Exploration Update for Golden Pike Project
Released
Released
Announcement PDF
Albright Metals Limited
191B Carr Place
Leederville, WA 6007
Phone: +61 8 9321 0001
Email: info@albrightmetals.com
ASX: ABR
ABN: 59 616 795 245
A S X A N N O U N C E M E N T
26 OCTOBER 2026
Exploration Update for Golden Pike Project
HIGHLIGHTS
• Exploration review of Golden Pike Project highlights Grant Brook and
Albright Brook potential for additional gold mineralisation.
• Albright Brook and Bond Road prospective for further antimony
mineralisation, with the Henderson Settlement Prospect also identified with
highly anomalous antimony surface geochemistry.
• 2026 rock chip samples from Grant Brook Prospect returned gold results:
o Sample 2306350 – 2.68 g/t Au
o Sample 2306351 – 0.35 g/t Au
o Sample 2306352 – 0.99 g/t Au, 1.45 g/t Ag and 0.38% Cu
• 2026 rock samples at Daley Brook Prospect on the Taylor Brook Fault
returned highly anomalous copper, lead, zinc, silver and/or molybdenum
results:
o Sample 2306331 – 3.19 g/t Ag, 13,800ppm (1.38%) Cu and 79.2ppm Mo
o Sample 2306332 – 1.18 g/t Ag, 887ppm Cu and 384ppm Mo
o Sample 2306357 – 1.85 g/t Ag, 20,800ppm (2.08%) Pb and 4,020ppm (0.4%) Zn
• Analysis of rock sample datasets has identified distinct mineral fields within
the Golden Pike Project, including gold-copper, gold-antimony and copper-
molybdenum targets.
• New Mineral Claims added to Albright Metals’ New Brunswick portfolio, with
expanded Golden Pike Project and addition of Winding Hill Project.
Albright Metals Limited (“Albright Metals” or “the Company”) provides an
exploration update on the Golden Pike Project and newly acquired Winding Hill
Project.
CEO, Greg Hill comments, “Our strategy is to maintain an active exploration
program alongside our high-grade Vail Road gold development project. Work
completed by our technical team has identified several new exploration
prospects at Golden Pike and on our newly acquired claims, which provide the
Company with a strong pipeline of exploration opportunities. This work has
significantly improved our understanding of the project area, with copper and
molybdenum areas of interest now also identified. I am looking forward to drill
testing these targets once detailed planning and prioritising has been
completed.”
ASX: ABR | albrightmetals.com 2
Albright Metals has secured additional high-quality land area for exploration
through Mineral Claim staking, in parallel with advancing the Vail Road Gold
Deposit towards a development pathway. Furthermore, significant progress has
been made reviewing new and historical datasets for the Golden Pike Project, to
target the next phase of exploration planned for the 2027 calendar year. Two high-
priority gold exploration targets at the Golden Pike Project are the Grant Brook
trend, just north of the Taylor Brook Fault and the Albright Brook Prospect, where
drilling by Albright Metals and previous companies has intercepted broad zones
of gold mineralisation with discrete internal antimony veins.1
Figure 1 shows the location of the Albright Metals’ projects in New Brunswick,
Canada. The proximity of the Golden Pike and Winding Hill Projects to excellent
road, port and rail provides infrastructure giving optionality for any development
opportunities.
Figure 1: Albright Metals Project Locations – New Brunswick, Canada
1
ASX announcement dated 25 June 2026 “Gold and Antimony Mineralisation Confirmed and Extended”
ASX: ABR | albrightmetals.com 3
Golden Pike Project
New Claims
Albright Metals has increased the size of the Golden Pike Project by staking
Mineral Claims north and south of Mineral Claim (MC) 7616, which is under option
by Albright Metals from Globex Mining Enterprises.2
The new claims, held solely by
Albright Metals, increase the Golden Pike Project area to approximately 5,277ha,
adding important land access extension over prospective geology for gold,
antimony, transition and base metal mineralisation. MC12123 in the north covers
Annidale Belt lithologies and MC12303 extends over New River Belt lithologies in
the south. The Vail Road Gold Deposit hosts a current Indicated and Inferred
Mineral Resource of 188kt at 9.0 g/t Au3
within Grant Brook Formation lithologies
of the New River Belt, located within MC7616. Figure 2 shows the Golden Pike
Project, with existing prospects by type.
Figure 2: Golden Pike Project Mineral Claims and Prospects
2
ASX announcement dated 21 May 2025 ‘Acquisition of Advanced High-Grade Gold Project’
3
ASX announcement dated 29 September 2026 “Mineral Resource Update for Vail Road Gold Deposit”
ASX: ABR | albrightmetals.com 4
Prospectivity Mapping – Defines Distinct Mineral Field
In late June to early July 2026, a program of prospecting was undertaken to
investigate areas of gold and antimony soil anomalism identified during work
programs executed by Rockport and Globex between 2010 and 2017.
Albright Metals has classified the project-wide rock sample dataset (including
2026 sample results) into mineral prospectivity groups using statistical analysis of
13 elements, being gold (Au), silver (Ag), arsenic (As), antimony (Sb), bismuth (Bi),
tellurium (Te), tungsten (W), copper (Cu), molybdenum (Mo), lead (Pb), zinc (Zn),
cadmium (Cd) and sulphur (S). Mineral prospectivity mapping for the rock sample
dataset is shown in Figure 3, with clear definition of distinct metal zonation.
Figure 3: Rock Sample Mineral Prospectivity Mapping at the Golden Pike Project
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The mineral prospectivity classification identifies clusters of rock samples with the
same metal associations, being:
• Au-Cu affinity at Vail Road Gold Deposit and Grant Brook Trend
• Au-Sb-As affinity at Bond Road, Albright Brook and Henderson Settlement
Prospects
• Cu-Mo-Bi-Te affinity on the Taylor Brook Fault at Daley Brook Prospect
(formerly Devil’s Pike Northwest)
Zn-Pb-Ag +/- Cu affinity groups shown in Figure 3 are the most dispersed, being
common in sediments of the Carpenter Brook Formation and rhyolite units of the
Bald Hill Formation in the Annidale Belt. There is preferred location for
accumulation of elevated base metals and silver at lithological contacts where
rheology contrasts provide pathways for fluid movement and some of the samples
in this category are concentrated at the Grant Brook Central area, where gold-
copper mineralisation in quartz veining demonstrates metal deposition.
The rock sample classification scheme applied has presented three mineralisation
styles for targeting in the next phase of exploration, being:
• Gold–copper mineralisation at Grant Brook Trend
• Antimony +/- gold mineralisation at Bond Road, Albright Brook and
Henderson Settlement Prospects
• Copper–molybdenum mineralisation potential at Daley Brook Prospect
around the Taylor Brook Fault and intersecting northwest structures, and
along the Albright Brook Fault (based on soil geochemical anomalies), with
these major crustal structures suspected to be hydrothermal fluid conduits.
Grant Brook Gold Trend Exploration
The Grant Brook Gold Trend consists of three prospect areas extending over a
1.5km strike distance, north of the Taylor Brook Fault (see Figure 3 showing three
zones of Au-Cu affinity classified rock samples defining the Grant Brook Trend).
The western end of the trend lies 400m north of the Taylor Brook Fault and the
eastern end about 200m north. The prospects form an arcuate east-west strike
roughly mimicking the orientation of the Taylor Brook Fault. At the west end, the
gold +/- copper mineralisation is associated with stockwork quartz veining with
sericite and pyrite alteration of rhyolite and metasediments of the Carpenter
Brook Formation. In the central area, the gold +/- copper mineralisation is in quartz
veining that crops out along a ridgeline, within a plagiogranite intrusion (as
mapped by the Government of New Brunswick). At the eastern extent, gold and
copper enrichment was found in sub-angular boulders of metasiltstone and
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tuffaceous graywacke with occasional boulders with quartz veining and up to 5
percent pyrite.
Previous companies at the Golden Pike Project completed rock sampling over the
entire trend and trenching at the west and east ends. At the west end, Noranda
drilled three drillholes in 1991 for 299.2m of core drilling, following up on
encouraging trenching results the previous year. The 1991 drilling was followed up
by an additional three core holes for 423.5m of drilling in 2011 by Rockport.
Grant Brook Drilling
Drilling by previous companies (Figure 4) targeted mineralisation found in
trenching by Noranda in 1990 and 1991 at the western end of the Grant Brook
Trend, which uncovered bedrock consisting of metasediments and stratiform
zones of silicified and pyrite rich mafic volcaniclastics, returning gold grades
peaking at 42.84 g/t Au in the northern most end of trench ANN-90-8EXT, which
was an extension of a trench that initially ended at a mineralised float sample
adjacent to bedrock in the trench floor, with the float sample grading 8.0 g/t Au.
The holes drilled by Noranda in 1991 returned a down hole width intercept of:
• AN-91-3: 5.6m at 1.82 g/t Au from 8.5m, including 2.1m at 2.68 g/t Au from
9.9m
Drilling by Rockport in 2011 returned best down hole intercepts of:
• DPN-11-01: 3.0m at 1.53 g/t Au from 14.5m
• DPN-11-05: 9.55m at 0.42 g/t Au from 63.6m, including 0.55m at 1.26 g/t Au
from 71.2m
Noranda and Rockport also drilled two holes north of the Grant Brook Trend near
Henderson Settlement (AN-91-4 and DPN-11-04) and Rockport drilled one hole to
the northwest of Grant Brook, targeting a geophysical anomaly. Only two modest
intercepts over one sample width at around 0.5 g/t Au were returned from the
Henderson Settlement drill holes and no significant intercept from the hole to the
northwest (DPN-11-03).
The drill hole location details, a full intercept table at 0.4 g/t Au cut-off from the
drill campaigns and sectional view of AN-91-3 and DPN-11-01 is provided in
Appendix 2: Historical drilling.
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Figure 4: Gold Results from Drilling and Rock Sampling at Grant Brook
Grant Brook Central Rock Samples
During Albright Metals’ prospecting, three rock chip samples were collected at the
Grant Brook Central showing over a 150m long east-west trending ridgeline from
quartz vein boulders (east end) and outcropping quartz veining (west end and
middle of ridge), with the three samples returning:
• Sample 2306350 – 2.68 g/t Au
• Sample 2306351 – 0.35 g/t Au
• Sample 2306352 – 0.99 g/t Au, 1.45 g/t Ag and 0.38% Cu
These new rock chip results (shown on Figure 5 below) follow on from existing
historical rock samples at the central area, with best previous results being:
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• 2006 – Sample GBW10101 – 10.9 g/t Au;
• 2006 – Sample GBW10104 – 3.35 g/t Au;
• 2006 – Sample GBW10106 – 3.62 g/t Au;
• 2016 – Sample 11274 – 5.18 g/t Au
Figure 5: Gold Results from Rock Sampling at Central and Eastern Grant Brook
The most eastern expression of the Grant Brook Trend is within a thick glacial till
profile, with mineralisation identified in sampling of boulders in trenching by
Brunswick Mining and Smelting Corp. in 1992. Trenching was unable to uncover a
convincing base of bedrock, but the till was noted to contain abundant fragments
of bleached siltstone, likely of the Carpenter Brook Formation. Some component
of movement of the mineralised boulders is likely at the eastern end and the
glacial movement direction will need to be quantified to follow up on prospecting
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and trenching sampling of boulders. Given the western and central areas that
have surface signs of mineralisation are 100 to 200m further north of the Taylor
Brook Fault, investigation that distance up ice-movement direction at the east
end is warranted.
The Grant Brook Trend has mineralisation similar to the Vail Road Gold Deposit,
with gold being the dominant mineralisation, with some samples having copper,
zinc and lead anomalism indicating polymetallic hydrothermal fluid circulation.
Exposure of quartz veining with gold mineralisation that has already been well
sampled through rock sampling and which can be mapped at surface in the
centre of the trend, presents a drill-ready target. Work is planned in 2027 to drill
the area of mineralised quartz veining, with a focus on structural data collection
on the drill core to be able to model where the vein extends beneath cover to the
east and west, and to evaluate for structures that may control mineralisation or
cause late offsets.
Work will also be conducted on the archive drill core in storage at the Sussex Core
Facility for the 1991 Noranda and 2011 Rockport drill holes, to evaluate whether
further sampling is required.
Antimony and Gold Exploration
Albright Brook Prospect
Extensional drilling is planned at Albright Brook Prospect, targeting gold zones
intercepted in both of the holes drilled by Albright Metals in 2026,4
adding to the
drill intercepts in drilling by Rockport in 2008 and Globex in 2016.1
Figure 6 is a plan
view of the existing drilling at Albright Brook Prospect and outlines the interpreted
gold system extensions to be drill tested.
Previously released down hole width gold intercepts in Albright Metals 2026 drill
campaign at the Albright Brook Prospect are:4
• AB-26-01 – 37.05m at 1.12 g/t Au from 60.95m, including 2.35m at 4.76 g/t
Au from 77.10, and including 0.70m at 28.80 g/t Au from 85.55m
• AB-26-02 – 13.20m at 1.14 g/t Au from 62.30m, including 1.55m at 2.19 g/t Au
from 63.70m, and including 1.30m at 3.70 g/t Au from 69.60m
• AB-26-02 – 1.88m at 2.28 g/t Au from 100.62m, including 1.38m at 3.01 g/t
Au from 101.12m
• AB-26-02 – 8.25m at 0.68 g/t Au from 151.82m, including 1.10m at 1.36 g/t Au
from 152.20m, and including 1.74m at 1.13 g/t Au from 154.94m
4
ASX announcement dated 25 June 2026 ‘Gold and Antimony Mineralisation Confirmed and Extended’
ASX: ABR | albrightmetals.com 10
Down hole width antimony intercepts at Albright Brook in drilling by Albright
Metals (2026) and Globex (2016), hosted within stibnite (antimony sulphide) veins
internal to gold intercepts is:4
• AB-26-02 – 2.46m at 0.5% Sb and 1.72 g/t Au from 62.3m, including 0.36m
at 3.23% Sb and 2.81 g/t Au from 64.4m
• DPA-16-01 – 0.50m at 12.5% Sb and 0.1 g/t Au from 76.5m
• DPA-16-03 – 0.30m at 4.74% Sb and 2.38 g/t Au from 17.7m
Figure 6: Albright Brook Drilling and Gold-Antimony Extension Potential
The interpreted 400m long prospective trend at Albright Brook Prospect is shown
in Figure 6. A gold mineralisation control is interpreted to be the Cameron Road
Granite contact with the Carpenter Brook Formation sediments, with the lithology
boundary likely a faulted contact oriented north-northeast, dipping about 75
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degrees to the southeast. Gold mineralisation sits within Cameron Road Granite
close to the contact, with strong sericite alteration, brittle fracturing and quartz
stringers with pyrite-arsenopyrite sulphides. Antimony is present in dendritic to
massive stibnite-quartz veins and is noted in both Cameron Road Granite broad
gold zones (DPA-16-01 and AB-26-02), and also as stibnite-quartz veins within
Carpenter Brook Sediments (DPA-16-03). The three stibnite occurrences form a
north south trend in plan view, however the geometry, true orientation and
relationship of the antimony bearing veins to the gold mineralisation requires
further exploration.
Drill testing will focus on extending to the north-northeast along the Cameron
Road Granite interpreted faulted contact to test the size potential of the gold
system and to collect further oriented drill core to measure the orientation of
stibnite (antimony sulphide) veins within the larger gold system. The brittle nature
of the Cameron Road Granite increases opportunity for gold mineralisation
compared to the more ductile sedimentary units.
Figure 7 below is a photo of the stibnite vein intercepted in drill hole AB-26-02. The
vein is within a broader zone of gold mineralisation associated with strong sericite
alteration, fracturing, quartz stringers and sulphides in the Cameron Road Granite.
Figure 7: Core Photo of Stibnite Vein within Broader Gold Intercept in AB-26-024
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Bond Road Prospect
At Bond Road, a campaign of trenching is planned over the strongest soil
anomalies, and to the east and north of the anomalies at about 150 – 200m step
outs. Information from the trenches will include depth of till cover and the
orientation of the sedimentary till fabric, to vector the up-ice direction, in addition
to checking for shallow buried antimony mineralisation in bedrock. If no base of
till or mineralisation is found within the trenches, geophysics Induced Polarisation
(IP) surveying will be planned to remote sense additional drill targets.
The strong antimony soil anomaly, and structures and strong sericite alteration
with anomalous antimony and gold results in the 2026 Bond Road drill core4
warrant further exploration for economic antimony mineralisation at the Bond
Road Prospect.
Henderson Settlement Prospect
The antimony-gold anomalism at the Henderson Settlement Prospect requires
geophysical survey extension of the existing Rockport Induced Polarisation lines,
to target resistivity highs. Additional exploration tools are being investigated to
evaluate large areas, focussing on the northwest wrench fault interactions with
the Albright Brook Fault.
Molybdenum – Copper Potential
Strong soil anomalism along the Albright Fault has previously highlighted likely
movement of granophile elements along the deep crustal structure (see Figure 8
below for Rockport soil sample results for molybdenum along the Albright Brook
Fault). The rock sample geochemical classification also highlighting Cu-Mo-Bi-Te
enrichment in rock samples at the Daley Brook Prospect, where a northwest
wrench fault intersects the Taylor Brook Fault, increases the prospectivity of the
Annidale Belt for copper-molybdenum concentrations in secondary faults.
Cu-Mo-Bi-Te affinity was characterised in 2026 rock chip sample 2306329 located
140m south of the drilling at Albright Brook Prospect, during a traverse south to
the Bond Road Prospect along a hypothetical north-northeast trending linking
fault. The rock sample was collected from outcrop of silicified sedimentary rocks
with copper staining and stockwork quartz veining. The presence of this
anomalism provides further evidence for presence of a significant fault. Sample
2306329 returned 0.96 g/t Ag, 0.25% Cu, and 7.18 ppm Mo, with the average crustal
abundance of Mo in sediments being about 1 ppm.
The conceptual exploration model to be tested is whether a large buried granitic
batholith is a hydrothermal fluid source for economic Cu-Mo enrichment with
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fluids passing up from the intrusion along the existing structural architecture.
Albright Metals is focused on on-going compilation and analysis of the
comprehensive historical dataset, in addition to scoping geophysics, remote
sensing analysis and geochemical survey techniques to progress the exploration
potential for copper-molybdenum mineralisation to a drill ready target.
Figure 8: Molybdenum Soil Anomaly along the Albright Fault – Henderson Settlement
Winding Hill Project
Recent Government of New Brunswick glacial till sampling and associated studies
identify potential for the northeast trending Fredericton Belt to host antimony
deposits. Based on this newly identified prospectivity, Albright Metals has staked
Mineral Claim 12279, approximately 60 km north of the city of Fredericton. The
Winding Hill Project has a historical gold, silver and lead prospect of the same
name, and results from the New Brunswick Government till sampling highlight
potential for bedrock antimony mineralisation. The government sampling has
returned numerous anomalous gold and antimony results in the Winding Hill
region. On the basis of the antimony anomalism in till, and the presence of the
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historical Winding Hill gold, lead and silver prospect, Albright Metals has secured
the Winding Hill Project within an emerging antimony-gold field.
Figure 9: Winding Hill Project – Antimony Potential
Next steps
The Company is developing detailed plans for exploration activities for the
remainder of 2026 and into 2027, including drill target ranking. Drilling will be
undertaken once all planning and preparation works are completed and is subject
to permitting and availability of suitable contractors.
For further information, please contact:
Greg Hill, Chief Executive Officer
+61 8 9321 0001
albrightmetals.com
This announcement has been produced in accordance with the Company's
published continuous disclosure policy and has been approved by the Board.
ASX: ABR | albrightmetals.com 15
ABOUT ALBRIGHT METALS
Albright Metals’ projects are located in Canada and Western Australia, both Tier
One mining and exploration jurisdictions.
Albright Metals has executed an agreement with Globex Mining Enterprises Inc.
(GMX-TSX, GLBXF-OTCQX, G1MN-FSE) to acquire the Golden Pike Gold and
Antimony Project in New Brunswick, Canada.5
The project covers approximately
5,277ha of contiguous mining claims which includes the Vail Road high-grade
gold deposit and the exploration-stage Bond Road and Albright Brook antimony
and gold prospects. The Golden Pike Project is in an area that is close to road, rail,
port and grid power infrastructure. Southern New Brunswick is on the Canadian
east coast, adjacent to Maine, USA. It enjoys a mild maritime climate, allowing year
round exploration activities. The province has a mature mining services industry
and has historically produced antimony and gold from multiple mines.
Vail Road Gold Deposit 2026 Mineral Resource by Resource Category:6
Category Tonnes (kt) Au Grade (g/t) Au (Ozs) Cu (ppm)
Indicated 33.5 20.9 22,500 3,107
Inferred 154.6 6.4 31,700 1,545
TOTAL 188.0 9.0 54,200 1,823
Note: Mineral Resource reported at 2 g/t Au cut-off grade. Numbers may not add up due to
rounding; Tonnages are dry metric tonnes; Kilotonne = 1,000 tonnes; 10,000 ppm = 1%
Albright Metals has a substantial $7M manganese joint venture on the Bryah Basin
licences with OM (Manganese) Ltd, a wholly owned subsidiary of ASX listed OM
Holdings Limited (ASX: OMH), with OM having already spent over $4.5 million to
earn-in to the Manganese Rights of the project.
5
ASX announcement 11 July 2025 ‘Option Exercised to Acquire High-Grade Canadian Gold Project’
6
ASX announcement 29 September 2026 ‘Mineral Resource for Vail Road Gold Deposit’
ASX: ABR | albrightmetals.com 16
COMPETENT PERSON STATEMENT – MINERAL RESOURCE
The information in this announcement that relates to the Vail Road Gold Deposit
Mineral Resource is based on and fairly represents information compiled by Mr
Lauritz Barnes, (Consultant with Trepanier) and Ms Gemma Lee (Principal
Geologist – Albright Metals Limited). Mr Barnes is a member of the Australasian
Institute of Mining and Metallurgy (AusIMM) and both Mr Barnes and Ms Lee are
members of the Australian Institute of Geoscientists (AIG). Both have sufficient
experience of relevance to the styles of mineralisation and types of deposits under
consideration and to the activities undertaken, to qualify as Competent Persons
as defined in the 2012 Edition of the Joint Ore Reserves Committee (JORC)
Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore
Reserves. Specifically, Mr Barnes is the Competent Person for the estimation and
Ms Lee is the Competent Person for the database, geological model and site visits.
Mr Barnes and Ms Lee consent to the inclusion in this announcement of the
matters based on their information in the form and context in which they appear.
COMPETENT PERSON STATEMENT – EXPLORATION RESULTS AND TARGETS
The information in this report that relates to Exploration Results is based on and
fairly represents information and supporting documentation prepared and
compiled by Ms Gemma Lee who is employed by Albright Metals Limited as
Principal Geologist. Ms Lee is a member of the Australian Institute of Geoscientists.
Ms Lee has sufficient experience of relevance to the styles of mineralisation and
types of deposits under consideration, and to the activities undertaken, to qualify
as a Competent Person as defined in the 2012 Edition of the Joint Ore Reserves
Committee (JORC) Australasian Code for Reporting of Exploration Results, Mineral
Resources and Ore Reserves. Specifically, Ms Lee consents to the inclusion in this
report of the matters based on their information in the form and context in which
they appear.
The Company is not aware of any new information or data that materially affects
the information included in the referenced ASX announcement and confirms 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.
FORWARD LOOKING STATEMENTS
This announcement may contain certain “forward-looking statements” which may
not have been based solely on historical facts, but rather may be based on the
Company’s current expectations about future events and results. Where the
Company expresses or implies an expectation or belief as to future events or
results, such expectation or belief is expressed in good faith and believed to have
ASX: ABR | albrightmetals.com 17
a reasonable basis. However, forward looking statements are subject to risks,
uncertainties, assumptions and other factors which could cause actual results to
differ materially from future results expressed, projected or implied by such
forward-looking statements. Readers should not place undue reliance on forward
looking information. The Company does not undertake any obligation to release
publicly any revisions to any “forward looking statement” to reflect events or
circumstances after the date of this report, or to reflect the occurrence of
unanticipated events, except as may be required under applicable securities laws.
ASX: ABR | albrightmetals.com 18
APPENDIX 1:
ROCK SAMPLE RESULTS
2026 Albright Metals Rock Sample Results
Co-ordinate System: NAD83 Zone 20
Prospect
Sample
ID East North Au g/t
Ag
g/t
As
ppm
Sb
ppm
Bi
ppm
Te
ppm
W
ppm
Cu
ppm
Mo
ppm
Pb
ppm
Zn
ppm S pct
Albright Brook 2306327 269837 5062837 0.0025 0.07 10.3 3.8 0.19 0.025 0.4 3.8 4.29 3 79 0.08
Albright Brook 2306328 269830 5062826 0.0025 0.04 10.9 2.2 0.21 0.025 0.4 15.7 2.16 27.1 82 0.005
Albright Brook 2306329 269819 5062819 0.021 0.96 50.5 9.4 0.4 0.22 0.2 2480 7.18 8.5 16 0.18
Daley Brook 2306330 271589 5062201 0.0025 0.33 16.7 12.6 3.03 0.47 3.9 1130 8.83 5.1 126 0.38
Daley Brook 2306331 271585 5062205 0.0025 3.19 20.3 6.1 6.75 0.51 1.9 13800 79.2 11.3 190 1.47
Daley Brook 2306332 271545 5062194 0.009 1.18 65.9 20.8 18.6 0.5 3.1 887 384 448 110 5.57
Albright Brook
Fault 2306333 271255 5063714 0.006 0.03 11.1 6 0.08 0.025 0.8 12.8 2.41 11.8 69 0.005
Albright Brook
Fault 2306334 271263 5063734 0.009 0.04 24.4 4.3 0.18 0.025 0.8 4.8 2.13 7.9 24 0.005
Central
Cameron Rd 2306335 270082 5063543 0.0025 0.02 3.4 0.7 0.05 0.025 0.5 3.1 1.43 9.1 41 0.005
Central
Cameron Rd 2306336 270090 5063542 0.0025 0.01 6 0.7 0.03 0.025 1.5 1.9 0.8 5.4 44 0.005
Central
Cameron Rd 2306337 271464 5063375 0.006 0.02 13.6 0.6 0.05 0.025 0.3 3.6 1.99 6 17 0.01
Central
Cameron Rd 2306338 271564 5063311 0.009 0.05 2.3 0.5 0.12 0.025 0.5 2.1 0.68 4.9 68 0.04
Albright Brook
Fault 2306339 271803 5063698 0.008 0.02 3.3 1.2 0.03 0.025 1.1 2.9 1.15 11.4 36 0.005
Albright Brook
Fault 2306340 271998 5064027 0.007 0.03 3.6 0.5 0.04 0.025 3 5.2 3.25 2.4 11 0.005
Quarry 2306341 271832 5065465 0.006 0.04 8.3 0.2 0.09 0.025 0.4 3.5 1.86 4.3 69 0.04
Quarry 2306342 272031 5065686 0.009 0.04 515 1.4 0.03 0.025 0.7 56.1 0.48 2.6 56 0.13
Highway 710 2306343 272718 5064496 0.008 0.05 31 15.1 0.03 0.025 0.4 83.4 0.72 2 94 0.21
Henderson
Settlement 2306344 273273 5064417 0.007 0.05 18.2 3.6 0.05 0.025 0.6 8 2.02 9.5 74 0.04
Henderson
Settlement 2306345 273275 5064418 0.033 0.05 844 11.6 0.1 0.07 3.4 15.2 1.06 9.9 155 0.05
Henderson
Settlement 2306347 273295 5064418 0.03 0.05 314 6.3 0.12 0.07 1 13.4 4.79 8.6 38 0.03
Henderson
Settlement 2306348 273771 5064394 0.007 0.04 17 3.8 0.04 0.08 0.4 16.1 0.7 3.9 38 2.07
Henderson
Settlement 2306349 273663 5064228 0.008 0.04 24.4 0.3 0.1 0.025 0.4 21.3 1.03 2.4 103 0.33
Grant Brook
Central 2306350 273607 5063655 2.68 0.44 76.6 1.7 1.43 0.26 0.2 19.7 5.93 147 56 0.79
Grant Brook
Central 2306351 273703 5063647 0.348 0.33 20.9 0.8 0.66 0.08 0.2 228 6.26 33.4 12 0.17
Grant Brook
Central 2306352 273746 5063647 0.993 1.45 4.5 0.7 0.24 0.025 0.3 3760 4.38 403 194 0.65
First Run Brook 2306353 270081 5058844 0.012 0.17 24.3 3 0.52 0.1 0.2 146 18.3 11.8 34 0.31
First Run Brook 2306354 270003 5059033 0.0025 0.02 10.1 1.1 0.04 0.025 0.1 49.4 1.28 3.1 111 0.14
First Run Brook 2306355 270000 5059057 0.012 0.02 3.8 1 0.06 0.025 0.3 9.5 2.63 4 27 0.005
Bond Road 2306356 269364 5062190 0.014 0.04 73 9.7 0.27 0.025 1.8 31.5 1.24 12.3 135 0.005
Daley Brook 2306357 271409 5062181 0.0025 1.85 7.3 2.4 1.66 0.33 0.2 43.6 0.73 20800 4020 0.41
ASX: ABR | albrightmetals.com 19
Historic Rock Sample Results – Anomalous Only
Co-ordinate System: NAD83 Zone 20
Anomalous Historic Rock Chips – Location, Year and Classification Score
Sample ID Prospect Year East North Min Score Mineral System
11210 Grant Brook 2016 273787 5063849 53.26 Pb-Zn-Ag vein affinity
11212 Grant Brook 2016 274073 5064115 36.49 Cu-Mo-Bi-Te affinity
11213 Grant Brook 2016 274078 5064110 34.58 Cu-Mo-Bi-Te affinity
11215 Henderson Settlement 2016 273195 5064395 23.51 Au-As-Sb quartz-vein affinity
11216 Henderson Settlement 2016 273205 5064383 20.26 Au-As-Sb quartz-vein affinity
11251 Albright Brook 20
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