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FRONTIER ENERGY LIMITED Capital/Financing Update 2018

Dec 17, 2018

64917_rns_2018-12-17_1c1f8c82-4885-496f-9fa5-80c8cec39b86.pdf

Capital/Financing Update

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ASX Announcement ASX: SUP 18[th] December 2018 superiorlake.com.au

Superior Lake drilling hits new footwall zone of 25.2% Zinc

Highlights

  • Drilling at the Superior Lake zinc project discovered a new footwall zone and confirmed high-grade mineralisation.

  • The intersections include:

  • New footwall zone - 0.35m @ 25.2% Zn, 0.18% Cu; and

  • Mid-Pick - 1.56m @ 20.12% Zn, 0.8% Cu.

  • Both areas are outside the current JORC resource, giving potential to increase it

  • Drilling continuing, with further results expected January 2019

  • Results have potential to increase 6.5-year mine life, lift production and lower costs

  • Company to release a Definitive Feasibility Study by mid-2019.

Superior Lake Resources Limited (ASX: SUP) is pleased to announce an exploration drill program at its Superior Lake Zinc Project (“Project”) in Ontario, Canada has intersected high-grade zinc at the Mid Pick zone and identified a new footwall zone within 9m of the Pick Lake deposit.

Results included:

  • Mid-Pick zone: 1.56m @ 20.12% Zn, 0.8% Cu (Figure 1)

  • New footwall zone: 0.35m @ 25.2% Zn 0.18% Cu.

These results have the potential to further improve project economics for Superior Lake.

An October 2018 Restart Study, forecasted the Project will produce approximately 46,000tpa Zn over an initial 6.5-year mine life, with an AISC of US$0.51/lb (see ASX announcement dated 10 October 2018). The Company will complete a Definitive Feasibility Study for the Project by mid-2019.

In addition to the first drill program, a litho-geochemistry and structural review of the Project has identified five high priority targets. These targets, in association with the drilling and the new geophysical anomaly defined by DHTEM, will be tested to 1,000m with a surface geophysics program over a 3km x 3km area scheduled for February 2019.

Figure 1: High-Grade Intersection PL-18-01

==> picture [504 x 121] intentionally omitted <==

Superior Lake Resources Limited ACN 139 522 553

Suite 23 513 Hay Street Subiaco WA 6008

T: +61 8 6143 6740 F: +61 8 9388 8824

Page 1

Superior Lake Chief Executive Officer David Woodall said:

“This is an outstanding start to the exploration program. Assuming similar success from the remaining hole in the current program, we are confident of defining an initial resource at Mid-Pick, as well as increasing the Project’s mine life.

“The Superior Lake Zinc Project has the potential to be in the lowest-cost quartile of zinc producers globally, given the low estimated operating costs and low estimated initial capital cost due to the infrastructure already in place. Further discoveries will improve our economics.”

Mid-Pick drill program

The Pick Lake deposit comprises high-grade zinc mineralisation that extends over a downdip distance of 1,200m and has a JORC resource of 2.15 Mt @ 17.7 % Zn, 0.9% Cu. Whereas the upper and lower areas have been intensively drilled from underground, the area between the upper and lower Pick, known as Mid-Pick, sits outside the resource and requires additional drilling to fully test this area.

The drilling program currently being executed comprises of approximately 1,750m, with a single parent hole combined with 'daughter' holes testing the up dip and strike of the area of interest. To date, the parent hole has been completed along with the first daughter hole (assays pending expected in January 2019) and a down hole geophysics survey.

Figure 2: Significant Brownfields Exploration Potential

==> picture [502 x 356] intentionally omitted <==

Page 2

Figure 3: Mid-Pick Drilling Program targeting Additional Resource Potential

==> picture [511 x 352] intentionally omitted <==

The single parent hole, the first drill hole at the Project in more than 20 years, successfully intersected highgrade zinc mineralisation of 1.56m @ 20.12% Zn, 0.8% Cu. Importantly, both the grade and thickness were in line with previous drilling completed at the Project, as highlighted in Table 1.

The intersection of a new zone 9m into the footwall, 0.35m @ 25.2% Zn, 0.18% Cu, will require follow up work reviewing the Pick Lake drilling database, additional intercepts of the present drill program, and geophysics. This high-grade zone of predominately sphalerite was intersected in hole PL-18-01 and PL-1801-W1 (awaiting assays – January 2019)

Down-hole geophysics successfully identified the higher grade and thickest portions of copper in the Pick Lake Ore Body and confirmed continuity of ore between upper and lower Pick resources. Superior Lake has planned follow-up work for February 2019 as part of a surface geophysics program over a 3km x 3km area, adjacent to the Winston and Pick deposits, that will test exploration potential to a depth of 1,000m.

This surface geophysics program is the first stage of an exploration strategy designed to test the area which hosts the Exploration Target* of between 2.1 to 5.2 million tonnes at a grade ranging between 13.3% to 15.4% Zn (see ASX Announcement dated 26 September 2018).

*The potential quantity and grade of the Exploration Target is conceptual in nature and therefore is an approximation. There has been insufficient exploration to estimate a Mineral Resource and it is uncertain if further exploration will result in the estimation of a Mineral Resource.

Page 3

Table 1: Historical drill intersections at Pick Lake[1]

Hole ID Width (m) Zn (%) Cu (%)
UP-0103 2.0 8.25 0.21
UP-0105 2.0 16.5 0.95
UP-0106 2.0 14.09 0.81
UP-0107 2.0 8.79 0.12
UP-0108 2.0 10.46 0.35
UP-0109 2.5 27 1.86
UP-0110 2.0 14.82 0.8
UP-0111 2.0 16.43 1.02

About the Company

Superior Lake Resources Limited

Superior Lake Resources Limited (ASX: SUP) is focused on the redevelopment of the Superior Lake Zinc Project in North Western Ontario, Canada. The Project is one of the highest-grade zinc deposits globally with a JORC resource of 2.15 Mt at 17.7% Zn, 0.9% Cu, 0.4 g/t Au and 33.5 g/t Ag. A Restart Study completed in 2018, forecasted the Project will produce approximately 46,000tpa Zn over an initial 6.5 year mine life, with an AISC of US$0.51/lb, putting the Project in the lowest cost quartile globally. The Company is currently working towards the release of a Definitive Feasibility Study by mid-2019.

Table 2: Superior Lake Mineral Resource at 3% Zn cut-off grade

Classification Tonnage
Zn%
Cu%
Au g/t
Tonnage
Zn%
Cu%
Au g/t
Tonnage
Zn%
Cu%
Au g/t
Tonnage
Zn%
Cu%
Au g/t
Ag g/t
Indicated 1,992,000 17.8% 0.9% 0.4 g/t 33.7 g/t
Inferred 152,000 15.4% 0.9% 0.4 g/t 31.2 g/t
Total 2,145,000 17.7% 0.9% 0.4 g/t 33.5 g/t

To learn more about the Company, please visit www.superiorlake.com.au, or contact:

David Woodall Chief Executive Officer +61 8 6143 6740

1 As per Superior Lake’s announcement dated 3 July 2018. Superior Lake confirms that it is not aware of any new information or data that materially affects the information included in the original announcement.

Page 4

Competent Persons’ Statement

Exploration Target and Exploration Results

The information contained in this announcement that relates to the exploration target and exploration results is based on, and fairly reflects, information compiled by Mr. Alfred Gillman, an independent consultant Superior Lake Resources Limited. Mr. Alfred Gillman is a Fellow and Chartered Professional of the Australian Institute of Mining and Metallurgy and was engaged as a consultant to Superior Lake Resources to complete the JORC (2012) resource. Mr. Gillman has sufficient experience which is relevant to the style of mineralisation and type of deposit under consideration and to the activity which he is undertaking to qualify as a Competent Person as defined in the 2012 Edition of the ‘Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves’. Mr. Gillman consents to the inclusion in this announcement of the matters based on his information in the form and context in which it appears.

Mineral Resources

The information in this announcement that relates to the Mineral Resources on the Superior Lake Project was first reported by the Company to ASX on July 3[rd] , 2018. The Company confirms that it is not aware of any new information or data that materially affects the information included in the original market announcements, and in the case of estimates of Mineral Resources, that all material assumptions and technical parameters underpinning the estimates in the relevant market announcement continue to apply and have not materially changed. The Company confirms that the form and context in which the Competent Person's findings are presented have not been materially modified from the original market announcement.

Page 5

Appendix 1

Drill hole information

The Company provides the following information in accordance with Listing Rule 5.7.2.

Hole ID Easting Northing RL Length Azimuth Dip Dip From To Interval
Zn%
Cu%
(m) (collar) (interval) (m) (m) (m)
PL-18-01
471530
542064 10422 879 290 -86.7 -75.75 839.5 840.0 0.5 3.83% 1.17%
840.0 841.06 1.06 27.8% 0.629%
848.84 849.19 0.35 25.2% 0.18%

At the date of this announcement the Company has only received the initial results shown above, further results from this program are expected in January 2019.

Page 6

Appendix 2

JORC Code, 2012 Edition Table 1

Section 1 Sampling Techniques and Data

Criteria Explanation Commentary
Sampling
Techniques
Nature and quality of
sampling (eg cut
channels, random
chips, or specific
specialised industry
standard
measurement tools
appropriate to the
minerals under
investigation, such as
down hole gamma
sondes, or handheld
XRF instruments, etc).
These examples
should not be taken
as limiting the broad
meaning of sampling.
Aspects of the
determination of
mineralisation that
are Material to the
Public Report.
The Pick Lake targets were sampled by diamond core drilling. The drilling was
carried out by Chibougamau Diamond Drilling Ltd. Drill core was sampled at
variable intervals guided by changes in geology.
The drill hole collar location was surveyed by Superior Survey Inc. Sample
preparation was undertaken at ALS Thunder Bay laboratory.
Samples were weighed and logged with details entered into a master sampling
tracking spreadsheet.
Sample preparation and analyses were conducted by ALS Laboratories
located at Thunder Bay and Vancouver.
Samples were dried and each sample was fine crushed to >70% passing a 2mm
screen. A 250g split was pulverised using a ring and puck system to >85%
passing 75-micron screen.
The analytical technique used for all samples initially involved a four-acid digest
followed by multi-element ICP-ES analysis producing results for base metals and
gold.
• Method OG62 for zinc,
• Method OG62 copper,
• Method FA- AA for gold,
• Method OG62 silver
Drilling
techniques
Drill type (eg core,
reverse circulation,
open-hole hammer,
rotary air blast,
auger, Bangka, sonic,
etc) and details (eg
core diameter, triple
or standard tube,
depth of diamond
tails, face-sampling
bit or other type,
whether core is
oriented and if so, by
what method, etc).
Drilling technique for all holes was diamond drilling with HQ-size (63.5mm
diameter) core. Drill core in angled holes is being oriented for structural
interpretation.
Downhole surveys were carried out at 30m intervals by gyro instrumentation.
Drill Sample
Recovery
Method of recording
and assessing core
and chip sample
recoveries and results
assessed.
recovery and ensure
representative nature
of the samples.
Whether a
relationship exists
betweensample
Depths were measured from the core barrel and checked against marked
depths on the core blocks. Core recoveries were logged and recorded in the
database. Sample recoveries were high with >85% of the drill core having
recoveries of >97%.
There is no discernible relationship between recovery and grade, and therefore
no sample bias.

Page 7

Detailed core logging was carried out with recording of weathering, lithology,
alteration, veining, mineralisation, structure, mineralogy, RQD and core
recovery.
Drill core was photographed indoors, wet and with flash, in core trays prior to
sampling. Each photograph includes core tray labels detailing hole number
and depth interval. All holes were logged in full.
100% of the core is logged.
Drill core was sawn in half using a core saw. All samples were quarter core and
were collected from the same side of the core.
Duplicate, standard and blank check samples are submitted with drill core
samples. The sample sizes are considered appropriate to the grain size of the
material being sampled.
All samples were taken from diamond core.
recovery and grade
and whether sample
bias may have
occurred due to
preferential loss/gain
of fine/coarse
material.
Logging Whether core and
chip samples have
been geologically
and geotechnically
logged to a level of
detail to support
appropriate Mineral
Resource estimation,
mining studies and
metallurgical studies.
Whether logging is
qualitative or
quantitative in
nature. Core (or
costean, channel,
etc) photography.
The total length and
percentage of the
relevant intersections
logged.
Detailed core logging was carried out with recording of weathering, lithology,
alteration, veining, mineralisation, structure, mineralogy, RQD and core
recovery.
Drill core was photographed indoors, wet and with flash, in core trays prior to
sampling. Each photograph includes core tray labels detailing hole number
and depth interval. All holes were logged in full.
100% of the core is logged.
Sub-Sampling
techniques and
sample preparation
If core, whether cut
or sawn and whether
quarter, half or all
core taken.
Drill core was sawn in half using a core saw. All samples were quarter core and
were collected from the same side of the core.
Duplicate, standard and blank check samples are submitted with drill core
samples. The sample sizes are considered appropriate to the grain size of the
material being sampled.
Sub-
sampling
techniques
and sample
preparation
If non-core, whether
riffled, tube sampled,
rotary split, etc and
whether sampled
wet or dry.
For all sample types,
the nature, quality
and appropriateness
of the sample
preparation
technique. Quality
control procedures
adopted for all sub-
sampling stages to
maximise
representivity of
samples.
Measures taken to
ensure that the
sampling is
representative of the
in-situmaterial
All samples were taken from diamond core.

Page 8

Sample preparation and analyses were conducted by ALS Laboratories
located at Thunder Bay and Vancouver.
Samples were dried and each sample was fine crushed to >70% passing a 2mm
screen. A 250g split was pulverised using a ring and puck system to >85%
passing 75-micron screen.
The analytical technique used for all samples initially involved a four-acid digest
followed by multi-element ICP-ES analysis producing results for base metals and
gold.
• Method OG62 for zinc,
• Method OG62 copper,
• Method FA- AA for gold,
• Method OG62 silver
Senior technical personnel from the Company (Project Geologist) collected
and inspected the samples.
Primary data were collected by employees of the Company at the project site.
All measurements and observations were recorded onto hard copy templates
and later transcribed into the Company’s digital database.
Digital data storage, verification and validation are managed by a Perth-based
data management consultant.
No adjustments or calibrations have been made to any assay data.
collected, including
for instance results for
field
duplicate/second-
half sampling.
Quality of
assay data
and
laboratory
tests
The nature, quality
and appropriateness
of the assaying and
laboratory
procedures used and
whether the
technique is
considered partial or
total.
For geophysical tools,
spectrometers,
handheld XRF
instruments, etc, the
parameters used in
determining the
analysis including
instrument make and
model, reading times,
calibrations factors
applied and their
derivation, etc.
Nature of quality
control procedures
adopted (eg
standards, blanks,
duplicates, external
laboratory checks)
and whether
acceptable levels of
accuracy (ie lack of
bias) and precision
have been
established.
Sample preparation and analyses were conducted by ALS Laboratories
located at Thunder Bay and Vancouver.
Samples were dried and each sample was fine crushed to >70% passing a 2mm
screen. A 250g split was pulverised using a ring and puck system to >85%
passing 75-micron screen.
The analytical technique used for all samples initially involved a four-acid digest
followed by multi-element ICP-ES analysis producing results for base metals and
gold.
• Method OG62 for zinc,
• Method OG62 copper,
• Method FA- AA for gold,
• Method OG62 silver
Verification
of sampling
and
assaying
The verification of
significant
intersections by either
independent or
alternative company
personnel.
The use of twinned
holes.
Documentation of
primary data, data
entry procedures,
data verification,
data storage
(physical and
electronic) protocols.
Senior technical personnel from the Company (Project Geologist) collected
and inspected the samples.
Primary data were collected by employees of the Company at the project site.
All measurements and observations were recorded onto hard copy templates
and later transcribed into the Company’s digital database.
Digital data storage, verification and validation are managed by a Perth-based
data management consultant.
No adjustments or calibrations have been made to any assay data.

Page 9

P01 Collar drill hole collar location was surveyed by Christina Burk of Superior
Survey Inc.
Drill collar AZ 291-12-16, 5424063.761N, 471530.525E and at an EL 421.900.

This drilling program is for exploration purposes and spaced up to 50m from the
nearest historic lode intersection.
On completion of the program, the data spacing and distribution will be
sufficient to establish the degree of geological and grade continuity
appropriate for Mineral Resource and Ore Reserve estimation procedures.
No sample compositing has been applied.
The mineralised zone comprises a steeply dipping planar body of massive
sulphide mineralisation. The drillholes intersect with the mineralisation at a high
angle such that drillhole intercepts are almost equivalent to true width.
However, the necessary corrections are applied to achieve true width
intercepts.
No sampling bias is believed to have been introduced.
Discuss any
adjustment to assay
data.
Location of
data points
Accuracy and
quality of surveys
used to locate drill
holes (collar and
down-hole surveys),
trenches, mine
workings and other
locations used in
Mineral Resource
estimation.
Specification of the
grid system used.
Quality and
adequacy of
topographic control.
P01 Collar drill hole collar location was surveyed by Christina Burk of Superior
Survey Inc.
Drill collar AZ 291-12-16, 5424063.761N, 471530.525E and at an EL 421.900.
Data
spacing
and
distribution
Whether the data
spacing and
distribution is
sufficient to establish
the degree of
geological and
grade continuity
appropriate for the
Mineral Resource
and Ore Reserve
estimation
procedure(s) and
classifications
applied.
Whether sample
compositing has
been applied.
This drilling program is for exploration purposes and spaced up to 50m from the
nearest historic lode intersection.
On completion of the program, the data spacing and distribution will be
sufficient to establish the degree of geological and grade continuity
appropriate for Mineral Resource and Ore Reserve estimation procedures.
No sample compositing has been applied.
Orientation
of data in
relation to
geological
structure
Whether the
orientation of
sampling achieves
unbiased sampling of
possible structures
and the extent to
which this is known,
considering the
deposit type.
If the relationship
between the drilling
orientation and the
orientation of key
mineralised structures
is considered to have
introduced a
sampling bias, this
should be assessed
The mineralised zone comprises a steeply dipping planar body of massive
sulphide mineralisation. The drillholes intersect with the mineralisation at a high
angle such that drillhole intercepts are almost equivalent to true width.
However, the necessary corrections are applied to achieve true width
intercepts.
No sampling bias is believed to have been introduced.

Page 10

Assay samples were placed in poly sample bags, each with a uniquely
numbered ticket stub from a sample ticket book. Sample bags were marked
with the same sample number and sealed with a plastic cable tie.
Company personnel delivered the sample bags directly to ALS Laboratories for
samplepreparation and analysis.
All digital data is subject to audit by the independent data manager.
and reported if
material.
Sample
Security
The measures taken
to ensure sample
security.
Assay samples were placed in poly sample bags, each with a uniquely
numbered ticket stub from a sample ticket book. Sample bags were marked
with the same sample number and sealed with a plastic cable tie.
Company personnel delivered the sample bags directly to ALS Laboratories for
samplepreparation and analysis.
Audits or
reviews
The results of any
audits or reviews of
sampling techniques
and data.
All digital data is subject to audit by the independent data manager.

Page 11

Section 2 Reporting of Exploration Results

Criteria Explanation Commentary
Mineral
tenement
and land
tenure status
Type, reference
name/number,
location and
ownership
including
agreements or
material issues
with third parties
such as joint
ventures,
partnerships,
overriding
royalties, native
title interests,
historical sites,
wilderness or
national park and
environmental
settings.
The Pick Lake Project comprises 297 claim units (each claim unit is 400mx400m or
16Ha in area) totalling 47.5km2. The claims are made up of a number of claims
acquired in August 2016 and claims recently staked and registered in October 2017.
The total of all claim areas is >17,000Ha. Superior is the legal and beneficial owner of
70% of the issue capital of Ophiolite Holdings Pty Ltd (ACN 617 182 966) (Ophiolite).
Ophiolite is a proprietary exploration company and is the legal and beneficial owner
of the zinc and copper prospective “Pick Lake Project”, located in Ontario. Please
see ASX announcement dated 6 December 2017. Superior Lake currently has an
option over the Winston Lake project claims. These claims are owned by FQM. For
further details please refer to ASX announcement dated 21st February 2018.
The security of
the tenure held
at the time of
reporting along
with any known
impediments to
obtaining a
licence to
operate in the
area.
The claims are in good standing.
Exploration
done by
other parties
Acknowledgment
and appraisal of
exploration by
other parties.
The Pick Lake deposit was discovered in 1983 and the Winston Lake deposit was
discovered in 1982. The Pick Lake and Winston Lake project areas have been the
subject of a variety of exploration campaigns. Some of the previous explorers include
Zenamc Metal Mines Limited, Falconbridge Copper Corporation, Minnova, Inmet
Mining, Noranda, and Silvore Fox. Please refer report filed on SEDAR for further details
- Independent Technical Report on the Pick Lake Property, Pays Plat Lake and Rope
Lake Area, Ontario, Canada, dated June 19, 2013 prepared by Bruno Turcotte, MSc,
P. Geo and Remi Verschelden, BSc, P. Geo (filed June 21, 2013 on SEDAR). This report
can be accessed via the url: http://www.sedar.com under the company name
“Silvore Fox”.
Geology Deposit type,
geological setting
and style of
mineralisation
The Pick Lake deposit occurs at the extreme western edge of the Winston-Big Duck
Lake sequence of volcanic rocks, approximately 35 metres above a granitic
contact. Aeromagnetics within the Project area depicts a distinctive V shaped
sequence of magnetic and non-magnetic units converging to a northern “V” apex
and appears remarkably similar to the aeromagnetic character of the older
Archean Warriedar Fold Belt in Western Australia which hosts the Golden Grove VMS
deposits. The Pick Lake deposit occurs as a large sheet like zone of massive sulphides
within a series of bedded pyroclastic rocks. Hydrothermal alteration exists in both
footwall and hangingwall rocks resulting in varying assemblages of quartz, cordierite,
biotite, anthophyllite, garnet, chlorite and sericite with minor disseminated sulphides.
The hydrothermal alteration zone appears to be spatially related to the Winston Lake
deposit; recent structural mapping provides evidence that Pick Lake and Winston

Page 12

==> picture [595 x 124] intentionally omitted <==

----- Start of picture text -----

Lake are hosted within the same stratigraphic horizon. The Anderson showing,
----- End of picture text -----

Lake are hosted within the same stratigraphic horizon. The Anderson showing, located near the southeast shore of Winston Lake, appears to be the surface expression of the Pick Lake deposit. This is a rusty pyritic weakly altered series of bimodal volcanics. Massive sulphides of the Pick Lake deposit occur from approximately 300m to 1200m vertically and over a strike length averaging 250 metres. The lower portion of the deposit appears to increase in strike length to approximately 500 metres. The deposit strikes at 20 degrees and dips to the east at 50 degrees. The thickness of the deposit is generally between 2 and 4m, however, locally it is up to 14 metres in width. Sulphide mineralisation is generally very consistent, composed of a fine-grained mixture of sphalerite (50-80%) and pyrrhotite (5-35%) with minor chalcopyrite (0-5%) and pyrite (0-3%). Commonly contained within the sulphides is up to 5% transparent rounded quartz inclusions up to 3mm in size as well as rare (1-3%) sub-rounded biotitic volcanic inclusions. The contacts to the deposit are typically knife sharp and commonly show the presence of minor amounts of silica.

The Winston Lake deposit lies at the top of the Winston Lake sequence within cherty exhalite and altered felsic-to-intermediate laminated ash tuff. In places, gabbro forms the hanging wall for the deposit. The footwall consists of altered mafic flow rocks and felsic-to-intermediate volcaniclastic rocks which are underlain by altered quartz and feldspar porphyritic rhyolite and feldspar pyritic basalt with intercalated sulphide-rich, bedded, tuffaceous rocks which, in turn, are underlain by the "Main" quartz fledspar porphyry which is intruded by gabbro and pyroxenite. Hydrothermal alteration, confined to the Winston Lake sequence, and later metamorphism of altered rock have resulted in spectacular assemblages of cordierite, anthophyllite, biotite, garnet, sillimanite, staurolite, muscovite and quartz coincident with an increase in iron, magnesium, and potassium and a decrease in sodium and calcium. Zinc content is directly proportional to the intensity of alteration. High copper values occur at the flanks and top of the alteration "pipe" with the core of the pipe containing relatively depleted copper values. The most common forms of ore are finely banded sphalerite and pyrrhotite and massive-to-coarsely banded sphalerite and pyrrhotite with minor pyrite and chalcopyrite and up to 45% of sub-angular mafic and felsic fragments averaging 3cm in diameter. The north-striking and 50 degrees eastwardly dipping deposit has a strike length of 750m and width of 350m. It has an average true thickness of 6m and is open to depth.

Drill hole A summary of all
Information information Hole ID East North RL Length Azimuth Dip Dip
material to the (collar) (intersection)
understanding of PL-18-01 471530 542064 10422 879 290 -86.7 -75.75
the exploration
results including a
tabulation of the
following
information for all
Material drill
holes:
easting and
northing of the
drill hole collar
elevation or RL
(Reduced Level –
elevation above
sea level in
metres) of the drill
hole collar dip
and azimuth of
the hole down
hole length and
interception

Page 13

Intercept grades are length weighted.
No cut-off grades have been used.
Downhole intercepts and true widths have been reported.
Refer to body of announcement for figures.
Assay results for significant intercepts have been tabulated in Appendix 1.
depth hole
length.
Data
aggregation
methods
In reporting
Exploration
Results, weighting
averaging
techniques,
maximum and/or
minimum grade
truncations (eg
cutting of high
grades) and cut-
off grades are
usually Material
and should be
stated
Intercept grades are length weighted.
No cut-off grades have been used.
Relationship
between
mineralisation
widths and
intercept
lengths
These
relationships are
particularly
important in the
reporting of
Exploration
Results.
If the geometry of
the mineralisation
with respect to
the drill hole
angle is known, its
nature should be
reported.
If it is not known
and only the
down hole
lengths are
reported, there
should be a clear
statement to this
effect (eg ‘down
hole length, true
width not
known’).
Downhole intercepts and true widths have been reported.
Diagrams Refer to body of announcement for figures.
Balanced
reporting
Where
comprehensive
reporting of all
Exploration
Results is not
practicable,
representative
reporting of both
low and high
grades and/or
widths should be
practiced to
avoidmisleading
Assay results for significant intercepts have been tabulated in Appendix 1.

Page 14

Exploration activities carried out by other parties include surface geochemistry,
drilling, surface geology mapping, VTEM, structural mapping.
Refer to the report filed on SEDAR for further details - Independent Technical Report
on the Pick Lake Property, Pays Plat Lake and Rope Lake Area, Ontario, Canada,
dated June 19, 2013 prepared by Bruno Turcotte, MSc, P. Geo and Remi
Verschelden, BSc, P. Geo (filed June 21, 2013 on SEDAR). This report can be
accessed via the url: http://www.sedar.com under the company name “Silvore Fox”.
The following work is planned for the Pick Lake Project:

Downhole geophysics

Surface TEM geophysics
reporting of
Exploration
Results.
Other
substantive
exploration
data
Other exploration
data, if
meaningful and
material, should
be reported
including (but not
limited to):
geological
observations;
geophysical
survey results;
geochemical
survey results;
bulk samples –
size and method
of treatment;
metallurgical test
results; bulk
density,
groundwater,
geotechnical
and rock
characteristics;
potential
deleterious or
contaminating
substances.
Exploration activities carried out by other parties include surface geochemistry,
drilling, surface geology mapping, VTEM, structural mapping.
Refer to the report filed on SEDAR for further details - Independent Technical Report
on the Pick Lake Property, Pays Plat Lake and Rope Lake Area, Ontario, Canada,
dated June 19, 2013 prepared by Bruno Turcotte, MSc, P. Geo and Remi
Verschelden, BSc, P. Geo (filed June 21, 2013 on SEDAR). This report can be
accessed via the url: http://www.sedar.com under the company name “Silvore Fox”.
Further work The nature and
scale of planned
further work (eg
tests for lateral
extensions or
depth extensions
or large-scale
step-out drilling).
The following work is planned for the Pick Lake Project:

Downhole geophysics

Surface TEM geophysics

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