3. TSXv:LK / FSE: 6LL / lakelandresources.com / @LakelandRes
Disclaimer: This Presentation has been prepared by Lakeland Resources Inc. (“Lakeland”) using
its best efforts to realistically and factually present the information contained. However,
subjective opinion, dependence upon factors outside Lakeland’s control and outside information
sources unavoidably dictate that Lakeland cannot warrant the information contained to be
exhaustive, complete or sufficient. In addition, many factors can affect the Presentation which
could significantly alter the results intended by Lakeland, rendering the Presentation
unattainable or substantially altered. Therefore, interested Users should conduct their own
assessment and consult with their own professional advisors prior to making any investment
decisions.
This Presentation does not constitute a prospectus or public offering for financing, and no
guarantees are made or implied with regard to the success of Lakeland’s proposed ventures.
Interested investors are advised to seek advice from their investment advisors.
Technical information has been prepared in accordance with the Canadian regulatory
requirements set out in National Instrument 43-101 and reviewed on behalf of the Company by
Neil McCallum P.Geo., a Qualified Person.
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5. TSXv:LK / FSE: 6LL / lakelandresources.com / @LakelandRes
LOCATION
Potential of area demonstrated by:
• Uracan/UEX Corp. Black Lake Project:
DDH BL-018: 0.69% U3O8 over 4.4 metres,
including 1.96% U3O8 over 0.50 m
UEX Corp. recently (Jan 2013) optioned 60%
to Uracan for C$10.0 million in exploration
over 10 years
• UEX Corp. Riou Lake Project:
Radioactive boulders in glacial till on the
property with up to 11.3% uranium; source
still to be identified
GIBBONS CREEK TARGET
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6. TSXv:LK / FSE: 6LL / lakelandresources.com / @LakelandRes
LOCATION
Potential of area demonstrated by:
• The presence of many un-tested
basement conductors in the area
• Exploration in the region has
identified some smaller deposits
• Fond Du Lac Deposit
1 million pounds U3O8 at 0.25%
• Nisto Uranium Mine (historic)
500 tons of ore were shipped to the
Loradio Mill. One shipment of 106 tons of
ore graded 1.6% U3O8.
• Middle Lake Zone
Initial exploration conducted prior to
reserve over project
GIBBONS CREEK TARGET
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LOCATION
step back for a regional setting
Importance of the continental-scale
SNOWBIRD TECTONIC ZONE
Associated with several uranium deposits:
Nisto Zone, Dufferin Zone, Middle Lake,
Centennial Deposit (Cameco & Areva)
• Intercepts up to 34 metres averaging
8.8% U3O8
Starting at a depth of 797 metres
• As of March, 2012, over $30.2 million has
been spent on the project
GIBBONS CREEK TARGET
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8. TSXv:LK / FSE: 6LL / lakelandresources.com / @LakelandRes
LOCATION
step back for a regional setting
Importance of the continental-
scale SNOWBIRD TECTONIC ZONE
Other fault splays to the west are likely areas
to find additional uranium mineralization.
Grease River Fault Zone Fond-du Lac Deposit
Platt Creek Fault Black Lake Zone
Complex magnetic setting suggests the
potential for many fault zones not yet
identified
Fond du Lac
Deposit
Black Lake
Zone
Nisto Uranium
Zone
South Pine
Showing
GIBBONS CREEK TARGET
DDH RLG-D10
showing
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9. TSXv:LK / FSE: 6LL / lakelandresources.com / @LakelandRes
STRUCTURE
The Snowbird Tectonic Zone (active at 1.9 Ga)
provides a weakness for re-activation during
1.75 Ga Trans-Hudson orogen, and Athabasca
Basin mineralization at 1.59 Ga.
Centennial deposit highlights the importance
for late “brittle” faulting:
“Mineralization is located approximately 300 m east of the
interpreted location of the post-Athabasca Dufferin Lake
fault. There, it straddles an unconformity high formed at the
contact between highly strained weakly mylonitic
metasedimentary and granitoid rocks of the basement. At
this contact is a steeply west-dipping zone of brittle
deformation which represents the reactivation of earlier
ductile structures of the Snowbird Tectonic Zone/VRSZ under
brittle conditions.
This structural interpretation map of the
Gibbons Creek area shows evidence for large-
scale disturbances and locations for possible
brittle faulting.
Strong Conductive
Zone
Weak Conductive
Zone
Gravity Low
identified
“lithologic” marker
for structural interp
Brittle fault displacing
basement “lithology”
Stony
Rapids
First
Nations
Reserve
UEX Drilling
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10. HISTORIC
DRILLING
Drilling on the property was conducted
for the most part by Eldorado Nuclear
in the 1977-1979 period.
An area with elevated uranium near
the unconformity occurs near the
gravity low and weak conductive zone.
• GC-15 was the highest with 0.18% U3O8
over 0.13 m
Radioactive boulders were discovered
during the last field season in the small
prospected area.
Prospected
area with
boulders up to
5.1% U3O8
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GC-15:
0.18% U3O8
over 0.13 m
Area with elevated
uranium near the
unconformity
