R E C O N N A I S S A N C E GEOLOGICAL A N D

GEOCHEMICAL I N V E S T I G A T I O N

H E N R Y , MAYE, WIZZARD, P U R P L E HAZE A N D

S T E P P I N G S T O N E MINERAL CLAIMS

S L O C A N MINING D I V I S I O N

K A S L O , B . C .

N T S 82 K 3

L A T I T U D E 50'05'N. L O N G I T U D E 117O06'W

P r e p a r e d for

HELENA R E S O U R C E S L T D .

G I E O L O G I C A L B R A N C H A S S E S S M E N T R E P O R T

A R C T E X ENGI N

P a u l Kallock G e o l o g i s t

N o r m a n C . D a v i d s o n , P . E n g . Consulting E n g i n e e r

F e b r u a r y 3, 1984

T A B L E O F C O N T E N T S

SUMMARY ....................................... 1

INTRODUCTION ................................. 2

LOCATION MAP ................................. 3

CLAIM MAP ...................................... 4

GENERAL GEOLOGY ............................. 5

GEOLOGY OF THE CLAIM AREA .................. 5

Stratigraphy ................................ 6

Structure .................................. 6 Mineralization and R o c k Geochemis t ry ........ 7

Soil and S t r e a m S e d i m e n t G e o c h e m i s t r y ...... 8

CONCLUSIONS .................................. 9

RECOMMENDATIONS ............................. 1 0

C O S T ESTIMATE ................................ 1 0

GEOLOGIST’S CERTIFICATE ..................... 12

ENGINEER’S CERTIFICATE ....................... 13 REFERENCES .................................... 1 4

ITEMIZED C O S T STATEMENT. 1983 PROGRAMME ............................... 15

APPENDIX : GEOCHEMICAL ANALYSES

MAPS : (Pocket inside back cover) GEOLOGY MAP

GEOCHEMICAL MAPS: Gold Silver

Nicke l

-

1

RECONNAISSANCE GEOLOGICAL AND

GEOCHEMICAL INVEST IGAT ION

HENRY, MAYE, WIZZARD, PURPLE HAZE AND

STEPPING STONE MINERAL CLAIMS

SLOCAN MINING DIVISION

KASLO, B .C .

SUMMARY

Geological mapping and geochemical surveys including soil, stream

sediment and rock sampling have taken place on the Henry et al. mineral claims during September 1983. The claims are underlain by rocks of the Milford, Kaslo and Slocan Groups. Numerous samples of soil and rock float contain greater than 100 par ts per billion gold and more than 2 par ts per million silver. Local anomalous base metals are also present. At least three areas w i t h multi-sample anomalous values warrant detailed rock geochemistry. A cost of $ 3 5 8 , 5 0 0 is estimated in three Phases.

2

INTRODUCTION

The Henry, Maye, Wizzard, Purple Haze and Stepping Stone mineral claims

are located in the Slocan Mining Division, between 37 and 54 kilometres northwest

of Kaslo, B . C .

Mount Schroeder and Mount Dryden. 1463 to 2866 metres (4800 to 9400 feet) .

NTS map sheet 82 K/3. N50°06' latitude and W117°071 longitude.

They are on the crest and northern flank of Blue Ridge between

Elevations of the property range from The claims lie within the east half of

The central par t of the claim group includes co-ordinates

A s can be seen from the accompanying claim map, the property is comprised of 7 8 units, less approximately 53 located claims overlying the Maye and Henry

claims. Statistics of the property are as listed:

Record or Claim Name Tag No. Size (Units) Record Date

Henry 3821 ( 4 )

May e 3823(4) Wizzar d 3824 ( 4)

Purple Haze 3a25(4)

Stepping Stone 3826 ( 4 )

16 April 25, 1983 18 1 2

20 1 2 1 1

11

I I

11

Highway 31A lies 4 km south of the property. Gravel roads from the

Whitewater-Retallack area lead to within 2 km of the south edge of the claims.

However, the rugged nature of the terrain on most of the claims makes helicop- ter transport most desirable. Nakusp and Nelson, B. C .

Helicopter flying services are available from

The 1983 programme of exploration included soil, stream sediment and rock

geochemistry on all of the claims.

the Henry and Stepping Stone claims.

Geological mapping was limited to par ts of

There is no recorded history of mineral production from the Henry et al .

claims.

remains of an abandoned pipeline aqueduct leading from the area of the Stepping

Stone claim to the head of Whitewater Creek.

The only sign of previous exploration activity found was the scattered

3

CONSULTING ENGINEER

OCTOBER, 1983

RESOURCES LIMITED

I HENRY PROJECT

>>>_)_?I + EXPIRY DATE JULY 15.1984

5

GENERAL GEOLOGY

Regionally the property lies near the west-central margin of the Kootenay Arc, an arcuate belt of structurally deformed, primarily Paleozoic sediments stretching from Washington State to Revelstoke, B .C .

Monger (1982) and Klepacki (1983) have indicated that volcanic and related rocks (greenstones) of the Kaslo Group may have formed the leading edge of Terranes including younger calcareous flysch of the Slocan Group, a s they accumulated on the ancient margin of North America (which included the Carbon- iferous Milford Group) , and were subsequently telescoped.

Recent studies by

In the Blue Ridge area the aforementioned rock units have a general north- west trend with dips moderate to steeply north and south. The Henry et al . claims span many of these sedimentary and volcanic rocks beginning in the east where the Henry and Maye claims straddle the Milford Group, a wedge of Slocan Group and part of the Kaslo Group. The Wizzard and Purple Haze, in the central par t of the claim group, are underlain primarily by the Kaslo Group, although some dark fine-grained sediments of the Slocan Group are locally present. dominated by Kaslo Group volcanics which include an ultramafic unit.

The Stepping Stone claim in the northwest part of the claim group is

GEOLOGY OF THE CLAIM AREA

During September 1983 geological mapping was undertaken in the Henry

claim along Rossiter Creek and at the Stepping Stone claim near the headwaters of the South Fork of Cooper Creek. A geology map at 1: 1 0 , 0 0 0 scale is included

in the pocket of this report. From mapping within the claim block and on adjoin- ing areas it was determined that the Kaslo-Slocan and the Slocan-Milford contacts cross diagonally through the property from southeast to northwest. Rock exposures are excellent on steep, upper slopes and ridge crests , however exten- sive talus cover and alluvial fill blankets the lower slopes and valley floors.

6

Stratigraphy

The oldest rocks in the claim group belong to the Milford Group of upper Mississippian to Pennsylvanian o r Permian age. corner of the Henry and east half of the Maye claim. Light green, tan or white

thinly laminated chert is characteristic of the upper part of the Milford Group. Grey and brown phyllite and metasandstone are also common. marble which are also common in the Milford Group probably occur northeast of

the Maye claim.

They occur in the northeast

Limestone and

The Mississippian and/or Permian Kaslo Group comprises the bulk of the

Henry et al. claims.

andesitic volcanics (greenstone) , but also includes fragmental or ttiffaceous volcanics and sediments, and pillow lavas. tinite, is also present within the Kaslo Group and was seen as abundant quantities of float in the west end of the Stepping Stone claim.

For the most par t , the Kaslo Group is composed of

An ultramafic belt, mostly serpen-

The Slocan Group of Triassic to Jurassic age disconformably overlies the Kaslo Group. quite common in the Slocan Group but was not seen in the claim area. Near the northwest corner of the Henry claim a calcareous sandstone and conglomerate were seen at the base of the Slocan Group.

It is composed primarily of black slaty argillite. Limestone is

Structure

The bedded formations in the Henry and Maye claims have northwest

trends with northeast dips. the Mount Dryden Anticline as described by Klepacki (1983) . Siliceous argillite observed in the Stepping Stone claim has southwesterly dips and may lie on the southwest limb of this anticline. latter argillite. Klepacki has included it within the Milford Group due to their similar siliceous nature.

Their position conforms to the northeast limb of

There is some question as to the age of the

Of importance to the structure of the Mount Dryden Anticline and the repetition of Slocan Group sediments on the north side of Blue Ridge is the Mount Schroeder Fault. This fault, of considerable normal displacement, separ- ates Slocan Group argillites from siliceous sediments of the Milford Group. I t

7

trends northwesterly through the Henry and Maye claims and passes near the northeast corner of the Purple Haze claim.

Mineralization and Rock Geochemistry

A diversity of sampling methods was used on the Henry Project to analyse the geochemical signature of the detritus. ly poor. extending geochemical coverage into inaccessible areas. Where neither stream nor talus fines were present, a composite sample of chips of 1 0 to 15 cobbles o r boulders was randomly collected from an area of two to three square metres. The type of sample at each particular location is indicated on the individual geo- chemistry maps in the pocket of this report.

Residual soil development is general- Often talus fines or stream sediments were collected in hopes of

During the limited geological mapping survey, one area of sulphide mineral- ization was noted. In the saddle area between Rossiter and Davis creeks outside the Henry claim, pyrite occurs in numerous veins with calcite in mafic volcanic float boulders. A sample of vein material assayed 1 .04 oz silver per ton, 2.55%

lead, and 130 par ts per billion gold. quartz-sericite altered basal Slocan Group conglomerate or breccia contained 115 ppb gold. Northwest structural and stratigraphic trends in this area may indicate that anomalous gold and silver value in the western Maye claim, such a s May-B-17-R with 145 ppb Au or May-B-22 with 2.3 ppm Ag, are genetically related.

Near the same area, soil from pyritiferous,

Results of other rock geochemical sampling are also very interesting, par- ticularly in an areaon the Purple Hazeclaim and adjoining area. samples Bren nos. 4 , 6 , 7 , 10 and 1 2 contained silver and/or gold of greater than 2 ppm Ag or 95 ppb Au. Sample Bren-12 contained 0.082 oz gold/ton and 1 . 0 2 oz silver/ton. Al l of these samples represent the float boulders or cobbles of talus material. and Whitewater creeks where Milford Group ( ? ) argillite may be present.

Composite rock

Source area lies on the steep north face of the ridge between Cooper

Another area in the north-central Purple Haze claim returned anomalous gold and silver from talus material; Bren-21 contained 170 ppb gold and 5.1 ppm silver, and Bren-23 contained 2 . 9 ppm silver. Greenstones of the Xaslo Group

8

or basal conglomerate of the Slocan group are projected to pass near this area. Elevated copper levels are generally associated with anomalous gold.

On the Wizzard claim rock samples number 3 and 4 contained 75 ppb gold and 2.5 ppm silver, respectively. rock.

Kaslo Group volcanics are probably the host Sample 4 also contained 480 ppm copper.

Close to the boundary of the Maye claim one rock sample contained anomal- ous gold. Sample May -B-17-R contained 145 ppb gold.

N o rock samples from the Henry e t al. claims contained significant nickel.

Soil and Stream Sediment Geochemistry

Considering anomalous gold in soils and stream sediments to be greater than 75 par ts per billion (ppb) , four soil samples near the west boundary of

the Purple Haze claim are anomalous.

gold. composite sample containing anomalous gold. Milford Group siliceous sediments may be the source or host of gold mineralization in this area.

Bren 2 , 4 , 5 and 8 contain up to 195 ppb This area of enriched soils is coincident with a previously described rock

On the Wizzard claim, five soil samples contain between 7 5 and 285 ppb gold. seen that several anomalous soil samples may conform to this direction.

Considering structural trends to be northwesterly in this area, it can be

Several areas on or near the Maye claim contain anomalous precious metals in soils or stream sediments. A tightly sampled area near the "Only Chance" claims (between Henry and Maye claims) contained five stream sediment samples with 2 . 0 to 3.7 ppm silver and a soil sample with 115 ppb gold. near the contact of Slocan and Milford groups. In the northwest corner of the Maye claim where the Slocan Group crosses into the Wizzard claim, stredm sedi- ment sample May-22 contained 2 .3 ppm silver. Farther east in the Maye claim another stream sediment sample, MA-D- 1 2 , contained 2 .7 ppm silver, Milford Group sediments underlie this area.

This area is

Significant concentrations of nickel are present in stream sediments in the south and west end of Stepping Stone claim. 200 ppm nickel with sample P-14 containing 0 .12 percent nickel. this nickel is undoubtedly serpentinite of the ultramafic unit within the Kaslo

Three samples contained over Source for

9

Group. westward into the Kane Creek drainage as it passes through the southwest corner of the Stepping Stone claim.

This belt is coincident with upper Whitewater Creek and trends north-

A single stream sediment sample, MAY-B-10, near the headwaters of Davis Creek contained 188 ppm nickel and 0 .14% zinc. Source for this sample may -

come from the Only Chance claims or possibly the Maye claim.

CONCLUSIONS

Several soil and rock composite samples in the southwest corner of the

Purple Haze claim contain significant quantities of gold and silver. up to 0.082 oz gold/ton and 1 .02 oz silver/ton. Rock types present in the area include the Kaslo Group greenstones and possibly argillite of the Milford Group.

Wizzard and Maye claims. Most of the Wizzard anomalies appear to be underlain by Kaslo Group volcanics. On the Maye claim, Slocan and Milford Group sedi- ments are present. on the Maye claim, the stratigraphic setting i s similar to the Nevermore claims of Red Diamond Mines Ltd. , approximately 6 km to the southeast. Significant gold enrichment in soils has been detected overlying Milford Group, and near the Slocan Group contact at this property.

Values range

Precious metal soil and stream sediment anomalies are also present in the

Although detailed geologic mapping has not been undertaken

Nickel has been encountered in stream sediments in tka Stepping Stone Quantities of up to 0 .12% have origins in the serpentinite belt of the claim.

Kaslo Group. Continued exploration of the Henry et al. claims must be carried out late in

the field season. Elevations of most anomalies are above 1830 m (6000 f t ) and several are on north-facing slopes. Tent camps established on each claim and serviced by helicopter are most feasible for the next phase of geological, geo- chemical and geophysical surveys.

1 0

RECOMMENDATIONS

A grid layout should be established on the claims. Soil and/or rock geo-

chemistry, magnetometer and VLF-Em surveys should be undertaken. geologic mapping is also required.

Detailed

Geological mapping combined with a modified grid and geochemical sampling should be used in follow-up of several stream sediment samples which may have a source area within the Maye or Henry claim.

Subsequent to the foregoing Phase 1 exploration, Phase 2 may include , detailed geophysical surveys or limited shallow diamond drilling. Follow-up

sampling and mapping of anomalous areas found during Phase 1 may be warranted. Extensive diamond drilling would be dependent on Phase 2 results.

COST ESTIMATE

Phase 1

Follow-up exploration of geochemical anomalies and geological mapping of

important areas.

Geological mapping Grid layout and geochemical sampling Geophysical surveys including magnetometer and VLF-EM Analyses Camp and supplies Helicopter support Data treatment and reporting Engineering and supervision

Travel

$ 8,000

8,000

3,000 1 0 , 0 0 0

3,000 6,000

5,000

2,000

2,000

Contingencies @ 10% 47,000

4,700

Total Phase 1 51,700 $ 51,700

11

Phase 2

Detailed geological mapping, rock geochemical studies, geophysics or

shallow drilling of initial targets.

Geological mapping $ 5 ,000

Detailed geochemical or geophysical grid and survey 1 5 , 0 0 0

Shallow hole diamond drilling programme 200 m (3 $120/m 24 ,000

Camp and supplies 6 , 0 0 0

Helicopter support 12.000

Data treatment and reporting 7 , 0 0 0

Engineering and supervision 8,000

Geochemical analyses, assays 1 0 , 0 0 0

Travel

Contingencies (3 20%

2,000

89,000 17,800

Total Phase 2 106,800

Phase 3

Diamond drilling with helicopter support , 1000 m (3 $ 1 2 0 / m , allow $200,000

$106,800

200,000

Total Phases 1, 2, and 3 $358,500

Results of each Phase should be compiled into an engineering report;

continuance to subsequent Phase should

able recommendati b@&/4bQ gineer . Respectful

be

Vancouver, B . C . , February 3 , 1984

contingent upon receiving favour-

'-% e \a

Norman C . Davidson: P. Consulting Engineer :,

EXPIRY UATE JULY 15, 1984

1 2

GEOLOGIST'S C E R T I F I C A T E

PAUL KALLOCK

I , Paul Kallock, do state:

Services, 301 - 1855 Balsam Street, Vancouver, B . C .

that I am a geologist with Arctex Engineering

I Further State That:

1.

2.

3 .

4 .

5.

I have a B.Sc. degree in Geology from Washington State University,

1970. I am a Fellow of the Geological Association of Canada.

I have engaged in mineral exploration since 1970 , both for major mining

and exploration companies and as an independent geologist.

I have co-authored the report entitled, "Reconnaissance Geological and

Geochemical Investigation, Henry, Maye, Wizzard, Purple Haze and

Stepping Stone Mineral Claims, Slocan Mining Division, Kaslo, B . C . The report is based on my fieldwork carried out on the property, and

on previously accumulated geologic data.

I have no direct o r indirect interest in any manner in either the property

or securities of Helena Resources Ltd. , or its affiliates, nor do I antici-

pate to receive any such interest.

I consent to the use of this report in a prospectus or in a statement

of material facts related to the I -aisin

Geologist

Vancouver, B . C .

February 3, 1984

13

ENGINEER'S CERTIF ICATE

NORMAN C. DAVIDSON

1. I , Norman C . Davidson , am a Registered Professional Engineer in the Provinces of British Columbia, Nova Scotia and Ontario. My address is

P.O. Box 39, St. Andrews, Antigonish County, Nova Scotia BOH 1x0. I am a graduate of Michigan Technological University, Houghton,

Michigan, U. S.A. , with a B . Sc. in Mining Engineering. of the Haileybury School of Mines a s a Certified Mining Technician.

registered a s a Mine Manager under the Coal Mines Regulation A c t of Nova Scotia. Nova Scotia. I have been engaged in mining exploration, development and mine produc-

tion for 21 years. A personal examination of the property was not undertaken.

completed report was reviewed and discussed with Arctex Engineering

Services personnel, the competence of whom is known to the undersigned.

I have no interest either directly or indirectly in the claims named herein or Helena Resources Ltd. , nor do I expect to receive any.

I consent to the use of this report in a prospectus or in a statement of material facts related to the raising of funds.

2. I am a graduate

I am

I am a member of C.I.M., A.I.M.E., and the Mining Society of

3 .

4. The

5.

6.

Vancouver, B . C . February 3 , 1984

n C . Davidson, P.Eng. lting Mining Engineer

1 4

REFERENCES

Goldsmith, L .B . and Kallock, P. 1983. Review of Base and Precious Metal

For Rayrick Grub- Resources, Kaslo-Lardeau-Whitewater Area, B. C . staking Syndicate.

Kaslo and Slocan Groups, Roseberry Quadrangle, Lardeau Map Area, B . C . In Current Research, Part A .

Klepacki, D . W . 1983. Stratigraphic and Structural Relations of the Milford,

G.S.C. Paper 83-1A.

Monger, J . W.H. et al . 1982. Tectonic Accretion and the Origin of the Two Major Metamorphic and Plutonic Belts in the Canadian Cordillera.

Geology, V , 10, pp. 70-75.

Read, P.B. and Wheeler, J.O. 1976. Lardeau West Half Geology,Map 93E.

G.S.C. Open File 432.

15

ITEMIZED COST STATEMENT, 1983 PROGRAMME

A . Wages

P. Kallock, geologist, Sept. 21, Oct. 29; Jan. l a , 1 9 , 1984 total 4 days 8 $300/day

J. Randa, prospector, Sept. 21 , 22 , total 2 days 8 $200/day W . Flanagan , prospector, Sept. 21, 22, total 2 days 8 $150/day

D. Richards, prospector, Sept. 2 1 , 22 , total 2 days 8 $150/day

N . C . Davidson, engineer, Jan. 28, 1984, 1 day 8 $400/day

$1 ,200 .00

400.00

300.00

300.00

400.00

2,600.00 $2 ,600 .00

B . Food, Accommodation

Sept. 21 , 22 , 7 man days, $235.13 + 7 = $33.59/man/day

C . Transportation

Helicopter

Travel, Vancouver-New Denver, pro-rated

235.13

$ 1 , 4 9 1 . 0 0

343.58

1,834.58 1,834.58

D . Analyses

164 samples cost $ 2 , 6 52.03 = $16.17/sample

E . Report

Enlargements, typing, drafting, photocopying, report material, prints

2,652.03

I, 384.00

A P P E N D I X

TO ;

P. Kallock ........................................................................ 1 .

LORING LABORATORIES LTD. Page # 1

SAMPLE No. oz./ToN 02. /m % % % % STT,VER cu Pb Zn Ni

"Assay Analyses"

Rock Samples HEN=-P-1-R

Stream Sediments

Step-Stone-P-14 MAY-B-10

.082

1.04

.17 1.02

2.55

.21

.12 .14

3 gerebg &ertifu THAT THE ABOVE RESULTS ARE THOSE LCI

ASSAYS MADE BY ME UPON THE HEREIN DESCRIBED SAMPLES . . . .

................. ............................ I

Rejects Retained one month.

Pulps Retained one month unless specific arrangements made in advance. . . . . . . . . .

Asarrver

............ ~~~. ....... <'. ...

nFi m 'FN . uz 96 LIJ Gdd Mdd Mdd Mdd Mdd Mdd

.... S3ldWVS 0381113830 N13113H 3Hl NOdn 3W A8 3OVW SAVSSV

3SOHl 311V SllnS311 3A08V 3Hl lVHl iiff43aD aqa-lau

'ON 3ldWVS

T?N OE OP ss OLT sz OT OOOT+ OPT S6 SLT T?N SET T?N 02 SE T?N OT TTN T?N T?N S

S OET

1

P' 9' 6'2 9' T-S 9' S' OE+ Z'Z T'T 6'T PO

6' E* 9' P' L' P' 8'T 6' L' POT

zz PP TP EP PT 8 ZE OP SP 8E TP TZ ES ZE TE TZ 82 ST P8 PT PT 99

SOT SL 6L 9P 2s zz L9 EL LS 0s E9 SP 6P 6E ZP ZP PP PS OOOT+ 98 89 ZST

8' PE TP OE+ TS PP

81 6E 8E PP OT6 02 TE SE LZ 9E PE 8P TO ZP PE TP 69 PE s9 9L 28 86T

PZ PTT OZL sz 9ET OE ZE SLT C9-t 99 0s 8s PP TP OP ZE 91 92 OOOT+ OZP ZET ZST

09s L9 OOOT+ P6

8-T -G-M m PZ - rn El - m zz - am3 TZ - m oz - ~3423 8'1 - dwa ZT - dl433 OT - rnL - m9 - ms - mP - 8-f -mff rnET - 8-L -

8-9 - 8-2 -a-w 8-z - 8-T -Tlrs/!Js 8-0s - H 8OT-d-3lDLS F-?

8-Z-6- ,

I 8-T-d-2XNZH

d rPY J@3q

0 .......................

.................... _____._. .....

E86T '82 x%0730 alea ....................... .... S6ESZ 'ON al!j

MAY-B- 2-R - 3-R - 4A-R - 4B-R - 13-R - 15-R - 17-R

WIZARD- 1-R - 3-R - 4-R - 6-R - 10 CaMP - 12 COMP - 1 4 CCM? - 20 COMP - 2 1 CQMP - 24 CQMP - 32 CQMP

L & A S S A Y up

LORING LABORATORIES LTD. Page # 3

~~~~~ ~

PPM PPM PPM PPM PPM PPB 0 1 Ph Zn Ni Am Ai i

12 40 51 34 19 29 18 34 38 30 82 440 18 177 17 28 27 28

480 16 22 24 30 16 37 17 51 23 82 29 58 22 72 44 30 16

54 19 480 37

79 7 96 18 46 48

193 44 34 31 83 9 57 24 56 12 16 15 32 18 46 26 46 32 64 26

118 43 113 62

23 10

.2

.9

.4

.5

.2 1.8

.8

.1

.2 2.5

.4

.2

.2

.4

.6

.2

.3

.4

Nil 5

N i l N i l N i l

65 1 4 5

30 75 30 30

5 20

N i l 5

N i l 5

10

3 Berpbp aertifu THAT THE ABOVE RESULTS ARE THOSE - ASSAYS MADE BY ivfE UPON THE HEREIN DESCRIBED SAMPLES . . . ,

Rejects Retained one month.

Pulps Retained one month unless specific arrangements made in advance.

Aasayer

m - p - 3 -P- 4 -P- 5 -P- 6 -P- 7 -P- 8 -P-11

L PPM PPM PPM P P L SAMPLE No. cu Pb Zn N i Ag - AU

LORING LABORATORIES LTD. Page # 4

3P-STCNE-P-11 -P-12 -P-13 -P-14

HEN - 50 - 51 - 52 - 53 - 54 - 55 - 56 - 57 - 58 ST/ST- 3

- 4 - 5 - 6 - 7 - 8 - 9 - 10

MA-D- 3 - 4

?ejects Retained one month.

W p r Retained one month inless specific arrangements nade in advance.

100 62 98 92 95 450 77 81 103 118 47 33 67 43

84 53 70 44 111 75 123 57 165 79 a2 41 45 52 66 45 105 47 70 43 a 1 39 73 38 64 36 96 28 54 120 157 33 92 49 50 73 72 52 108 38 121 51 108 53 67 14 6

113 146 17 3 192 164 131 184

a4 62 93 94 16 1 158 300 18 3 121

117 173 168 67 74 81 86 92 83 78 102 104 43

189

60 61 54 42 61 26 52

550 68 520

+loo0 152 45 48 48 78 51 42 54 47 198 32 20 36 76 14 6 320 79 24 11

1.2 1.3 1.8 1.5 1.3

.8 1.3

.9

.8

.9

.9 1.0 .9 1.2 1.4 .8 1.3 1.7 1.8 1.0 .9 .7 .9 .7 .8 1.0 1.0 1.0 1.0 .7

N i l N i l 5

10 N i l 15 5

Rerebg aertifu (r, THAT THE ABOVE RESULTS ARE THOSE

ASSAYS MADE BY ME UPON THE HEREIN DESCRIBED SAMPLES . . . .

5 N i l

5 15

5 N i l N i l N i l N i l N i l 5

N i l 5

N i l 10

N i l N i l 35

N i l 20 5 20 5

Aseayer

........ ...... ..~ ............................ & ............ -9 -

.... S3ldWVS 0391M3S30 N13M3H 3Hl NOdn 3R A9 30VW SAVSSV

3SOHl 3aV SllllS3M 3AOQV 3Hl IVHl 53f833n aqa.la& r,

OT OT T?N OT T?N S 001 OT SE T?N 5 oz ST 07: S S OT 0s ST T?N S T?N OT ST T?N OP S S T?N T?N T?N

S' 8' Z*T E-T E*Z P'Z 8'2 6'2 S'T TOT P'T ED€ L'E L'Z 9' 0'7: 6' L' S'T 9' 8' L' 8' 8' 6' 6' L'Z O'T L' 8' 8'

TL EL LL ES 09 E9 8s 69 8 87: 89 PS L8 66 28 LP zs 8E EE 8P OE ZE 9E 8E PZ 9P 82 TZ 6P OE PZ EE

98 S8 PET TTT OOE OEE 0 PP oz9 OOOT+ 867: 09z 085 oss 08P 29 7:S-t ZET 607: OEP 9o-r LZT ZZT EET 68 ZPT 9TT EST ELT POT EOT TOT

ZE 801 8E L6 SE 8TT ZP ZOT 09 26 LE €8 6E LZT PE ZTT EP PZT SE 9ET OL 8CT 9ZT EET ZTT 89T 69 86 6Z 88 92 06 EE ;b9 PE EL PP 08E PE TPT zs 8LT 8E EOT 9P ZPT OE 85 zs z ET 6S LST 8ET PLT 8P S8 8P LL P9 PTT 06 8TT

ntl f%? ?N UZ 9d n3 ffdd Ndd Ndd Ndd Kdd Kdd

MSSV

JLEXWd Xm3 83LISSCH/J33mtrd X3'ElH pas .~a;r7s-.. sa,dlueS

.................................... E86T '81 JWOqX

................................ S6ESZ 'ON aI!j

87: - LT - 97: - ST - PT - €7: - ZT - TT - 07: - 6- 8- L- 9- s -en T -ma PZ - EZ - ZZ - TZ - oz - 67: - 87: - LT - 91 - sT - PT - ZT - TT - OT - 6- 8 4-W

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