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GALILEO MINING LTD Investor Presentation 2019

May 27, 2019

64962_rns_2019-05-27_e9e74371-bee0-4dae-923d-dae083cd1720.pdf

Investor Presentation

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28 May 2019 ASX: GAL

HIGH GRADE COPPER AT NORSEMAN PROJECT

Corporate Directory

Directors

Non-Executive Chairman Simon Jenkins

Managing Director Brad Underwood

Technical Director Noel O’Brien

Fast Facts

Fast Facts
Issued Shares 120.4m
Share Price $0.17
Market Cap $20.5m
Cash (31/03/19) $8.0m

Projects Norseman Project Fraser Range Nickel Project

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Contact Details

T: +61 8 9463 0063 E: [email protected] W: www.galileomining.com.au

Highlights

  • Assays from surface sampling return maximum value of 19.9% copper

  • Historic prospecting shaft and pits with small scale production recorded of 13 tonnes @ 8.36% copper[(1)]

  • Potential for significant Volcanic Massive Sulphide (VMS) copper mineralisation exists over two kilometres of strike length

  • Ground electro-magnetic (EM) surveying is planned to define targets prior to drill testing

Galileo Mining Ltd (ASX: GAL, “Galileo” or the “Company”) is pleased to announce surface sampling results from the new Subzero copper prospect at the Company’s 100% owned Norseman Project.

High grade copper oxide samples with up to 19.9% copper, and multiple iron rich gossan samples up to 1.1% copper, were recorded from a zone of outcrop centred around the historic workings. Further prospectivity exists to the north and south in the same rock unit over a 2-kilometre strike length, and to the west where the same prospective host rock occurs under shallow cover material.

Galileo Mining Managing Director Brad Underwood commented; “ This is a fantastic result from initial work carried out by the Company based on our inhouse prospectivity analysis of mineral potential at Galileo’s Norseman Project.”

Figure 1 –Oxide breccia sample with 6.5% copper & 0.8 ppm gold (CWRK013)

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(1) Refer to the GSWA 250k Norseman Map Sheet Explanatory Notes,1973 accessible at www.dmirs.wa.gov.au

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“Our recently completed ultra-detailed magnetic survey has allowed us to undertake a geological interpretation of the area not possible by previous explorers. In doing so we have uncovered historic copper prospects that were last looked at in the 1970’s.

“We will now focus on building up the prospects to drill ready status through the use of modern electromagnetic (EM) surveying methods aimed at identifying significant sub-surface copper mineralisation.”

The surface samples recorded were taken from a volcano-sedimentary rock unit where it outcrops. This rock unit can be traced for over two kilometres and also occurs to the west where it is covered by shallow alluvial sediments. The best samples relate to an area named the Subzero prospect adjacent to a historic shaft and prospecting pits (Figs 2 & 3). Small scale production from the historic workings was registered in 1953 with approximately 13 tonnes of ore extracted at an average grade of 8.36% copper. Regulatory issues at the time prevented the grant of a mine lease and no further work was recorded at the prospect.

Work completed in 1971 by Barrier Exploration at the Cowan West prospect 1.3km to the southwest of Subzero (Figure 4) identified layers of volcanic material, including tuff and agglomerate, in diamond core drilling[(2)] . No other work was conducted and Barrier’s attention returned to nickel exploration on their other tenements. The area around Cowan West is covered by shallow alluvial material which prevents traditional prospecting techniques. Galileo’s detailed magnetic survey, combined with the historic drilling, has allowed the definition of the prospective volcanic unit which can now be targeted by ground EM looking to identify mineralisation not visible on surface.

Figure 2 – Historic prospecting shaft. A copper oxide sample from beside the shaft returned a copper assay of 19.9% (JM013341).

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(2) Refer to the Barrier Exploration Annual Report on Cowan West Claim Group B, 1971 accessible at www.dmirs.wa.gov.au

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The high-grade copper samples relate to an area of outcrop of approximately 80 metre strike length centred around the historic shaft and pits (Figure 3). North and south of the outcrop area the contact zone between the volcanic/sediments and the gabbro intermittently outcrops. The strike length of the prospective zone around Subzero is estimated at 2 kilometres based on magnetic interpretation and on ground prospecting. A ground EM survey to cover the entire strike length has been planned with the intention of defining subsurface conductors related to copper mineralisation.

Figure 3 – Subzero Prospect plan view of high-grade copper samples around historic workings.

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Regional copper prospectivity has been demonstrated by the historic work at the Cowan West prospect. Volcanic material of the type frequently associated with VMS copper mineralisation has been identified and the prospective zone occurs over an area of 2.4km strike by 0.6km width (Figure 4). The ground EM survey targeting the Subzero prospect will also cover the extent of the prospective rock units associated with the Cowan West prospect.

Figure 4 – Regional geology map of prospective volcanic rock units and copper sampling. The western volcanic unit is under shallow alluvial cover. Geological interpretation is based on GSWA mapping, detailed

magnetic surveying, prospecting, and drilling data.

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53 rock chip samples were collected, mostly from the volcanic/sediment unit which occurs between the western basalt and the eastern gabbro (see Figure 4). Rock chip locations and assays are shown below in Table 1 for samples with greater than 0.1% copper.

The volcanic-sedimentary unit, from which the high-grade copper samples were obtained, falls into the GSWA described Mount Kirk Formation. This formation is listed as “acid and basic volcanic rocks and sedimentary rocks, intruded by basic and ultrabasic rocks” and is immediately above the Woolyeenyer Formation in the Norseman Stratigraphy. The Woolyeenyer Formation is the host of the major gold deposits found around Norseman.

Iron rich gossan and copper oxide samples from the Subzero prospect display highly anomalous copper values up to 19.9% (JM013341). Petrographical description of gossan sample JM013345 recognised exsulphide cubes and a matrix of goethite for which sulphide minerals may have been the precursor . Minor remnant grains of pyrite, pyrrhotite and chalcopyrite were also identified.

Galileo considers that the surface copper mineralisation evident at the Subzero prospect indicates good potential for the presence of economic copper resources in the area. Ground EM surveying aims to define conductive drill targets to test for copper sulphide ore bodies hosted in the volcanic rock sequence.

Table 1 – Rock chip assays (0.1% copper cut-off).

SampleID Easting Northing Sample Description Au (ppb) Ag
(ppm)
Cu (%) Fe (%) Pb
(ppm)
Zn (%)
CWRK004 376,582 6,443,845 Gossan 11 0.45 0.99 31.3 386 0.64
CWRK005 376,587 6,443,843 Gossan 4 1.72 1.09 46.8 197 0.46
CWRK006 376,588 6,443,844 Gossan 8 2.06 0.82 28.3 170 0.35
CWRK007 376,595 6,443,839 Altered basalt/sediment 12 0.5 0.10 5.8 56 0.03
CWRK008 376,604 6,443,830 Copper oxide breccia 25 0.61 3.71 11.4 184 0.17
CWRK013 376,585 6,443,832 Copper oxide breccia 811 4.29 6.53 20.3 311 0.07
CWRK017 376,624 6,443,962 Altered basalt/sediment 9 0.7 0.11 13.2 25 0.02
CWRK022 376,659 6,444,374 Altered basalt/sediment 3 4.19 0.10 4.7 37 0.02
CWRK026 376,591 6,443,809 Gossan 6 3.4 0.30 33.2 129 0.20
CWRK027 376,603 6,443,582 Altered basalt/sediment 8 0.09 0.22 13.3 156 0.01
JM013337 376,595 6,443,823 Gossan 6 10.75 0.21 40.8 115 0.30
JM013338 376,594 6,443,839 Gossan 34 0.32 1.06 33.8 190 0.35
JM013339 376,587 6,443,846 Gossan 3 0.51 0.97 33.9 347 0.31
JM013340 376,605 6,443,853 Altered basalt/sediment 11 1.36 0.37 14.8 270 0.65
JM013341 376,594 6,443,876 Copper oxide breccia 48 33.85 19.86 10.6 206 0.09
JM013342 376,600 6,443,911 Altered basalt/sediment 8 1.21 0.10 16.8 61 0.04
JM013345 376,593 6,443,797 Gossan 5 0.62 0.12 33.3 82 0.15

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Competent Person Statement

The information in this report that relates to Exploration Results is based on information compiled by Mr Brad Underwood, a Member of the Australasian Institute of Mining and Metallurgy, and a full time employee of Galileo Mining Ltd. Mr Underwood has sufficient experience that is relevant to the styles of mineralisation and types of deposit under consideration, and to the activity being undertaken, 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” (JORC Code). Mr Underwood consents to the inclusion in the report of the matters based on his information in the form and context in which it appears.

Investor information: phone Galileo Mining on + 61 8 9463 0063 or email [email protected]

Media: David Tasker Managing Director Chapter One Advisors E: [email protected] T: +61 433 112 936

About Galileo Mining:

Galileo Mining Ltd (ASX: GAL) is focussed on the exploration and development of cobalt and nickel resources in Western Australia. GAL holds tenements near Norseman with over 26,000 tonnes of contained cobalt, and 122,000 tonnes of contained nickel, in JORC compliant resources (see Figure 5 below). GAL also has Joint Ventures with the Creasy Group over tenements in the Fraser Range which are highly prospective for nickelcopper-cobalt sulphide deposits.

Figure 5: JORC Mineral Resource Estimates for the Norseman Cobalt Project (“Estimates”) (refer to ASX “Prospectus” announcement dated May 25[th] 2018 and ASX announcement dated 11[th] December 2018, accessible at http://www.galileomining.com.au/investors/asx-announcements/). Galileo confirms that all material assumptions and technical parameters underpinning the Estimates continue to apply and have not materially changed).

Cut-off
Cobalt %
Class Tonnes Mt Co Ni
% Tonnes % Tonnes
MT THIRSTY SILL
0.06 % Indicated
Inferred
Total
10.5
2.0
12.5
0.12
0.11
0.11
12,100
2,200
14,300
0.58
0.51
0.57
60,800
10,200
71,100
MISSION SILL
0.06 % Inferred 7.7 0.11 8,200 0.45 35,000
GOBLIN
0.06 % Inferred 4.9 0.08 4,100 0.36 16,400
TOTAL JORC COMPLIANT RESOURCES
0.06 % Total 25.1 0.11 26,600 0.49 122,500

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Appendix 1:

Galileo Mining Ltd – Norseman Cobalt Project JORC Code, 2012 Edition – Table 1 report template

Section 1 Sampling Techniques and Data

(Criteria in this section apply to all succeeding sections.)

Criteria JORC Code 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.
Include reference to measures taken to ensure
sample representivity and the appropriate
calibration of any measurement tools or
systems used.
Aspects of the determination of mineralisation
that are Material to the Public Report.
In cases where ‘industry standard’ work has
been done this would be relatively simple (eg
‘reverse circulation drilling was used to obtain 1
m samples from which 3 kg was pulverised to
produce a 30 g charge for fire assay’). In other
cases more explanation may be required, such
as where there is coarse gold that has inherent
sampling problems. Unusual commodities or
mineralisation types (eg submarine nodules)
may warrant disclosure of detailed information.
•The rock chip samples reported were
collected in 2019 with sample
numbers, locality information and
descriptions recorded by employees of
Galileo Mining Ltd.
•Each sample represents a spot
location from the area prospected and
is not intended to represent a
quantitative determination of copper at
the prospect. Drilling will be required to
determine in-ground representative
grade and thickness distributions.
•Sample weights ranged from 0.4kg to
1.5kg.
•QAQC standards (blank & reference)
were included routinely with 1 per 50
samples being a standard or duplicate.
•Samples were sent to an independent
commercial assay laboratory.
•All assay sample preparation
comprised oven drying, jaw crushing,
pulverising and splitting to a
representative assay charge pulp.
•A four acid digest was used for a multi-
element analysis suite including Ag, Al,
As, Ba, Be, Bi, Ca, Cd, Ce, Co, Cr, Cs,
Cu, Fe, Ga, Ge, Hf, In, K, Li, Mg, Mn,
Mo, Na, Nb, Ni, P, Pb, Rb, Re, S, Sb,
Sc, Se, Sn, Sr, Ta, Te, Th, Ti, Tl, U, V,
W, Y, Zn, Zr by ICP-MS or ICP-OES
for all samples.
•High grade copper (>2.0% Cu) was
analysed using an ore grade 4 acid
digest
•A 50g Lead Collection Fire Assay with
ICP-MS was used to determine Au, Pt
andPdresults
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 ifso, by what method, etc). _
•Not applicable
Drill sample
recovery
Method of recording and assessing core and
chip sample recoveries and results assessed.
Measures taken to maximise sample recovery
and ensure representative nature of the
•Not applicable.

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Criteria JORC Code explanation Commentary
samples.
Whether a relationship exists between sample
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. _
•Rock chips were logged in the field
and checked in the office.
•Logging is mostly qualitative in nature
except for one sample (JM013345)
which was sent for petrographic
analysis.
Sub-sampling
techniques
and sample
preparation
If core, whether cut or sawn and whether
quarter, half or all core taken.
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 situ material collected,
including for instance results for field
duplicate/second-half sampling.
Whether sample sizes are appropriate to the
_grainsize of the material being sampled. _
•Not applicable.
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. _
•QAQC standards and blanks were
routinely included at a rate of 1 per 50
samples.
•Further internal laboratory QAQC
procedures included internal batch
standards and blanks
•Sample preparation was completed at
Intertek Genalysis Laboratory,
(Kalgoorlie) with digest and assays
conducted by Intertek Genalysis
Laboratory Services (Perth) using a
four-acid digest for multi-element
analyses and a fire assay for Au, Pt, &
Pd.
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.
• _Discuss any adjustment to assay data. _
•Field data is collected on site using a
standard set of logging templates and
entered into a laptop. Data is then sent
to the Galileo database manager (CSA
Global - Perth) for validation and
upload into the database.
•Verification of sample locations was
completed in the field.

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Criteria JORC Code explanation Commentary
•Assays are as reported from the
laboratory and stored in the Company
database and have been rounded to
two decimalplaces.
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.
•Sample locations were surveyed with a
handheld GPS with an accuracy of +/-
5m which is considered sufficient for
sample location accuracy.
•Co-ordinates are in MGA94 datum,
zone 51.
•Topographic control has an accuracy
of 2m based on detailed satellite
imagery derivedDTM.
Data spacing
and
distribution
Data spacing for reporting of Exploration
Results.
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. _
•Sampling
was
completed
where
outcrop exists
•Data spacing and distribution is not
sufficient to establish geological and
grade continuity.
•Drilling will be required to determine
whether a Mineral Resource exists at
the prospect
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 and reported if material.
•Rock chip spot sampling was limited
by the extent of outcrop and as such is
biased by the occurrence of outcrop.
•Structural controls on mineralisation
have yet to be determined
•No drilling has yet been undertaken
Sample
security
The measures taken to ensure sample security. •Each sample was put into a tied off
calico bag and then several placed in a
large plastic “polyweave” bag which
was zip tied closed.
•Samples were delivered directly to the
laboratory in Kalgoorlie by Galileo
employees or to the laboratory in Perth
by Galileo’sfreight contractor.
Audits or
reviews
The results of any audits or reviews of sampling
techniques and data.
•Continuous improvement reviews of
sampling techniques and procedures
are ongoing. No external audits have
beenperformed.

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Section 2 Reporting of Exploration Results

(Criteria listed in the preceding section also apply to this section.)


(Criteria listed in

the preceding section also apply to this section.)
Criteria JORC Code 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 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 Norseman Project comprises two
granted exploration licenses and
eighteen granted prospecting licenses
covering 278km2, and one Mining
Lease Application covering 6.54 km2
•All tenements within the Norseman
Project are 100% owned by Galileo
Mining Ltd.
•The Norseman Project is centred
around a location approximately 10km
north-west of Norseman on vacant
crown land.
•All tenements in the Norseman Cobalt
Project are 100% covered by the
Ngadju Native Title Determined Claim.
•The tenements are in good standing
and there arenoknown impediments.
Exploration
done by other
parties
Acknowledgment and appraisal of exploration by
other parties.
•Barrier Exploration completed three
diamond drill holes at the Cowan West
VMS prospect in 1971
•The GSWA 250k Norseman Map Sheet
Explanatory Notes records that 13
metric tonnes of ore were produced
from the pits and shaft at the Subzero
prospect in 1953. Average ore grade
was 8.36% copper.
Geology Deposit type, geological setting and style of
mineralisation.
•The target geology and mineralisation
style is volcanic hosted massive
sulphide (VHMS) mineralisation
occurring within the GSWA mapped
Mount Kirk Formation
•The Mount Kirk formation is described
as “Acid and basic volcanic rocks and
sedimentary rocks, intruded by basic
and ultrabasic rocks”
Drill hole
Information
A summary of all information material to the
understanding of the exploration results
including a tabulation of the following information
for all Material drill holes:
o easting and northing of the drill hole collar
o elevation or RL (Reduced Level – elevation
above sea level in metres) of the drill hole
collar
o dip and azimuth of the hole
o down hole length and interception depth
o hole length.
If the exclusion of this information is justified on
the basis that the information is not Material and
this exclusion does not detract from the
understanding of the report, the Competent
Person should clearly explain why this is the
_case. _
•No drilling reported

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Criteria JORC Code explanation Commentary
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.
Where aggregate intercepts incorporate short
lengths of high-grade results and longer lengths
of low grade results, the procedure used for
such aggregation should be stated and some
typical examples of such aggregations should be
shown in detail.
The assumptions used for any reporting of metal
_equivalent values should be clearly stated. _
•No weighted averaging has been used
•Assays are reported as returned from
the laboratory
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’). _
•No drilling completed
•The mineralisation occurs on surface
with a general strike of 010° similar to
the host rock
•Geometry from surface outcrop is best
described as sub-vertical however no
reliable quantitative measurements
exist.
Diagrams Appropriate maps and sections (with scales) and
tabulations of intercepts should be included for
any significant discovery being reported These
should include, but not be limited to a plan view
of drill hole collar locations and appropriate
_sectional views. _
•Plan map of the general prospect area
and detailed location plan map with
high grade samples has been included
along with accurate hand-held GPS
sample locations (Garmin GPS 78s) +/-
5m in X/Y/Zdimensions.
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
avoid misleading reporting of Exploration
_Results. _
•All significant results are reported.
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.
•Detailed 50m line spaced aeromagnetic
data has been used for interpretation of
underlying geology. Data was collected
by Magspec Airborne Surveys Pty Ltd
using a Geometrics G-823 caesium
vapor magnetometer at an average
flying height of 30m.
•Petrography was undertaken by R.N.
England Consulting Geologist.
Further work The nature and scale of planned further work
(eg tests for lateral extensions or depth
extensions or large-scale step-out drilling).
Diagrams clearly highlighting the areas of
possible extensions, including the main
geological interpretations and future drilling
areas, provided this information is not
_commercially sensitive. _
•Detailed moving loop electro-magnetic
(MLEM) surveying has been planned to
cover the extent of the prospective rock
units
•Drilling will be undertaken using MLEM
results, rock chip samples, and
mapping to target potentially economic
mineralisation

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