well sh'd and alt'd. 30% qtz-carb str's/bx Tr-1%71407 G Poorly exp. wk-mod strength sh. Weak chl-ser nil-tr71408 CH200 Well frac. to mod sh'd. S edge s.z. at E'ern stripp.? Tr71409 G Mod sh'd mafmvolc wwkchl-mod calc alt. Tr71410 CH130 V. well sh'd, intensely carb alt'd. Amyg. noted Tr71411 GQtz bx. Just SW of centre of 23938 3-4%

0+30S, 0+15W 0+3 5 S, 0+03E 0+35S, 0+06W 0+3IS, 0+06W

0+29S, 0+05W0+37S, 0+08W 0+48S, 0+45E 0+44S, 0+38E 1+20S, 0+45E 1+01S, 0+08E

0+87S, 0+04W

11

APPENDIX 1 cont'd

Sample # Description Pyrite Content Location

71412 Comp71413 G71414 GEdge71415 SB

71416 CH6071417 CH20071418G71419 SB71420 CH10071421 CH707 1422 G71423 CH3571424 CH10071425 CH15071426CH60

Loose but in place Qtx bx. 3m NE of 7141 1Unalt'd and unminerised amyg Andesite

ofqtzbx. 1m N of 7141 1 2-3%Loose block of white qv in maf mvolc/tuff bx? withchloritic crack-seal planes. Py in qtz and w chlRusty, mod fissile shear w mod carb-ser, 1 qc strSim to 71416, but more fissile, deeply weatheredTrench muck from natural trapsites near pitLoose well min'd w.rock within 2m S of pitAcross bottom of trench. 30-40% veinletsAdjoins 71421 . 12cm qc veinlet, 2 <2cm str'sV. well min'd alt'd and sh'd w. rock, E side of TShovel sample. Talc mush+rotten shear in h.wallMargin of strong shearing, shear parallel veinletsAlmost 50% sm. shear parallel qtz-carb stringersS'ernmost exp. of trenched qv. Two 5cm veinlets

(GPS5-7%nil

0+86S,

3-4%Tr-1%Tr-1%1%?6-7%3%, tr cp3%8-10%

: E,N or local grid)0+86S, 0+0 1W0+77S, 0+02E

0+05W

0+70S, 0+85W0+40S, 0+47W0+45 S, 0+47W0+02S, 0+01.5E0+03 S, BL0+2.5S,0+01E0+2.5S, BL0+02S, 0+02E

!%?15%q-c str's 0+06S, 0+01 WTr-1%1%<1%

0+33S, 0+09W0+3 IS, 0+05W0+30S, 0+06W

487001 G

487002 G487003 G487004 WR487005 WR486006 WR487007 CH1 50487008 CH60487009 CH 70487010 CH70487011 CH115

Vein qtz+prev. unmapped int-felsic unit. Near E boundary of claim1178315. Unit well veined, prob dacite tuff. N contact 080/70NSample 80% w.rock w strs, 20% qv w diss. ox'd carb TrFissile carb-ser sh w 15% qs. Loose beneath a tree Tr-1%Sm. wk carb-st. chl alt'd narrow shear. Tuff-bx? <1%Wk-mod sh'd, mod chl-calc alt'd Tuff-Bx? nil-trTuffaceous7 Dacite. 4m S of 487004 nil-trFine grained massive Andesite, mod-st. calc alt. nil-tr5m W along shear strike from 71425 TrAdjoins 487007 to N TrStrong shear adj. to vein 085/sv. Rare str's. TrVein to 35cm wide+15-20cm w.rock on either side <1%~5m S of pit, 1.5m N of 487009. Vein 65-70cm wide 1-2%

454345, 5455182453966, 54550120+75S, 0+48W0+7 IS, 0+52W0+75S, 0+54W0+53 S, 0+54W

0+07S, 0+2. 5W0+08S, 0+02W0+05S, 0+01W

12

Chemex Labs Ltd,Analytical Chemists * Geochemists " Registered Assayers

5175Timberlea Blvd., MississaugaOntario, Canada L4W 2S3PHONE: 905-624-2806 FAX: 905-624-6163

o: NUINSCO RESOURCES LIMITED

908 THE EAST MALL ETOBICOKE, ON M9B6K2

Project: CAMERONComments: ATTN: PAUL JONES FAX: JIM WILSON

Pagt ,ber : 1 Total Pages : 1 Certificate Date: 27-OCT-97 Invoice No. : 19747612 P.O. Number : Account : LVY

CERTIFICATE OF ANALYSIS A974761 2

SAMPLE

2390323904239052390623907

23908239092391O2391123912

2391323914239152391623917

2391823919 239202392123922

2392323924239252392623927

23928

PREPCODE

2052052O5205205

2052052052052O5

205205205205205

205205 2052O5205

2052052052052O5

205

226226226226226

226226226226226

226226226226226

226226 226226226

226226226226226

226

Au ppbFA+AA

530

< 5< 510

1455

< 5< 51OO

40< 5165215555

7020 30

11025

< 510105

80

710

^>*~n"~oW

DXNJ

CERTI

Chemex Labs Ltd,Analytical Chemists " Geochemists " Registered Assayers

5175 Timberlea Blvd., MississaugaOntario, Canada L4W 2S3PHONE: 905-624-2806 FAX: 905-624-6163

,: NUINSCO RESOURCES LIMITED



Page I jer : 1 Total Pages : 1 Certificate Date: 30-OCT-97 Invoice No. : 19748053 P.O. Number : Account : LVY

CERTIFICATE OF ANALYSIS A9748053

SAMPLE

239292393O239312393223933

2393423935239362393723938

2393923940239412394223943

2394423945239462394723948

2394923950239512395223953

2395423955239562395723958

PREP

CODE

205205205205205

205205205205205

205205205205205

2O52O52O52O5205

2052052O5205205

2O52052O5205205

226226226226226

226226226226226

226226226226226

226226226226226

226226226226226

226226226226226

Au ppbFA+AA

< 5800110

125070

351565

< 5215

< 5< 5410815280

105505390370125

240645

5< 5< 5

75< 5< 5< 510

>"0"Owz2'K)

OO3

Ou

Chemex Labs LtdAnalytical Chemists" Geochemists" Registered Assayers

5175 Timberlea Blvd.. MississaugaOntario, Canada L4W 2S3PHONE: 905-624-2806 FAX: 905-624-6163

NUINSCO RESOURCES LIMITED

908 THE EAST MALL ETOBICOKE, ON M9B 6K2

Project: Comments:

CAMERONATTN: PAUL JONES FAX: JIM WILSON

Page i <er : 1 Total PayrfS : 1 Certificate Date: 29-OCT-97 Invoice No. : 19748054 P.O. Number : Account : LVY

SAMPLE

2395923960

PREP CODE

208208

226226

A1203 \ XRF

16.0512.25

CaO % XRF

6.561.07

Cr203 % XRF

< 0.01< 0.01

Fe203 % XRF

9.613.89

K20 % XRF

0.270.99


MgO \ XRF

5.281.02

MnO % XRF

0.150.07

Na20 % XRF

3.474.00

P205 % XRF

0.120.05

Si02 % XRF

54.6873.56

T102 % XRF

0.750.34

LOI % XRF

2.151.92

TOTAL

99.0999.16

zDX

o03

CL

CERTIFICATION:,

Chemex Labs Ltd,Analytical Chemists' Geochemists * Registered Assayers

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: NUINSCO RESOURCES LIMITED


Project: CAMERONComments: ATTN: C.A.WAGG FAX: JIM WILSON

Page t^ ar : 1 Total Payes : 1 Certificate Date: 06-NOV-97 Invoice No. : 19749008 P.O. Number : Account : LVY


SAMPLE

2395923960

PREP CODE

244244

__

Au ppb FA+AA

< 5< 5

mz;DXtor>Of-t-

CERTIFICATION:

Chemex Labs LtdAnalytical Chemists' Geochemists" Registered Assayers




Project: CAMERON Comments: ATTN: C.A.WAGG

Page , >er : 1 Total Payes :2 Certificate Date:07-NOV-97 Invoice No. : 19749006 P.O. Number : Account : LVY

FAX: JIM WILSON


SAMPLE

2396123962239632396423965

2396623967239682396923970

2397123972239732397423975

2397623977239782397923980

7140171402714037140471405

7140671407714087141071411

7141371414714157141671417

7141871420714217142271423

PREP

CODE

205205205205205

205205205205205

205205205205205

205205205205205

205205205205205

205205205205205

205205205205205

205205205205205

226226226226226

226226226226226

226226226226226

226226226226226

226226226226226

226226226226226

226226226226226

226226226226226

Au ppbFA+AA

30OO60

4440< 5< 5

< 515

< 5< 535

3530

< 5< S< 5

< 5< 5

555

55

< 5< 5530

10< 5< 5< 5560

< 54801720

10< 5

1859595

120965

>"T3

Wz;oX1 'K>

OO3f K

CL

CERTIFICATION:,

Chemex Labs LtdAnalytical Chemists" Geochemists" Registered Assayers

5175 Timbetlea Blvd., Mississauga



Page jer :2 Total Payes : 2 Certificate Date: 07-NOV-97 Invoice No. : 19749006 P.O. Number : Account : LVY

00

m^^r* Ontario, Canada L4W2S3 Proiect CAMERON - " B|^^^ PHONE: 905-624-2806 FAX: 905-624-6163 Comments: ATTN: C.A.WAGG FAX: JIM WILSON


SAMPLE

714247142571426

PREPCODE

205205205

226226226

Au ppbFA+AA

5< 5

50

raDX

ob« K

Cu

CERTIFICATION:.

Chemex Labs Ltd.Analytical Chemists" Geochemists" Registered Assayers

5175 Timbertea Blvd., MississaugaOntario, Canada L4W 2S3PHONE: 905-624-2806 FAX: 905-624-6163



Project: Comments:

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Page iber : 1 Total Pages : 1 Certificate Date: 10-NOV-97 Invoice No. : 19749125 P.O. Number : Account : LVY


SAMPLE

71409487001487002487003487004

487005487006487007487008487009

487010487011

PREPCODE

2O5205205205205

205205205205205

205205

226226226226226

226226226226226

226226

Au ppbFA+AA

< 5< 5< 5585< 5

< 5< 5< 5< 525

14515

>TJ-offl

aXto0o1 f

Ou

CD

CERTIFICATION:,

Chemex Labs Ltd,Analytical Chemists" Geochemists ' Registered Assayers





Page oer : 1 -A Total Hayes : 1 Certificate Date: 08-NOV-97 Invoice No. -.19749009 P.O. Number : Account : LVY


SAMPLE

7141271419

PREPCODE

205205

226226

Au ppb Ag Al As Ba Be Bi Ca Cd Co Cr Cu Fe Ga Hg K La Mg MnFA+AA ppm % ppm ppm ppm ppm % ppm ppm ppm ppm % ppm ppm % ppm % ppm

210 < 0.2 0.69 14 10 < 0.5 < 2 2.39 < 0.5 14 41 49 3.21 < 10 < 1 0.03 < 10 0.92 47580 < 0.2 0.85 < 2 30 < 0.5 < 2 4.05 < 0.5 22 137 36 4.55 < 10 < 1 0.07 < 10 1.69 995

rdz;otooO3

K) O

CERTIFICATION:

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Page ber :1-B Total Pages : 1 Certificate Date: 08-NOV-97 Invoice No. : 19749009 P.O. Number : Account :LVY


SAMPLE

7141271419

PSEP CODE

205205

226226

Mo Na Hi P Pb Sb Sc Sr Ti Tl U V W Zn ppm % ppm ppm ppm ppm ppm ppm % ppm ppm ppm ppm ppm

< 1 0.07 49 180 < 2 < 2 7 79 < 0.01 < 10 < 10 24 < 10 46< 1 0.05 53 280 < 2 < 2 9 125 < 0.01 < 10 < 10 24 < 10 56

———————————————————————————————————————————————————————————————————————————————————————————————————————— . ———————————————————————————————— _ —————————————————————————————————————————————— . ——— ft —————————————————————————————————————————— - —————————————

T3tfl

oX

oo3

ol

CERTIFICATION:

Chemex Labs Ltd,Analytical Chemists * Geochemists ' Registered Assayers


j: NUINSCO RESOURCES LIMITED



Page i _>er : 1 Total Pages : 1 Certificate Date: 11-NOV-97 Invoice No. : 19749126 P.O. Number : Account : LVY

SAMPLE

487004487005487006

PEEP CODE

299299299

_ _--

A1203 % XRF

18.9616.1615.66

CaO % XRF

3.585.186.22

Cr203 % XRF

< 0.01< 0.01< 0.01

Fe203 % XRF

7.548.219.00

K20 % XRF

3.001.180.82


MgO % XRF

4.183.823.15

HnO % XRF

0.090.130.14

Na20 % XRF

1.231.273.31

P205 % XRF

0.070.090.14

Si02 % XRF

52.7253.7852.60

Ti02 % XRF

0.660.710.82

LOI % XRF

6.968.107.59

TOTAL \

98.9998.6399.45

NJ NJ

"dm zdh ^

X

CERTIFICATION:

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Project: DOUG REIDComments: ATTN: PAUL JONES FAX: JIM WILSON

Page .ber : 1 Total hdges : 1 Certificate Date: 06-NOV-97 Invoice No. : 19749124 P.O. Number : Account : LVY

toGO

CERTIFICATE OF ANALYSIS A97491 24

SAMPLE

487050

PREP CODE

205 226

Au ppb FA+AA

35

mzoX

r>O

CERTIFICATION:

Chemex Labs Ltd,Analytical Chemists * Geochemists * Registered Assayers


To: NU1NSCO RESOURCES LIMITED


Project: CAMERONComments: ATTN: C.A.WAGG FAX: JIM WILSON

Page nber : 1 Total Pages : 1 Certificate Date: 11-NOV-97 Invoice No. : 19749007 P.O. Number : Account : LVY

SAMPLE

23966 23967 23968 23969

PEEP CODE

299 299 299 299

A1203 \ XEF

15.16 15.83 14.82 15.59

x

CaO % XEF

4.80 4.99 7.11 5.47

Cr203 \ XRF

< 0.01 < 0.01 < 0.01 < 0.01

Fe203 \ XKF

8.32 9.08 7.63 8.15

-

K20 \XRF

0.49 0.52 0.51 0.28


MgO % XEF

3.94 3.81 3.87 3.70

MnO \XKF

0.13 0.10 0.12 0.12

Na20 % XKF

4.68 3.31 4.06 4.38

P205 * XKF

0.16 0.16 0.16 0.13

Si02 % XRF

51.30 50.73 51.66 51.38

Ti02 % XKF

0.79 0.84 0.77 0.79

LOI %XEF

9.01 9.64 8.46 9.37

TOTAL %

98.78 99.01 99.17 99.36

CERTIFICATION:

APPENDIX 3

Summary of Expenditures

ItemD7 BulldozerBackhoeTransportConsultantAccomodationReportDraftingAssaysShipping (Assays)

Descriptionaccess, preliminary stripping

geological, supervision

Quantity53hrs

lOOhrs6hrs

38 days

70hrs

3501bs

Kwte$85/hr + GST$55/hr + GST

$100/hr + GSTincluding GST

$50/dayincluding GST$20/hr + GST

including GST + P$0.995/lb + GST

Cos*4820.355885.00642.00

7923.211900.002214.901498.001687.68

35.76GST (included)

Total Expenditures1627.08

$26.606.90

25

05/06/1998 16:24 4166260890 NUINSCO RESOURCES PAGE 02

2.

n^p^l29 / I

ROWAN LAKE• R.I •UllllfTIMnl ItXTIICT

KENORA / FORT FRANCES_•!•••« limtfl

KENORAU» TITIM* fcttlim I IVIIMI

KENORA•«

OnlMie

G-2639

Location of Trenching.

Ftirservice OptionNutnsco Resources Limited

BROOKS LAKEM «.«. lOUiHIJ-HATlH ClITtlCT

FORT FRANCES

KENORAUCD TITlU/ PjenTUT tl¥IJie»

KENORAMirii!.>vol

Onurto

G-2670

SCALE: 1 INCH - 40 CHAINS

II II CM)

MflY 06 '99 16=31 4166260890 PflGE.02

Ontario Ministry ofNorthern Developmentand Mines

Declaration of Assessment Work Performed on Mining LandMining Act, SubMCtlon 65(2) and 86(3), R.S.O. 1990

Transaction Number (office usa)Ii Lira,Assessment Fimen! FileaTResearch Imaging

Personal information collected on this form is obtained under the aulhoi Mining Act, the information is a public record. This information will be use* Questions about this collection should be directed to the Chief Mir 933 Ramsey Lake Road, Sudbury, Ontario, P3E 6B5.

52F05SE2001 2.18206 ROWAN LAKE 900

Instructions: - For work performed on Crown Lands before recording a claim, use form 0240. - Please type or print in ink.

1. Recorded holder(s) (Attach a list if necessary). 1820 6

NameT.

Client Number

Address Telephone Number

Fax' Number

Name Client Number

Address Telephone Number

F̂ax- Number

2. Type of work performed: Check ( ^ ) and report on only ONE of the following groups for this declaration.

DWork

Geotechnical: prospecting, surveys, assays and work under section 18 (regs)

Type Zee*

&£ o\j ~<-

r-jxPhysical: drilling, stripping, Li-f trenching and associated assays

CH i/° SVfyvt/'c/,J<5, vTTTZ

Day | Month

<?Yaw

Global Positioning System Data (if available)

? TO

Day

f s>f>f ~±G <ty,s^ £

/<c>| Month

/

YearTownship/Area

M or G-Plan Number£-26 3*? « <5-~L4ffc

D Rehabilitation

Office UseCommodity

Total $ Value of Work Claimed

NTS Reference

Mining Division _

Resident Geologist District

ZAjAj.

^\f-.AV c

'r\ l >; L i

' 'S^

«-r

JPlease remember to: - obtain a work permit from the Ministry of Natural Resources as required;

- provide proper notice to surface rights holders before starting work;- complete and attach a Statement of Costs, form 0212;- provide a map showing contiguous mining lands that are linked for assigning work;- include two copies of your technical report.

3. Person or companies who prepared the technical report (Attach a list if necessary)Name

Gftyt/J l^/T^rS /?-f^ /vnJ/fJSfs &tfS-Address '

Name

Address

Name

Address

Telephone Number / Q&f\ *T& *—- — // 0 ^ _

Fax Number

Telephone Number

Fax Number

Telephone Nu

Fax Number

4. Certification by Recorded Holder or Agent

«^ \v:. 10FE8 C 3 1 398

GEOSCIENCE ASSfcSSMFNTJ OFFIff " !

I, I / , do hereby certify that I have personal knowledge of the facts set(Print Name)

forth in this Declaration of Assessment Work having caused the work to be performed or witnessed the same during or after its completion and, to the best of my knowledge, the annexed report is true.

5. Work to be recorded and distributed. Work can only be assigned to claims that are contiguous (adjoining) to the mining' land where work was performed, at the time work waaj>erformed. A map showing the contiguous link must accompany this form. f± t ft O C\

Mining Claim Number. Or if work was done on other eligible mining land, show in this column the location number indicated on the claim map.

eg

eg

eg

1

2

3

4

5

6

7

8

9

10

11

12

13

14

15

TB 7827

1234567

1234568

//7-S 328//?£ 32.^//?$ ?-?o//T-%3/f

•W Number of ClaimUnits. For other mining land, list hectares.

16 ha

12

2

/u' (o

&

/T.

^6Column Totals

Value of work performed on this claim or other mining land.

$26, 825

0

$ 8, 892

2(> £ o4/

°2«* £o (t

Value of work applied to this claim.

N/A

$24,000

$4,000

6,</Ot>'/

Z,<f<rt/4 £ tfb

/£} 60 0

Value of work assigned to other mining claims.

$24,000

0

0

// T-Oo

//, ^oo

Bank. Value of work to be distributed at a future date.

$2,825

0

$4,892

/o 4cc}

/O £c 6

, do hereby certify that the above work credits are eligible under(Print Full Name)

subsection 7 (1) of the Assessment Work Regulation 6/96 for assignment to contiguous claims or for application to the claim where the work was done.Signature of Recorded Holder or AgenX^uthorized in Writing

I 0Instructions for cutting back credits that are not approved.

Date

Some of the credits claimed in this declaration may be cut back. Please check ( ^ ) i n the boxes below to show howyou wish to prioritize the deletion of credits:

D 1. Credits are to be cut back from the Bank first, followed by option 2 or 3 or 4 as indicated. D 2. Credits are to be cut back starting with the claims listed last, working backwards; or D 3. Credits are to be cut back equally over all claims listed in this declaration; or D 4. Credits are to be cut back as prioritized on the attached appendix or as follows (describe):

Note: If you have not indicated how your credits are to be deleted, credits will be cut back from the Bank first, followed by option number 2 if necessary.

For Office Use Only_______________Received Stamp Date Notification Sent

0241 (02/98)

Deemed Approved Date

Date Approved Total Value of Credit Approved

Approved for Recording by Mining Recorder (Signature)

o. 1820 6APPENDIX 3

Summary of Expenditures

ItemD7 BulldozerBackhoeTransportConsultantAccomodationReportDraftingAssaysShipping (Assays)

Descriptionaccess, preliminary stripping

geological, supervision

Quantity53hrs

lOOhrs6hrs

38 days

70hrs

3501bs

Rate$85/hr+GST$55/hr + GST

$100/hr + GSTincluding GST

$50/dayincluding GST$20/hr + GST

including GST + P$0.995/lb + GST

Cost4820.355885.00642.00

7923.211900.002214.901498.001687.68

35.76GST (included)

Total Expenditures1627.08

$26.606.90

Ministry ofNorthern Developmentand Mines

Ministere du DeVeloppement du Nord et des Mines

May?, 1998

ROBERT JOHN FAIRSERVICEP.O. BOX 627155 MAIN STREET SOUTHKENORA, ONP9N-1T1

OntarioGeoscience Assessment Office 933 Ramsey Lake Road 6th Floor Sudbury, Ontario P3E 6B5

Telephone: (888)415-9846 Fax: (705) 670-5881

Dear Sir or Madam:

Subject: Transaction Number(s):

Submission Number: 2 .18206

W9810.00031Status

Deemed Approval

We have reviewed your Assessment Work submission with the above noted Transaction Number(s). The attached summary page(s) indicate the results of the review. WE RECOMMEND YOU READ THIS SUMMARY FOR THE DETAILS PERTAINING TO YOUR ASSESSMENT WORK.

If the status for a transaction is a 45 Day Notice, the summary will outline the reasons for the notice, and any steps you can take to remedy deficiencies. The 90-day deemed approval provision, subsection 6(7) of the Assessment Work Regulation, will no longer be in effect for assessment work which has received a 45 Day Notice.

Please note any revisions must be submitted in DUPLICATE to the Geoscience Assessment Office, by the response date on the summary.

If you have any questions regarding this correspondence, please contact Lucille Jerome by e-mail at [email protected] or by telephone at (705) 670-5858.

Yours sincerely,

ORIGINAL SIGNED BYBlair KiteSupervisor, Geoscience Assessment OfficeMining Lands Section

Correspondence ID: 12219

Copy for: Assessment Library

Work Report Assessment Results

Submission Number: 2 .18206

Date Correspondence Sent: May 07, 1998 AssessorLucille Jerome

Transaction First ClaimNumber Number Township(s) / Area(s) Status Approval DateW9810.00031 1178315 ROWAN LAKE, BROOKS LAKE Deemed Approval May 07, 1998

Section:10 Physical PSTRIP

Correspondence to: Recorded Holder(s) and/or Agent(s):Resident Geologist ROBERT JOHN FAIRSERVICEKenora, ON KENORA, ON

Assessment Files Library Paul Pitman Sudbury, ON NUINSCO RESOURCES LIMITED

TORONTO, ONTARIO

Page: 1Correspondence ID: 12219

wagg mineral exploration and consulting inc. · 2017-01-17 · to values strongly anomalous in gold...

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