Charlie Mortimer

Dore Project

Assessment Report on

Diamond Drilling

Claim #4202945

Dore Township NTS 41 0/NE

RECE VED APR 2 1 2010

GEOSCIENCE ASSESSMENT . IC

ApriJ 20, 2010 Todd Keast

TABI,E OF CONTENTS

Page Introduction ................................................................... 1

Location and Access ......................................................... I

Property ........................................................................ I

Topography .................................................................... 2

Regional Geology ............................................................. 2

Property Geology ............................................................ 2

Exploration PrograJil .......................................................... 3

Recommendations ............................................................ 4

References ..................................................................... 5

Appendix I

Diaiilond Drill Log

Drill Section

Plan Map

2

INTRODUCTION

During 2009, Charlie Mortimer continued drilling a diamond drill hole on a claim in Dore

Township, situated approximately 100 kilometres southwest of Timmins Ontario, within

the Porcupine Mining Division.

The claim is located in the Swayze greenstone belt of the Abitibi Subprovince. The

greenstone belt is an east-west trending sequence 45km by 25km. Rock types include

massive and fragmental rhyolite volcanic rocks, massive and pillowed basaltic flows, and

scattered feldspar porphyry intrusions. Sedimentary rocks are a minor component and

include greywacke, argillite, and conglomerate. East-west trending fold axis, are

prevalent throughout the stratigraphic package.

Diamond drilling was planned to test a surface showing of quartz carbonate veins within

a wide alteration system which was uncovered during a mechanical trenching program.

The drill hole 2008-1 was planned to be drilled to a depth of approximately 300 metres,

however drilling was suspended in the fall of 2008 due to weather conditions. In the

spring of 2009 and throughout the summer the drilling of this hole was resumed. The

author of this report visited the property on April 14 2010 to log the drill core. Mr

Mortimer intends to continue drilling this hole as widespread quartz carbonate alteration,

and shearing has been intersected as the bottom of the hole.

LOCATION AND ACCESS

The property is situated 100 kilometres southwest ofTimmins, Ontario. The project is

located inDore Township of the Porcupine Mining Division. The latitude and longitude

of the project is NTS 41 0 I NE, 47° 45 'N 82° 40' E.

Access to the property is excellent. The Folyet Timber road crosscuts the property. The

logging road is accessed from Hwy 101 approximately 100 km southwest ofTimmins.

The property is approximately 55km south of the Hwy. A logging access trail can be use

to drive to the drill setup.

PROPERTY

The Dore Project consists of 17 unpatented mining claims. The claims are situated in

Dore Township (01108) and Swayze Township (G 3249) ofthe Porcupine Mining

Division. The holder of claim 4202495 is Charles Mortimer (1 00% ).

TOPOGRAPHY

The Dore project is characterized by flat to gently rolling topography. The vegetation

consists predominantly of balsam and spruce in the low areas, and a mixture of poplar

and balsam in the high areas. Outcrop exposure is approximately five to ten percent.

REGIONAL GEOLOGY

The project is situated in the Swayze greenstone belt of the Abitibi Subprovince. The

greenstone belt is an east-west trending sequence 45 km by 25 km. Rock types include

massive and fragmental rhyolite volcanics, massive basalt flows, and scattered feldspar

porphyry intrusions. Sedimentary rocks are a minor component and include greywacke

and conglomerate. East-west trending fold axis are prevalent throughout the stratigraphic

package.

The Ontario Geological Survey completed a mapping project ofDore Township O.D.M.

Report 33.

PROPERTY GEOLOGY

The claims are situated over a major east west trending rhyolite I basalt contact.

Lithological contacts are preferential sites of structural development, thus important

exploration targets.

The geology of the project consists of a thick sequence of volcanic rocks which include

mafic volcanic flows, mafic lapilli tuffs, conglomerates, feldspar porphyry intrusions, and

narrow north-south trending diabase dykes, and an east-west oriented 50m wide shear

2

zone. Alteration within the shear zone consists of chlorite - sericite - carbonate schist.

Quartz veins were identified at a number of locations along the structure. Charlie

Mortimer has completed considerable mechanical trenching on the property. The author

has visited and mapped these trenches. Once the maps are compiled it is hoped that a

better understanding of the property geology will be apparent. The goal of the mapping is

to get a basic understanding of the major rock types, possible marker horizons,

distribution of alteration, and orientation of structures and vein systems. The field

mapping is complete but still needs to be compiled on proper maps. The mapping portion

will be the subject of a separate assessment report.

EXPLORATION PROGRAM

Charlie Mortimer has been undertaking exploration activities for a number of years on

this project area. Work has included considerable mechanical trenching, diamond

drilling, prospecting and gold analysis. Mr. Mortimer is currently drilling a hole to

evaluate a newly discovered gold showing that was uncovered during the mechanical

trenching program. Drill hole 2008-1 was planned to be drilled approximately 300

metres in depth. Mr. Mortimer owns and operates his own diamond drill rig. In the

summer and fall of 2008 Mr. Mortimer drilled 90.1 metres on this hole but suspended

drilling because of poor weather conditions. The hole was continued in the summer of

2009 to a depth of218.9 m. The author visited the drill on April14, 2010, site and

logged and the drill core. The location plan of the drill hole, the drill section and drill log

are included in the Appendix I of this report.

Mafic volcanic flows are the major unit intersected to date and typically massive to

weakly foliated. The drill hole intersected quartz carbonate sericite altered porphyry at

206m with increasing alteration an shearing to the bottom of the hole 218.9 m (Photo 1

and 2).

CONCLUSIONS AND RECOMMENDATIONS

3

The author agrees with Charlie Mortimer's plan to continue the drill hole through the

alteration system.

4

Photo 1- Drill core for 2008-1 hole extended to 218.9 m (UTM 380908 E 5299463 N)

Photo 2- Progressive alteration in Feldspar Porphyry. (measurements marked in feet, converted to metres in log)

REFERENCES

References:

Donovan,J.F. 1965

Geology of Swayze and Dore Townships. Ontario Department of Mines

Geological Report No. 33. Accompanied by Map 2070, coloured.

O.G.S. 1982

Airborne Electromagnetic an Total Intensity Magnetic Survey, Swayze Area, Cree

Lake Sheet, District of Sudbury, 80541.

5

CERTIFICATE OF QUALIFICATION

I, Todd Keast, of 78 Nova Drive, Sudbury, Ontario, do hereby certify that:

1. I am the author of this report.

2. I am a graduate of the University of Manitoba, Winnipeg, Manitoba, having

received an Honors Bachelor of Science (Geology), in 1986.

3. I have practiced in the field of mineral exploration since 1987, for a number of

exploration companies throughout Manitoba, Ontario, and Quebec.

4. I am a registered P.Geo, in Ontario.

Dated at Sudbury, Ontario this 20th day of April, 2010.

Todd Keast, P.Geo

6

Appendix I

Diamond Drill Log

Drill Section

Drill Location Sketch

7

Charlie Mortimer DoreTwp

DOH# 20081 : -Claim 4202945

ft From (mJ To(mJ 0.00 0.50

0.50 11.28

11.28 91.10

91.10 206.70

206.70 218.90

19J() Az" th a d o· 1Jf61-50 lmU n lp: Acid test, "no test" : E.O.H: 218.9m

Rock Type Casina

Feldspar Porphyry Dike

Mafic Volcanic Flows

Mafic Volcanic Flows

Feldspar Porphyry

Code CAS

2008-1 extend

Drill Company: UTM type· 380908E 5299463N Charlie Mortimer

' ' )_~~ _L Start : August 22, 2008 Logged by: End: November 10 2009 T.Keast '//V~ ~ Description Hardness MS Recovery Bedrock setup Light pink, fine grained. Hard siliceaous unit with 3-5% euhedral feldsapr phenocrysts up to 5 mm in size. Massive non foliated unit. 7 99 Dark green mafic flows, chloritic, slighlty silicified, hard dense unit. Moderately foliated 55 degress to Core axis. Local section of flow breccia rare pillow seledge. Scattered carbonate viens, rare grain of pyrite. 7 99

Hole stopped Fall 2008, upper portion applied for assessment work

Dark green mafic flows, chloritic, slighlty silicified, hard dense unit. Moderately foliated 55 degress to Core axis. Local section of flow breccia rare pillow seledge. Scattered carbonate viens, rare grain of pyrite.

Light green intrusion with 1 0-15% white feldspar phenocyrsts up to 4mm in size. Siliceous matrix, unit is hard, weakly foliated at top of unit becoming stronly foliated downhole. Foliation 85 deg to CA. Sericite alteration, carbonate alteration and overall shearing is increasing down unit, feldspar outlines flattened and indistinct. outlines. Unit is gradational into a qtz sericite carbonate schist.

EOH = 218.9 m Casing still in hole.

Drill is still on the setup should continued in the spring of 2010.

1 of 1 4/20/2010

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Date:2110412010 200

Scale: 1 :5,000

Office: Sudbury

Drawing: Map 1

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Township Boundary

Claim, wtth number

Patent, wl1h label

Trail, Secondary Road

Road

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Lake

Drill hOle wtth trace projee1lld to surface

Charles Mortimer Property Dore and Swayze Townships

Drill hole Plan

Projection: UTM Zone 17 (NAD 83)