32D04NW2015 2.19015 LEBEL

REPORT ON DIAMOND DRILLING

KING KIRKLAND PROPERTY

LEBEL TOWNSHIP

LARDER LAKE MINING DIVISN

ONTARIO

010

Michael LeahyKirkland Lake, Ontario

December, 1998

32D04NW2015 2.19015 LEBEL 010C

TABLE OF CONTENTS

INTRODUCTION

ACCESS

REGIONAL GEOLOGY

PROPERTY GEOLOGY

HISTORY 3,4,5,6

1998 DIAMOND DRILL PROGRAM

RESULTS OF DRILLING PROGRAM

CONCLUSIONS

RECOMMENDATIONS

KEY MAP

CLAIM MAP

DRILL HOLE LOCATION l O

DRILL HOLE SECTION 11

DRILL LOG Appendix A

INTRODUCTION

The property herein described consists of 14 contiguous unpatented mining claims in central Lebel Township (G-639), Larder Lake Mining Division, Ontario. Latitude 480 10' N, Longitude 79058' W. NTS map sheet 42A/SE. The village of King Kirkland lies immediately on the west boundary of the claim group. The town of Kirkland Lake lies about 5 km west of the property. Claims are numbered as follows:

1211849 1219943 1220019 1220179 1220180 1221653 1222232 1222233 1225271 1225284 1225285 1226845 1226949 1227041.

ACCESS

The property is traversed by Highway 66, between Kirkland Lake and Dobie. At the west end of the property, a gravel road leads south from Smitty's Drive Inn to the Ontario Northland Railway near the King Kirkland shaft, a distance of about 800 m. This road continues south across the tracks to the Pawnee Mine Property and Turtle Lake. At the east end of King Kirkland, another gravel road leads north and east through the property toward the Bidgood Mine Property and Crystal Lake. None of the property lies more than l km from a road. Several power lines also traverse the property.

REGIONAL GEOLOGY

The King Kirkland property lies within the Abitibi Greenstone Belt located in the southeastern portion of the Superior tectonic province. The Abitibi belt is the largest and most continuous greenstone belt in the Canadian Shield, extending some 700 km from east to west with a width of approximately 200 km and is of Archean age. It is bound to the east by the Grenville Front and to the west by the Kapuskasing Structure. The belt consists of repetitive volcanic cycles ranging from ultramafic to felsic in composition. Clastic sediments are intercalated with the volcanic rocks, and in narrow fault bounded zones. Ultramafic to mafic intrusions as well as granitoid complexes exist.

The dominant structural style of the belt reflects the presence of local granitoid bodies with concordant external structures, the east-west trending isoclinal folds of regional extent. The belt has been deformed into a major east-west trending synclinorium that transects the central portion of the Ontario segment of the Abitibi belt.

Within the southern part of the belt, many steeply dipping, east-west trending discontinuous shear zones of undetermined displacement have been identified. Two major breaks have been identified including the Porcupine-Destor and Larder Lake breaks. These breaks follow lithofacies boundaries for the most part, including sedimentary volcanic interfacies. Many of the gold deposits of the area are closely associated with the shear zones especially in the Kirkland Lake-Larder Lake and Malartic-Cadillac areas. Approximately 75*Yo of historical gold production in Canada is derived from the Abitibi belt.

The Kirkland Lake area is dominated by what is called the Upper Volcanic Cycle

comprising a lower ultramafic sequence (Larder Lake Group) disconformably overlain by a tholeiitic sequence (Kinojevis Group) which is in turn disconformably overlain by a calc-alkalic sequence (Blake River Group). This entire sequence is unconformably overlain by the late Archean Timiskaming Series of clastic sediments and felsic volcanics. All of the above have been intruded by stocks and bosses of mafic to syenitic composition and diabase, also of late Archean age.

The Larder Lake Break is postulated to cut through the south central portion of Lebel Township, however, its exact location is obscured in part by the Lebel syenitic stock of which occupies the south 1/3 of the township. The location of the Break is approximately 6,500 feet south of the King Kirkland shaft.

PROPERTY GEOLOGY

The entire property as part of Lebel Township was mapped in between 1936-39 by O.D.M. geologist A. MacLean (Map No. 53 A, O.D.M. Bulletin No. 150). Mapping indicates the extreme northern and southern portions of the property to be underlain by Timiskaming Series sediments comprising tuffs south of the King Kirkland showing and boulder conglomerates north of the Lebel-Oro showing. Mapping by Canico in 1981 over the four northern claims indicates bedded conglomerates with minor alkali tuff breccias, possibly trachytic. These units strike either east-west to slightly north of west with steep dips to the south.

Timiskaming Series sediments and volcanics represent the top of the last volcanic cycle in the Kirkland Lake-Larder Lake area and are thought to have been deposited in graben structures as high energy clastic sedimentation. Volcanic lithologies are generally of alkaline chemistry dominated by trachytic tuffs and tuff breccias. The central portion of the property is underlain for the most part by highly altered Timiskaming sediments intruded by late Archean syenitic sequences including feldspar porphyry, basic syenite and minor lamprophyre. Alteration of the host sediments and tuffs is so intense that it is difficult to distinguish altered sediments from intrusive. The ambiguous term "porphyrite" has been used in the literature to describe metasomatized and digested tuffs and sediments. This rock type prevails over both the King Kirkland and Lebel-Oro shaft areas as well as other gold showing on the property. Mapping by G.E. Parsons in 1984, for R. Lawrence suggested the porphyrite may in fact be an extrusive crystal tuff. Gold mineralization at both the King Kirkland and Lebel-Oro are related to northeast trending veins. Carbonatized wall rock with appreciable pyrite mineralization is present at the Lebel-Oro and to a lesser extent at the King Kirkland prospect.

The mineralization is further complicated by north-south trending post-ore faults. These faults have disrupted the ore shoots such that they are of limited strike length which discouraged early underground development at both the Lebel-Oro and King Kirkland prospects. The strongest structure (although yet to be defined) is the projected west extension of the Bidgood Fault which hosts the Bidgood Mine (past producer) located 3 km to the northeast and the Bidgood No. l shaft l .5 km to the northeast. The Bidgood fault has been projected through the King Kirkland property roughly between the Lebel-Oro and King Kirkland prospects. It has yet to be defined by either mapping or drilling and its location is speculative. Locating the Bidgood Fault is a priority as gold mineralization may be spatially associated with this structure.

HISTORY

Early exploration on the property was generally confined to the Lebel-Oro and King Kirkland prospects with later exploration examining areas further east and south of the two shafts.

Exploration at the King Kirkland prospect was initiated in 1918 following the discovery of gold and the company, King Kirkland Gold Mines Ltd., incorporated in 1920. Between 1920-23 an inclined shaft was sunk (750 NW) and two levels were opened up at 90 feet and 400 feet. Over 30 narrow parallel veins or fractures, with a northeasterly strike and steep dip to the north were identified in the porphyry east of King Lake. The shaft was sunk on the #5 vein which was considered to be the most important vein. On surface, the #5 vein was exposed over a length of 300 feet, 30 feet of which was enriched over a width of 4 to 5 feet. The enriched vein material was described as containing hair-like seams of fine-grained pyrite and a little black material (tourmaline or chlorite?) in which visible gold may sometimes been seen with a hand lens. Drifting on the #5 vein identified some gold mineralization on the 400' level over a 30' strike length west of the shaft.

The property was then optioned to Tonapah Mining in early 1923 who worked not only on the King Kirkland but on the Moffat-Hall and Wood-Kirkland properties. Additional development work on the 400' level at the King Kirkland was completed consisting of extending the 400' level both east and west. Tonapah Mining dropped the option in late 1923.

King Kirkland Gold Mines was reorganized in 1936 as Kirkking Gold Mines Ltd. and proceeded to de-water the shaft and workings. Their work included geological mapping and re sampling the drifts. Channel sampling on the 400' level near the west end showed some high gold values over narrow widths and lengths of 2O-30'. Twelve underground drill holes were completed in 1937. Significant assays were reported in the #5 hole which assayed 0.292 oz/ton over a core length of 8' with a true width of approximately 4.0'. This hole was located on the 400' level. Drill hole #1 1 was collared at the same location as the #5 hole but with a l O0 steeper dip (800). The #1 1 hole intersected 0.30 oz/ton over a core length of 2.0'. Further drilling was recommended but not completed. The charter of Kirkking Gold Mines was surrendered in 1938 and the property again became King Kirkland Gold Mines Ltd.

At the Lebel-Oro prospect, an inclined shaft was sunk to 60 feet in 1920, deepened to 203 feet in 1923 with levels opened at 100 and 200 feet by Lebel-Oro Mines Ltd. Shaft sinking was on the widest of three exposed veins on surface which trend N300 E dipping 65-70" NW. The mine was closed down in 1924, then reopened in 1927 followed by extensive exploration. The exploration included 900 feet of drifting and 450 feet of crosscutting as well as sampling. In 1927 the Nipissing Mining Company optioned the property and completed three underground and three surface diamond drill holes between 1927-29. Nipissing dropped the option in 1928 although work continued by Lebel-Oro Mines through 1928. Underground drilling for Lebel-Oro Mines was guided by W.P. Murdock, the surface drilling by E.W. Todd. Work was terminated in 1929 and the mine was allowed to flood.

In 1936 the workings were de-watered by Lebel-Oro Mines followed by 1,800 feet of underground drilling (3 holes) and 900 feet of surface drilling completed under the direction of B.S.W. Buffan. Operations ended in October, 1936 and the mine was once again allowed to flood.

In 1948, the Geo-Technical Development completed detailed geological mapping, resistivity and magnetic surveys for Lebel-Oro Mines under the guidance of S.V. Burr. Diamond drilling followed the surveys which included eight holes (two of which were abandoned in overburden) with a total footage of 3,347 feet. These holes were exploratory in nature and generally tested the possible northeast extension of the Lebel-Oro. New mineralization was intersected in the #3 hole (0.60 oz/ton over 1.4') and in the #4 hole (0.18 oz/ton over 1.3').

S.V. Burr stated after his overview of the Lebel-Oro that no further work should be undertaken due to the low quantity and erratic distribution of gold mineralization.

In 1975, E.G. Deloye held a group of claims forming the northeast and east portion of the present King Kirkland property. Deloye completed trenching over the northeast corner of present claim 1206580. No assays or mapping from the trenches is recorded.

In 1977 the Haas-Warner Mining Company optioned the one claim from Deloye and completed a 220' diamond drill hole on present claim 1211849. The hole was logged as trachyte and no sampling or assaying is reported in the drill log.

In 1980, the Canadian Nickel Co. Ltd. (CANICO), which held the four extreme north claims of the present property (1225271, 1221653, 1220019) completed geological mapping. Very low gold assays were reported from limited sampling, though not unexpected as little alteration or mineralization was noted.

In 1982, Lampe Resources Company Ltd., optioned eleven claims including the King Kirkland prospect and completed two diamond drill holes in the vicinity of the King Kirkland prospect. KK82-1 was collared so as to undercut the King Kirkland vein. KK82-2 was located northwest of the shaft and appears to have been targeted on the possible west extension of the Bidgood Fault. No significant faulting was intersected implying that either the fault does not extend this far west or (more likely) the Bidgood fault lies further to the north. A VLF-Em and magnetic survey was completed over the entire eleven claims as well as stripping and sampling in the shaft area. No assays were reported from the drill logs. Sampling from the trenching returned assays as high as 0.68 oz/ton with the majority assaying trace gold. The VLF survey results were inconclusive due to cultural contamination (ie. power lines).

In 1984, R. Lawrence completed a radiometric survey, geological mapping as well as stripping and sampling over three claims (present claims 1206580, 1211849,1220180, east portion of present property) in 1984. This work was completed under the guidance of G.E. Parsons. Sampling of a vein in the rock cut along the highway returned assays of 0.08 and 0.15 oz/ton, (Rock Cut Showing). A sample of rock fill along the highway assayed 0.30 oz/ton and prospecting inland from the highway uncovered yet another mineralized shear which assayed 0.90 oz/ton. This new discovery, on present claim 1206580, was called the "Cliff Showing". Stripping on the Cliff Showing in 1984 revealed a northeasterly striking fault which dips 55" to the west. Mineralization comprising blue quartz and molybdenite was uncovered over a length of 100' with mineralized widths varying from nil to 3'. Chip samples assayed up to 0.40 oz/ton over 3.0'.

Two short drill holes (ML-84- l, ML-84-2) were completed totaling 302'. The first hole testing the Rock Cut showing, was drilled northwest (down-dip?) at a dip of 650. No significant mineralization was intersected, the best assay being 0.02 oz/ton over 3.0'. The second hole tested the Cliff Showing and was drilled east at a dip of 800. No significant assays were reported. It seems unlikely, given the attitude of the showings and collar dips, that neither of these holes could

have intersected the targeted veins.In 1984 Aurage Mineral Corporation optioned four claims comprising the King Kirkland

portion of the present claim group including a portion of the area held by Lampe Resources in 1982. G.E. Parsons completed a radiometric survey for Aurage. The survey results indicated that three different rock types could be distinguished by radiometric, including porphyrite, sediments and trachyte.

Additional sampling and a radiometric survey by Lawrence was completed over the cliff showing in 1986 but failed to expand on the 1984 sampling. The radiometric survey results indicated that different rock units could be distinguished based on potassium/argon radiation.

A final program of stripping, sampling and geological mapping by G.E. Parsons for R.W. Lawrence in 1987, was centered on the Lebel-Oro shaft area and the King Kirkland townsite. Further work was proposed on the north claim of the townsite, unfortunately the townsite has now been withdrawn from staking. The entire property, including the Lebel-Oro and King Kirkland prospects, were allowed to lapse and subsequently staked by Ramshackle Resources in 1989-90.

In 1991, Premier Explorations completed an airborne EM and magnetic survey over the present block. The most recent work was by Ramshackle Resources which completed gridding and ground magnetics over the north half of the property with detailed work over the Lebel-Oro shaft area. A Time Domain Induced Polarization was performed over the Lebel-Oro shaft area, as well. The magnetic survey showed an increased magnetic response over the Lebel-Oro shaft area and the east section of the property, including the gold showing on claim 1206580 (Cliff Showing). Other areas of elevated magnetics were not defined, however, it should be noted that the coverage was over the north half of the claim group. The higher magnetics likely reflect trachytic sequences which often exhibit strong magnetic gradients.

The Induced Polarization survey delineated three units or relatively high resistivity reflecting changes in bedrock lithologies. One of the units has a direct correlation with the Lebel Oro shaft area. Weak chargeability anomalies area associated with south magnetic contact approximately 25-50 metres south of the Lebel-Oro shaft. This contact was recommended for further work. A discontinuous weak relatively conductive zone was located on LOE/412N, LIE/375N and L250E/387N. The zone, which is not chargeable, may represent a barren fault. Sections of relatively high chargeability were located as well indicating possible disseminated sulfides. These chargeability anomalies are generally confined to the Lebel-Oro shaft area, though not within the defined underground workings. Upon completion of these surveys, the property was optioned to International Homestead Resources Inc. (IHR).

In July of 1994 IHR completed l .9km of gridding followed by 1.5 km of Induced Polarization over the Cliff Showing area. An attempt to extend one of the grid lines (6+OOE) north to cover the possible location of the Bidgood Fault failed due to flooded conditions near Mud Lake. The Cliff Showing does not appear to be defined by the survey, however, a weak to moderate north-south chargeability anomaly was located on the three lines surveyed, possibly representing a mineralized structure.

Minor recent sampling in 1994 by D. Guindon of the Kirkland Lake Resident Geologists office located a new quartz vein a few hundred feet north of the King Kirkland shaft which

assayed 0.03 oz/ton.Past producers in the immediate area of the property include the Bidgood (160,184 oz Au,

3 km east northeast), Morris Kirkland (16,861 oz Au, 1.2 km east southeast) and the Moffatt-Hall (4,769 oz Au, adjoining the Bidgood Mine).

The Pawnee-Kirkland Gold Mines property, located 1,000' SE of the south boundary, was explored underground in 1922 and 1936, however, no production is recorded.

The King Kirkland property also lies within 4.3 kilometers of the Toburn Mine, the eastern most producer of the prolific Kirkland Lake camp which included the Toburn, Sylvanite, Wright Hargreaves, Lakeshore, Teck Hughes and Macassa. Total gold production (as of 1994) is close to 24,000,000 oz Au, most notably from mines which include the Lakeshore, Wright-Hargreaves, Teck Hughes, Sylvanite and Macassa. Only the Macassa Mine is still in operation.

1998 DIAMOND DRILL PROGRAM

In October 1998, one hole was drilled on the property. The hole was designed to intersect the Bidgood fault and to test the area between the magnetic trachytes and the fault. There is a weak I.P. anomaly at about 3SON with asssociated anomalous gold values obtained from old trenches earlier in 1998. The target area lies just southwest of the Lebel Oro shaft. An earlier hole (1982 - 2) had already attempted to intersect the Bidgood fault from the south, without success. The 1998 hole was collared on L 150E @ 450N and was drilled with an azimuth of 1700 . The dip of the hole was 45" at the collar and 470 at 553' (eoh). The drilling was supervised by the author; the hole was logged by Frank Ploeger at the Queenston core shack in Dobie, Ontario.

RESULTS OF DIAMOND DRILLING

The diamond drill hole successfully intersected both the I.P. anomaly and the Bidgood fault. The rock types encountered were a relatively unaltered weakly magnetic syenite trachyte and various phases of altered and unaltered syenite feldspar porphyry. The alteration minerals consisted mainly of carbonate, sericite and ankerite. Pyrite content averaged about 1*^, with local enrichments to 507o. For a detailed description of the rocks and alteration, see logs. The hole was drilled to a depth of 553'. The Bidgood fault was intersected at 456 -461 feet.The best values were obtained from this zone, with highly anomalous values from 454" to 464'.

The total number of samples was 82, with only 14 samples grading less than 20 ppb, 2^ 100 ppband2M,OOOppb.

CONCLUSIONS

The drill hole intersected a highly alteres suite of rocks containing elevated gold values. The rocks are similar to those intersected in DDH 1982-2 which also contained a wide gold bearing alteration zone. The entire area between the railway and Highway 66 consists of porphyritic rock cut by at least four gold bearing alteration zones, including the King Kirkland and Lebel Oro shaft zones. The total width of the porphyritic unit is about 1,800 feet. This unit is highly enriched with gold, with values as high as 0. l oz/ton across 10' in DDH1982 - 2.

RECOMMENDATIONS

The porphyry unit should be tested with several more drill holes. The priority target is the zone intersected in DDH 1982-2. Two holes should be drilled below and beside DDK 1982-2 to firmly establish strike and dip of the gold bearing zone. At least two more holes should be drilled to the east, where a crosscutting structure is projected (cliff showing) to traverse the formation. The crosscutting structure is probably an extension of the regional fault zone that runs up Boston Creek, Through Mud Lake and Victoria Lake and on through Kennedy and Verna Lakes.

Jt KING KIRKLAND PROPERTY

Lakt

~2.CC. M l l S O C O

b b H K fe ^ ft - l

Tuj p

DDHKK1998- l

Azimuth 170" @-45"Collar LI50E + 450N

Claim #1222232Lebel Township

Syenite Trachyte

Altered Syenite Feldspar Porphyry

1000ppb73'@425

Feldspar Porphyry altered Syenite 1536ppb71.5'@460 Bidgood Fault Zone

553

APPENDIX A

Drill Hole:

Property: Northing: Easting: Elevation:

KK98-1

King Kirkland450.00150.00

11000.00

Collar Azimuth (Grid) 170.00Collar Dip: -45.0(O Degrees Grid equals 035 degrees True)Hole Length: 553.0

Date Printed: 23 Nov, 1998

QUEENSTON MINING INC

DIAMOND DRILL HOLE RECORD

*** Dip Tests ***

Depth Azi. Dip

*** Dip Tests ***

Depth Azi. Dip

553 -47.0

Page : l of 5

Date Started: Date Completed:

Oct 15, 1998 OCT 19, 1998

Drilled by: YOSTCore Size: BQMaterial left in hole BX CASINGCore Location: Leahy Core ShackLogged by: F. Ploeger

From To (ft) (ft)

Geology Sample No.

From (ft)

To (ft)

Len (ft)

PY AU

OZ/T

AU1

OZ/T

AU2

ppb

SUMMARY LOG

.0 3.0 CASING

3.0 326.0 SYENITE TRACHYTE

326.0 386.0 ALTERED SYENITE FELDSPAR PORPHYRY

386.0 553.0 FELDSPAR PORPHYRY ALTERED SYENITE

553.0 553.0 END OF HOLE

Drill Hole KK98-1 Page : 2 of 5

From To (ft) (ft)

Geology

.0 3.0 CASING

3.0 326.0 SYENITE TRACHYTE

This is an odd unit in terms of texture, alteration, mineralogy and general appearance. It has a basic trachytic texture with the apparent mineralogy of the Kirkland Lake 'felsic syenite'. Although visually, there seem to be a number of lithologies defined by changes in grain size and colour, the contacts are all gradational and due to alteration effects. The following intervals define the various major changes described above.3.0 59.3 Trachytic Syenite -This is probably the freshest/ least altered

interval of the hole. The overall colour of this section is mediumgrey to medium brown grey. The host exhibits a trachytic texturedefined by pale grey/ dull white feldspar needles and/ or smallelongate grains to l mm (20%) with about 5% black stubbyferromagnesian (pyroxene?) laths in a medium brown grey colouredfine grained groundmass. Also present are green black, fine grainedmafic inclusions which average approximately l cm and amount to 2%of the rock. Overall, the interval is medium grained with localfiner grained patches which may represent an internal flow texture.Locally, some of the white equant/ rhombic grains are calciticmetacrysts. The host is cut by 3*r randomly oriented fine white topale pink calcite veinlets and threads. At 30.5 and 31.0', the coreis cut e 40 t 55 TCA by 7 cm wide calcite vein zones that containabout 5% very fine dusty sulphides in the vein and walls over adistance of about 25 cm. The remainder of the interval has onlytrace sulphides with slightly anomalous sections surroundingcalcite veinlets and weakly altered patches. There is a gradationallightening of the unit down hole as a result of an increase inalteration (bleaching/ sericitization). The unit begins moderatelymagnetic but gradually decreases in strength down hole with theincrease in alteration. There appears to be a direct correlationbetween magnetic strength and alteration perhaps implying aconversion of magnetite to pyrite (?). There is a minor amount ofbroken core along oxidized slips over the first 20' of core.

59.3 124.0 Altered Trachytic Syenite -There is a gradational increase inalteration to about 76.0' and a corresponding decrease to thetrailing contact- Overall the colour ranges from medium to paleolive grey. The textures, although somewhat obscured byalteration and changes in the colour of the minerals, is thesame. The feldspar grains are dull green grey; the ferromagnesiangrains are buff white to waxy green with local greenish remnantchlorite (?) in the core; the mafic inclusions are pale to mediumgrey green; and, the groundmass imparts the overall olive greycoloration. The pyrite content averages about n.% overall with 6%between 70 k 78'and elevated amounts in the more highly alteredsections and adjacent to carbonate veinlets. The most intensealteration focuses around a 10 cm white and pale grey carb quartzvein which appears to be related to enclosing shears and foliatedwalls S 50 TCA. The foliation in the walls is accompanied byseveral minor carbonate veins. Weak in situ crushing/ brecciationassocited with creamy pink grey bleaching has occurred over about

SampleNo.

533015330253303533045330553306533075330853309

533105331153312533135331453315533165331753318533195332053321533225332353324

533255332653327533285332953330533315333253333533345333553336533375333853339533405334153342

From(ft)

29.59.62.63 .66.70.74 .77.

80.84.97.

103.106.107.110.113.116.120.211.212215217220223226229232

235238241

244247249

251254257

261267

280287292324

938450

535

0900

0.0.5.5.0.0.0.0.0.0.0.0.0.0.0.0.0

.0

.0

.4

.3

.0

.0

.2

.5

.0

.3

.5

.0

To(ft)

32.

62.63.66.70.74.77 .80.

84.

87,99,

106,107.110,113.116,120124212215217220223

226229232235238241244247249251

254257260263270283288294327

Len

88450S35.0.0,0.0.0.0.5.5.0.0.0.0.0.0.0.0.0.0.0.0.0.0.0.4.3.0.0.0.8.2.0.0.5.0

(ft)

2.3.

3.3.4.

2.3.

3.3.1.

3.1.3.3.3.3.4.1

32

333333333321233223

23

956155

82

5

0100

05.0.5.0.0.0.0.0.0.0.0.0.0.0.0.0.0.4.9.7.0.0.6.7.0.7

.0

.0

PY%

1li11551

1

10.250.25

0.250.250.25

TR

TRTR

0.50.52.00.50.50.50.50.5

0.50.50.50.50.50.50.50.50.50.50.50.50.50.5

0.50.5

AUOZ/T

.002

nil.006nilnil.001.004.002.000.002.004.002.002.001nil.001nil.002.004.001.008.005.002.003.002.006.008.003.011.001.001.001.001

nil.002.002

.001

.003

.001

.001

.001

.001

AU1OZ/T

. 000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

. 000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

AU 2

Ppb

5510

2019

1019

13555

060

12551

51245

241570

13227

26118672

9653

21629094

353332426217

8357

27

9127

382121

Drill Hole KK98-1 Page: 3 of 5

From To Geology Sample From To Len PY AU AU1 AU2 (ft) (ft) . No. (ft) (ft) (ft) % OZ/T OZ/T ppb

25 cm centered at 81 i 85' . From this point, the host gradually becomes mottled medium grey reflecting less intense but spotty alteration aa well as minor bleaching adjacent to carb veinlets. A 3 cm shear carb vein at 106' trending about 85 TGA defines the start of a 30 cm fault structure which ends in an irregular zone of crushing. At 118' is a grey shear slip at 23 TGA. By 124', the rock has again become fairly fresh and the moderate magnetic signature has returned.

124.0 206.5 Trachytic Syenite- There is a return here to the less alteredhost similar to that described at the start. The overall colouris medium grey with local sections containing a bluish orbrownish tinge. There appears to be a slight change to agenerally more medium grained phase in which the elongatefeldspar crystals are not visible, perhaps being replaced bylarger, more tabular white chalky grains. Ferromagnesian grainsappear as dark grey clots or are altered (carbonatized?) to apale grey; mafic inclusions occur as dark grey irregular shapedblebs. In several areas, white ^mm carbonate rhombic metacrystsoverprint some of the texture of the host. The sulphide contentover this interval is trace but ranges up to 2% locally adjacentto carbonate veinlets and alteration patches. The host is cut bya network of 5% crossing pale pink carbonate veinlets S 25/ 40/50 TGA. Noteable carb veins with associted anomalous sulphidesoccur at 142.6' (2cm 9 55 TGA), at 174.0' (2cm 60TCA), and, at191.3' (0.5cm ® 60 TGA).

206.5 324.0 Bleached Zone- There is a gradational change to very stronglybleached/ altered host. At this point there is almost noresemblance to the original trachytic syenite as described atthe start. The overall colour has become a pale creamy greyishyellow to pale greenish grey and the texture is washed outyielding a fine grained look for most of the interval. Theslightly greyer sections that occur as patches and streaks,generally near or adjacent to carbonate veinlet clusters, areindicative of elevated sulphide (pyrite) concentrations.Overall, the pyrite content averages about D.5%, but locally inareas mentioned above, may reach 5% over several feet. About theonly indication of the original texture is the presence of theubiquitous mafic inclusions. Although generally altered tochlorite or weak green carbonate, perhaps indicating a mafic andultramafic origin, the inclusions have retained their shapes anddimensions. Occasionally, relic ferromagnesian grains andpossible feldspar grains may be visualized. The core is cut by4% creamy white carbonate veinlets that occur as dilatant gashveinlet clusters. There appears to be a fundamental change inthe carbonate from calcite to ankerite within this alterationpackage. The alteration/ bleaching is pervasive yet does notseem to be related to any major penetrative structure or intensemicrofracturing of the host. A strong shear gouge fault whichcuts the unit about 80 TGA between 215.6 Si 216.8', is followedby a 15' sulphide enriched zone d-2%) . 5 cm wide carbonateveins trending at 70/ 60 TGA are centered at 232.6 Se 238.6' and

Drill Hole KK98-1 Page: 4 of 5

From To (ft) (ft)

Geology Sample No.

From(ft)

TO

(ft)

Len (ft)

PY AU

OZ/T

AU l

OZ/T

AU2 p'pb

a 15cm carb quartz vein with accompanying foliated walls (9 55 TGA) cuts the unit at 240'. The fine grained texture persists to about 326' at which point a faint porphyritic texture becomes evident.

326.0 386.0 ALTERED SYENITE FELDSPAR PORPHYRY

There is no defined contact indicating an intrusive relationship between the finer grained strongly altered host and this intermittent porphyritic transition phase. Basically, there is a mix of 1^ weakly porphyritic phase and 85% of the fine grained strongly altered host decribed in the interval above at 206.0'. Contacts between the two phases are gradational possibly indicating internal comagmatic phases within the 'syenitic' intrusive. The porphyritic phase fades in and out of this interval; the contacts are defined by subtle and gradational increases in the size and quantity of creamy white sub- anhedral feldspar phenocrysts to a point where they comprise approximately 35% of the rock. The average size of the phenos is 2-3 mm in maximum dimension. The groundmass is fine grained but the mineralogy is difficult to determine because of the intense bleaching which has unified the colours to pale yellowish grey. Mafic inclusions stand out as angular green carbonate and chloritic fragments and streaks. At this point, the rock appears to have been very finely microfractured on a granular scale. The pervasive alteration consists mainly of sericitization, carbonatization and bleaching. Scattered disseminated grains and streaks of pyrite average about Q.25% over this transitional phase. Creamy white and pale grey carbonate and quartz veins to 10cm of no apparent economic significance, cut the host at various, but generally low, angles TCA. The odd vein contains splashes of a pale brown resinous mineral (sphalerite/ carbonate?).

386.0 553.0 FELDSPAR PORPHYRY ALTERED SYENITEThis phase of the intrusive is dominantly porphyritic (75^0 with the remainder as the finer grained phase, both as described above. The overall colours range between pale to medium grey in the less altered porphyritic sections and pale greyish yellow in the finer grained well altered zones. Feldspar phenos amount to about 35% of the porphyritic phases which again grade into the finer grained phases. The host is microfractured on an intergranular level and pyrite, which occurs as disseminated grains and clots, amounts to approximately Ik on average. Random carbonate tensionalf?) veining which constitutes about 3% of the host, again contains patches of the resinous pale brown mineral. Between 435 4 440', the core is blocky/ broken along nested fractures.457.0 461.0 Fault Zone -A major silicified and carbonatized vein structure

forms the core of a strong fault which cuts the porphyry @ about 25 TCA. The fault is characterized by 40% medium to dark grey silicification and quartz veining parallel to the fabric with 50% pale to medium grey/ yellow grey fine grained carbonatized host. The remainder is made up of a lense of porphyry and 3% fine lacey white carbonate threads. The fault zone is peppered with about 2% sulphides (py with very minor cp) which mainly occurs in the walls of veins.

530.7 553.0 Feldspar Porphyry - From this point on, the host is completely

5334353344

342.0348.8

345.0351.8

3.0

3 .0

0.25

0.25nil .001

.000

.0001226

53345533465334753348533495335053351533525335353354

533555335653357

53358533595336053361533625336353364

53365

390.393.396.399.402.417.420.423.426.429.433.436.439.442.445

448

451

454

457

459

461

0

.0

.0

.2

.2

.0

.5

.5

.5

.5

.0

.0

.0

.0

.0

.0

.0

.0

.5

.5

.0

393.396.399.402.405.420423426

429

433436439442445448451454

457

459

461

464

.0

.0

.2

.2

.0

.5

.5

.5

.5

.0

.0

.0

.0

.0

.0

.0

.0

.5

.5

.0

.0

3.3.3.3.2.3.

3.3.

3.

3.

3.3.

3,3.3

33

3

2

1

3

00

208.5

.0

.0

.0

,5

.0

.0

.0

.0

.0

.0

.0

.5

.0

.5

.0

0.

0.

0.

0.

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1.

1

1

1

1

1

1

1

1

1

1

22

2

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.5

.5

.5

.5

.5

, 5

.0

.0

.0

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.0

.0

.0

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.0

.0

.0

.0

.0

.0

.001

.001

.010

.004

.001

.001

.003

.039

.014

.002

.011

.001

.013

.003

.002

.002

.002

.007

.020

.045

. 004

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

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.000

.000

.000

38

21337141

24

3989

1322

480

53374

43

444

91

81

84

79

238

688

1536139

Drill Hole KK98-1 Page: 5 of 5

From To (ft) . (ft)

Geology

porphyritic with no fine grained phases. The colour has darkened to medium grey with a strongly porphyritic texture amounting to 4(H of the rock. The phenos are dull grey, equigranular (ave 2.5mm), subhedral, feldspathic and somewhat aligned in their long dimension indicating possible internal flow banding. The groundmass is a medium grey, fine grained mix of feldspar and chloritized ferromagnesians. There is a gradational decrease in alteration preceeding this interval; at this point, the host is fairly fresh. The carbonate veining drops off to Hi and the sulphide content averages D.5% near the start and trace at the end.

S amp 1 eNo.

533665336753368533695337053371

533725337353374533755337653377

5337853379533805338153382

From(ft)

464.467.470.473.476.479.

482.485.488.

491.494.497.

500.

503.530.538.550.

000050.0.0.0

.0

.0

.0

.0

.0

.0,0.0

To(ft)

467.470.473.476.479.482.485.488.491.

494497

500503506533541.553.

Len PY(ft) *

0005.0.0.0.0.0.0.0.0.0.0.0.0.0

3.3 .332333333333333

.0

.0

.0

.5

.5

.0

.0

.0

.0

.0

.0

.0

.0

.0

.0

.0

.0

1.1.1.1.1.0.0.

0.0,00

00000.0.

000.0.0,5.5.5,5.5

.5

.5

.5

.5

.5

.5

.5

AU

OZ/T

.003

.003

.006

.001nil.002.001.004.001.002.001

nilnil.001.001.001nil

AU1OZ/T

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

.000

AU2

ppb

87

91216347

55

4615347653110

14

2433193

553.0 553.0 END OF HOLE

SSSfvl ,__, Declaration of Assessment WorkNorthernD*v*toprr*rt - m , L?. ,andMnat Performed on Mining Land

Mining Act, Subsection 65(2) and 66(3), R.S.0.1990

Transaction Number (office use)

Assessment Files Research Imaging

bsectlon 65(2) and 66(3) of the Mining Act. Under section 8jf the Mining Act, lesrnent work and correspond with the niinlno'""f-VllraTTP'^it'''"i about this :hem Development and Mm f, IM PMT^S PMitBV iLJkel Road. Sudbury,

32D04NW2015 2.19015 900

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

f-"3* "'"

1. Recorded holder(s) (Attach a list if necessary)Name ,I^-c , Client Nunnber

Address Telephone Number1* r-

Fax Number

Client Number . ^. t T tf /f?

Address Telephone Number-70^ -S*?-

Fax Number

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

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

Physical: drilling stripping, trenching and associated assays

Rehabilitation

Work Type

\^(L^#^L v^LU

Dales Work From Performed Day /i | Month /C1 i

Global Positioning System Data (if available)

'^

To 0 'ear f ft DayO / | Worth /Z- 1 Year #0

Townshtp/Area ^ ̂ ̂ ^ ̂

M or G-Plan Number

Office Use

Commodity

Total S Value of Work Claimed ^(r^O

NTS Reference

M,n,ng Division ^^ ̂ ̂

Resident Geologist rDistrict ^VWnnd A/i.H&CEiVt^

Please 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.

vi' "'

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

-70 r - it 7-ress Fax Number

Name Telephone Number

Fax Number

Name Telephone Number

Address Fax Number

4. Certification by Recorded Holder or Agentl, MA cL\o- g-i ^ ̂ ^- A. y_______ , do hereby certify that l have personal knowledge of the facts set forth in

(Print Name|

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.

Signature of Recorded Holder or Agent

Telephone NurrfberAgent's Address Fax Number

0241 (03/97)

/,/n i

Ministry ofNorthern Developmentand Mines

Schedule for Declaration of Assessment Work on Mining Land

Transaction Number (office use)

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.

/z/sgyql~2, X ^? ^ V 3/* ~2~ Z- o o t ^

^Z-o/79/Z-LO/ to

/zz/ts'S

/ZZZZ,!^

/^^^ 1*5

/2ZS2,-? f

f f-~ ^. *^ ^-^~o ^j

i ^ ^~ -^ ^J f

/^Z&tt/S

/?l6f/?

/zz7^yy

Number of Claim Units. For other mining land, list hectares.

1

1

-^

1

Z.

1t

1l11

12.

f

RELAR

MININ

UfcC

Column Totals

Value of work performed on this claim or other mining land

y.ooo

.tf ) (o (/O

3EIVED)ER LAKE S DIVISION

1 1996 —— —

3 (D VO

Value of work applied to this claim

V 60

t/oo&0Z)

VcrO

g^O

*YCrOt/OQ

(/crOt/OO

YoO

t/frO

L/QT)

3&0

ty&fa

v

^

^80^

Value of work assigned to other mining claims

RECEDECS

GEOSCIENC^1 — ~-

' /oe/0

L/2- ^ 'O

'i

^fiKSTO

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

WEB ——

3 1.023 i\SSESSMMT.if: ——— —'i '

*-^ C? CJf~\ ^-^c5 *-r (j

i^ELf^jQQQ) M

2-SYo0290(0096)

Ontario MlnMryolNorthern Oevelopmenland Mine*

Statement of Costs for Assessment Credit

Transaction Number (office UM)

Personal Information collected on this form Is obtained under the authority of subsection 6(1) of the Assessment Work Regulation 6/M. Under •action 6 of the Mining Act, the Information Is a public record. This Information will be used to review the assessment work and correspond with the mining land holder. Questions about this collection should be directed lo the Chief Mining Recorder. Ministry of Northern Development and Mines. 6th Floor. 933 Ramsey Lake Road, Sudbury, Ontario, P3E 685. '——————" "'"' "~'Q C(~* C 1 \/ !Z Pi

Work TypeUnits of Work

Depending on the type ot work, 11*1 the number of hours/days worked, metres of drilling, kilo metres of grid line, number of samples, etc.

Cost Per InltGEOSCI

i 13. , So

- n Q ^3 u TbTai Cost

NCFASSESSMENTofnce————

0695" •7SQ

5S**5- -TOOi ̂ '

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

Transportation Costs / frf)

RECEIVEDLARDER LAKE

MiNIMG OIVISIOFood and Lodging Costs

J99ft

Total Value of Assessment Work

Calculations of Filing Discounts:

1. Work filed within two years of performance is claimed at 100^ 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 SC^/b 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 ol 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,.pnMo.3i for verification and/or correction/clarification, i! vert'K:at'0!i t;!v-v: ..orruv ; : .v ; ;c ! r //k.atioi' ^3 not medo, the Minister may reject all or part ot the assessment worK submiued.

Certification verifying costs:

l, M(CUA.-feA i—6-AHs/ , do hereby certify, that the amounts shown are as accurate as may(please print lull 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 certification.

i/^H ^7(recorded holder, agent, company pedion with signing authority)

am authorized

Dale

Ministry ofNorthern Developmentand Mines

January 7, 1999

Michael LeahyRAVEN RESOURCES INC.139 CARTER AVENUEKIRKLAND LAKE, OntarioP2N-2A1

Ministere du Developpement du Nord et des Mines Ontario

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

Telephone: (888)415-9846 Fax: (877)670-1555

Dear Sir or Madam:

Subject: Transaction Number(s):

Submission Number: 2.19015

StatusW9880.00742 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. Allowable changes to your credit distribution can be made by contacting the Geoscience Assessment Office within this 45 Day period, otherwise assessment credit will be cut back and distributed as outlined in Section #6 of the Declaration of Assessment work form.

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 lucille.jerome@ndm.gov.on.ca or by telephone at (705) 670-5858.

Yours sincerely,

ORIGINAL SIGNED BYBlair KiteSupervisor, Geoscience Assessment OfficeMining Lands Section

Correspondence ID: 13257

Copy for: Assessment Library

Work Report Assessment Results

Submission Number: 2.19015

Date Correspondence Sent: January 07, 1999 Assessor: Lucille Jerome

Transaction Number

W9880.00742

Section:16 Drilling PDRILL

First Claim Number

1220179

Township(s) / Area(s)

LEBEL

Status

Deemed Approval

Approval Date

January 07, 1999

Correspondence to:Resident Geologist Kirkland Lake, ON

Assessment Files Library Sudbury, ON

Recorded Holder(s) and/or Agent(s):Michael LeahyRAVEN RESOURCES INC.KIRKLAND LAKE, Ontario

MICHAEL JOHN DAVID LEAHY KIRKLAND LAKE, Ontario

Page: 1Correspondence ID: 13257

o oOJ

Ei]m

o en H

n ts

573000m E 40eo8oo' 790 54'

20 583QO o mg

MORRISETTE TOWMSHIP

98I93J, 901934

- — -L —

IIII537 7- \ 1111536.^^ i......982328

- - -H - - -4 -r.-1165428

L/J9 L "- 4-

9B2JI9 "4 -,J '"98232rj~

, U2200I9 h:^ .*MI i^,aatM*w.

L I220IS3500

12063-05 \i206374S32879 \ .jj 532877

^ •f;- r^tr HR ^'' .3 j 644007 \ 644008^^'

K iR K L AN D1220182

L u - - - - 4- -' 1046425 T. ! L

4— — — —

.-A---- H----

1046435 ' 1046436 1046521

""" ""_ 42 25201 i _ ̂ 22 5[2^

42219 ^ iIO4&44O l 1046439 i

" . t-' '

046491 1047122

1046,539 l I0465S6 \ ^1046555 j 10*6554l j I0465ii\wv_- -^'^- xVj

1046766 l IO46767 l I04677J

1047131 , 1047120 l 10471*9 1047164 1047163j IT546757 ,/ l -1 ' 1046758 l" 1048799 ^L 1046768 ' 104^771

-h- —1047133 1047132 , IO47I66 l 1047165

t

iS-: 'IO46795|

I04S779 , .104(6787 , 1046792 ' ' '047135L j l i.,——M /l L

j \(' 1046^*9 (l

BOSTON TOWNSHIP

573QOO mf 40 eocoo'SMD 639 95 04

Ontario

Ministry ofNaturalResources

Ministry ofNorthern Developmentand Mines

INDEX TO LAND DISPOSITION

PUN

G-639TOWNSHIP

LEBEL

M.N.R. ADMINISTRATIVE DISTRICT

KIRKLANDMINING DIVISION

LARDER LAKELAND TITUS/REGISTRY DIVISION

TIMISKAMING

Seal* 1:20000

1000HMTM

2000

1000 1000 2000 3000 •000 7000ft*

10000^n F*

Contour Interval 10 Metro*

SYMBOLSBoundary

Township, Meridian, Baseline.

Road allowance; surveyed. . shoreline.. .

Lot/Concession; surveyed, unsurveyed

Parcel; surveyed unsurveyed

Right-of-way; roadM

railwayutility.... ...... ................. -

Reservation .................................... ;x: :: :: :: : : : :: :: :: : : : :v:v

Cliff, Pit, Pile

Contour ................ .......................... ^InterpolatedApproximateDepression.

Control point (horizontal) ............................ .......... A

Flooded land...,............... ........ ......... :-.----::- ~~~^~

Mine head frame ................................... ........... a

Pipeline (above ground) .......... ..... ........

Railway; single track. .. ... ...... ........... ————'——~-

double track........... .................. ———~——^abandoned............................... -1— —'— ——

Road; highway, county, township .................... —=- —access ..................................... - - - - - -trail, bush ................................... - — — — — -

Shoreline (original)................................. ---"'"" ""'-----

Transmission line

Wooded area...................................... -

DISPOSITION OF CROWN LANDSPatent

Surface A Mining Rights . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .9Surface Rights Only . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .OMining Rights Only . . . . . . . . . . . . . . . . . . . . . . . . . . . . . , . . . . . . . . . . . .O

LeaseSurface A Mining Rights . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .1Surface Rights Only . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .HMining Rights Only . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .B

Licence of Occupation . . . . . . . . . . . . . . . . . . . . . . '1-5*^^^ . . . . . . . . . . . . V

Order-in-Council. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .'"T . . . . .OC

Cancelled ...................................................9

Reservation . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 0

Sand 4 Gravel. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 0

NOTICE OF FORESTRY ACTIVITYTHIS TOWNSHIP l AREA FALLS WITHIN THE ———

AND~MAY~BE~SUBJECT TO FORESTRY OPERATIONS. THE MNR UNIT FORESTER FOR THIS AREA CAN BE CONTACTED AT: P.O. BOX 129

SWASTIKA. ONT,POK ITO705-642-3222

AREAS WITHDRAWN FROM DISPOSITIONMRO - Mining Rights OnlySRO- Surface Rights OnlyM * S - Mining and Surface Rights

20/11/69

l SEC. 36/80 w - i7/ 83

S R. O '

S.R.O.

FH*

165484

164586

REOPENED O-L-16/97 IS/10/97 S. K M. 157*9

JSEC.35 W-L-14/98 17/04/98 M*S 195150

NOTES

KINS KIRKLAND TOWNSITE

CIRCULATED JULY 6/95 ARCHIVED AUGUST 02,1995 ARCHIVED DECEMBER 13, 1996

THE INFORMATION THAT APPEARS ON THIS MAP HAS BEEN COMPI1 ED FROM VARIOUS SOURCES, AMD ACCURACY IS NOT GUARANTEED THOSE WISHING TO i^AKE WIN ING CLAIMS oh-OULD CON SULT WITH T i|; MINING RECORDER. 1.1 SJISTRY OF NORTHERN DEVELOP MENTAN' 1 ^11,', ^S PDR AD- DITIONA l'\. FORMATION ON THE : iA US OF THE LA r J OS SHUWN1 HEREON.

Map base and land disposition drafting by Surveys and Mapping Branch. Ministry of Natural Resources.

The disposition of land, location of lot fabric and parcel boundaries on this index was compiled for administrative purposes only.

CDi

O) 01 CD

mODm

H

ro

CD tCD OJ (D