Assessment Report Title Page and Summary

ASSESSMENT REPORT TITLE PAGE AND SUMMARY

TITLE OF REPORT: Orientation Property Inspection and Rock Geochemistry on the Veritas Property

TOTAL COST: $1,832.50

AUTHOR(S): CHRISTOPHER DELORME SIGNATURE(S):

NOTICE OF WORK PERMIT NUMBER(S)/DATE(S): STATEMENT OF WORK EVENT NUMBER(S)/DATE(S ):5397072

YEAR OF WORK:2011 PROPERTY NAME: VERITAS CLAIM NAME(S) (on which work was done):852925 (SIMONE), 852931 (SIMONE 2), 852932 (SIMONE 3)

COMMODITIES SOUGHT:GOLD

MINERAL INVENTORY MINFILE NUMBER(S),IF KNOWN:092JNE031

MINING DIVISION: LILLOOET NTS / BCGS:092J/15 LATITUDE: 50°50’26” LONGITUDE: 122°54’50” ______" (at centre of work) UTM Zone: 10 EASTING: 506063 NORTHING:5632098

OWNER(S): CHRISTOPHER DELORME

MAILING ADDRESS:PO BOX 1904 VOIGHT STREET, MERRITT, B.C. V1K1B3

OPERATOR(S) [who paid for the work]: CHRISTOPHER DELORME

MAILING ADDRESS: SAME AS ABOVE

REPORT KEYWORDS (lithology, age, stratigraphy, structure, alteration, mineralization, size and attitude. Do not use abbreviations or codes) BRALORNE INTRUSIONS, CADWALLADER GROUP – HURLEY FORMATION, CADWALLADER GROUP – PIONEER FORMATION, BRIDGE RIVER GROUP, SERPENTINE, DIORITE, ANDESITES, QUARTZ VEIN, GOLD

REFERENCES TO PREVIOUS ASSESSMENT WORK AND ASSESSMENT REPORT NUMBERS: 6971,14390,15209,18436

TYPE OF WORK IN EXTENT OF WORK ON WHICH CLAIMS PROJECT COSTS THIS REPORT (in metric units) APPORTIONED (incl. support)

GEOCHEMICAL (number of samples analysed for …)

Soil

Silt 4 ALONG 75 852925 1562.85 Rock METERS OF ADIT

Other

RELATED TECHNICAL 4 34 ELEMENT ICP + 96.00 Sampling / FIRE ASSAY GOLD Assaying

Petrographic

Mineralographic

Metallurgic 173.65 Other – TITLE SEARCH TOTAL COST $1832.50

ORIENTATION PROPERTY INSPECTION AND ROCK GEOCHEMISTRY ON THE VERITAS PROPERTY, LILLOOET MINING DIVISION

MINERAL TENURES #852925, 852931, 852932

122°54'50"W X 50°50'26"N

NTS MAP 092J/15

LILLOOET MINING DIVISION

OWNER: CHRISTOPHER DELORME, F.M.C. #141575

OPERATOR: CHRISTOPHER DELORME

AUTHOR: CHRISTOPHER DELORME

MERRITT, BRITISH COLUMBIA

OCTOBER 28, 2012

EVENT #5397072

TABLE OF CONTENTS INTRODUCTION ...... 5 TENURE INFORMATION ...... 6 LOCATION ...... 7 ACCESS...... 8 PHYSIOGRAPHY ...... 9 REGIONAL GEOLOGY ...... 9 PROPERTY GEOLOGY ...... 10 EXPLORATION HISTORY ...... 12 2011 EXPLORATION PROGRAM ...... 14 RECOMMENDATIONS ...... 15 REFERENCES ...... 16 STATEMENT OF COSTS ...... 17 STATEMENT OF QUALIFICATIONS ...... 18 APPENDIX ...... 19

INTRODUCTION

This report describes the results of a 2.5 man-day (inclusive of travel time) property visit to the VERITAS property, owned and operated by Christopher Delorme (the author).

The program described herein was conducted between August 10th and 13th, 2011, and work was completed on tenure #852925.

The work program consisted of inspecting the old workings on the Veritas claims, and collecting (and subsequently assaying) 4 “grab” rock samples from the so-called “Adit #2” on the Veritas occurrence. Approximately ½ a day was also spent visiting the Land Title Office in Kamloops, to confirm the reversion of certain crown grants on the property.

The work resulted in the location of certain underground workings, referred to in the historical literature (and herein) as Adits 1 through 4. These adits were developed in the 1930s to explore, on multiple levels, a quartz vein exposed at surface.

Rock geochemistry (gold assay) results were disappointing, with only sub-anomalous gold enrichment of between 5 and 30ppb Au from Adit 2.1 Sulfides were inferred from the high concentrations of sulfur (to 2.99%), iron (to >10%) and some anomalous copper (to 712ppm).

The four adits were inspected and G.P.S. logged for orientation purposes. This should aid in future data compilation and program planning. The mine workings identified in the literature were observed, and portal locations were logged by G.P.S.

1 The adit numbering practice was previously utilized by Gruenwald in A.R. 6971, and by Cooke and Robins in A.R. 15209.

TENURE INFORMATION

The VERITAS property consists of the following three mineral tenures. At the date of this report these tenures were owned and operated as to a 100% beneficial and registered interest by Christopher Delorme, and were not subject to any royalty, option or earn-in right, joint venture agreement or the like.2

Tenure # Tenure Name Area (ha) Good-to-date Owner (100%) 852925 Simone 81.63 May 1, 2013 Christopher Delorme 852931 Simone 2 61.22 May 1, 2013 Christopher Delorme 852932 Simone 3 224.50 May 1, 2013 Christopher Delorme

The good-to-dates shown above are pending acceptance of this report.

The property is partially underlain by three reverted crown grants, Lots 2355, 2356 and 2357 in the Lillooet Mining Division.

These appear to have been reverted to the Crown by 1961, and as a result, it is the understanding of the author that: (1) the reverted crown grants hold no further mineral interest, and (2) all mineral interests within the boundaries of the Veritas property are secured by the above mineral tenures. The work program described herein was largely conducted within the borders of the former reverted crown grants.

2 A mineral property option granted by the author on the VERITAS property had expired prior to the effective date of this report with no interest earned.

Due to the reversion of these former lots, no further consideration has been given to those reverted crown grants in this report. However, the reader is cautioned that should those titles in fact remain valid, then the work program described herein may be invalid for assessment report purposes and the mineral rights effectively conveyed by the current tenures would be significantly reduced and diminished. The particulars of the forfeiture of the Veritas reverted crown grants are not known. A legal title opinion was not obtained.

LOCATION

The VERITAS property is located 4 kilometers west-south-west of the community of Gold Bridge, B.C., in the Lillooet Mining Division. As its name suggests, Gold Bridge has been a center of gold mining in B.C. for over 100 years to the present day, given its location approximately 10km north of the famous Bralorne mining camp.

The Veritas property is centered on the small Lajoie Lake (also known as “Little Gun Lake”). The property is between Gun Lake on its northeast boundary and Downton Lake on its southwest boundary. Gun Lake, the smaller of the two, is a mountain lake used for recreation, and Downton Lake is a hydroelectric reservoir operated by B.C. Hydro.

The Veritas prospect (MINFILE record #092JNE031) is recorded at 505965E x 5632221N, elevation 1,000m above sea level, within the central portion of tenure #852925.

The Bridge River gold camp was the largest producer in Western Canada, with successful exploration and some production continuing to the present day. According to MINFILE, major producers in the district included:

Gold Average Tonnes Recovered grade Mine Minfile # Mined (grams) (g/t) BRALORNE 092JNE001 4,981,419 87,643,244 17.6 PIONEER 092JNE004 2,314,459 41,525,831 17.9 MINTO MINE 092JNE075 80,650 546,106 6.8 CORONATION 092JNE007 11,155 219,399 19.7 WAYSIDE 092JNE030 39,109 166,122 4.3 7,426,792 130,100,702 17.5

The exploration model at the Veritas property has historically been for quartz-vein hosted lode gold associated with the Bridge River intrusives within a volcanic and sedimentary sequence. This is the productive deposit type in the district.

Spotty gold enrichment has reportedly been encountered in the quartz veins exposed at surface and underground at the Veritas property, though ore has never developed from these quartz veins, nor were economically compelling interceptions obtained. However, the author acquired the property to facilitate exploration for vein extensions at depth and along strike, in the hopes that if extensions to the quartz vein are located, these shoots might prove gold-bearing. These efforts are encouraged, in part, by the observation in the B.C. Minister of Mines Annual Report from 1932 that: “the vein has been traced a couple of thousand feet on the surface by open-cutting and stripping. In places on the surface [the operator] finds high gold values, but the upper tunnel has not been advanced far enough to get under these points” (emphasis added).

ACCESS Access to the property is from the nearest community of Gold Bridge, B.C. From the Gold Bridge townsite, head 0.75km west on the Bralorne Road. Immediately upon crossing the Bridge River turn left at a junction and head southwest on the maintained gravel Gun Lake Rd. After travelling approximately 5.5km, you will enter on the Veritas property near its southeast corner. After an additional 0.9km, turning left (westerly) at a junction at 507058Ex5631992N takes one onto a network of secondary roads that provide good access throughout the property.

Access to Gold Bridge can be obtained from two highway networks:

(1) From the Trans-Canada Hwy at Lytton, proceed approximately 63km northwest via Hwy 12 to Lillooet. From Lillooet, travel another 104km to Gold Bridge, via the Moha Road, which in turn becomes the Bridge River Road and Carpenter Lake Road en route to Gold Bridge.

(2) From Hwy 99 at Pemberton, travel 22km northwest on the Pemberton Meadows Road. Turn right and proceed approximately 9km on the Lillooet Forest Service Road. Turn right on the Hurley River Forest Service Road and continue 46km to Gold Bridge, B.C.

Lillooet and Pemberton, and the Greater Vancouver and Kamloops areas (both located within 4 hours by road) have all services necessary for mineral exploration and development. Electrical power is available in Gold Bridge, and the local Bridge River Valley is an area with a long history of mining and exploration and development.

Access to certain portions of the property may be subject to surface right notification requirements, due to private surface holdings near Lajoie Lake within the claimblock.

PHYSIOGRAPHY The property is covered in pine and fir forest. It is in the rain-shadow of the Coast Mountains, and has a relatively semi-arid climate, though snow accumulations can be severe in winter.

The property elevation ranges from 840m on the southwest corner, above Downton Lake, to over 1,180m above sea level at the northwest corner. The terrain is fairly steep, being on the slope of Mt. Penrose of the Coast Mountain range, which rises to over 2,500m.

Vegetion is thinner, and outcrop more conspicuous, near the Veritas workings. Approximately 6 hectares of the property is covered by pasture on the north shore of Lajoie Lake.

REGIONAL GEOLOGY Information on Regional geology is from the B.C. Geological Survey bedrock maps available from MAPPLACE, and from historical Assessment Reports and public geoscience reports, as noted.

From MAPPLACE:

The oldest rocks in the area belong to the Mississippian to Middle Jurassic Bridge River complex, which is a northwest trending belt of marine sedimentary and volcanic rocks. Rocks of this unit belong to the Bridge River Terrane, which accreted to ancestral North America in the Jurassic.

Fault-bounded bands of Paleozoic to Permian-aged serpentine ultramafic rocks, Permian-aged diorites of the Bralorne Intrusions, Upper Triassic “Cadwallader Group/Hurley Formation” coarse clastic sedimentary rocks and Jurassic to Cretaceous aged “Cayoosh” group sedimentary rocks also outcrop in the map area, along the same northwesterly trend.

Intruding all units are Late Cretaceous granodioritic rocks of the Coast Plutonic Complex, and to the east of the Veritas property, Late Cretaceous to Tertiary intrusive rocks of the Bendor batholith. Economic mineralization in the camp is believed to be from the mid-Cretaceous, co-eval with the Bendor intrusions (Church, 1996), cutting primarily Permian to Mesozoic country rock.

Several major producers of the Bralorne camp (including the Bralorne, Pioneer and Wayside mines) appear to be spatially associated with north-trending thrust faults, and in certain instances later cross- faulting. Regional scale faults are important controls on mineralization in the camp.

Assessment Report 6971 summarizes the regional geology well, situating the regional geology:

“…on the eastern margin of the Coast Crystalline Belt marked in the area by a series of granitic plutons known as the Bendor Intrusions. These plutons have intruded the southwest margin of a large northwest trending antiform composed primarily of Mesozoic sediments, low grade metamorphic rocks, and minor volcanics. Also trending northwesterly through the area are

serpentinites and the augite diorite-soda granites (Bralorne Intrusions) that are in part host to the Bralorne-Pioneer Gold Mines” (Gruenwald, 1978; p. 14)

LKgd Late Cretaceous Unnamed granodioritic intrusive rocks Upper Triassic to Jurassic Noel Mountain East Succession uTrJNM mudstone, siltstone, shale fine clastic sedimentary rocks ?gb Age unknown gabbroic to dioritic intrusive rocks Jurassic to Cretaceous Cayoosh Assemblage JKCsf mudstone, siltstone, shale fine clastic sedimentary rocks Mississippian to Middle Jurassic Bridge River Complex MmJBsv marine sedimentary and volcanic rocks Upper Triassic Cadwallader Group - Hurley Formation uTrCHsc coarse clastic sedimentary rocks Permian Bralorne-East Liza copmlex PBEus serpentine ultramafic rocks Jurassic to Cretaceous Cayoosh Assemblage JKCsf undivided sedimentary rocks Late Cretaceous to Paleogene LKTgd Unnamed granodioritic intrusive rocks

PROPERTY GEOLOGY The property is centered on Paleozoic to Permian serpentine and Bralorne Intrusion group dioritic units. The Veritas quartz vein is located near the contact between these intrusive units. The serpentine rocks were variably classified by prior workers as belonging to either the President group or the Bralorne East- Liza ophiolitic complex.

Flanking these rocks to the south are the younger coarse clastic sedimentary rocks (including argillites and limestones) and, locally, volcanic rocks (andesitic) of the Hurley and Pioneer formations of the Triassic-aged Cadwallader Group.

To the north the marine sedimentary and volcanic rocks of the Mississippian to Jurassic Bridge River group are shown to flank the intrusive units.

In places on the property, the country rock apparently includes a “pale green, massive, fine grained andesitic volcanic rock” (Gruenwald), which Cooke and Robins appear to include in the Pioneer formation. Again, a good summary of the geology is provided by Assessment Report 6971:

“The geology of the Veritas property consists of a northwesterly trending band of diorite in close association with serpentinized ultrabasic rocks similar to those found in the Bralorne-Pioneer area. The main rock type surrounding the diorite and serpentinite is a pale green, massive fine grained andesitic volcanic rock. Subparalleling the diorite-serpentinte contact is a quartz vein(s) and/or shear zone that has been explored by at least four adits” (Gruenwald, 1978, p. 16).

In describing the vein system, a later worker (Assessment Report #18349) apparently describes this andesitic unit as a porphyrite greestone:

“The Veritas vein…appears to be related to a porphyrite flow (greenstone) with the mineralized veins of up to 1.2 meters (four feet) mineralized with erratic sulphide contact. The vein is revealed for 304 meters (1,000 feet) horizontally with a vertical height of 122 meters (400 feet) as indicated from old workings.” (Brewer, 1988, p. 5).

Numerous different workers appear to use different terminology in mapping the bedrock, and the Bridge River group unit does not directly relate to stratigraphy, as it appears to include a number of geological ages. (Church and Jones).

Perhaps the most concise description of the Veritas vein is provided by Cooke and Robins, and is quoted in its entirety from A.R. #15209:

The Veritas vein has been traced for 300 meters along strike and 80 meters down dip by several old trenches and four old adits. It is typically up to 1 metre wide consisting of white quartz and carrying minor disseminated pyrite, arsenopyrite, galena, tetrahedrite and gold.

Some of the best old gold assays were reported to come from surface samples beyond the underground workings. Certainly the best recent dump samples have come from the No. 3 and No. 4 dumps, at the western end of the known vein.

Underground mapping and sampling was conducted in the Veritas Nos. 2, 3 and 4 adits. The No. 1 adit was caved and inaccessible at the time of this report. These adits explore a Bralorne-type quartz vein which generally follows the contact between Bralorne diorite and the President Serpentinite. A feldspar porphyry dike trends parallel to this contact, commonly in the hanging wall to the vein.

The quartz vein ranges from a few centimeters to over a meter in width and is oriented approximately 115o, dipping steeply to the north. It is composed predominantly of a white milky quartz with sparse sulphide mineralization in the form of pyrite, arsenopyrite and galena. Tetrahedrite anda free gold have also been reported in the past. The altered hangingwall and footwall typically contain up to 3% disseminated sulphides, predominantly pyrite and arsenopyrite.

Carbonate alteration is also evident near the contact with the vein, where the ultrabasics (serpentinte-peridotite) are listwanitized and typically contain abundant fuchsite. In the Veritas #3 adit a narrow chloritized lamprophyre (?) dike crosscuts the vein and the feldspar porphyry (p. 9- 10).

EXPLORATION HISTORY The Veritas occurrence (located in present-day mineral tenure #852925) was originally crown granted in the 1930s.

According to the B.C. Geological Survey MINFILE database, four adits developed on the crown grants explored a number of quartz veins between a few centimeters and 1 meter in width. These quartz veins are reported to host sparsely disseminated sulfides, with gold reported in the footwall, associated with carbonate and ankerite alteration. West of the developed area, a secondary zone of serpentine-hosted stockworks of calcite, ankerite and quartz veins containing some chalcopyrite and arsenopyrite is reported.

The Assessment Reporting database describes the modern exploration history of the project in more recent decades:

Gruenwald, W. Geochemical and Geological Report on the Pike #1 - #8, Artomas #1 - #5 Claims, and the Ranch, Veritas, and Veritas #2 Claims (Lots #2355 – 2357). 1978. A.R. 6971.

Work described in this report consisted of rock chip sampling from Adit #2, and portal vein samples from Adits #3 and #4. No gold mineralization was returned from Adit #2 nor the portal vein exposed in Adit #3, though a single sample from the vein at the portal of Adit #4 returned a moderately interesting 485ppb gold (sample #3159).

The only significant results were from the dump of adit #3. A minor amount (<1%) of the dump material at Adit #3 contained massive sulfides; one grab sample of such material returned 5000 ppb Au and 36ppm Ag. The author considered following up on any such localized pods of sulfide-rich material in Adit 3 to be a low priority recommendation, though overall the program results discouraged additional work.

Sampson, Chris. Report on Preliminary Geochemical Soil Sampling, Veritas Claim Group. For Coral Energy Corp. 1986. A.R. 14390.

This report described two north – south orientation soil lines over the historical Veritas workings. A small soil anomaly (up to 75ppb Au, with proximate samples of 30ppb and 45ppb) was found across 100meters on Line 0 near Adit #4; no other multi-station gold-in-soil anomalies were noted.

Of significance, this report describes the identification of two well mineralized samples from the Adit #2 area, as follows:

Adit #2 vein sample (grab?): 0.202 oz/ton gold

Adit #2 dump (float): 0.147 oz/ton gold

No citation was provided for the source of these results.

Cooke, Bradford and Robins, John. Assessment Report on the Veritas Property Near Goldbridge, B.C. For Coral Energy Corp. 1986. A.R.15209.

This report describes the results of underground mapping sampling of the #2, #3 and #4 adits, and soil geochemistry, expanding on the orientation soil work described in the earlier Sampson report A.R. 14390.

Based on their underground mapping, the authors described the quartz vein at the Veritas occurrence as located between a Bralorne diorite and a serpentine unit.

The only significant rock geochemical results were obtained from the vein exposed at the portal of the Adit #4 – with three 30cm chip samples returning between 0.032 oz/ton and 0.075 oz/ton (between approximately 1.1 and 2.6 grams per tonne). However, the other 27 rock samples assayed significantly lower, ranging to a maximum of 390ppb Au.

The authors felt that the 1986 soil results provided some encouragement that the vein had exploration potential at depth or along strike. From A.R. 15209:

“A number of B horizon soil anomalies were located strike from the Veritas vein, running up to 350ppb Au, 188ppm As, 1.3ppm Ag and 23ppm Sb and extending the strike potential of the known vein for another 800 meters west-northwest. Several other spot anomalies were also detected” (p. 2).

Gold responses were spotty, however; of the 364 samples for which analytical data was provided, only 6 (<2%) were 30ppb or greater.

Brewer, Lloyd. Geophysical report on Airborne Magnetic and VLF-EM Surveys over the Ernie, Burt & Veritas Mineral Claims. For Coral Gold Resources Ltd. 1988. A.R. 18436.

Brewer’s 1988 report describes airborne geophysical (magnetic and VLF-EM) surveying performed over the Veritas claim.

This work led to the recognition of several geophysical anomalies in and around the present-day Veritas property, including a 1,500m x 100 conductive anomaly noted in the VLF-EM survey which was deemed to be of particular interest as to runs near the Veritas workings, and a 700m northeast striking conductor which appears to crosscut the local stratigraphy.

The magnetic survey mapped the serpentine units well, particularly where they contrasted with Cadwallader group sediments.

2011 EXPLORATION PROGRAM The 2011 exploration program consisted of the following:

. Locating the workings and assessing vehicle access. . Grab sampling portal veins and dumps selectively, based on visual prospectivity. . Obtaining GPS survey control over old workings, utilizing a Garmin GPS.

In respect of those objectives, the following results were obtained.

. Good vehicle access was found to the working areas along existing gravel resource roads. . Adits 1 through 4 were located. o 4 rock samples were obtained from Adit 2, which was approximately 95 meters deep, with 2 crosscuts and a stope. The crosscuts were approximately 5m wide. A stope was noted in Adit 2. o Adit 3 was also examined; this appeared also to be approximately 75 meters long with several crosscuts and a stope. o Adit 1 was visited, but as had been noted by prior operators was inaccessible due to rock-fall. o Adit 2 was sampled, as follows.

Result Sample Source Note (ppb Au) 11S121001 Adit 2 5 meters in 10 11S121002 Adit 2 30 meters into adit 5 11S121003 Adit 2 60 meters into adit 20 11S1210044 Adit 2 75 meters into adit, 30 from crosscut

There was significant iron and sulfur content in certain samples (Samples 11S121002 through 11S121004 had iron between 4.88 and >10%, with accompanying sulfur concentrations of 0.26 to 2.99%). There was also some copper concentration, with the same three samples ranging between 350 and 712ppm.

. Adit locations were as follows:

Adit Portal location (UTM Zone 10) Elevation 1 506113E 5631982N 907m 2 506073E 5632085N 948m 3 506040E 5632125N 977m 4 505970E 5632196N 1013m

Other work

During the course of the mobilization, the author stopped at the Land Titles Office in Kamloops and confirmed that the former crown grants located on the Veritas property had been reverted. Approximately 0.25 days were incurred in completing this.

Analytical

In the field, grab samples were taken by rock hammer and placed in a poly bag. Each sample was approximately fist-sized.

The samples were submitted to EcoTech Laboratory Ltd. in Kamloops British Columbia for gold and 34 element ICP with aqua regia digestion. Analysis was by fire assay with atomic absorption finish.

RECOMMENDATIONS Visiting the property and local area provided a good orientation which can assist in planning future programs. GPS control on adit locations will assist in compiling historical data and building a dataset. With that information in hand, effort should be made to fully compile and integrate all historical results, and consider past exploration efforts, methods and insights in light of recent exploration success reported in the camp, namely at the Bralorne mine approximately 10km southwest.

However, failure to identify anomalous gold enrichment from the known Adit #2, together with prior operators’ middling results from the workings, suggests that future exploration efforts should “step out” from the underground development. A good start would be extending the Cooke and Robins grid (A.R. 15209) north, as their best soil results (deemed indicative of possible “strike extent” potential) were obtained on their northernmost line, the Baseline 0N line.

REFERENCES Ash, Chris.. Bulletin 108: Chapter 4 – Bridge River Terrane, Bralorne-Pioneer Camp. British Columbia Geological Survey. Retrieved from: http://www.empr.gov.bc.ca/Mining/Geoscience/PublicationsCatalogue/BulletinInformation/Bulletin sAfter1940/Documents/Bull108_4.pdf

British Columbia Minister of Mines. Annual Report of the Minister of Mines of the Province of British Columbia for the Year Ended December 31, 1932.

British Columbia Minister of Mines. Annual Report of the Minister of Mines of the Province of British Columbia for the Year Ended December 31, 1933.

Brewer, Lloyd. Geophysical report on Airborne Magnetic and VLF-EM Surveys over the Ernie, Burt & Veritas Mineral Claims. For Coral Gold Resources Ltd. 1988. A.R. 18436.

Church, B.N. Bridge River Mining Camp: Geology and Mineral Deposits. 1996.

Church, B.N. and Maclean, M. Open File 1987-11:Geology of the Gold Bridge Area. Ministry of Energy, Mines and Petroleum Resources. 1987.

Church, B.N., Maclean, M., Gaba, R.G., Hanna, M.J., and D.A. James. Open File Map 1988-03: Geology of the Bralorne Map Area. B.C. Ministry of Energy, Mines and Petroleum Resources. 1988.

Cooke, Bradford and Robins, John. Assessment Report on the Veritas Property Near Goldbridge, B.C. For Coral Energy Corp. 1986. A.R.15209.

Gruenwald, W. Geochemical and Geological Report on the Pike #1 - #8, Artomas #1 - #5 Claims, and the Ranch, Veritas, and Veritas #2 Claims (Lots #2355 – 2357). 1978. A.R. 6971.3

MINFILE 092JNE031 “Veritas”. Retrieved from B.C. MINFILE Database Online.

Sampson, Chris. Report on Preliminary Geochemical Soil Sampling, Veritas Claim Group. For Coral Energy Corp. 1986. A.R. 14390.

3Please note that the rock samples taken underground from Adit #2 were mapped in the attached appendix using the base map from A.R. 6971 (the “Cook” map) and all attribution for the base map remains with that report. The 2011 work did not enhance the quality of the mapping utilized in that report. It was only modified to show the 2011 sample locations, in red.

STATEMENT OF COSTS Exploration Work Comment Days Totals type

Personnel (Name)* / Field Days Days Rate Subtotal* Position (list actual days) Christopher August 10- 2.5 $225.00 $562.50 $562.50 Delorme, Owner 13, 2012 Office Studies List Personnel Report preparation Christopher 3.25 $240.00 $780.00 Delorme Literature search Christopher 0.5 $200.00 $100.00 Delorme $880.00 Transportation No. Rate Subtotal Fuel and mileage Merritt to 730km $0.30 $219.00 $219.00 Veritas, via Kamloops Meals and No. Rate Subtotal accommodation Meals (day rate) 2.5 $30.00 $75.00 $75.00 Assay No. Rate Subtotal Gold assay 4 $24.00 $96.00 $96.00

TOTAL $1,832.50 Expenditures

STATEMENT OF QUALIFICATIONS

I, Christopher Delorme of Merritt, British Columbia, here by certify that:

1. I have been active as a prospector, diamond driller and mineral exploration worker in British Columbia for over 10 years.

2. I did visit the property on the days stated and conduct the work described herein.

“CHRISTOPHER DELORME”

Christopher Delorme

October 28, 2012

APPENDIX

LOCATION MAP

ADIT #2 MAP