^^k HU^'dT^lo

Soil Geochemistry < hi For Roundtop Mountain Exploration Inc. «* Q*

Tenures: 412065, & 412066

Cariboo Mining District

NTS 93A094

July 10th & September 14th 2008 Bryan T Muloin BSc, BEd Geologist Box 1312 Fort St James British Columbia V0J1P0 Telephone 250 996 2253

E C E f V E SERVICE BC

SMITHERS

FEB2 3 NOT AN OFFICIAL RECEIPT

TRANS #

Table of Contents

Table of Contents Introduction Location and Access History Regional Geology Geochemistry Conclusions and Recommendations Survey Costs Statement of Qualifications References

Roundtop Mountain Location Map Roundtop Mountain Claim Map

Appendix: Assayers Canada Invoice Assayers Canada Analysis Certificates

Geochemical Plots: Gold in ppb Silver in ppm

VLF EM traverse location & cross over description map Soil sample UTM coordinates

Page 1

Introduction This study is a continuation of last year's surveys on this claim group.

Several VLF conductive features were found last year. To evaluate the most promising of these conductors a soil sampling traverse along the previously identified, JK, structure was conducted. Nineteen samples were excavated along this conductor.

The notion of an orientation survey to evaluate appropriate sample spacing and evaluate other factors is this primary endeavor.

Location and Access The JS 7 and JS 8 claim blocks are situated in the Cariboo Gold

Fields of British Columbia. They straddle the upper reaches of Lostway Creek. Roundtop Mountain, elevation 2061 meters, dominates the claims near their west boundary. Middle Mountain and its north trending ridge bind the west side of the claims. NTS 93A094; centers on: 121°18'W, 52°25'N; with UTM boundaries near 612600E to 612100E, and 5863000N to 5866500N.

Access from Wells is Highway 26 for 7 kilometers to the 3100 Logging road. At the Bowron Lakes, 3100 road junction proceed southeast for 15 kilometers to the X road. The X road turns east after 4 kilometers, the N road or Yanks Peak road continues on the west side of Cunningham Creek. At Penny creek access is by ATV or by foot along trails east.

Page 2

Roundtop Mountain Exploration Inc. Location Map

i » Roundtop Mountain Exploration Inc. Location Topographic Layers

□ Lakes 1:6M

Rivers 1:6M BC Border Layers

IK?! BC Border 1:6M

0 v /

SCALE 1 : 10,424,460

H M M'

Roundtop Mountain Exp

100 100 MILES

200 300 A

>

. . ■■■ '■'..'/ ' i..H.;.."'.:i, ': ~ .

f ort Jpgjohn ~ ^?V^»-~ -■- -Terrace,. ~--.-,\:.

- - >■ . ,

Wibiams Lake ,M<^§toKe ■

VatTcfew^-^raH^; Vicfbria

This map is a user generated static output from an Internet mapping site and is for general reference only. Data layers that appear on this map may or may not be accurate, current, or otherwise reliable. THIS MAP IS NOT TO BE USED FOR NAVIGATION.

History The mining history of Cunningham Creek started in 1860 with the initial

exploration of the Cariboo. Its recorded history is partially available from the annual reports to the Minister of Mines. The story starts in 1876 and 1877 with the Victoria Company doing shafts to access the deep ground. This history including to Amos Bowman's study of quartz exposures which as is explained in Geology interests the author:

" 1876 Report to the Minister of Mines page 418

"The Victoria Co., on Cunningham Creek, have erected costly machinery and employed twenty men, for the exploring of the deep ground, which had been previously attempted by other companies, but without success. They have pumped the water out of the old shaft and will proceed to sink without delay."

" 1877 Report to the Minister of Mines page 394

"I regret to say the Victoria Co., of Cunningham Creek, whose exertions have been watched with much interest the past year, have, after expending some $35,000, taken their pumps out of the shaft and abandoned the ground, having thoroughly tested the channel, but without finding ground to pay."

The industrious Chinese were also active on Cunningham Creek as the report of 1879 attests.

"1879 Report to the Minister of Mines page 237

"Cunningham Creek exceeds it's last years returns. Gold is, however taken out principally by the Chinese, which is, therefore of little benefit to the community."

Pearce Gulch draining into Cunningham Creek appears to be first explored in 1882 a full twenty years after the initial mining work.

Page 5

History continued " 1882 Report to the Minister of Mines page 355

"Messrs. Pearce and Bennett, the fourth party assisted in their outfit by the Government, found paying diggings on a tributary of Cunningham Creek. This discovery tends to confirm the opinion that Cariboo has, so far, been only partially prospected, for Cunningham Creek has been well-known for more than twenty years."

Page 357

"Messrs. S. Pearce and W. Bennett, who also received assistance in their outfit from the exploration fund, discovered a small gulch putting into Cunningham Creek, which will pay fair wages. The discoverers have built themselves a cabin, and will work there the coming season. Two companies have recorded ground on the stream, which has been named Pearce's Gulch."

The partners Pearce and Bennett were dedicated miners as their subsequent activities indicate: Granite Creek Tulameen, 1885, Samuel Pearce has moved on from the Cariboo:

" On Sunday morning, the 1st instant, the Point Company, situated about two miles above Capt. Sherburne's ground, washed up 45 ounces, or over $750, as the result of the labour of eight men for thirty hours. This claim is owned by Messers. Pearce and Harvey, the former of whom is one of the pioneers of Cariboo, and well known throughout that district."

William Bennett appears to have gone to the West Kootenay's as a Crown Granted claim "Mountain Con #9841 was granted 22 June 1910.

In 1911 the "Mountain Con" at Sandon shipped ore bearing gold, silver, lead! With partners he also acquires the Crown Grant "Winslow #8680 " dated 24 August.

1915 Report to the Minister of Mines 121

The Mountain Con is a property very high up the mountain, and, on account of lack of transportation and snow, can only work about four months in the year. It is worked under lease to Wm. Bennett, of Sandon; in the short time he worked with a small crew last summer he took out about $30,000 worth of ore of very high grade.

L

History continued The Chinese remain on Cunningham Creek and as usual are the recipients of

official disdain. The European experts underplay their mining activity as of little importance as the report of 1886 indicates.

1886 Report to the Minister of Mines 196

"On Cunningham Creek the ubiquitous Chinese made a fortunate strike during the summer in the hill, and a company of four men have been taking cut from twenty to fifty dollars per day to the hand. "Investigation, however, goes to show that the discovery is not of importance, their location being on a point across which the old bed of the creek passed at a much higher level than the present bed of the stream."

In 1886 Amos Bowman visits the Cunningham Creek area and is not impressed with the quartz seen along Roundtop to Middle Mountain ridge. He of course has not had experience with the core drilling or geophysical or geochemical study of porphyry mineralization.

1886 Report to the Minister of Mines 229

"Round Top Mountain and Cunningham Creek" Excerpted from Amos Bowman as to the Quartz Question, numbers refer to outcrops visited and samples taken

"No. 96.~On Round Top Mountain, comb of quartz or quartzite at transit station. Evidently too massive to be anything else than barren. The summit itself is mostly quartz or quartzite, which rises into peaks and strikes with the rest of the country rock ; strike N. 80° W., dip northward 40°. "No. 97.—Big ledge or comb of quartz, or quartzite, on the eastern member of Round Top Mountain one mile S.E. of last. Oxides of iron in small quantity with very little pyrites. Strike more to the S. E. than on the main summit transit station; dip also northerly, but steeper. Country rock, slate. " This comb runs from one-quarter to three-quarters of a mile E. S. E. from our Round Top camp, striking over the summit of the eastern mountain. Slides from it on the north side form parallel bands of quartz, or quartzite, show oxides of iron in sufficient quantity to colour the side hill of the northern escarpment red ; visible at a mile's distance.

Page 7

History continued "No 28.-Cunningham Creek, near the head of Sharp's Ditch, (Alexander Sharp) two miles west of Round Top, and 100 feet above ditch. Iron pyrites nearly pure. Assay in hand. " No. 29.- Same locality ; ore more or less decomposed, with quartz; course, N. W. And S. E. with the rock; dip northerly less than 48°. In quantity there is considerable, but the continuousness of the ore body has not been proved. "On Cunningham Creek a quartz vein crosses the creek just below the trail, crossing between Sharp's and the Harvey Creek summit. This was not seen by me. "No. 21.- Sharp's Diggings, Cunningham Creek. In bed of creek iron 'rock,' with quartz and feldspar ; assay not completed. It is called the 'Big Iron ledge,' and is in iron stained dyke containing pyrites. "No. 22.-Chinaman's diggings, on hill-side, west side of Creek, half a mile below Sharp's on Cunningham Creek. Decomposed pyrites; hornstone with iron oxide cement. "Great numbers of quartz boulders like specimen are found scattered, indicating proximity to a ledge of good character, both as to quality and quantity. The diggings in 1886 yielded well. It is a side-hill gravel deposit of local origin.

Bowman attests to the significance of the quartz. Of historic interest is the reference to Sharp's ditch which must be either of the ground flumes still evident. The era of its digging probably predates 1874, the beginning of Mines Annual reports. Sharp was an active Mining Engineer on into the 1930's.

The Cariboo Hudson Mine on Peters Gulch had its start in 1922. It operated as a 50 ton per day mine employing 50 persons in the late 1930's.

Tungsten mining was reported from both the Cariboo Hudson and Coniagas Mines in the era between 1930 and 1950.

Coast Interior Ventures Ltd. explored for base metals between 1971 and 1974 identifying 11 geochemical anomalies. They did an IP survey and 1000 meters of diamond drilling.

Kerr Addison between 1973 and 1976 did soil sampling with the intention of identifying a large tonnage gold deposit.

Rio Canex, between 1976 and 1978 had a 20 man camp on Penny Creek. In 1978 a 60 meter adit was run just off Penny Creek by Wallace Chaput,

previous president of Coast Interior Ventures.

Page 8

Regional Geology The peaks of Roundtop and Middle Mountains show a flood of quartz rock.

Bowman's cockscombe elegantly expresses this quartz exposure. Where such quartz flooding has been seen on other ventures it has shown felsic subtle hues of green and mauves and blues. These extensive exposures are gray cryptocrystalline quartz with veins of white bull quartz cutting in a northwest trend characterizes both mountains. These are not included in the mythic sediment package. They are silica flooding seen with porphyry type intrusives.

In the Lightning Creek to Wells area the quartz expresses as alteration bosses or noses, subdued examples of Bowman's cockscombe. The fine grained nature is often amygdular with a hyaline cast or very pauchy opalescence. There is an occurrence at the Dominion Claims, Crown Granted claims, on Anderson near Stanley.

Just east of the adit, an extent of 70 meters is composed of quartz amygdules that increase in diameter toward the center of these outcropings. These coarser spheres have calcite associated. This is an alteration petrology and texture. Across Lightning Creek and up the left branch of Jawbone Creek another similar silica zone expresses itself as a silica nose.

Quartz alteration. Flooding on Roundtop and Middle mountains, patterns as parallel orientation and regular spaced with the four conductive vein structures identified in the previous VLF-EM studies.

They parallel the quartz flooding of the mountain peaks expressing radial tension release generated by a deep intrusive. The lowest of these structures passes through the author's Coniagas claim, record number 369928. It covers the Coniagas adit on which the author has done detailed magnetometer and VLF EM surveys. Here a characteristic tension release pattern is identified as one of these parallel conductors. Where the author has seen this pattern on other prospects it has been labeled a shatter envelope expressing its patterned and enclosing nature. There are four basic components to the envelope:

• Longitudinal radiating tension fractures; which both the JK structure and the Coniagas structure represent at their scale, part of a progression that includes the two other VLF conductors between.

• Transverse tension fractures; as seen at the Coniagas and including the Lostway and C road structure.

• Oblique shears; of which the Coniagas adit follows. • Stress focus pipes, at the junction of fractures and shears . They represent as

weak magnetic, inductive, and conductive anomalies. At the Coniagas they are expressed as ferro magnetic anomalies on strike, and as the two excavated shafts: at the portal, and ten meters in.

<?.

Geochemistry This initial geochemical traverse of 19 samples should be considered as an

orientation study. It addresses the question what can you learn from a minimal sample regime of only 19 samples. It is also different than an orientation survey in that it examines an identified conductive structure, identified as the JK conductor.

Soil samples were taken with a small D handled spade. As Kraft paper sample bags were not available plastic lunch bags were used, They are markable but because they do not dry well, they require further sample handling. Drying.

Assayers Canada were requested to carry out a high accuracy gold and multi element ICP analysis. No standards or blanks were included in the 19 samples.

Analysis was by mixed acid digestion. Gold analysis was on a 30gram sample was fire geochem with AA/ICP finish as outlined in their schedule.

Gold assays give an exciting response. Two samples only give a response of interest at 18 and 36 parts per billion. They are at the end of the traverse pointing to the northwest as the direction to do further exploration.

Conclusions and Recommendations The geochemical assaying was excellent for discovering which way to

explore along the JK structure. Further discoveries are anticipated with exploration in this direction.

Page 10

Survey Costs This assessment project was contracted on a share participation agreement.

No monies were exchanged. Bryan Muloin, BSc, BEd., Geological Superviser: 2 travel days FS James to Wells area return $1200

10 July geochemical sample survey supervision 600 2 days report writing 1200

Other participants, 10th July, sampling traverse, each: Gilbert Muloin, experienced sampler 300 Joy Stepan, project manager 300 George Froese, prospector 250

Participants, 14th September, second sampling day: Joy Stepan, project manager 300 Sherrill Madore, prospector 250 Bill Beaulieu, ATV driver 200 Debbie Beaulieu, ATV driver 200 Soil sample management including drying 650 ATV's, 2o fa t$60each 120 Vehicle usage, 6 days at $50 300

Field Accommodation, 6 people at $120 720 Assays 456.86

Total work effort $7046.86

Statement of Qualifications I, Bryan Thomas Muloin, am a Graduate of Queen's University, Kingston,

Ontario where I received Bachelors Degrees from both: the Faculty of Applied Science in the Geological Sciences in 1971, and the Faculty of Education as a high school teacher of science and mathematics in 1972. Since then I have been actively employed in the mining industry. Recent employment has been at: Eagle Peak Resources Miocene and Big Onion properties; Terrane Resources Mt. Milligan; BCM Resources Shan prospect; and Alpha Gold's Silver Creek, Bralorne prospect near Takla. - /

'X /HJ Bryan Muloin

Page 11

References: In addition to the "Minister of Mines Annual Reports" Campbell, RB. 1978 GSC Open File 574 Campbell, RB, Mountjoy, EW, and Young, FG. 1973 Geology of McBride Map Area British Columbia GSC Paper 72-35 Campbell, KV, and Campbell, RB. 1970 Quesnel Lake Map Area British Columbia (93 A) in Report of Activities GSC paper 70-1 (A) pages 38-41 Holland, SS. 1954 Geology of the Yanks Peak Roundtop Mountain Area, Cariboo District,British Columbia, BC Dept of Mines Bulletin 34 Mansy, JL, and Campbell, RB. 1970 Stratigraphy and Structure of the Black Stuart Synclinorium Quesnel Lake Map Area, British Columbia (93A) GSC Paper 70-1 (A) pages 38-41 Mitchell, JA. 1973 Summary Report on work completed on properties of Coast Interior Ventures Ltd. Rio Canex Report Barkerville Project 1978 Volumes 1 and 2 Muloin, BT. 1987 Cunningham Creek Claims Chaput Logging Ltd Assessment Report 17115 Sutherland Brown, A. 1957 Geology of the Antler Creek Area Cariboo District British Columbia, BC Dept of Mines Bulletin 38 Sutherland Brown, A. 1963 Geology of the Cariboo River Area British Columbia BC Dept of Mines Bulletin 47

Page 12

A D

Geochemical Analysis Certificate Company: Roundtop Exploration Inc Project: Attn: Joy Stepan

We hereby certify the following geochemical analysis of 19 soils samples submitted Nov-03-08

Sample Au Name ppb #1 36 #2 18 #3 2 #4 <1 #5 3 #6(or#15) <1 #7 2 #8 3 #9 <1 #10 3 #11 <1 #12 2 #13 5 #14 3 #15(or #6) <1 #16 3 #17 <1 #18 <1 #19 2 *0211 2151 *BLANK <1

Certified by

Roundtop Exploration Inc Attention: Joy Stepan Project: Sample type: Soils

Assayers Canada 8282 Sherbrooke St., Vancouver, B.C., V5X 4R6

Tel: (604) 327-3436 Fax: (604) 327-3423

Multi-Element ICP-AES Analysis Aqua Regia Digestion

Report No Date

8V3837SJ Nov-12-03

Sample Number

#i #2 #3 #4 #5

#6(or#15) #7 #8 #9 #10

#11 #12 #13 #14 #15(or #6)

#16 #17 #18 #19

Ag Al As Ba Be Bi Ca Cd Co Cr Cu Fe Hg K La Mg Mn Mo Na Ni P Pb S Sb Sc Sr Th Ti Tl U V W Zn Zr ppm % ppm ppm ppm ppm % ppm ppm ppm ppm % ppm % ppm % ppm ppm % ppm ppm ppm % ppm ppm ppm ppm % ppm ppm ppm ppm ppm ppm

0.7 1.06 18 113 <0.5 <5 0.60 1 13 89 29 2.92 <1 0.07 16 0.34 601 <2 0.01 34 2620 41 0.08 <5 1 31 <5 0.01 <10 <10 37 <10 131 5 0.6 1.02 21 126 <0.5 <5 0.84 2 15 86 34 3.14 <1 0.07 15 0.32 798 <2 0.01 38 3115 37 0.12 <5 2 44 <5 0.01 <10 <10 36 <10 119 7 0.3 1.05 24 109 <0.5 <5 0.48 2 21 61 44 4.20 <1 0.06 20 0.34 668 2 0.01 49 2186 43 0.06 <5 2 28 5 0.01 <10 <10 31 <10 134 8 0.4 1.15 14 104 <0.5 <5 0.66 1 13 89 22 3.13 <1 0.06 17 0.45 523 <2 0.01 36 2794 26 0.10 <5 2 34 <5 0.01 <10 <10 36 <10 108 5 0.5 1.01 43 101 <0.5 <5 0.46 2 22 95 33 3.70 <1 0.06 19 0.32 689 <2 0.01 47 1946 28 0.06 <5 2 26 6 0.01 <10 <10 36 <10 131 9

0.2 1.05 16 106 <0.5 <5 0.28 1 18 55 21 3.30 <1 0.07 19 0.48 802 <2 0.01 40 2384 48 0.06 <5 <1 22 <5 0.01 <10 <10 37 <10 94 2 0.6 1.26 20 120 <0.5 <5 0.72 2 17 51 24 3.36 <1 0.08 15 0.38 798 2 0.01 32 4566 34 0.13 <5 1 42 <5 0.01 <10 <10 39 <10 105 5 0.7 1.01 32 108 <0.5 <5 1.03 2 18 97 26 2.87 <1 0.08 11 0.36 682 2 0.01 35 3588 33 0.15 <5 2 51 <5 0.02 <10 <10 40 <10 109 6 0.2 0.83 16 71 <0.5 <5 0.18 1 19 28 23 3.83 <1 0.05 20 0.21 902 2 0.01 29 1577 32 0.04 <5 <1 12 <5 <0.01 <10 <10 22 <10 100 2 0.2 1.02 20 85 <0.5 <5 0.25 1 24 37 21 3.68 <1 0.07 19 0.29 1446 <2 0.01 30 2134 31 0.05 <5 <1 16 <5 0.01 <10 <10 31 <10 107 2

0.3 1.33 14 145 <0.5 <5 0.35 1 20 44 19 3.72 <1 0.08 18 0.39 1498 <2 0.01 33 3514 29 0.08 <5 1 21 <5 0.01 <10 <10 40 <10 150 3 0.3 1.47 11 73 <0.5 <5 0.30 1 15 39 26 3.78 <1 0.06 27 0.40 591 <2 0.01 35 2380 42 0.05 <5 1 18 <5 0.02 <10 <10 29 <10 129 4 0.5 1.24 14 83 <0.5 <5 0.43 1 18 39 47 3.46 <1 0.06 30 0.36 875 <2 0.01 35 2638 46 0.07 <5 1 28 <5 0.01 <10 <10 27 <10 111 4 0.6 1.03 12 85 <0.5 <5 0.58 1 16 25 25 3.57 <1 0.06 22 0.29 538 <2 0.01 36 3964 27 0.10 <5 2 43 <5 0.01 <10 <10 20 <10 113 7 0.3 0.98 24 84 <0.5 <5 0.51 2 23 23 28 4.50 <1 0.06 15 0.29 861 4 0.01 42 3510 60 0.09 <5 2 38 <5 0.01 <10 <10 21 <10 175 8

0.6 1.07 13 77 <0.5 <5 0.64 1 15 23 36 4.05 <1 0.06 14 0.27 488 <2 0.01 43 4065 29 0.12 <5 2 48 <5 0.01 <10 <10 18 <10 160 10 0.5 0.95 7 89 <0.5 <5 0.47 1 19 23 38 4.10 <1 0.05 15 0.26 660 2 0.01 45 3397 36 0.10 <5 2 35 <5 0.01 <10 <10 18 <10 176 9 0.2 0.80 15 73 <0.5 <5 0.19 2 33 20 92 4.73 <1 0.03 20 0.26 645 4 <0.01 73 921 41 0.02 <5 2 14 5 0.01 <10 <10 16 <10 345 5 0.3 0.65 9 87 <0.5 <5 0.16 1 24 20 30 3.99 <1 0.06 14 0.18 1397 3 0.01 33 2147 29 0.07 <5 <1 9 <5 <0.01 <10 <10 25 <10 129 2

A .5 gm sample is digested with 5 ml 3:1 HCI/HN03 at 95°C for 2 hours and diluted to 25ml.

Page 1 of 1 Signed:

ASSAYERS C A N A D A

Assayers Canada 8282 Sherbrooke Street Vancouver, B.C. V5X4R6 Canada Tel: 604.327-3436 Fax: 604.327-3423

Invoice Date Invoice #

15/11/2008 76952

Invoice To

Roundtop Exploration Inc. P.O. Box 107 Wells, BC V0K 2R0 Attn: Joy Stepan

P.O. No. Project Terms Due Date File

15/11/2008 8v-3837

Description Qty Rate Amount Tax

SAMPLE PREP: Soil FIRE GEOCHEM: Au 30g ICP: Aqua Regia Digestion GST On Sales

19 19 19

1.90 13.00 8.00

5.00%

36.10T 247.00T 152.00T 21.76

G G G

Subtotal $43510

9osr 9^7 /=> C'U/J^ ' * " ■ « S a l e s Tax Total $2176

OfJcX « /oo, c zs T o t a l $456.86

GST/HST No. 8900136^ f folyd /]sC . &Q Payments/Credits $o.oo

E-mail Web Site Payments/Credits $o.oo

E-mail Web Site

info@assayers.com www.assayers.com E balance Dm Q $456. 86

864500 864500

Soil Geochenical T r a v e r s e Round-top Mountain Claims

Gold assays, in pplo's

dr V %o

N *° . 0

Scalei as Identified by UTM grid coordinates

864000 864000

864500

Soil Geochenical T r a v e r s e Roundtop Mountain Clains

Silver, Ag, in ppn

4&L m^: 4& <&

•^ x^

0 » O c? • £'■ ° ^ 4°^ *o ^

_+_ 864000

864500

N Scalei as identified by UTM grid coordinates

864000

Round-top Mtn

-865000N Like Middle Mtn the Quartz ridge Is alteration quartz T865000N

-864000N

10#E-

10*E-jW—io*w 10*E-■X( —1 ( r w

r \ ^ - i ( T V , FS 1507 10*E-^A /^Jv-iO*V

FS 130%, 37 I, 10*E—y/v^/ i

FS 1307., 57. lyWEr^ \ yiihftV., 15*E~

W , F \ 1057., 37 I AP* clif\ FS 1357, 87 inag.

\ p&'V, FS 1307 V y > \>HL4*W, FS 957 ^S_>^3r40*V

/ / F S 13p^20*E~ y ^ i \ / \ dip 1257 /^•E-7\A-Vi0*V

\ /^W VLF (inoj/^^^^ y 30 dip, FS ^^J1/^ / /

DOtf, 10'E-7 y / W E - /

Scale 500m

864000N

VLF anon 30 dip, FS

Midas Fm copper nin. in t rench

-863000N

' (cross onto conductor f ron 12degree/ dip has 1107 field s t reng th , looks like hojtspring outwash)

rf,

10*E FS 1307 inag 207

LEGEND

Transmitter used wasi Seattle, Wash. FS refers to field strength, I or Imag refers to the Imaginary component, dip angle Is in degrees with direction as east E or west '

Middle Mtn

<w

<this quartz i te the backbone of this ridge is not a sedinent It Is al terat ion quartz typical of porphyry intrusives)

!uartz reef

,.863000N

Roundtop Exploration Inc. Soil Samples

2008

51 10 0613042 5864286

52 10 0613046 5864282

53 10 0613049 5864278

54 10 0613051 5864274

55 10 0613062 5864262

56 10 0613076 5864248

57 10 0613086 5864231

58 10 0613094 5864218

59 10 0613118 5864188

510 10 0613134 5864175

511 10 0613147 5864163

512 10 0613161 5864157

513 10 0613176 5864145

514 10 0613188 5864131

515 10 0613199 5864115

516 10 0613210 5864099

517 10 0613223 5864083

518 10 0613235 5864067

519 10 0613246 5864053

MIO Online Report Page 1 of 1

ISapFIace.ca Mineral Titles Online Report Click on Tenure Numbers for more information.

Click column headings to sort results. 0 ownload to Excel

Tenure Hur isbsr ! \ £*? O o u r : Nj?'j>0 Good Until Mli;S ! ha) 412065 Mineral JS7 20100320 500 412066 Mineral JS8 20100320 3751

LIBC Metadata

Mineral Title Online

Total Area: 875 ha

EC Geological Survey British Columbia Ministry of Energy, Mines and Petroleum Resources

Last updated in April 2007

http:/7 webmap.eni.gov .bcxa/mapplaee/minpot/mto. asp : 1/2010