RECESSION LARDER PROS - RPT ON THE 1996 ......angldUmaque explorations inc. a 450 dip. These holes...

2864, chemin SullivanSullivan (Quebec) JOY 2ND

Tel.: (819) 824-1030Fax: (819) 824-1003

email: [email protected]

angiaiJmaqueexplorations inc.

2. I o

Kalahari Resources Inc.Recession Larder ProspectReport on the 1996 Exploration

ProyamKJridand LakCj Ontano

NTS32D04

Richard Roy November 1997

32D04NE0163 2.17933 MCGARRY 010

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SUMMARY

The Recession Larder Prospect is located in McGarry Township, east of Kirkland Lake, Ontario. It consists of 8 claims covering an area of 320 acres. The property was optioned by Kalahari Resources Inc. from 2973090 Canada Inc.

The property lies within part of the Abitibi Orogen, consisting of metamorphosed Early Precambrian volcanic, sedimentary and intrusive rocks in an east-plunging synclinorium between the Abitibi and Round Lake Batholiths. Two major east-west trending fault zones cut the northern and southern units of the synclinorium; the Destor-Porcupine Fault Zone and the Kirkland Lake-Larder Lake Fault Zone respectively. The gold deposits of the Kirkland Lake area are related to the latter structure. The rocks consist of komatiitic, tholeiitic and calc-alkaline volcanics of the Wabawewa, Catherine and Skead Groups respectively, with a basal unit of Pacaud tuffs. The younger, Upper Supergroup volcanic cycle is comprised of komatiitic lavas of the Larder Lake Group, tholeiitic rocks of the Kinojevis Group and calc-alkaline rocks of the Blake River Group. A northwest- southeast trending wedge of rhyolitic pyroclastic rocks is located east of Victoria Lake, and is thought to be a rhyolitic portion of the Blake River Group called the Gauthier Group.

Two main lithologies were delineated on the property: Timiskaming conglomerate to wacke, and trachytic flows with local fragmental breccias. Three small outcrops of diabase were also located, cutting both the conglomerates and the trachytes.

Several past and present gold-producers lies in the immediate vicinity of the Recession Larder property. They include the Kerr Mine (l .6 km southeast), Armistice Mine (l .5 km southeast), and Chesterville (1.6 km southeast). Numerous showing are also located close to and adjacent to the property including the Arjon Prospect (south border), Ivan Larder Prospect (west boundary), and the McGarry Gold/ Lee Geo Indicators property (north boundary) on which reserves of 110,000 tons grading 0.10 oz/t Au have been outlined.

The first known work done on the property itself was completed by Drummond in 1939. Three holes were drilled and two shallow shafts were sunk. Values of up to l .33 opt Au are reported from this work.

In 1981, Lampe Resources drilled two holes which aimed to the north. They were done in the NW part of the property on line 0+75E at 0+25N. The first hole was 61 meters long at a 45 0 dip while the other, positioned 3 meters north of the first one, was 148m long at

angldUmaqueexplorations inc.

a 450 dip. These holes both intersected the trachyte of the Timiskaming volcanic sequence but results obtained did not show any significant values.

The 1996 drilling program encountered strong shearing, alteration and quartz veining with local pyrite mineralization. The gold values obtained are low, but consistently in detectable quantities in hole -01. Although quite disappointing, the samples rarely contained significant amounts of sulphides.

The drill program also helped to better define the stratigraphy in the southeast portion of the property. Hole -05 encountered altered sedimentary rocks which are also sheared. No significant gold values were obtained from this hole but the lack of sulphides within the shear explains the low values.

The 1996 exploration program added significantly to our knowledge of the property, establishing the structural nature of the Ivan Larder Fault and locating other significant structures such as within the sediments in the eastern part of the property. Adding an IP survey to the existing database could provide specific targets along the favourable structures already defined and may point to new areas where no work has been done so far. In addition it is recommended to complete a 2,500 feet drilling program to test the IP anomalies obtained. A total of S85 600.00 is required to complete the program.

angiaUmaqueexplorations inc.

TABLE OF CONTENT

1.0 INTRODUCTION

2.0 PROPERTY, LOCATION AND ACCESS

3.0 REGIONAL GEOLOGY

4.0 LOCAL GEOLOGY

5.0 PREVIOUS WORK HISTORY

6.0 1996 EXPLORATION PROGRAM

7.0 DISCUSSION

8.0 CONCLUSION

9.0 RECOMMENDATIONS

10.0 BUDGET

4

4

4

8

10

12

18

20

20

21

REFERENCES

FIGURE 1: CLAIM MAP AND GENERAL LOCATION

FIGURE 2: REGIONAL GEOLOGY, KIRKLAND LAKE AREA, ONTARIO______7

FIGURE 3: RECESSION LARDER PROSPECT GEOLOGY________________9

TABLE l DIAMOND DRILLING STATISTICS_________________________13

APPENDIX 1: DIAMOND DRILL LOGS

MAP 1; RECESSION LARDER PROSPECT COMPILATION. 1:2500 BACK POCKET

SECTION l TO 7 GEOLOGICAL SECTIONS. 1:500____________BACK POCKET

32D04NE0163 2.17933 MCGARRY 01 OC


1.0 INTRODUCTION

The Recession Larder Project is located in central McGarry Twp, near Kirkland Lake Ont. (NTS 32D/04). It includes eight claims covering 320 acres (Figure l). It is currently under option by Kalahari Resources Inc. of Vancouver.

An exploration program consisting of line cutting and diamond drilling was done between October 8l and 29th , 1996. All work was done through the supervision of Anglaumaque Explorations Inc. Diamond drilling was contracted to Forage Val d'Or Inc.

Following is a brief account of the regional and local geology and a list of the historical work done on the current property. The report also provides a detailed description of the holes drilled and a discussion of the results obtained. Based on this information, a series of recommendations are proposed.

2.0 PROPERTY, LOCATION AND ACCESS

The Recession Larder Property is located 40 km east of the town of Kirkland Lake, Ontario and consists of 8 claims (1167658 and 1167665). It lies in the central part of McGarry Township on NTS Map Sheet 32D/04. The claims are registered with the Office of the Mining Recorder at Kirkland Lake, Ontario under the name of 297 3090 Canada Inc. The property is currently under option by Kalahari Resources Inc.

Access to the property is via HWY 66 which reaches the towns of Kirkland Lake to the west and the Quebec border to the east. A dirt road from the Virginiatown provides direct access to the property.

3.0 REGIONAL GEOLOGY

The property lies within part of the Abitibi Orogen, consisting of metamorphosed Early Precambrian volcanic, sedimentary and intrusive rocks in an east-plunging synclinorium between the Abitibi and Round Lake batholiths. Two major east-west trending fault zones cut the northern and southern units of the synclinorium; the Destor-Porcupine Fault Zone and the Kirkland Lake-Larder Lake Fault Zone respectively. The gold deposits of the Kirkland Lake area are related to the latter structure.

NgSSIANTWP

McGARRYTWP

QUEBEC

RECESSION LARDER emeus****)PROSPECT *l, - ' - i t '

-!-,... .•j"^' '. . TIMMIMS* */* *:.".i-'^ VA . 3\ WLDW ,;"'î'^^^ W*"*',lii*WQHftWAM f OUBMB-

RECESSION LARDER PROSPECT

McFADDENTWP

LARDER LAKE

angl maqueexplorations inc.

KALAHARI RESOURCES INC. Recession Larder Prospect

Claim Map and General Location___________Figure 1__________

LOCATION CW


According to Pyke (1982) the belt is comprised of two complete and one incomplete cycles of volcanic and plutonic rocks (figure 2). The oldest rocks (Lower Supergroup) occur near the outer margins. To the southeast of Kirkland Lake, these rocks consist of komatiitic, tholeiitic and calc-alkaline volcanics of the Wabawewa, Catherine and Skead Groups respectively, with a basal unit of Pacaud tuffs. The younger, Upper Supergroup volcanic cycle is comprised of komatiitic lavas of the Larder Lake Group, tholeiitic rocks of the Kinojevis Group and calc-alkaline rocks of the Blake River Group. A northwest- southeast trending wedge of rhyolitic pyroclastic rocks is located east of Victoria Lake, and is thought to be a rhyolitic portion of the Blake River Group called the Gauthier Group. These are unconformably overlain by the important alkaline igneous regional geology rocks of the Timiskaming Group. The Blake River, Kinojevis and Timiskaming Groups are separated by sedimentary rocks comprising chert-carbonate-iron formation (the Boston iron formation), conglomerate, sandstone and argillites. Trachytic predominate the Timiskaming volcanics which cap the second volcanic sequence. Algoman intrusive rocks, including dykes and stocks of syenite, monzonite and quartz monzonite cut the volcanic-sedimentary pile. The sequence is south facing, south dipping and is cut by numerous vertical strike faults and cross faults.

The property is surrounded by several advanced-stage development projects, including Armistice Resources (south), Edomar Resources (west), Transpacific Resources Inc. (north), and Northern Dynasty Resources (east), Deak/GSR (southeast).

The Kerr Mine property also borders the claims to the southeast. The main orebody is located 1500 meters southeast of the Recession Larder Prospect, as is the past producing Chesterville property (358,000 oz). Gold production to date from the Kerr Mine totals in excess of 11 Million ounces. These properties were taken over by Deak Resources *fe G.S.R. Mining in 1990 with the Kerr Mine put back into production (1989 A 1990: Deak Resources Corp., Annual Reports). Reserves were stated as 2,467,000 tons of 0.12 oz/t Au (Northern Daily News, p. 20A, 03/21 1192).

Drill defined reserves at Armistice are 553,000 tons of 0.15 oz/t Au (1989: Armistice Resources Ltd., Annual Report) with exploration continuing to search for the Ken- Horizon at depth. The shaft was deepened to 2,250 feet in 1988-89 in order to permit deep drilling for the faulted Kerr Zone. Values of up to 0.375 opt over 18 feet have been obtained from this drilling.

The McGarry Gold Corp. (Transpacific Resources Inc.) property lies to the north of the Recession Larder Prospect. This property has been the site of several drill campaigns since 1983. Several zones of interest have been identified (i.e.: "F"-zone with drill

ALKALIC INTRUSIVE

GOWGANDA FORMATION

FELSIC INTRUSIVE

SYENITE, MONZONITE

GABBRO, DIORITE

PERIDOTITE, DUNITE

CONGLOMERATE

TRACHYTE

VOLCANIC ROCK

GEOLOGICAL . CONTACT

. CWOSS FAULT

m GOLD DEPOSIT

O 5km

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explorations inc.


Regional Geology_______ Figure 2 ^^—^^—


indicated reserves of 110,000 tons of 0.10 oz/t Au). Recently, Transpacific has exercised its option to purchase 100*^ of the property following a 24 hole drill program which has intersected significant gold values in 17 holes. Values of up to 14 opt over l .4 feet and 29 feet at 0.05 opt are reported (Northern Daily News Friday October 17th 1997).

4.0 LOCAL GEOLOGY

Geological mapping by S.J. Carmichael was completed in 1992 at a scale of 1:2500 over grid lines cut at either 100 meter or 50m centers (figure 3). The author described the geology of the property as consisting of two main lithologies including Timiskaming conglomerate and wacke, and trachytic flows and fragmental breccias. Three small outcrops of diabase were also located, cutting both the conglomerates and the trachytes".

I) Timiskaming ConglomerateAll outcrops of conglomerate were located north of the Ivan Larder Fault. They are typical, unaltered and contain the occasional diagnostic jasper pebbles. Exposure is generally limited to small cliff faces and are void of any bedding or dip features. Cobble lithologies vary from syenide to volcanic with intrusive varieties dominating. The clasts are relatively undeformed and show little if any stretching or flattening. The maximum clast size is roughly six inches.

II) Timiskaming TrachyteTrachytic units underlie most of the property and occur south of the Ivan Larder Fault. They vary from dark green chloritic fragmental flows, often moderately magnetic to buff carbonated sericitic units where cut by shears of faults. Lesser interbedded siltstone units were located on line 3+OOE, 2+OOS. The bedding of these units strike east-northeast with a dark green chloritic groundmass with up to 25*^0 syenitic clasts. Where higher proportions of syenitic fragments are present, the trachyte appears as dark red to pink in colour. One such location is line 2+50E, 4+25S.

The dominant structure on the property is the Ivan Larder Fault which transects the entire claim group. It appears to mark a lithological contact between the Timiskaming conglomerate to the north and the Timiskaming trachyte to the south.

According to S.J. Carmichael the mineralization on the property is associated to a series of secondary faults which trend roughly east-northeast. Quartz veining and carbonate/sericite alteration are related to these secondary faults. Mineralization is confined to the trachytic units and consists of quartz veins and flat-lying small quartz

IVAN LARDER FAULT

BASELINE AzBO'

CONGLOMERATE

TRACHYTE

DIABASE

150m

X

Outcrop

Fault; Shear

Drill Hole

Trench; Pit

Quartz Vein

VLF-EM Anomaly

Maxl-Probe Anomaly

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LOCAL GEOLOGYFigure 3

10


stockworks. On the property, a total of eight areas were manually stripped and sampled.

Most of the veins contain up to l 07o of pyrite with minor chalcopyrite. The best assays

returned from the sampling was 0.02 oz/t Au an other samples returned Q.29% Cu from a

vein mineralized with irregular pods of malachite and chalcopyrite.


The Kirkland Lake-Larder Lake area has been actively explored since the early part of the

century when the Kirkland Lake Break was discovered. Although exploration efforts

came in pulses throughout the century, important discoveries were made in most decades,

the most recent being Sudbury Contact's Victoria Creek Project in 1993.

The first known work done on the property itself was completed by Drummond in 1939.

Three holes were drilled and two shallow shafts were sunk. They obtained an interesting

result of 1.33 oz/t Au. Two of the three holes were located on claim #1167659 where

one of the shaft is found (on Line 2+1OE at 0+75N). The first hole was drilled towards

the south at a low angle. The second one was drilled at a dip of 700 to the north. Gold

values were reported over a 50 cm width in the first hole. The third hole, located about

100m south of the other holes, was drilled at a 45 0 angle to the north. Unfortunately,

none of the collars were found during a mapping campaign in 1992.

However, during this campaign, four old drill holes were located at the following

coordinates: 3+60E, 0+00; 3+90E, 0+00; 1+25E, 3+30S and 1+60E, 2+90S. The drill

core from these holes was found at the intersection of the baseline and 3+60S, near the

collar of the two first holes. Many of the core boxes were overturned, rendering the core

useless.

A fifth hole, drilled at a nearly vertical dip probably during that same period, is located at

the southern limit of the property on line 8+25E. These holes, which seem to be over

thirty years old, were never mentioned or described in any report.

In 1981, the property was held by M. Leahy and C. Forbes who did some ground

magnetic and electromagnetic surveys (VFL) and then was optioned to Lampe Resources.

Two drill holes, aimed to the north, were done in the NW part of the property on line

0+75E at 0+25N. The first hole was 61 meters long at a 45 0 dip while the other,

positioned 3 meters north of the first one, was 148m long at a 45 0 dip. These holes both

intersected the trachyte of the Timiskaming volcanic sequence but results obtained did

not show any significant values.

10


stockworks. On the property, a total of eight areas were manually stripped and sampled.

Most of the veins contain up to Wo of pyrite with minor chalcopyrite. The best assays

returned from the sampling was 0.02 oz/t Au an other samples returned Q.29% Cu from a

vein mineralized with irregular pods of malachite and chalcopyrite.


The Kirkland Lake-Larder Lake area has been actively explored since the early part of the

century when the Kirkland Lake Break was discovered. Although exploration efforts

came in pulses throughout the century, important discoveries were made in most decades,

the most recent being Sudbury Contact's Victoria Creek Project in 1993.

The first known work done on the property itself was completed by Drummond in 1939.

Three holes were drilled and two shallow shafts were sunk. They obtained an interesting

result of 1.33 oz/t Au. Two of the three holes were located on claim #1167659 where

one of the shaft is found (on Line 2+10E at 0+75N). The first hole was drilled towards

the south at a low angle. The second one was drilled at a dip of 700 to the north. Gold

values were reported over a 50 cm width in the first hole. The third hole, located about

100m south of the other holes, was drilled at a 45 0 angle to the north. Unfortunately,

none of the collars were found during a mapping campaign in 1992.

However, during this campaign, four old drill holes were located at the following

coordinates: 3+60E, 0+00; 3+90E, 0+00; 1+25E, 3+30S and 1+60E, 2+90S. The drill

core from these holes was found at the intersection of the baseline and 3+60S, near the

collar of the two first holes. Many of the core boxes were overturned, rendering the core

useless.

A fifth hole, drilled at a nearly vertical dip probably during that same period, is located at

the southern limit of the property on line 8+25E. These holes, which seem to be over

thirty years old, were never mentioned or described in any report.

In 1981, the property was held by M. Leahy and C. Forbes who did some ground

magnetic and electromagnetic surveys (VFL) and then was optioned to Lampe Resources.

Two drill holes, aimed to the north, were done in the NW part of the property on line

0+75E at 0+25N. The first hole was 61 meters long at a 45 0 dip while the other,

positioned 3 meters north of the first one, was 148m long at a 45 0 dip. These holes both

intersected the trachyte of the Timiskaming volcanic sequence but results obtained did

not show any significant values.

11


In 1981, Geo Indicators owned the northern part of claim #1167659 which was part of

the McGarry Gold option located north of the present property. One hole, with a north

direction and a dip of 45 0, is located on the actual line 1+75E at 2+50N. This hole

intersected the Timiskaming conglomerate but no significant mineralization was noted.

In 1984-85, Leahy completed a three hole drill program with two of them located on the

Geo Indicators portion of the property aimed towards the south. These two holes were

abandoned because of extensive caving. It is possible that these holes intersected the Ivan

Larder Fault but the hole coordinates written in the logs would place them too far north

of this structure to intersect the fault. The third hole was drilled from 1+45E, 1 + 10N

towards the south and intersected only trachyte. Analyses did not return any significant

results.

G. Mullan staked the property in December 1990. In 1992, he hired S.J. Carmichael to

do an exploration program which consisted of a geological, ground magnetic and

electromagnetic survey. Both geophysical surveys were done at a 25m line spacing, thus

allowing to locate more precisely the geological contact between the volcanic rocks

(magnetic high) and the conglomerates (magnetic low) which correspond to the Ivan

Larder fault. The electromagnetic survey (VLF-II) confirmed and located four interesting

conductors. A Maxi-Probe multi-frequency survey by Geoem Inc. on a few lines (3)

allowed a better understanding on the nature of the conductors.

The Ivan Larder Fault is traceable from both the VLF-II and Maxi-Probe surveys

(anomaly "A") a strong conductor. The conductivity is reported to increase toward the

east. A second deformation zone is interpreted to cross the central part of the property.

This central zone follows a Maxi-Probe anomaly over a strike length of 700 meters

(anomaly "B") and joins most historical showings within the property. The Maxi-Probe

survey report characterizes anomaly "B" as a "possible tight shear zone type target

surrounded by very high resistivity material, possibly quartz or silicification". A

northeast trending late brittle fault is also interpreted to cross the entire property based on

geophysical surveys. This late fault does not seem to have caused significant displacement of the volcanic and sedimentary sequences.

Kalahari Resources Inc. established an exploration program which commenced in

October of 1996 and was supervised by Anglaumaque Explorations Inc.

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6.0 1996 EXPLORATION PROGRAM

Prior to diamond drilling, the 17 lineal kilometer of grid was re-cut. Between October 8th

and 29th, 1996 a total of nine holes were drilled on the property. The total footage for the

1996 drilling program is 2583 feet (table 1). Among these holes, DDH 96REC-01 and

96REC-02 were stopped prematurely. Hole -01 was stopped in overburden after the casing

broke at a depth of 40 feet due to large boulders. The rig was moved 40 meters north and

hole 96REC-01A was successfully drilled. Hole 96REC-02 was abandoned at a depth of 121

feet due to excessive caving and sanding within the hole. Hole 96REC-02A was

subsequently drilled 5 meters from the original hole.

The following sections lists the target tested by each hole a gives a brief description of

the results obtained.

96REC-01A: The first hole was aimed to test the Ivan Larder Fault near the

northwest corner of the property where the fault waves, following a northeast (0700 AZ.)

direction which may represent a jog within the fault. These jogs create localized tension

openings favorable for quartz vein injections and gold mineralization.

0-56 Casing

56 - 196 Timiskaming ConglomerateRelatively massive but locally fractured. Alteration and

quartz veining is weak. Only traces of sulfides locally.

196-375 Sheared Timiskaming ConglomerateStrongly sheared and fractured conglomerates with intense

stretching of cobbles (5 to 1). Alteration consists of

gradually increasing carbonatisation, and hematization up

to a depth of 300 feet. Fuchsitic alteration is also progressively stronger. Quartz veining is mostly between

266 and 300 feet where it amounts to 2007o of the rock.

Pyrite is only found in trace amounts within the shear zone.

From 300 to 375, alteration is weak to moderate while up

to lOô of quartz veining is observed. At 338 feet, a one foot section contains 50*/^ quartz veining with 2Vo fine grained pyrite stringers within the vein.

" ;3 " :s ":; 'if^Âi'iAiii;ftEî^Jft^5feS;-ii^!i :;;

RECESSION LARDER PROPERTYTABLE 1: DIAMOND DRILLING STATISTICS

HOLE No.

96R EC-01

96REC-01A

96R EC-02

96REC-02A

96REC-03

96REC-04

96REC-05

96REC-06

96REC-07

LONG

275E

275E

900E

900E

200E

375E

400E

1425E

900E

LAT

175N

21 5N

200N

205N

01 5S

0403

110S

075S

255S

AZ

170

170

170

170

350

350

350

350

350

DIP

-50

-50

-50

-50

-45

-48

-50

-50

-45

FROM (ft)

0

0

0

0

0

0

0

0

0

TO (ft)

80

496

121

356

306

316

296

356

306

CUMMUL. (ft)

80

576

697

1053

1359

1675

1971

2327

2633

PLANNED EOH

500

500

350

350

300

300

300

350

300

START

08/10/96

09/10/96

16/10/96

1 7/1 0/96

18/10/96

19/10/97

20/10/96

21/10/96

23/10/96

FINISHED

09/10/96

16/10/96

17/10/96

18/10/96

19/10/96

20/10/96

21/10/96

23/10/96

29/10/96

COMMENTS

Test maxiprobe anomaly A, hole aband.

Test maxiprobe anomaly A

Test maxiprobe anomaly A, hole aband.

Test maxiprobe anomaly A

Test maxiprobe anomaly 3

Test maxiprobe anomaly B

Test maxiprobe anomaly C

Test maxiprobe anomaly B

Test maxiprobe anomaly D

a Umaqueexplorations inc.

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375 - 477 Sheared Timiskaming Trachyte375 - 401 : Strongly sheared trachyte with low hematiticalteration and moderate carbonate alteration. Up to 5 07oquartz veining with traces of pyrite is observed within theunit.401 - 477 : Moderately sheared trachyte with moderatehematization and up to 15 07o quartz veining in the form ofveinlets (^2 inches in width.). Traces of sulfides.

477 - 496 Massive Timiskaming TrachyteMassive and weakly chloritized trachyte. Traces of quartz veinlets locally.

496 End of Hole

The Ivan Larder Fault was therefore crossed between 196 and 477 feet. Deformation and alteration peaks at a depth of 300 feet. Although only minor sulfides were observed in this hole, the intensity of deformation and alteration confirms the potential of this important structure.

Assays obtained for this hole are quite disappointing. The best result is 110 PPB Au over 5 feet between 217 and 222 feet. Up to 507o quartz veining with traces of pyrite was observed within this interval. Nevertheless, the Ivan Larder Fault did contain detectable gold from 182 to 251 feet. Values within this interval range from 10 to 110 PPB Au.

96REC-02A: 500m east of the above target, the Ivan Larder Fault was tested where the coincident Maxi-Probe anomaly shows the strongest conductivity. This area is also 200m west of the northeast trending brittle fault.

O- 14 Casing

14-85.5 Timiskaming ConglomerateRelatively massive but locally fractured. Alteration and quartz veining is weak. Only traces of sulfides locally.

85.5-258 Sheared Timiskaming Conglomerate and TrachyteStrongly sheared and fractured conglomerates and trachyte at 700 to the core axis, with intense stretching of cobbles (5 to l). The contact with the trachyte is probably at 196 feet (strongly sheared therefore difficult to establish clearly).

15

angiaiimaqueexplorations inc.

Near the central portion of the shear, hematite and fucshite

alteration is very strong. Quartz is mostly is found as local veinlets. Pyrite is only found in trace amounts within the shear zone.

258 - 356 Altered Timiskaming TrachyteModerately foliated trachyte. Pervasive hematite alteration throughout. Locally moderately sericitized where quartz

veining is observed. Up to 3Vo pyrite in the sericitized wall rock of the veins309 - 331.5 : 5 to 4007o quartz veining with traces to 3 07o

pyrite (approx. Wo this entire section).

356 End of Hole

Hole 96REC-02A shows an net improvement in alteration, quartz veining and pyrite

mineralization compared to hole -O l A. This observation confirms the interpreted increase

in conductivity towards the east from the Maxi-Probe survey.

Although hole -02A was visually more promising, assay results of the hole were all below

100 PPB Au. The highest value is 90 PPB Au over 3.5 feet (313 to 316.5 feet) from a

strongly sericitized trachyte containing 25^0 quartz veining and 3*^b fine pyrite. This interval

lies well below the fault itself.

Holes 96REC-03 and -04 are located 175 meters from each other and tested the Maxi-Probe

B anomaly. The holes were strategically located where old pits revealing quartz veining

were noted.

96REC-03:

O- 10 Casing

10-175 Hematized Timiskaming TrachyteModerately hematized fine grained, massive trachyte. Local quartz veining and associated sericite alteration as follows:

23-81 : 2007o quartz veins (some up to 3 feet wide), moderately sericitized, traces of pyrite

175-226 Hematized Timiskaming Fragmental TrachyteAs at 10 to 175 apart from the presence of up to 25ô strongly hematized fragments ^cm. Locally moderately

16

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sericitized. From 175 to 187, injection of 5 to 2007o quartz veinlets with traces to 3ô fine grained pyrite.

226 - 306 Massive Green Timiskaming Fragmental TrachyteAs 1 75 to 226 but without the alteration. It is fresh looking. Only minor quartz veinlets with traces of pyrite.

306 End of Hole

The two sections containing quartz veining probably correspond to the two pits mapped

near the collar of the hole.

96REC-04:

Hole was collared 175 meters east of hole -03 on October 19th 1996. The target for this hole was a linear magnetic anomaly coincident with the Maxi-Probe anomaly. The hole

reached bedrock at a depth of l O feet and was stopped at a depth of 306 feet on October 20th 1996.

The rock encountered consists of a monotonous sequence of weakly to moderately hematized fragmental trachyte. It is locally magnetic in the center of the hole (which

explains the targeted anomaly). Only minor quartz veining and traces of pyrite was noted.

Although hole -03 encountered significant quartz veining along with up to Wo pyrite, the

only anomalous gold value obtained is 140 ppb Au over 5 feet (61 to 66 feet) from a

moderately sericitized trachyte containing I 07o disseminated pyrite in 10*54 quartz veining. Hole -04 encountered a monotonous sequence of hematized trachyte and assay results are all below 0.0 1 g/tAu.

96REC-05: Hole 96REC-05 tested anomaly C (Maxi-Probe) along with down dip

extension of an old pit which returned a assay result of 557 ppb Au (grab sample). The hole

was collared 100 meters southeast of hole -04.

0-20 Casing

20 - 89 Timiskaming WackeModerately carbonated and well foliated wackes showing good bedding locally. A fold axis was also noted at a depth of 79 feet. Assuming that the foliation strikes perpendicular to the hole, the fold observed is a tight fold plunging 30 to

17


400 to the east. Only minor quartz veining and traces of disseminated pyrite was observed in the sediments.

89 - 296 Hematized Fragmental TrachyteMassive, weakly carbonated but strongly hematized trachyte. Only rare white quartz veins were seen. Traces of pyrite in the trachyte.From 263 to 267 feet a quartz vein containing SO'Ki brecciated trachyte fragments was noted. It contains Q.5% pyrite and traces of chalcopyrite.

296 End of Hole

No significant assays were obtained from this hole.

96REC-06: Hole 96REC-06 was designed to test a moderate VLF anomaly located

near the eastern limit of the property. Immediately east of the property limit, a band of

sedimentary rocks are shown on government geological maps.

0-38 Casing

38-306 Hematized Fragmental TrachyteMassive, weakly carbonated but strongly hematized trachyte. Only rare white quartz veins were seen. Traces of pyrite in the trachyte.

From 42 to 49: moderately sheared fragmental trachyte which is locally strongly sericitized and contains traces of pyrite associated with the sericite.

306 End of Hole

96REC-07; The presence of the carbonated wackes in hole -05 added significantly

to the potential of anomaly D located 80 meters south of anomaly C, as it would occur in the

center of the sedimentary package. In light of this new information, a proposed hole -07 to

test anomaly D on line 9^00E was established.

18

angldllmaqueexplorations inc.

0-46 Casing

46-126 Hematized Fragmental TrachyteMassive, weakly carbonated but strongly hematized trachyte. Only rare white quartz veins were seen. Traces of pyrite in the trachyte.

126-306 Wackes and siltstoneModerately carbonated and well foliated wackes showing good bedding locally.From 179 to 196 the wackes are moderately sheared and well carbonated. 5 07o quartz veinlets with traces of pyrite throughout the shear. P/o chalcopyrite within the veinlets from 182 to 184 feet.

306 End of Hole

Hole 96REC-07 did confirm the continuity of the sedimentary package but only the

narrow shear zone observed within the sediments can serve as an explanation for the

Anomaly D.

Unfortunately, results were quite disappointing as no samples assayed more than 0.10 g/t Au.

7.0 DISCUSSION

The 1996 drilling program followed a detailed mapping and geophysical program which

included Mag, VLF, and Maxi-Probe multi-frequency surveys. The most significant

feature identified in the field and on the geophysical maps was the Ivan Larder Fault

which runs across the northern part of the property. Drilling along this trend did

encounter strong shearing, alteration and quartz veining with local pyrite mineralization.

The gold values obtained though are very low, but consistently in detectable quantities in

hole -01. Although quite disappointing, the samples rarely contained significant amounts

of sulphides.

The drill program also helped to better define the stratigraphy in the southeast portion of

the property. Hole -05 encountered altered sedimentary rocks which are also sheared. No

significant gold values were obtained from this hole but the lack of sulphides within the

shear explains the low values.

19

angldLimaqueexplorations inc.

The altered and sheared sedimentary unit still holds excellent potential of hosting

economic gold mineralization. In order to select better targets along this shear zone, an IP

survey should be done to locate coincident chargeable sections. In addition, other

potential targets may be defined elsewhere in this overburden covered area. For example,

the ENE trending Bear Creek follows a subtle depression which could hide an important

fault zone. Current available data does not justify diamond drilling below the creek but

an IP survey may provide targets along this trend.

The Recession Larder Prospect has similar geology, structure and alteration to other

surrounding properties where gold mineralization does occur in economic concentrations.

The 1996 exploration program added significantly to our knowledge of the property,

establishing the structural nature of the Ivan Larder Fault and locating other significant

structures such as within the sediments in the eastern part of the property. Adding an IP

survey to the existing database could provide specific targets along the favourable

structures already defined and may point to new areas where no work has been done so

far.

20


8.0 CONCLUSION

1- The Recession Larder Property is underlain by trachytes and conglomerates.

A fine sedimentary sequence also occurs near the southwest portion of the

property.

2- The background gold content on the claim group is very low. Most samples

returned values of less than 5 ppb Au. The highest value obtained is 140 ppb

Au in hole -03. Hole -01 did return detectable gold values across a good portion of the Ivan Larder Fault.

3 - A new shear zone within fine grained sediments in the southwest portion of

the property was uncovered. Although little sulphide was noted, it does

represent a new potential structure for gold mineralization.

4- The low values are explained by the lack of significant sulphide

mineralization in most holes. The Maxi Probe anomalies tested are related

to topographical features, some caused by important shearing.

9.0 RECOMMENDATIONS

1 - The grid should be covered by a new geophysical survey. Mag-VLF and IP

should be done in order to better define the deformation zones and locate

significant sulphide mineralization within structures.

2 - A further 2 500 feet (760 meters) should be completed to test the most

promising geophysical targets. Some footage should also be reserved to testing

the area below Bear Creek. A NNE trending structure could follow the river.

21


10.0 BUDGET

l - Geophysics:Complete magnetic, VLF, and I.P. survey over the entire grid,

17kmatS900perkm

2 - Diamond Drilling:Approximately 5 holes - 500 feet each,

2 500 feet at S25 per foot

S15300

S62 500

SUBTOTALcontingencies (~1007o)

TOTAL

S77 800 S7800

S85 600

r

Richard Roy

22

angldLimaqueexplorations inc.

REFERENCES

Armistice Resources Ltd., Annual Report. 1989

Carmichael, S.J., 1992: Report on the Recession Larder Gold Property, McGarry Twp.

internal report for 297 3090 Canada Inc.

Deak Resources Corp., Annual Report. 1989-1990

Deer W.A. et al 1966: An Introduction to Rock Forming Minerals, ed. John Wiley

and Sons Inc.

Pyke D.R. 1982: Geology of the Timmins Area, District of Cochrane; Ontario Geological

Survey Report 219, 141p. Accompanied by Map 2455, Scale 1:50 000, 3

Charts, and l Sheet Microfiche.


23

APPENDIX l

DIAMOND DRILL LOGS

Anglaumaque Explorations Inc,

COMPANYPROJECT

DRILL HOLETOWNSHIP

CLAIM

KALAHARI RESOURCES INC.RECESSION LARDER (M)96REC-01MC 6ARRY1167660

LOTZONE

. REF.RANGE

NTS

PRINTED : November 24,199?

32D/04

COORDINATES AT COLLAR

GRID 11LINE

STATIONELEVATION

02+75E OH75N 10000.000

GRID 12LINE : OOtOOE

STATION : 00+OON ELEVATION : 0.000

GRID *3LATITUDELONGITUDEELEVATION

.000

GRID MLATITUDELONGITUDEELEVATION

175.000275.000

10000.000

SAMPLING

BASIC ASSAYS LITHOLOGY

DATE

NONE

PEOPLE

GEOLOGISTCONTRACTOR

RELOG

RICHARD ROY FORAGE VAL D'OR

DATE OF JOURNALSURVEY DATE

CEMENTING DATE

DRILLING STARTED DRILLING FINISHED

October 08,1996 October 09,1996

LENGTH COLLAR FINAL : 24.38

CORE STORED : NO CORE SIZE : NONE CASING LEFT : No

PURPOSETARGETREMARKS

TEST ANOMALY MAXIPROBE A IVAN LARDER FAULT HOLE ABANDONED IN OVERBURDEN Grid aziauth 350 degrees

DIRECTIONAL DATA AZIMUTH : 170 1 O' DIP : -50' O 1

Anglaumaque Explorations Inc.

FROM (PI)

TO DESCRIPTION

0.00 24.38 CAS.RRR

CASINGCasing removed.Hole abandoned in overburden due to large boulders.

24.38 END OF HOLE

PAGE: 2 GEOLOGICAL DESCRIPTION HOLE NO; 96REC-01


COMPANY KALAHARI RES : PROJECT RECESSION LA DRILL HOLE 96REC-01A

TOWNSHIP MC GARRY CLAIM 1167660


GRID #1 LINE 02+75E

STATION 02+15N ELEVATION 10000.000

SAMPLING

1 BASIC ASSAYS : 101-168 LITHOLOGY :

PEOPLE

1 GEOLOGIST : RICHARD CONTRACTOR : FORAGE V

RELOG :

LENGTH

' CORE STORED :

PURPOSE TEST ANOMALY TARGET IVAN LARDER REMARKS Grid azimuth

OURCES INC. RDER (M)

GRID S2 LINE 00+OOE

STATION 00400N ELEVATION 0.000

ROY AL D'OR

COLLAR : 0.00

ANGLAUMAQUE OFFICE

MAXI PROBE A FAULT 350 degrees

LOT ZONE

NO. REF. RANGE

NTS 32D/04

GRID #3 LATITUDE : LONGITUDE : ELEVATION :

FINAL : 151.18

SIZE : BQ

PRINTED : November

GRID #4 ).000 LATITUDE : ),000 LONGITUDE : ),000 ELEVATION : 1

DATE

DATE OF JOURNAL SURVEY DATE

PFUFMTTWR RiTF

DRILLING STARTED : October 09 DRILLING FINISHED : October 16

CASING LEFT : No

24,1997

215.000 275.000 0000.000

,1996 .1996

DIRECTIONAL DATA AZIMUTH : 170' O' DIP : -50* O'

Length Azimuth Dip

30.48 170 O' -52 O'74.68 170 O'91.44 170 O 1121.92 170 O'151.18 167 O 1

-50 O 1-49 O 1-49 O 1-47 O 1


FROM TO W

DESCRIPTION

0,00

17.07

17.07

59.74

59.74 114.30

114.30 145.C

145,( 151.18

151.18

CAS.RRR

CASINGCasing removed.

S4F,Mas,lFol,nGN

POLYGENIC MATRIX SUPPORTED CONGLOMERATEMassive unaltered polygenic conglomerate with 20 to 50X fragments ()2 in). Weakly foliated and stretching of fragments (2 to 1). Fragments composed of 30X granitic, 40X volcanic and 30X sedimentary (wackes with minor cherts and jasper). Rare quartz veining and traces of sulfides.

56.08 - 59.74 ZFrc,nFrc,lCar,2VNq(py)

FRACTURED ZONEModerately fractured conglomerates. Fracturing at 45 to 90 degrees to the core axis. Foliation still weak at 45 degrees to the core axis. Low carbonate alteration throughout and low hematization locally. A pyrite rich fragment? found at 185.5 feet.

M8,ssShr65,S4F,lCar,lFuc,lHem(VNqc)

SHEARED CONGLOMERATEStrongly sheared and fractured conglomerate at 65 degrees to the core axis. A gradual bleaching gives it a light green color. Local carbonate, fucshite and hematite alteration throughout. Minor quartz carbonate veining with traces to 1X fine pyrite and traces of chalcopyrite locally. Pyrite is very fine grained. Lost core locally as described below.

62.18 - 63.25 LC

LOST CORE

LC

LC

LC

67.67 - 68.43

LOST CORE

70.56 - 71.32

LOST CORE

73.15 - 73.76

LOST CORE

M8,n-sShr,Y2D,sChl,sCar,lHen(VNqc)

MODERATELY TO STRONGLY SHEARED TRACHYTEStrongly chloritized and sheared trachyte. Shearing at 45 degrees to the core axis. Local faint hematitealteration observed. Quartz veining is low in the strongly sheared section but increases within themoderately sheared trachyte near the end of the section, irdecreases down hole.

V2D,Mas,fg,nChl,mCar l lHem

Traces of pyrite throughout. Shearing gradually

MASSIVE TRACHYTEMassive weakly foliated trachyte at 50 degrees to the core axis. It is fine grained, locally showingfragmental texture. Weakly hematized and moderately chloritized, Some sections are well carbonated.

END OF HOLE

PAGE: 2 GEOLOGICAL DESCRIPTION HOLE NO: 96REC-01A


FROM ("i)

55.47

56.08

56.69

58.22

59.74

61.26

63.25

65.38

66.14

68.43

69.49

71.32

71.93

73.76

74.98

75.59

76.50

77.11

78.03

78.94

80.16

81.53

84.12

85.65

87.17

88.09

88.85

90.53

92.35

93.88

95.40

TO ( )

56.08

56.69

58.22

59.74

61.26

62.18

65.38

66.14

67.67

69.49

70.56

71.93

73.15

74.98

75.59

76.50

77.11

78.03

78,94

60.16

81.53

84.12

85.65

87.17

88.09

88.85

90.53

92.35

93.88

95,40

96.32

DESCRIPTION

Massive conglomerate, trace pyrite.

One to tKO inch pyrite quartz fragment, probably vein fragment, strongly fractured pyrite.

Moderately fractured conglomerate, trace fine grained pyrite, weakly carbonatized.

As above,

Moderately sheared conglomerate, 5X quartz vein fragments, trace pyrite.

As above, 205! lost core.

305! quartz veining, strongly shreared, 15! fine grained pyrite.

As above, trace pyrite.

55! quartz veining, strongly sheared, trace pyrite.

Strongly sheared, trace quartz vein, trace pyrite.

As above.

205! quartz vein, 0.5X fine grained pyrite.

As above,

Moderately bleached, moderately carbonatized, trace pyrite.

As above, 205! quartz vein, 0.5X fine grained pyrite.

As above.

155! quartz carbonate vein, 0.55! pyrite.

As above, strongly bleached, trace pyrite.

As above.

As above.

As above, 105! quartz veinlets.

505! lost core, 30X quartz, trace pyrite.10X quartz veining, trace pyrite.

Moderately bleached, 105! quartz carbonate, trace pyrite.

As above.

Strongly bleached igneous clast, trace pyrite.Strongly bleached, 105! lost core, trace pyrite.As above.

As above.

As above, 25! quartz carbonate vein, trace pyrite.

As above.

SAMPLE N.

101

102

103

104

105

106

107

108

109

110

111

112

113

114

115

116

117

118

119

120

121

122

123

124

125

126

127

128

129

130

131

LENG. (i)

0.61

0.61

1.53

1.52

1.52

0.92

2.13

0.76

1.53

1.06

1.07

0.61

1.22

1.22

0.61

0.91

0.61

0,92

0,91

1.22

1.37

2.59

1.53

1.52

0,92

0.76

1.68

1.82

1.53

1.52

0.92

AU1 PPB

30

10

10

20

20

20

10

110

10

^

30

30

10

10

^

90

^

^

^

(5

^

^

^

20

^

^

^

^

^

^

^

AU2 G/T

AUCHK PLP PPB

100

10

(5

AUCHK REJ PPB

50

50

^

PAGE: 3 ASSAY SAMPLE RESULTS #1 HOLE NO: 96REC-01A


FROM (i)

96.32

97.84

99.36

100.28

101.50

102.72

103.17

103.94

105.46

106.98

108.51

110.03

111.56

113.08

114.30

115.82

117.04

117.65

119.18

120.70

122.22

123.75

125.27

126.80

128.32

129.84

131.37

132.89

134.42

135.94

137.46

138.99

TO (m)

97.84

99.36

100.28

101.50

102.72

103.17

103.94

105.46

106.98

108.51

110.03

111.56

113.08

114.30

115.82

117,04

117.65

119.18

120.70

122.22

123.75

125.27

126.80

128.32

129.84

131,37

132.89

134.42

135.94

137.46

138.99

140.51

DESCRIPTION

As above.

As above.

As above.

Weakly bleached, 2X quartz vein, trace pyrite.

As above.

30X quartz veining, 2X fine grained pyrite, strongly bleached.

As above, trace pyrite.

fleakly bleached, 2X quartz veinlets, trace pyrite.

As above.

As above.

As above.

As above.

As above.

As above.

Strongly sheared trachyte, 10X quartz carbonate vein, trace pyrite.

As above, 2X quartz vein.

As above.

As above.

As above.

As above,

5X quartz veining perpendicular to the foliation, trace pyrite.

As above.

As above,

10X quartz veining parallel and perpendicular to the foliation, trace pyrite.

As above.

As above.2X quartz veining perpendicular to the foliation, trace pyrite.

As above.

As above.

As above.

As above.

5X quartz veinlets parallel to the foliation, trace pyrite.

SAMPLE N.

132

133

134

135

136

137

138

139

140

141

142

143

144

145

146

147

148

149

150

151

152

153

154

155

156

157

158

159

160

161

162

163

LENG. (m)

1.52

1.52

0.92

1,22

1.22

0.45

0.77

1.52

1.52

1.53

1.52

1.53

1.52

1.22

1.52

1.22

0,61

1.53

1.52

1.52

1.53

1.52

1,53

1.52

1.52

1,53

1.52

1.53

1.52

1.52

1.53

1.52

AIM PPB

^

20

^

^

10

(5

^

^

(5

^

^

(5

^

(5

20

^

^

^

(5

^

(5

^

^

^

AU2 6/T

^.10

^.10

^.10

-:0.10

^.10

^.10

^.10

^.10

AUCHK PLP PPB

^

5

AUCHK REJ PPB

^

^

j

PAGE: 4 ASSAY SAMPLE RESULTS #1 HOLE HO: 96REC-01A


FROM ( )

HO. 51

142.04

143.56

145.08

146.61

TO ( )

142.04

143.56

145.08

146.61

148.13

151.18

DESCRIPTION

As above.As above.As above.

Massive fragmental trachyte, 2X quartz carbonate veinlets, trace pyrite.As above.

END OF HOLE

SAMPLE N.

164

165

166

167

168

LENG. (n)

1.53

1.52

1.52

1.53

1.52

AU1 PPB

AU2 6/T

(0.10

(0.10

(0.10

(0.10

(0.10

AUCHK PLP PPB

AUCHK REJ PPB

PAGE: 5 ASSAY SAMPLE RESULTS Si HOLE NO: 96REC-01A


COMPANY KALAHARI RESOURCES INC. PROJECT RECESSION LARDER (M)

DRILL HOLE 96REC-02 TOWNSHIP MC GARRY

CLAIM 1167660


GRID fi LINE 09+OOE

STATION 02400N ELEVATION 10000.000

GRID 12 LINE

STATION ELEVATION

LOT ZONE

NO. REE. RANGE

NTS 320/04

GRID S3 00+OOE LATITUDE : ( 00+OON LONGITUDE : ( 0.000 ELEVATION ; (

SAMPLING

BASIC ASSAYS : 241-251 LITHOLOGY :

PEOPLE

1 GEOLOGIST RICHARD ROY 1 CONTRACTOR FORAGE VAL D 'OR

RELOG

LENGTH

CORE STORED :

COLLAR :

ANGLAUMAQUE OFFICE

PURPOSE TEST ANOMALY MAXIPROBE A TARGET IVAN LARDER FAULT

REMARKS Hole abandoned due to fault down Grid azimuth 350 degrees

0.00 FINAL : 36.88

SIZE : BQ

PRINTED : November 24,1997

GRID 14 1.000 LATITUDE : 200.000 1.000 LONGITUDE : 900.000 1.000 ELEVATION : 10000.000

DATE


CEMENTING DATE


CASING LEFT : No

.1996 ,1996

hole, Core barrel jammed, Lost Material in hole.

DIRECTIONAL DATA AZIMUTH : 170* O 1 DIP : -50* O'

Anglaumaque Explorations Inc,

FROM (n)

TO DESCRIPTION

4.86 CAS.RRR

CASING. Casing removed.

4.88 19.81 S4F,Mas,lFol,GN

POLYGENIC MATRIX SUPPORTED CONGLOMERATE.Massive unaltered polygenic conglomerate. 20-50X fragments )2 inch diameter.Weakly foliated Kith stretching 2-1 locally. Fragments composed of 30X granitic, 40X volcanic (trachyte) and30X sedimentary (wacke, minor cherts and jasper).Rare quartz veimng and traces of sulfides. Matrix is wacke in composition.Local sections of homogeneous wacke with less than 10X larger clasts.

19.81 - 36.88 M8,ssShr70,S4F,lCar,mHeii,mChl

SHEAR ZONE.Moderately to strongly sheared conglomerate at 70 degrees to core axis. Generally weakly carbonated,moderately hematized, and chloritized.Contains local volcanic or wacke sections (difficult to establish, strongly chloritized). Stretchingof up to 5 to 1. Only minor quartz veinlets and traces of pyrite,

36.88 END OF HOLE

PAGE: 2 GEOLOGICAL DESCRIPTION HOLE NO: 96REC-02


FROM W

19.81

21.34

23.16

24.69

26.21

27.74

29.26

30.78

32.31

33.53

35.36

TO (m)

21.34

23,16

24.69

26.21

27.74

29,26

30.78

32,31

33.53

35.36

36.88

36.68

DESCRIPTION

Moderately chloritized, volcanics or wacke,traces quartz vein, traces pyrite.Strongly sheared volcanics or wacke at 45 degrees to core axis, 5X carbonate veinlets,traces pyrite.

As above, traces veins, traces pyrite.As above.

Moderately henatized conglomerate, moderately chloritized, traces vein, traces pyrite.As above.

As above.

As above.As above.As above.Strongly chloritized volcanics, 10X carbonateveinlets, traces pyrite.END OF HOLE

SAMPLE fi.

241

242

243

244

245

246

247

248

249

250

251

LENG. ("l)

1.53

1.82

1,53

1.52

1.53

1.52

1.52

1.53

1.22

1.83

1.52

AU1 PPB

AU2 G/T

10.10

10.10

10.10

10.10

10.10

10.10

10.10

10.10

10.10

10.10

10.10

AUCHK PLP PPB

AUCHK REJ PPB

PAGE: 3 ASSAY SAMPLE RESULTS #1 HOLE NO: 96REC-02


COMPANY KALAHARI RESOURCES INC, PROJECT RECESSION LARDER (M)

DRILL HOLE 96REC-02A TOWNSHIP MC 6ARRY

CLAIM 1167660


GRID 11 GRID 12 LINE 09tOOE LINE 00+OOE

STATION 02+05N STATION 00+OON ELEVATION 10000.000 ELEVATION 0.000

SAMPLING

BASIC ASSAYS : 281-341 LITHOLOGY :

PEOPLE

GEOLOGIST RICHARD ROY CONTRACTOR FORAGE VAL D 'OR

RELOG

LJLNGIH COLLAR : 0.00

CORE STORED : ANGLAUMAQUE OFFICE

PURPOSE TEST ANOMALY MAXIPROBE A TARGET IVAN LARDER FAULT

REMARKS Grid azimuttl 350 degrees

LOT ZONE

NO. REF. RANGE

NTS 32D/04

GRID 13 LATITUDE t

LONGITUDE ( ELEVATION (

FINAL : 108.51

SIZE : BQ

PRINTED : November

GRID #4 .000 LATITUDE : 1.000 LONGITUDE : .000 ELEVATION : 1

DATE


PFUFWTTWfi DATF


CASING LEFT : No

24,1997

205.000 900.000

0000.000

.1996

.1996

DIRECTIONAL DATA AZIMUTH : 170' O 1 DIP : -50 s O'

Length Azimuth Dip

60.96 170 O' -49 O' 100.58 170 O' -46 O'


FROM TO (m)

DESCRIPTION

0.00 4.27 CAS.RRR


1.27 26.06 S4F,Has,lFol,GN

POLYGENIC MATRIX SUPPORTED CONGLOMERATE.Massive unaltered polygenic conglomerate, 20-50X fragments >2 inch diameter.Keakly foliatedwith stretching 2-1 locally. Fragments composed of 30X granitic, 40X volcanic (trachyte) and305! sedimentary (wacke, minor cherts and jasper),Rare quartz veining and traces of sulfides. Matrix is wacke in composition.Local sections of homogeneous wacke with less than 10X larger clasts.

26.06 78.64 M8,ssShr70,S4F,lCar,in-sHei),iiChl ,(sFuc)

SHEAR CONGLOMERATE AND TRACHYTE.Moderately to strongly sheared conglomerate and trachyte at 70 degrees to core axis,Contains local volcanicor wacke sections (Difficult to establish, strongly chloritized).Stretching of up to 5 to 1. Near the central portion of the shear, hematite and fucshite alteration is verystrong.Local sections are also strongly carbonated. Some occasional quartz veinlets and traces to IX of pyrite.The contact between the conglomerate and the volcanics is approximately at 196 feet but deformation intensitymakes it difficult to establish precisely.

78.64 108.51 Y2D,nFol60,llHem,llSil,(mSer)

FOLIATED TRACHYTE.Moderately foliated trachyte with foliation at 60 degrees to core axis. A pervasive moderately hematizationalso exist throughout.The rock is only locally weakly carbonated and generally moderately sililcified. Locally moderatelysericitized associated with veining.Most veins are between 309 and 331.5 feet with traces to 3X py locally in walls of veins,

108,51 END OF HOLE

PAGE: 2 GEOLOGICAL DESCRIPTION HOLE NO: 96REC-02A


FROM (m)

26.06

27.74

2S.26

30.78

32.31

33.83

35.36

36,88

38.40

39.93

41.45

42.98

44.50

46.02

47.55

49,07

49.68

50.60

52.12

53.64

55.17

56.69

58.22

59,74

61,26

62.79

64.31

65.84

67.36

TO ( )

27.74

29.26

30.78

32,31

33,83

35.36

36.88

38.40

39.93

41.45

42,98

44,50

46.02

47.55

49.07

49.68

50.60

52.12

53.64

55.17

56.69

58.22

59.74

61.26

62.79

64.31

65.84

67.36

68.88

DESCRIPTION

Moderately sheared at 45 degrees to core axis, strongly chloritized volcanics traces pyrite.

As above.

Moderately sheared conglomerate at 45 degrees to core axis, traces pyrite.

As above, weakly hematized.

Strongly sheared conglomerate at 60 degrees to core axis, noderately hematized, strongly chloritized, traces quartz, traces pyrite.

As above,

As above,

As above.

As above.

Strongly hematized sheared conglomerate, 2X quartz veining.

As above.

As above.

Moderately sheared conglomerate, traces quartz veining, traces pyrite.

As above,

Strongly fucshitized conglomerate, strongly bleached 10X quartz veiniets, traces pyrite.

As above.

Hematized and moderately carbonated, strongly sheared, 55! quartz veiniets, traces pyrite.

As above.

As above.

As above.

Strongly sheared, moderately chloritized, minor folding of shear at 184.5 feet, traces pyrite.

Strongly sheared, moderately chloritized, 10X quartz carbonate vein, traces pyrite.

Strongly henatized strongly sericitized, weakly fucshitized, 5X qtz ankerite vein, traces pyrite.

As above.

As above, 10X qtz ankerite vein.

Strongly henatized, weakly sericitized, tr quartz vein, traces pyrite.

As above.

Strongly henatized with moderate lueshite, 2X quartz vein, traces pyrite.

Moderately hematized, weakly sericitized, traces quartz, traces pyrite.

SAMPLE N.

281

282

283

284

285

286

287

288

289

290

291

292

293

294

295

296

297

298

299

300

301

302

303

304

305

306

307

308

309

LEN6. (m)

1.68

1.52

1.52

1,53

1,52

1.53

1.52

1.52

1.53

1.52

1.53

1,52

1.52

1.53

1.52

0.61

0.92

1.52

1.52

1.53

1.52

1.53

1.52

1.52

1.53

1.52

1.53

1.52

1.52

AIM PPB

15

AU2G/T

10.10

10.10

10.10

10.10

10.10

10.10

10.10

10.10

10.10

10,10

10,10

10,10

10.10

10,10

10.10

10.10

10.10

10.10

10.10

10.10

10.10

10,10

10.10

10.10

10.10

10.10

10.10

10,10

AUCHK PLP PPB

15

AUCHK REJ PPB

15

PAGE: 3 ASSAY SAMPLE RESULTS H HOLE NO: 96REC-02A


FROM W

68.88

70.41

71.93

73.46

74.98

76.50

78.03

78.64

79.55

81.08

82.60

84.12

85.65

87.17

88.70

90.22

91.74

93.27

94.18

94.79

95.40

96.47

97.23

97.69

98.45

99.36

100.28

101.04

102.41

103.94

TO W

70.41

71.93

73.46

74.98

76.50

78.03

78.64

79.55

81.08

82.60

84.12

85.65

87.17

88.70

90.22

91.74

93.27

94.18

94.79

95.40

96.47

97.23

97.69

98.45

99.36

100.28

101.04

102.41

103.94

105.46

DESCRIPTION

As above.

As above.

As above.

As above,

As above.

As above.

As above.

Moderately foliated, noderately hematized trachyte, 5X quartz carbonate veinlets, traces pyrite.

As above.

As above.

As above.

As above.

As above.

Moderately sericitized with 15X quartz veinlets, 0.5X pyrite.

Moderately hematized trachyte, 5X quartz veinlets at 40 degrees to core axis.

As above.

As above.

As above,

Strongly sericitized with 405! quartz veining, 2X fine grained pyrite.

Moderately sericitized trachyte, traces quartz, traces pyrite.

25X veining and 3X fine grained pyrite in strongly sericitized trachyte.

As above, 0.5X pyrite.

Moderately sericitized, 2X quartz veinlets, traces pyrite.

30X quartz veining, 0.5X pyrite in sericitized trachyte.

Moderately hematized trachyte, traces of pyrite.

30X quartz veining in strongly sericitized trachyte, 0.5X pyrite.

Moderately sericitized trachyte, 2X quartz veinlets, traces to 0.5X pyrite.

As above.

As above.

As above.

SAMPLE N,

310

311

312

313

314

315

316

317

318

319

320

321

322

323

324

325

326

327

328

329

330

331

332

333

334

335

336

337

338

339

LENG. (m)

1.53

1.52

1.53

1.52

1.52

1.53

0.61

0.91

1.53

1.52

1.52

1.53

1.52

1.53

1,52

1.52

1.53

0.91

0.61

0.61

1.07

0.76

0.46

0.76

0.91

0.92

0.76

1.37

1.53

1.52

AU1 PPB

^

^

(5

(5

^

^

^

^

^

^

^

^

^

(5

^

^

10

^

20

^

90

10

10

^

^

(5

50

^

^

^

AU2 G/T

AUCHK PLP PPB

20

50

^

AUCHK REJ PPB

30

50

(5

PAGE: 4 ASSAY SAMPLE RESULTS tl HOLE NO: 96REC-02A


FROM W

105.46

106.98

TO ( )

106.98

108.51

108.51

DESCRIPTION

As above.

As above.

END OF HOLE

SAMPLE N.

340

341

LENG. (m)

1.52

1.53

l

AU1 PPB

^

^

AU2 6/T

AUCHK PLP PPB

AUCHK REJ PPB

PAGE: 5 ASSAY SAMPLE RESULTS li HOLE NO: 96REC-02A

Anglaumaque Explorations Inc

COMPANY KALAHARI RESOURCES INC. PROJECT RECESSION LARDER (M)

DRILL HOLE 96REC-03 TOWNSHIP MC GARRY

CLAIM 1167659


GRID *1 LINE 02+OOE

STATION 00+15S ELEVATION 10000,000

GRID #2 LINE 00*OOE

STATION OOtOON ELEVATION 0.000

LOT ZONE

NO. REF. RANGE

NTS 32D/04

GRID 13 LATITUDE : (

LONGITUDE : ( ELEVATION : (

SAMPLING

BASIC ASSAYS : 342-365 1 LITHOLOGY :

PEOPLE

GEOLOGIST RICHARD ROY CONTRACTOR FORAGE VAL D 'OR

RELOG

LENGTH

CORE STORED :

COLLAR : 0.00

ANGLAUMAQUE OFFICE

FINAL : 93,27

SIZE : BQ


GRID 14 ).000 LATITUDE -15.000 ).000 LONGITUDE 200.000 J.OOO ELEVATION 10000.000

DATE


CEMENTING DATE


CASING LEFT : No

.1996

.1996

PURPOSE TEST ANOMALY MAXIPROBE B TARGET Central Showings REMARKS Grid azinuth 350 degrees.

DIRECTIONAL DATA AZIMUTH : 350' O 1 DIP : -45* O'

Length Azinuth Dip

30.48 350 O' -45 O 160.96 350 O' -45 O'91.44 350 O' -44 O 193.27 348 O' -40 O 1


FROM (l)

TO (n)

DESCRIPTION

0.00 3.05 CAS.RRR


3,05 53.34 V2D, Mas, tiHei, rCar, (VNq.nSer)HEMATIZED TRACHYTE.Moderately hematized and carbonated trachyte. It is massive and reddish in color from hematite. Pervasivemoderately henatization exist throughout.Abundant quartz veining, mostly between 23 and 81 feet. Moderate sericite alteration associated with veiningalong with traces of pyrite in the walls of the veins. Local minor galena in the veins.

7.01 - 24.69 ZVNq,i)Ser,mHem,mCar

ZONE OF QUARTZ VEINS.Zone containing 20X Quartz veins, some up to 3 feet wide. Walls of veins are moderately sericitizedand contain traces of pyrite.Core angles of veins varies from 20 to 70 degrees to the core axis.

53.34 68.88 V2D,Frg,mHem,mCar,(VNq,mSer)

HEMATIZED FRAGMENTAL TRACHYTE.Moderately hematized and carbonated trachyte. It is massive and reddish in color from hematite. Contains 25Xstrongly nematized autoclasts ()2cm).Pervasive moderately hematization exist throughout. Stronger sericite associated with quartz veining.

53.34 - 57.00 ZVNq,mSer,iiHem,mCar,3py

ZONE OF QUARTZ VEINS.Zone containing 2OX quartz veins. Halls of veins are moderately sericitized and contain traces to 3Xof pyrite.Core angles of veins varies from 20 to 70 degrees to the core axis.

68.88 93.27 V2D,6N,Frg,Mas,5VLqc

GREEN FRAGMENTAL TRACHYTE.Massive unaltered fragmental trachyte. Shows some minor chloritization associated with 5X quartz carbonateveinlets throughout. No sulfides.

93.27 END OF HOLE



FROM (n)

6.40

7.01

7.92

8.53

9.45

10.06

10.97

12.50

17.07

18.59

20.12

21.64

23.16

24.69

49.07

50.60

52.12

53.34

54.25

55.78

56.54

57.00

58.22

59,74

TO (m)

7.01

7.92

8.53

9.45

10.06

10.97

12.50

14.02

18.59

20.12

21.64

23.16

24.69

26.21

50.60

52.12

53.34

54.25

55.78

56.54

57.00

58.22

59.74

61.26

93.27

DESCRIPTION

Massive henatized trachyte, traces pyrite.

10X qtz injections, 1X galena in vein, tracepyrite.

Massive hematized trachyte, traces pyrite.

Quartz carbonate vein at 60 degrees to coreaxis, bull white, traces galena.

2X quartz veinlets, traces pyrite.

Quartz carbonate vein at 60 degrees to coreaxis, 1X galena, bull white.

30X pink color quartz injections, tracespyrite.

IX disseminated pyrite in massive hematizedtrachyte.

35X quartz injections in massive hematizedtrachyte, traces pyrite.

IX disseminated pyrite in hematized andsericitized trachyte with 10X quartzinjections,

As above, 5X quartz injections.

As above, 5X quartz injections.

Hera t i zed trachyte, traces pyrite.

As above.

Hematized trachyte, traces pyrite.

As above, 2X quartz veinlets at 30 degrees tocore axis,

As above.

Moderately sericitized trachyte, 50X quartz injections, 3X pyrite.

5X quartz injections, 2X pyrite in henatizedtrachyte.

2X quartz injections, 2X pyrite in hematizedtrachyte.

30X quartz veins in henatized and sericitizedtrachyte, 3X pyrite.

IX pyrite in henatized fragmental trachyte.

IX pyrite in henatized fragmental trachyte.

As above.

END OF HOLE

SAMPLE N.

342

343

344

345

346

347

348

349

350

351

352

353

354

355

356

357

358

359

360

361

362

363

364

365

LENG. (m)

0.61

0.91

0.61

0.92

0.61

0.91

1.53

1.52

1.52

1.53

1.52

1.52

1.53

1.52

1.53

1.52

1.22

0.91

1.53

0.76

0.46

1.22

1,52

1,52

AU1 PPB

^

(5

^

^

10

^

^

O

^

140

^

^

^

(5

(5

^

^

(5

^

^

10

^

^

^

AU2 G/T

AUCHK PLP PPB

^

130

^

AUCHK REJ PPB

^

130

^

PAGE: 3 ASSAY SAMPLE RESULTS H HOLE NO: 96REC-03


COMPANYPROJECT

DRILL HOLETOHNSHIP

CLAIM

KALAHARI RESOURCES INC.RECESSION LARDER (M)96REC-04MC GARRY1167660

LOTZONE

. REF.RANGE

NTS


32D/04


GRID fiLINE

STATIONELEVATION

03475E 00+408 10000.000

GRID t2LINE

STATIONELEVATION

00+OOE 00+OON 0.000

GRID S3LATITUDE

LONGITUDEELEVATION

0.0000.0000.000

GRID 14LATITUDE

LONGITUDEELEVATION

-40.000375.000

10000.000

SAMPLING


366-376

PEOPLE

GEOLOGISTCONTRACTOR

RELOG

RICHARD ROY FORAGE VAL D'(

DATE


CEMENTING DATE



LENGTH COLLAR : FINAL : 96.32

CORE STORED : ANGLAUMAQUE OFFICE SIZE : BQ CASING LEFT : No

PURPOSETARGET

REMARKS

TEST ANOMALY MAXIPROBE BCentral ShowingsGrid azimuth 350 degrees.

DIRECTIONAL DATA AZIMUTH : 350' O' DIP : -48' O'

Length Aziauth Dip

30.48 350 O' -48 O 160.96 350 O' -46 O'96.32 352 O' -44 O'


FROM (m)

TO (m)

DESCRIPTION

0.00 3.05 CAS.RRR

CASING.Casing removed.

3.05 96.32 V2D,Frg,inHeig,Mas,(YNq,iiCar)

HEHATIZED FRA6HENTAL TRACHYTE.Moderately henatized and carbonated trachyte. It is massive and reddish in color from hematite. Contains 20Xstrongly henatized autoclasts ()2cm).Pervasive moderately hematization exist throughout, Carbonate alteration weak throughout except from 26 to196 feet where it is moderate.Only minor quartz veinets throughout at 20 degrees to core axis, Compared to possible foliation (E-fl), theveins are vertical and NNE.Up to n disseminated pyrite in walls of some veins, traces of chalcopyrite locally.

96.32 END OF HOLE



FROM ( l

S. 40

7.92

30.18

42.37

43.89

44.50

45.72

46,33

51.36

68.28

78.64

TO ( i)

7.92

9.45

31.39

43.89

44.50

45.72

46.33

47.55

52,12

69.49

78.94

96.32

DESCRIPTION

5X quartz veinlets at 40 degrees to core axis,1X pyrite.

Massive fragmental trachyte, traces pyrite.

2X quartz veins at 45 degrees to core axis, traces of galena.

5X quartz veins at 30 degrees to core axis,traces of pyrite,

As above, 10X veins.

As above, 2X veins.

As above with strongly hematized wall rock ofveins, IX pyrite.

Massive fragmental trachyte, traces pyrite.

10X quartz vein at 20 degrees to core axis, traces of chalcopyrite.

2 OX quartz vein at 45 degrees to core axis,barren.

A 6 inch quartz veining at 45 degrees to core axis, traces of chalcopyrite.

END OF HOLE

SAMPLE N.

366

367

368

369

370

371

372

373

374

375

376

LENG. ( )

1.52

1.53

1.21

1.52

0.61

1,22

0.61

1.22

0.76

1.21

0.30

AU1 PPB

AU2 G/T

(0.10

(0,10

(0.10

(0.10

(0.10

(0.10

(0.10

(0.10

(0.10

(0.10

(0.10

AUCHK PLP PPB

(5

(5

AUCHK REJ PPB

(5

<5

PAGE: 3 ASSAY SAMPLE RESULTS H HOLE NO: 96REC-04


COMPANYPROJECT

DRILL HOLETOWNSHIP

CLAIM

KALAHARI RESOURCES INC.RECESSION LARDER (M)96REC-05MC CARRY1167661

LOTZONE

. REF.RANGE

NTS


320/04


GRID fiLINE

STATIONELEVATION

04400E CHIOS 10000.000

GRID 1*2LINE

STATIONELEVATION

00+OOE 00+OON 0.000

GRID *3LATITUDE

LONGITUDEELEVATION

GRID #4LATITUDE

LONGITUDEELEVATION

-110.000400.000

10000,000

SAMPLING


377-388

PEOPLE

GEOLOGISTCONTRACTOR

RELOG


DATE


CEMENTING DATE



LENGTH COLLAR : FINAL : 90.22

CORE STORED : ANGLAUMAQUE OFFICE SIZE : BQ CASING LEFT : No

PURPOSETARGETREMARKS

TEST ANOMALY MAXIPROBE CCentral ShowingsGrid azimuth 350 degrees.

DIRECTIONAL DATA AZIMUTH : 350' O' DIP : -50* O'

Length Azinuth Dip

30.48 350 O' -50 O'60.96 350 O 1 -48 O'90.22 349 O' -45 O'

1


FROM (n)

TO DESCRIPTION

0.00 6.10 CAS.RRR

CASING.Casing removed,

6.10 27.13 S3-S6A,fg,mFol60,mCar(mBed,Fld)

HACKES AND SILTSTONE?.Fine grained, moderately foliated at 60 degrees to core axis and moderately carbonated wackes and siltstones.Local bedding confirms the sediments. A foid hinge at 79 feet is observed.It indicates an east plunging axis at 30 to 40 degrees if the foliation is perpendicular to core.No observed reliable graded bedding. Minor quartz veining and trace pyrite.

27.13 90.22 V2D,Frg,sHen,Mas,(nCar)

HEHATIZED FRAGMENTAL TRACHYTE.Strongly hematized trachyte. It is massive and reddish in color from hematite. Contains 40X stronglyhematized autoclasts ()2cm) generally syenjtic.Contains only a few minor quartz veining with no pyrite.

90.22 END OF HOLE

PAGE: 2 GEOLOGICAL DESCRIPTION HOLE HO: 96REC-05


FROM ( )

20.42

21.64

23.16

24.38

25.30

25.60

27.13

28.65

44.20

79.55

80.31

81.38

TO W

21.64

23.16

24.38

25.30

25.60

27.13

28.65

29.26

45.11

80.31

81,38

82.60

90.22

DESCRIPTION

Moderately fractured wacke and siltstone,moderately carbonatized, trace pyrite.

As above.As above with a fold hinge at 79 feet.As above.

As above with 2 OX quartz veining at 60 degreesto core axis, trace pyrite.As above.

Upper contact with sediments, trace pyrite.10X quartz veinlets at 20 to 65 degrees to coreaxis, trace pyrite,

One foot quartz carbonate vein at 20 to 60degrees to core axis, IX chlorite, tracepyrite.Massive trachyte, 5X quartz veinlets, tracepyrite.Quartz breccia with with 50X trachyte fragment, 0.5X pyrite and trace chalcopyrite.

Massive trachyte, trace pyrite.

END OF HOLE

SAMPLE N.

377

378

379

380

381

382

383

384

385

386

387

388

LEN6. (n)

1.22

1.52

1.22

0.92

0.30

1.53

1.52

0.61

0.91

0.76

1.07

1.22

AU1 PPB

AU2 6/T

(0.10

^.10

(10,10

(0.10

0.10

^.10

(0.10

(0.10

(0.10

(0.10

(0.10

(0.10

AUCHK PLP PPB

90

(5

AUCHK REJ PPB

50

(5

PAGE: 3 ASSAY SAMPLE RESULTS 81 HOLE NO: 96REC-05


COMPANYPROJECT

DRILL HOLETOWNSHIP

CLAIM

KALAHARI RESOURCES INC.RECESSION LARDER (M)96REC-06MC 6ARRY1167664

LOTZONE

NO. REF.RANGE

NTS


32D/04


GRID 11LINE

STATIONELEVATION

H+25E 00+75S 10000.000

GRID 12LINE

STATIONELEVATION

OOtOOE OOtOON 0.000

GRID *3LATITUDE

LONGITUDEELEVATION

0.0000.0000.000

GRID *4LATITUDE

LONGITUDEELEVATION

-75.0001425.000

10000.000

SAMPLING


389-397

PEOPLE

GEOLOGISTCONTRACTOR

RELOG


DATE


DATE



LENGTH COLLAR : 0,00 FINAL : 108.51

CORi STORED : ANGLAUMAQUE OFFICE SIZE : BQ CASING LEFT : No

PURPOSETARGET

REMARKS

TEST EXTENSION ANOMALY MAXIPROBE B East limit of property. Grid azinuth 350 degrees.

DIRECTIONAL DATA AZIMUTH : 350' 0' DIP : -50' 0'

Length Azimuth Dip

30.48 350 0' -50 0'60.96 350 0' -49 0'91.44 350 O 1 -47 0'


FROM (n)

TO (m)

DESCRIPTION

0.00 11.58 CAS.RRR


11.58 108.51 V2D,Frg,iHei,Mas l iCar

HEMATIZED FRAGMENTAL TRACHYTE.Moderately to strongly hematized and weakly carbonated trachyte. It is massive and reddish in color fromhematite. Contains 30X strongly hematized autoclasts ()2cm) generally syenitic.Contains a zone of shearing near the collar and only a few minor quartz veining with trace pyrite.

11.58 - 14.33 lU.iShrGO.lHei.sSer.sCar

SHEARED TRACHYTEModerately sheared trachyte at 60 degrees to core axis. It is strongly carbonatized and sericitizedand weakly hematized. Contains a few sericitized gouged slips.No quartz veining and trace pyrite in sericite.

108.51 END OF HOLE



FROM ( )

11.58

12.50

13.72

14.33

15.54

17.07

18.29

18.75

56.69

TO W

12,50

13.72

14.33

15.54

17.07

18.29

18.75

20.12

58.22

108.51

DESCRIPTION

Moderately sheared trachyte, neakly sericitized, trace pyrite,

As above, strongly sericitized trace pyrite.

As above, strongly sericitized, moderately henatized, trace pyrite.

Keakly hematized trachyte, trace pyrite.

As above.

As above.

Quartz carbonate vein at 45 degrees to core axis, barren.

Massive trachyte, no sulphides.

10X quartz veins at 10 to 40 degrees to core axis, trace

END OF HOLE

SAMPLE N.

389

390

391

392

393

394

395

396

397

LENG. (m)

0.92

1.22

0.61

1.21

1.53

1.22

0.46

1.37

1.53

AU1 PPB

AU2 G/T

(0.10

(0.10

(0.10

(0.10

(0.10

(0.10

(0,10

(0.10

(0.10

AUCHK PLP PPI

(5

(5

AUCHK REJ PPE

(5

(5

PAGE: 3 ASSAY SAMPLE RESULTS 11 HOLE NO: 96REC-06


COMPANYPROJECT

DRILL HOLETOHNSHIP

CLAIM

KALAHARI RESOURCES INC.RECESSION LARDER (M)96REC-07MC CARRY1167662

LOTZONE

. REF.RANGE

NTS


32D/04COORDINATES AT COLLAR

GRID t]LINE

STATIONELEVATION

09+OOE 02+55S 10000.000

GRID (2LINE

STATIONELEVATION

00+OOE OOtOON

GRID *3LATITUDE

LONGITUDEELEVATION

0.0000.0000.000

GRID *4LATITUDE

LONGITUDEELEVATION

-255.000900.000

10000.000SAMPLING


427-450

PEOPLE

GEOLOGISTCONTRACTOR

RELOG


DATE


CEMENTING DATE

DRILLING STARTED : October 23,1996 DRILLING FINISHED : October 29,1996LENGTH COLLAR : FINAL : 93.27CORE STORED : ANGLAUMAQUE OFFICE SIZE : CASING LEFT : NoPURPOSE

TARGETREMARKS

TEST ANOMALY MAXIPROBE DWithin SedimentsGrid azimuth 350 degrees.

DIRECTIONAL DATA AZIMUTH : 350' O' DIP : -45' O'


FROM TO (n)

DESCRIPTION

0.00 14.02 CAS.RRR

CASING.Casing removed.

14.02 38,40 Y2D,Frg,mHen,Mas,iiCar

HEMATIZED FRAGMENTAL TRACHYTE.Moderately to strongly hematized and weakly to moderately carbonated trachyte. It is massive and reddish in color from hematite. Contains 305! strongly hematized autoclasts ()2cm) which show blurred contacts. Contains only a few minor quartz veining with no pyrite.

38.40 93,27 S3-S6A,fg,mFol70,RiCar(inShr,sCar)

JAQUES AND SILTSTONES.Fine grained, moderately foliated at 70 degrees to core axis and moderately carbonated wackes and minorsiltstones beds. One narrow 4 inch cherty looking bed at 165 feet.fleakly sheared from 179 to 196 and more altered in this area.Also carbonate alteration continues to a depth of 226. Minor quartz veining and trace pyrite and up to 15!chalcopyrite locally.

53.64 - 61.26 M8,lShr70,nCar,(FLT,VLqc,cpy)

SHEARED SEDIMENTS.Weakly sheared sediments at 70 degrees to core axis. Moderately carbonatized. Local fault gouge andminor quartz carbonate veinlets with trace to 15! chalcopyrite and trace pyrite.

93.27 END OF HOLE



FROM (l)

44.81

46.33

47.55

49.07

49.99

50.60

52.12

53.64

55.17

55.78

56.39

57.00

58.22

59.74

61.26

62.79

64.31

65.84

67.36

67.97

68.68

79.71

86.56

87.48

TO (n)

46.33

47.55

49.07

49.99

50.60

52.12

53.64

55.17

55.78

56.39

57.00

58.22

59.74

61.26

62.79

64.31

65.64

67.36

67.97

68.88

70,41

80.01

87.48

89.00

93.27

DESCRIPTION

Moderately carbonatized sediments, 5X quartzveinlets, trace pyrite.

As above.

As above.

As above, moderately fractured.

As above, moderately fractured nit h 4 inch ofcherty layer.

As above.

As above.

Weakly sheared sediments, 2X quartz veinlets,trace pyrite.

55! quartz veinlets, 0.5X pyrite.

As above, 1S chalcopyrite.

5X quartz veinlets, minor fault gouge, tracepyrite.

Reakly sheared sediments, trace pyrite.

As above.

As above.

Moderately foliated, trace pyrite.

As above.

As above.

As above.

10X quartz vein, trace pyrite.

As above, IX disseminated pyrite,

Trace quartz, trace pyrite.

10X quartz carbonate vein at 60 degrees to coreaxis, 0.5X pyrite.

20X quartz carbonate vein at 60 degrees to coreaxis, trace pyrite.

5X quartz carbonate vein at 60 degrees to coreaxis, trace pyrite.

END OF HOLE

SAMPLE N.

427

428

429

430

431

432

433

434

435

436

437

438

439

440

441

442

443

444

445

446

447

448

449

450

LENG. (i)

1.52

1.22

1.52

0.92

0,61

1.52

1.52

1.53

0.61

0.61

0,61

1,22

1.52

1.52

1.53

1.52

1.53

1.52

0.61

0.91

1.53

0.30

0.92

1.52

A Ui PPB

AU2 G/T

(0.10

(0.10

(0.10

(0.10

(0.10

(0.10

(0.10

(0.10

(0.10

(0.10

(0.10

(0.10

(0.10

(0.10

(0.10

(0.10

(0.10

(0.10

(0.10

(0.10

(0.10

(0.10

(0.10

(0.10

AUCHK PLP PPB

(5

(5

(5

AUCHK REJ PPB

(5

(5

(5

PAGE; 3 ASSAY SAMPLE RESULTS #1 HOLE NO: 96REC-07

Ontario Ministry Declaration of Assessment WorkMine* Performed on Mining Land

Mining Act. *-1- and M0). ftJ.O. IMO

Personal Information coif*~* Mining Ac* Ouestioni 933 Ram.

Instructli 32004'

900

ww 65(2) and 66(3) o* the usessment work and Ministry of Northern

Transection Numb** (office us*)'

..., lda on Crown Lands bef. .vase type or print in ink.

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

RECEIVED!*re recording a claim, use

NOV li

GEOSCIENCE ASSESSMENT 2. 17933Name

vvL'^^W^ o^t. V exTelephone Number

*X Or OujuWrFax

Name Clteni Number

Addreee Telephone Number

Fax Number

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

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

Physical: drilling, stripping, trenching and associated assays Q Rehabilitation

Work Type

O\dYô A A -\\ -v~)C\ C\iT\\UvA^

JDales Work ————

Performed Fnm Q , |0 1^(0 To 39 l 1 O jl'H/pGtoba) PosrUoning System Data (if available) Township/Area

Me Ga rru \uj~OM or G^lan Number J '

Office UseCommodity

Total S Value of n Work Claimed 3 ft. *J fa (o

NTS Reference

fciirÔhrfsion /AA diA j J)AJKJJ

Resident Geologist

Please remember to: - obtain a work permH 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)NameR;Addreee

Name

cWw\ K 04j f

^\ r\ /5 \ C \ \/ 1 I/O r"\ ri tVvl w\V iu\ C\fVni YT^VXP CCOV-tf' VfX l ri UV" vJ.uoJ '

Addr*"*

Name

Addrea*

Telephone Number

(# ^^2-^- !o3O

^TRP^MI- l&^^-t&ifoTelephone Number ~~

fax Number

Telephone Number

Fax Number

4. Certification by Recorded Holder or Agent

———1., do hereby certify that l have personal knowledge of the facts setforth 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.SfgnaturaToT 55.-

3M \ZLelephone Number SxHumbeir

25/1*

5. Work to be recorded and distributed. Work can only be assigned to claims thai are contiguous

the minino land where work was performed, at the time work was performed. A map showing the contiguous Onk

must accompany this form. ' ^ . .vo*^*.

Mining Claim Number. Or N work wae done on' other eligible mining land, show In this column the location number indicated on the claim map.

•g•g•g12

3

4

5

6

7

8

9

10

11

12

13

14

15

1.

TB7827

1234567

1234568

L- ll&ft&sqlUruollfÛ,!H13UZ.

" [j V}(43

li (tlLL^li 63 U5

Ôrru J- or

Number of Claim Unto. For other mining land, 1st hectares.

16 ha

12

2

^ \* -f" ' ;

- l '* i' i" j

i

Column Totals

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

126,825

0

f 8, 892

'3jc| jiTT^fTW""

*.-*lTf^-"- -- - . — ~- -

-tbfeo^- — —.

.

®7QL(l(j

Value of workapplied to this claim.

N/A

J24.000

S 4,000Sfa'uorT'""

SlHo oôo•"Smoc-3 M* n D S3400otM-OO

*- .1

^llfeDD

Value of work assigned to other mining dakna.

S24.000

" '';r-q 0

0

-^ ——— .:. :

a^^TODtr ~~^ — ........,.... .— — — ~ --...

—- ,. .

"!-

.^ —

NJ 1 i t^)kj vJ, (^ f*} f~~\

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

S2.825

0

14,892

tt-klT^/"

-ttttb^ -- 4,422 S

6"? 1 9 S

t

Sc5D9

H l lo L, C,

^ x ^^ , do hereby certify that the above work credits are eligible under(Print Ful N*nw)

subsection 7 (ifof the Assessment Work Regulation 6/96 for assignment to contiguous claims or for application to

the claim where the work was done.

Signature of

6. Instructions for cutting back credits that are not approved.

Some of the credits claimed in this declaration may be cut back. Please check ( s ) in the boxes below to show how

you wish to prioritize the deletion of credits: -

Oa 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 wRh the claims listed last, working backwards; or

G* 3. Credits are to be cut back equally over all claims Hsted 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

RECEIVEDDeemed Approved Octe

D*te Approved

Dal* Notification Sent

Total V*hM of dvdK ApprovH

ApprovM lor (woordlnQ by Mining Recorder (Slgnatura)

Ontario Ministry ofNorthern Developmentand Mines

Statement of Costs for Assessment Credit

Transaction Nurabar

DIVTSIOPersonal information collected on this form Is obtained under the authority of subsection 6(1) of the Assessmam Work Ragylasection B of the Mining Act, the Information is a public record. This Information will be used to review the aaSBtstwUv&t andfcbfrakpondfcitrithe mining land holder. Questions about this collection should be directed to the Chief Mining Recorder, Ministry of Northern Development andMines, em Moor, 933 namsey Laxe noaa, auaoury, umario, rje oao. ——————— ———— — - LJ

RECEIVE.Work Type

ftwvvncî ry;U,^P \ ' VA\ (L,^r\ p \^ rv c^l VN r. t- 1 cArl

Q^\ ^ 0O

Units of WorkDepending on (he type of work, list the number of hours/days worked, metres of drilling, kilo metres of grid line, number of samples, etc.

3/^0, 5t(rV-\ . i \

LYVLTD [^ffAoM-snrr\ r\ ; A Ai^H(r tt^nusMUo

^ o

Associated Costs (e.g. supplies, mobilization and demobilization).

Q m t F VfvrV R^ Y-^Vr* \r~ ~~ \ \ O- ' \

l ^ A \ (j -i- W1 -Li ' f-V^vf\"i~"TL'^ r. 0 LV|"^ VÔ prx~'r \ r^^Cn r\ (i YrorySO

Transportation Costs

\jp.WcVr Vc.vVfi l

Food and Lodging Costs

\^nU\ (\Â V^^^

Cost Per Unit of work

i

i

t

lÛ f, 0 ^ j.

Total Value of Assessment Work

Total Cost

^L[4 -^qcj^/;

n3 J ksq 3^f H 35. rt

,^/ q/^ll

S ]R5o.c rl^^. c C

^ l.SSn.nT(G no .oT

14 o^^.^-C

^13 4 k 5.^

Calculations of Filing Discounts:

1. Work filed within two years of performance is claimed at 1000xb of the above Total Value of Assessment Work.2. If work is filed after two years and up to five years after performance, it can only be claimed at 500Xo of the Total Value of Assessment Work. If this situation applies to your claims, use the calculation below:

TOTAL VALUE OF ASSESSMENT WORK x 0.50 Total S value of worked claimed.

Note:- Work older than 5 years is not eligible for credit.- A recorded holder may be required to verify expenditures claimed in this statement of costs within 45 days of a request for verification and/or correction/clarification. If verification and/or correction/clarification is not made, the Minister may reject all or part of the assessment work submitted.

Certification verifying costs:

i. L-.OL vr u "CT. , do hereby] certify, that the amounts shown are as accurate as may(pieces print full name)

reasonably be determined and the costs were incurred while conducting assessment work on the lands indicated on

the accompanying Declaration of Work form as

to make this certificatl

0212 (02/96)

'RECEIVEDNOV 2 1 199/

GEOSCIENCE ASSESSMENT ______OFFICE

(recorded holder, agernT or slate company position with signing authority)l am authorized

Ministry ofNorthern Developmentand Mines

Ministere du Developpement du Nord et des Mines Ontario

Februarys, 1998

GLENN J. MULLAN 152 chemin de la Mine Ecole Val d'Or, Quebec J9P 4N7

Geoscience 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: 2.17933

StatusW9780.01144 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: 11875

Copy for: Assessment Library

Work Report Assessment Results


Date Correspondence Sent: February 05, 1998 Assessor:Lucille Jerome —^^^—^-—^^—-.^—^-—

Transaction First ClaimNumber Number Township(s) l Area(s) Status Approval Date

W9780.01144 1167659 MCGARRY Deemed Approval January 28, 1998

Section:16 Drilling PDRILL

Assessment work credit has been redistributed, as outlined on the attached Distribution of Assessment Work Credit sheet, to better reflect the location of the

work.

Correspondence to: Recorded Holder(s) and/or Agent(s):

Resident Geologist Larry J. Stoliker

Kirkland Lake, ON KIRKLAND LAKE, ONTARIO, CANADA

Assessment Files Library GLENN J. MULLAN

Sudbury, ON Val d'Or, Quebec

Page: 1Correspondence ID: 11875

Distribution of Assessment Work Credit

The following credit distribution reflects the value of assessment work performed on the mining land(s).

Date: February 05, 1998


Transaction Number: W9780.01144

Claim Number Value Of Work Performed

1167659 9,416.00

1167660 27,463.00

1167661 7,062.00

1167662 9,416.00

1167663 14,124.00

1167664 10,985.00

Total: $ 78,466.00

Page: l

Correspondence ID: 11875

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IVAN LARDER FAULT

1+OON

Baseline

96REC-02A 96REC-0296REC-01A

96REC-01

: l Glacial85-1 o; \

12ppb * .02XCu/

...............™- *........ .............,.:.......... x...... ............................... ...A . mm,.-......;......,::.^.,

'—— . ^^ f B 2a(m)X 2a(m) , .^- . __ ,'—— . ^— ' —**. .1'

: .07XCu96REC-03/

1 Unsubdivided 1a Greywacke 1b Siltstone 1c Conglomerate

FELSIC METAVOLCANICS

2 Unsubdivided Trachyte2a(m) Fragmental Trachyte (with magnetic attraction) 2b Pink Fragmental Trachyte (Syenitic Fragments) 2c Buff Carbonated Trachyte

MAFIC INTRUSIVES

3 Diabase

x

80

OUTCROP BOUNDARY, SMALL OUTCROP

FAULT, SHEAR

STRIKE AND DIP OF FOLIATION

STRIKE AND DIP OF BEDDING

VLF-EM ANOMALY (WEAK, STRONG)

MAXI-PROBE ANOMALY

carb

pycpy mal

D

QUARTZ VEIN, STRINGERS

QUARTZ STOCKWORK

CARBONATE ALTERATION

PYRITECHALCOPYRITEMALACHITE

TRENCH, PIT

SHAFT

17933

210

lUi mexplorations inc

SCALE 1: 2 500

50 100I^^MBMI

METRES

150

KALAHARI RESOURCES INC.


SURFACE GEOLOGY PLAN

N.T.S : 32 D/4

DATE : 14/11/97

MAP NO. : 7

TOWNSHIP : UcGARRY

PROVINCE : ONTARIO

DRAWN BY : C.B.

APPROVED BY : R.R.R

(S).o o

v.er

IppppEL4 ,'- i;

O*.0' *

,- 4 ,'- |-4 .' C Afl ,"- (S ,'- 4 t'- C o 4 4 4 *- * * ' *

WACKESAND

SILTSTONES

êf

t^*#

.e^ *0'

O: Q: O:

Q:CM;

10000EL

HEMATIZEDFRAGMENTAL

TACHYTE

9900EL ............. .; . ........................................................................J..........^ ,. - - - -— rr—--^" - 9900EL

32D04NE0163 2.17933 MCGARRY 220

9800EL

(f)O: O

O :o;



RECESSION LARDER PROSPECT SECTION 4+OOE

10 O 10 20 30 m

ECHELLE 1 : 500

N.T.S.: 32 D/4

DATE 13/11/97

MAP NO.:

TOWNSHIP: McGARRY

PROVINCE: ONTARIO

DRAWN BY: C.B.

APPROVED BY: R.R.R.

CO: O ; O: CN:

CO:O: O :

SHEARED CONGLOMERATE

10000EL

^HEMATIZED TRACHYTE ,o^

,^'y4f^

WACKES

4ft

CONGLOMERATE

9900EL

AND TUFFS

HEMATIZED TRACHYTE

9900EL

1^933

9800EL

CO:o;O: CM:

32D04NE0163 2.17933 MCGARRY 230

CO: O : O:

O :o;

Uiexplorations inc.



SECTION 9+OOE10 10 20 30 m

ECHELLE 1 : 500

N.T.S.: 32 D/4

DATE 13/11/97

MAP NO.:

TOWNSHIP: McGARRY

PROVINCE: ONTARIO

DRAWN BY: C.B.

APPROVED BY: R.R.R.

HEMATIZEDFRAGMENTAL

TRACHYTE

O:

9900EL

O : O:

O- O:

O:

O: Q:

10000EL

•ao 9900EL

32D04NE0163 2.17933 MCGARRY 240

o o;(N:

Uiexploration inc.

KALAHARI RESOURCES INC. l

RECESSION LARDER PROSPECT SECTION 14+25E

ECHELLE 1 : 500

APPROVED BY: R.R.R.

9800EL

(f) oO:

O O O:

Q:CM;

^: : O ^ : Cf\ j Q' ^ \ j? : : j i

10000EL.................. ........................................J...............................................................................^ 10000EL^•••••••••••'••••••'•••••••••••:.^'

o9900EL .... i..........................................................................^ ~ w * 9900EL

32D04NE0163 2.17933 MCGARRY 250

CO: O :o;

9800ELo.

O :o:

exploratiore inc


RECESSION LARDER PROSPECT SECTION 2+OOE

10 10 20 30 m

ECHELLE 1 : 500

N.T.S.: 32 D/4

DATE 13/11/97

MAP NO.:

TOWNSHIP: MCGARRY

PROVINCE: ONTARIO

DRAWN BY: C.B.

APPROVED BY: R.R.R.

(f) oO':

z;o

10000EL ! i . ............^............................................................................J.......................................^^

•:- -:-:- ^kv -:-;/; v ::- ^ ̂ :.-;";;" -:- -:-;- v.

CONGLOMERATE

\ SHEARED\ TRACHYTE

SHEARED CONGLOMERATE

9900EL

HEMATIZE TRACHYTE

COo :

9800EL

O:

O ;o;

lUiexplorations inc.


RECESSION LARDER PROSPECT SECTION 2+75E

10 10 20 30 m

ECHELLE 1 : 500

N.T.S.: 32 D/4

DATE 13/11/97

MAP NO.:

TOWNSHIP: MCGARRY

PROVINCE: ONTARIO

DRAWN BY: C.B.

APPROVED BY: R.R.R.

c/roo;

O: O-

O: Q: CM!

10000EL

10000EL

HEMATIZED TRACHYTE

. ^ Y*i1 7 s? o

9900EL i ......... ............................t..............................................................................^............................................................-...........^^

32D04NE0163 2.17933 MCGARRY 270

COo : o;

o o;

9800EL

exporaons nc.



SECTION 3+75E10 o 10 20 30 rn

ECHELLE 1 : 500

N.T.S.: 32 D/4TOWNSHIP: MCGARRY

DATE 13/11/97

MAP NO.:

PROVINCE: ONTARIO

DRAWN BY: C.B.

APPROVED BY: R.R.R.

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