Exhibit 99.2
REPORT
On the
Tulameen Mountain Project
New Westminster, Similkameen Mining Division, B.C., Canada
NTS Map 092H06E
Latitude 49(Degree) 25' 19" North
Longitude 121(Degree) 08' 10" West
For
Treasure Explorations Inc.
Suite No. 400, 114 West Magnolia Street
Bellingham, Washington
U.S.A.
98225
by
Alex Burton P.Eng., P.Geo.
Consulting Geologist
Burton Consulting Inc.
1408 Seventh Avenue
New Westminister, B.C., V3M 2K3
Phone/Fax 604.525.8403
aburton@shaw.ca
July 14, 2006
TABLE OF CONTENTS
SUMMARY......................................................................4
INTRODUCTION.................................................................9
Purpose of Report.........................................................9
Sources of Information....................................................9
Extent of Field Involvement...............................................9
RELIANCE ON OTHER EXPERTS...................................................10
PROPERTY DESCRIPTION AND LOCATION...........................................10
ACCESSIBILITY, CLIMATE, LOCAL RESOURCES, INFRASTRUCTURE & PHYSIOGRAPHY......12
Topography, elevation and vegetation.....................................12
Access to the Property...................................................12
Proximity to Population Centre...........................................12
Climate..................................................................12
Surface Areas............................................................13
HISTORY.....................................................................13
GEOLOGICAL SETTING..........................................................14
DEPOSIT TYPES...............................................................14
MINERALIZATION..............................................................15
EXPLORATION.................................................................15
DRILLING....................................................................15
SAMPLING METHOD AND APPROACH................................................16
SAMPLE PREPARATION, ANALYSES AND SECURITY...................................16
DATA VERIFICATION...........................................................16
ADJACENT PROPERTIES.........................................................17
U.S. Rambler Showing.....................................................17
Halls Showing............................................................17
Argentum Showing.........................................................18
Summit...................................................................19
Treasure Mountain........................................................20
MINERAL PROCESSING AND METALLURGICAL TESTING................................21
MINERAL RESOURCE AND MINERAL RESERVE ESTIMATES..............................21
OTHER RELEVANT DATA AND INFORMATION.........................................21
INTERPRETATION AND CONCLUSIONS..............................................22
RECOMMENDATIONS.............................................................23
REFERENCES..................................................................24
Certificate of author Alex Burton...........................................25
Page 2 of 25
LIST OF FIGURES
Figure 1 LOCATION MAP.......................................................6
Figure 2 CLAIM LOCATION MAP.................................................7
Figure 3 REGIONAL GEOLOGY MAP...............................................8
Page 3 of 25
SUMMARY
The Tulameen Mountain Project consists of one Mineral Claim (Tulameen Mountain,
Tenure No: 534417) located in the New Westminster, Similkameen Mining Division
of British Columbia Canada (Figure 1). The Project area is located approximately
140 km east of Vancouver and 23-km east-northeast of Hope (Figure 2).
Mr. Howard Gelfand, President of Treasure Explorations Inc., owns 100% of the
Tulameen Mountain Mineral Claim. The Tulameen Mountain Mineral Claim consists of
16 Cells totaling an area of 336 hectares.
The Blackjack showing is only known mineralized occurrence on the Tulameen
Mountain Mineral Claim (Figure 2). THE BLACKJACK SHOWING IS HOSTED BY
INTERBEDDED TUFF, QUARTZITE AND ARGILLITE WHICH ARE CROSSCUT BY A COARSE
GRAINED, BLACK FELSIC DIKE TRENDING BETWEEN NORTH AND NORTH-NORTHEAST. THE MAIN
SHOWING, LOCATED ON THE WEST SIDE OF THE JUNCTION OF DEWDNEY CREEK, IS EXPOSED
IN AN OPENCUT ABOUT 6 METERS FROM THE CREEK. DISSEMINATED PYRITE, GALENA AND
SPHALERITE OCCURS IN AN OXIDIZED BAND WHICH RANGES FROM 25 TO 30 CENTIMETERS IN
WIDTH, AND CONSISTS OF SHEARED AND ALTERED WALLROCK (GOV. OF B.C. MINISTRY OF
ENERGY, MINES AND PETROLEUM RESOURCES, MINFILE NO. 092HSW046, DETAIL REPORT).
From the available history of the Tulameen Mountain Mineral Claim area, it
appears that the majority of the claim has had no mineral exploration. The known
mineralized occurrences are located along the eastern edge of the mineral claim
beside Dewdney Creek.
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The nearby Treasure Mountain area has been recently explored with mixed results
for silver-lead-zinc polymetallic veins.
The Tulameen Mountain Project is located in coarse clastic sedimentary rocks of
the Dewdney Creek formation (Figure 3). This formation is known to host
polymetallic veins containing silver, lead and zinc.
In the author's opinion, the Tulameen Mountain Project is a worthy exploration
target.
A Phase 1 exploratory work program consisting of geological mapping, soil
sampling and rock sampling is recommended. Phase 1 will cost $25,200 (USD).
Contingent upon favorable results from Phase 1, A Phase 2 program is also
recommended. Phase 2 will consist of a magnetometer survey and trenching, which
will cost $30,600 (USD).
Page 5 of 25
FIGURE 1 LOCATION MAP
Page 6 of 25
FIGURE 2 CLAIM LOCATION MAP
Page 7 of 25
FIGURE 3 REGIONAL GEOLOGY MAP
Page 8 of 25
INTRODUCTION
PURPOSE OF REPORT
Mr. Howard Gelfand, President of Treasure Explorations Inc., contracted Alex
Burton P.Geo., P.Eng., to examine the company's Tulameen Mountain Project and
make recommendations for further exploration and development. The terms of
reference used for this report are from the ESTIMATION OF MINERAL RESOURCES AND
MINERAL RESERVES BEST PRACTICE GUIDELINES adopted by the CANADIAN INSTITUTE OF
MINING AND METALLURGY. This report was also written in accordance with NATIONAL
INSTRUMENT 43-101 - STANDARDS OF DISCLOSURE FOR MINERALS PROJECTS.
SOURCES OF INFORMATION
Sources of information noted in the text are ITALICIZED and listed in the
References. Notes on Figures 1 through 3 list the sources of the maps. For a
glossary of geological terms, I recommend using a computer online search engine
such as "Google". Search on "dictionary rocks", then lookup the geological term
in question.
EXTENT OF FIELD INVOLVEMENT
I am very familiar with the area around the Tulameen Mountain Mineral Claim. In
1968 I worked at the neighboring Treasure Mountain Mine. The Treasure Mountain
Mine is located 6 kilometers to the east of the Tulameen Mountain Mineral Claim.
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RELIANCE ON OTHER EXPERTS
The author performed no legal title searches.
PROPERTY DESCRIPTION AND LOCATION
The Tulameen Mountain Project consists of one Mineral Claim (Tulameen Mountain,
Tenure No: 534417) located in the New Westminster, Similkameen Mining Division
of British Columbia Canada (Figure 1). The Project area is located approximately
140 km east of Vancouver and 23 km east-northeast of Hope (Figure 1).
The Tulameen Mountain Mineral Claim (Tenure No. 534417) was staked on May 26,
2006 using the British Columbia Mineral Titles Online computer Internet system
(Figure 2). All claims staked in British Columbia require $0.40 per hectare
worth of assessment work to be undertaken in year 1 through 3, followed by $0.80
per hectare per year thereafter. Mr. Howard Gelfand, President of Treasure
Explorations Inc., owns 100% of the Tulameen Mountain Mineral Claim. The
Tulameen Mountain Mineral Claim consists of 16 Cells totaling an area of 336
hectares.
A logging road up Dewdney Creek provides access to the northeast corner of the
mineral claim. Much of the area has been logged.
The Blackjack showing is located on the northeast corner of the Tulameen
Mountain Mineral Claim (Figure 2).
The Blackjack showing is hosted by interbedded tuff, quartzite and argillite
which are crosscut by a coarse grained, black felsic dike trending between north
and north-northeast. The main showing, located on the west side of the junction
of Dewdney Creek, is exposed in an opencut about 6 meters from the creek.
Page 10 of 25
Disseminated pyrite, galena and sphalerite occurs in an oxidized band which
ranges from 25 to 30 centimeters in width, and consists of sheared and altered
wallrock (Gov. of B.C. Ministry of Energy, Mines and Petroleum Resources,
MINFILE No. 092HSW046, Detail Report).
There are no known environmental liabilities.
No permits have been applied for or acquired for the proposed work.
Page 11 of 25
ACCESSIBILITY, CLIMATE, LOCAL RESOURCES, INFRASTRUCTURE & PHYSIOGRAPHY
TOPOGRAPHY, ELEVATION AND VEGETATION
The Tulameen Mountain Mineral Claim is located within the Hozameen Range, which
is characterized by high, rugged mountains separated by narrow, deeply incised
valleys. The mineral claim is situated on the northwest flank of the Tulameen
Mountain.
Elevations on the mineral claim range from 900 meters in the Dewdney Creek on
the northeast portion, to over 1800 meters on the southwest corner.
ACCESS TO THE PROPERTY
The mineral claim is accessible from the Coquihalla Highway at the Carolin Mine
turnoff, approximately 21-road kilometers northeast of Hope (Figure 1). From the
highway turnoff, another 12 kilometers is traveled along a logging road up
Dewdney Creek. The lower part of the logging road is in good condition, but the
remainder has several poor sections. A four-wheel drive vehicle is required to
travel the latter part of the road.
PROXIMITY TO POPULATION CENTRE
The City of Hope is closest major population center. Travelling by car, the
Tulameen Mountain Mineral Claims are located about 33 Kilometers by road to
Hope. Vancouver is about 150 kilometers east of Hope.
CLIMATE
Snow normally covers the claims from the end of September to late June.
Page 12 of 25
SURFACE AREAS
The lower part of the valley along Dewdney Creek has been logged. The Upper
slopes of the valley are partly logged in areas.
HISTORY
The general area of the Tulameen Mountain Mineral Claim was explored
intermittently from the late 1800's to the present times. Most of the
exploration and mining activity was concentrated on Treasure Mountain located to
the east of the Tulameen Mountain Mineral Claim (Figure2).
The Blackjack Showing is located on the northeast corner of the Tulameen
Mountain Mineral Claim (Figure 2). The Blackjack showing is first mentioned in
the 1913 British Columbia Mines Annual Report. It is reported to have a vein
structure mineralized with small amounts of pyrite, marcasite, galena and
sphalerite.
In the mid 1980's Silver Saddle Mines Limited, conducted prospecting and
geological mapping on the easterly adjoining and overlapping Argentum claim
(Gov. of B.C. Ministry of Energy, Mines and Petroleum Resources, Geological
Branch Assessment Report 14,714 and 17,117). On the Blackjack showing a 0.2
meter chip sample from a leached contact zone assayed 23.31 grams silver per
tonne (GOV. OF B.C. MINISTRY OF ENERGY, MINES AND PETROLEUM RESOURCES, MINFILE
NO. 092HSW046, DETAIL REPORT).
Page 13 of 25
GEOLOGICAL SETTING
The area is underlain by Lower-Middle Jurassic Dewdney Creek Formation (Ladner
Group) tuffaceous sediments comprised of volcanic sandstone, siltstone, wacke,
tuff, and argillite with interlayered fossiliferous limestone. These rocks are
separated from the Lower-Upper Cretaceous Pasayten Group sediments to the east,
by the major northwest trending Chuwanten fault.
The Blackjack showing is hosted by interbedded tuff, quartzite and argillite
which are crosscut by a coarse grained, black felsic dike trending between north
and north-northeast. The main showing, located on the west side of the junction
of Dewdney Creek, is exposed in an opencut about 6 meters from the creek.
Disseminated pyrite, galena and sphalerite occurs in an oxidized band which
ranges from 25 to 30 centimeters in width, and consists of sheared and altered
wallrock.
Another showing, located about 500 meters south of the creek junction, occurs in
courser grained sediments. The same black, felsic dike crosscuts these bedded
sediments nearly at right angles. On both sides of the dike, which averages 6
meters in width, mineralization consists of disseminated galena and sphalerite.
The contacts are highly altered with oxidized and leached wallrock averaging 0.5
meters in width. In 1985, a 0.2 - meter sample from this leached zone assayed
23.31 grams per tonne silver (Assessment Report 14714). (Gov. of B.C. Ministry
of Energy, Mines and Petroleum Resources, MINFILE No. 092HSW046, Capsule
Geology).
DEPOSIT TYPES
A vein, stockwork type deposit similar to the nearby Treasure Mountain mine is
being explored for (Figure 2). The origin of the deposit is classified as
hydrothermal and epigenetic, with carbonate and chloritic alteration. The
polymetallic veins contain silver, lead, zinc and minor amounts of gold
Page 14 of 25
MINERALIZATION
The Blackjack showing is only known mineralized occurrence on the Tulameen
Mountain Mineral Claim. The Blackjack showing is hosted by interbedded tuff,
quartzite and argillite which are crosscut by a coarse grained, black felsic
dike trending between north and north-northeast. The main showing, located on
the west side of the junction of Dewdney Creek, is exposed in an opencut about 6
meters from the creek. Disseminated pyrite, galena and sphalerite occurs in an
oxidized band which ranges from 25 to 30 centimeters in width, and consists of
sheared and altered wallrock. Another showing, located about 500 meters south of
the creek junction, occurs in courser grained sediments. The same black, felsic
dike crosscuts these bedded sediments nearly at right angles. On both sides of
the dike, which averages 6 meters in width, mineralization consists of
disseminated galena and sphalerite. The contacts are highly altered with
oxidized and leached wallrock averaging 0.5 meters in width. In 1985, a 0.2 -
meter sample from this leached zone assayed 23.31 grams per tonne silver
(Assessment Report 14714). (Gov. of B.C. Ministry of Energy, Mines and Petroleum
Resources, MINFILE No. 092HSW046, Capsule Geology)
EXPLORATION
The nature of all relevant work to date on the Maple Mountain Project has been;
1. the gathering of all past information,
2. reviewing and analyzing the information, and
3. the writing of this report.
DRILLING
No drilling was done on the Tulameen Mountain Project.
Page 15 of 25
SAMPLING METHOD AND APPROACH
No sampling was done on the Tulameen Mountain Project
SAMPLE PREPARATION, ANALYSES AND SECURITY
This section is not applicable to this report.
DATA VERIFICATION
The sources of information, which are not based on personal examination, are
quoted in the report and listed in the references. The information provided by
the various parties is to the best of my knowledge and experience correct.
Page 16 of 25
ADJACENT PROPERTIES
U.S. RAMBLER SHOWING
The U.S. Rambler showing is located adjacent to the northeast corner of the
Tulameen Mountain Mineral Claim (Figure 2).
The U.S. Rambler showing occurs in bedded quartzite which strikes 015 degrees.
There is minor shearing along the bedding planes. The rock is altered and
oxidized with extensive limonitic staining. Vein filling along these shears is
comprised mainly of altered hostrock and contains disseminated pyrite, galena
and sphalerite.
In 1913, a 15-meter adit was driven along on along one of these shears and a
0.76-meter sample taken near the face of the tunnel assayed trace gold and 17.14
grams per tonne silver. In 1985, a 10-centimeter sample taken 100 meters east of
the main fork of Dewdney Creek from the oxidized shears along the bedding
planes, yielded 15.43 grams per tonne silver (Assessment Report 14714). (Gov. of
B.C. Ministry of Energy, Mines and Petroleum Resources, MINFILE No. 092HSW045,
Capsule Geology)
HALLS SHOWING
The Halls showing is located about 1-1/2 kilometers east of the Tulameen
Mountain Mineral Claim (Figure 2).
The Halls showing is hosted by bedded quartzite which trends 090 degrees. The
quartzite consists of alternating grey and limonitic bands which are highly
fractured and blocky in places. Fine-grained pyrite is disseminated throughout
the grey bands while the oxidized limonitic bands host some disseminated
sphalerite and galena. Several opencuts were excavated in the oxidized bands. In
1913, a sample taken across1.2 meters assayed 0.69 grams per tonne gold and 24.0
grams per tonne silver (Gov. of B.C. Ministry of Energy, Mines and Petroleum
Resources, MINFILE No. 092HSW047, Capsule Geology).
Page 17 of 25
ARGENTUM SHOWING
The Argentum showing is located approximately 2 kilometers east of the Tulameen
Mountain Mineral claim (Figure 2).
The Argentum occurrence is underlain by north-northwest striking (340-350
degrees), west dipping (60 degrees) volcanic sediments consisting of sandstone,
conglomerate, agglomerate, tuff and argillaceous tuff intruded by dioritic sills
and dikes. Shearing along dike contacts is sometimes accompanied by a narrow
zone of quartz veinlets. The hostrocks belong to the Dewdney Creek Formation.
Pyrrhotite and lesser pyrite are commonly disseminated throughout these
lithologies. The tuffs and argillaceous tuffs are distinctive units in that they
contain limonite coatings along fracture planes and have a higher percentage of
pyrrhotite and pyrite. A fault is evidenced by offsets of some rock units. Some
minor shears occur in the volcanic sandstone, tuffaceous argillite and argillite
units. The shears are highly fractured and oxidized and contain sparse pyrite,
sphalerite and galena. Locally, unmineralized quartz veins to 25 centimeters
wide also occur. Rock chip samples from the mineralized shear zones assayed up
to 70.95 grams per tonne silver (Assessment Report 14714). (Gov. of B.C.
Ministry of Energy, Mines and Petroleum Resources, MINFILE No. 092HSW153,
Capsule Geology).
Page 18 of 25
SUMMIT
The Summit property, a past underground producer is located 31/2kilometers east
of the Tulameen Mountain Mineral Claims (Figure 2).
In 1951, 18 tonnes were mined and milled from the Summit property. Recovery was
14,867 grams of silver (826 grams Ag per tonne), 3,079 kilograms lead (17% Pb),
and 2,675 kilograms zinc (15% Zn). (Gov. of B.C. Ministry of Energy, Mines and
Petroleum Resources, MINFILE No. 092Hsw023, Summary Production).
In 1988, mineral exploration work consisting of geochemical, geophysical,
geological and trenching was performed on the Summit property. The summary from
ASSESSMENT REPORT 18,111 is as follows;
The subject property is underlain by tuffaceous and pelitic sediments of the
Upper Jurassic Dewdney Creek Group. Mineralization is generally consistent in
character throughout the area. It consists of silver-bearing sulfides in quartz
carbonate veins localized along locally prominent, steeply dipping fault
structures, subsidiary faults and tension fractures. The veins varies in width
and usually consist of a central core of massive sulfides with veinlets and
disseminations distributed outward.
The 1988 geochemistry survey delineated 8 anomalous zones, 7 of which have
coincident EM conductors. The Basil Vein, discovered during this year's program,
is located within one of these anomalous zones. The size and intensity of the
anomaly indicates a larger structure than the Basil Vein or perhaps series of
parallel structures.
The trenching program exposed the Indiana vein for 390 meters and sampling of
the trenches have shown that the vein is mineralized, though in varying degrees,
throughout the entire exposed strike length.
Page 19 of 25
TREASURE MOUNTAIN
The Treasure Mountain Mine is located 6 kilometers east of the Tulameen Mountain
Mineral Claim.
The first significant underground work was done from 1909 to 1912. Work ceased
in the area during World War I. From 1929 to 1932, 1,148 tonnes of ore were
mined from the Treasure Mountain mine. No further production was recorded until
1988 when another 362 tonnes were mined. Of the total 1510 tonnes mined from the
Treasure Mountain Mine, 1,283 tonnes were milled. The 1,283 milled tonnes
produced 2,186,372 grams of silver (1,704 grams Ag / tonne), 93 grams gold (
0.07 grams Au / tonne), 292,342 kilograms lead (22.8 % Pb), 64,582 kilograms
zinc (5.0% Zn),(Gov. of B.C. Ministry of Energy, Mines and Petroleum Resources,
MINFILE No. 092HSW016, Production Detail Report).
In 1988 Huldra Silver Inc. reported for the Treasure Mountain Mine combined
reserves (probable / possible / inferred) in all zones totaling 160,000 tonnes.
The grade reported is 850 grams silver per tonne, 4.0 % lead and 5.0 % Zn. A
cutoff grade of 500 grams per tonne equivalent silver was used. (Gov. of B.C.
Ministry of Energy, Mines and Petroleum Resources, MINFILE No. 092HSW016,
Inventory Detail Report).
NOTE: Mineral Resources and Mineral Reserves NOT compliant with National
Instruments 43-101 standards.
Page 20 of 25
MINERAL PROCESSING AND METALLURGICAL TESTING
No metallurgical testing done.
MINERAL RESOURCE AND MINERAL RESERVE ESTIMATES
No Mineral Resource or Mineral Reserve estimates.
OTHER RELEVANT DATA AND INFORMATION
None
Page 21 of 25
INTERPRETATION AND CONCLUSIONS
From the available history of the Tulameen Mountain Mineral Claim area, it
appears that the majority of the claim has had no mineral exploration. The known
mineralized occurrences are located along the eastern edge of the claim beside
Dewdney Creek.
The nearby Treasure Mountain area has been recently explored with mixed results
for silver-lead-zinc polymetallic veins.
The Tulameen Mountain Project is located in coarse clastic sedimentary rocks of
the Dewdney Creek formation (Figure 3). This formation is known to host
polymetallic veins containing silver, lead and zinc.
In the author's opinion, the Tulameen Mountain Project is a worthy exploration
target.
Page 22 of 25
RECOMMENDATIONS
The following work program is recommended for the Tulameen Mountain Project.
Phase 1 of the work program will consist of geological mapping, soil sampling
and rock sampling.
PHASE 1 BUDGET
Geologist 12 days @ $700/day $ 8,400
Technologist 12 days @ $300/day $ 3,600
Vehicle 12 days @ $100/day $ 1,200
Rock Samples 20 @ $50 each $ 1,000
Soil Samples 100 @ $40 each $ 4,000
Expenses, food, field supplies $ 4,000
Report $ 3,000
-------
TOTAL (US DOLLARS) $25,200
=======
Contingent upon favorable results from Phase 1, the following Phase 2 work
program is recommended. Phase 2 will consist of a magnetometer survey and
trenching.
PHASE 2 BUDGET
Bond $ 5,000
Geologist 6 days @ $700/day $ 4,200
Technologist 6 days @ $300/day $ 1,800
Vehicle 6 days @ $100/day $ 600
Magnetometer Survey $ 5,000
Excavator 2 days @ $1500/day $ 3,000
Rock Samples 100 @ $50 each $ 5,000
Expenses, food, field supplies $ 3,000
Report $ 3,000
-------
TOTAL (US DOLLARS) $30,600
=======
Page 23 of 25
REFERENCES
Chung, P.L., Geochemical, Geophysical, Geological and Trenching Report on
the Summit Camp Property, Harrisburg-Dayton Resource Corp.,
Geological Branch Assessment Report 18,111
Government of British Columbia Ministry of Energy, Mines and Petroleum
Resources, MINFILE No. 092HSW023, 092HSW045, 092HSW046,
092HSW047,092HSW153, 092HSW016,
Jones, H.M., 1987, A GEOLOGICAL REPORT ON THE ARGENTUM CLAIM, Silver Saddle
Mines Ltd., Geological Branch Assessment Report 17,117
Rodstrom, H.J., 1985, PROSPECTING REPORT, Silver Saddle Mines Ltd.,
Geological Branch Assessment Report 14,714
Page 24 of 25
Certificate of author Alex Burton
I, Alex Burton, Consulting Geologist hereby certify that:
1. I have a consulting office at 1408 7 Avenue, New Westminster, B.C., Tel and
fax 604 525 8403. email: aburton@shaw.ca
2. I am a graduate geologist from the University of British Columbia. Further,
I am registered as both a Professional Engineer and Professional
Geoscientist with the Association of Professional Engineers and
Geoscientists of B. C., #6262. I am also a Life Member of the Canadian
Institute of Mining and Metallurgy, and the Association of Geoscientists
for International Development. I am a founding member of the Association of
Applied Geochemists.
3. I have practiced my profession for over fifty years, both as a manager of
exploration for major international mining companies, and as an independent
consultant, and have written many qualifying reports.
4. As a result of my experience and qualifications I am a Qualified Person as
defined in National Instrument 43-101.
5. I have no interest in the "Tulameen Mountain Project" or in Treasure
Explorations Inc., nor do I expect to receive any such interest.
6. I am very familiar with the area around the Tulameen Mountain Mineral
Claim. In 1968 I worked at the neighboring Treasure Mountain Mine.
7. As of the date of this certificate, to the best of my knowledge,
information, and belief, the technical report contains all scientific and
technical information that is required to be disclosed to make the
technical report not misleading.
This report titled Tulameen Mountain Project has been prepared for Treasure
Explorations Inc. Permission is hereby granted to Treasure Explorations Inc. for
the inclusion of this report in support of any filings with the US SEC, and/or
other regulatory bodies.
Dated this 14th day of July, 2006 in New Westminster, B. C. CANADA
/s/ Alex Burton P.Eng., P.Geo. [SEAL]
- -------------------------------------
Alex Burton P.Eng., P.Geo.
Consulting Geologist
Page 25 of 25