GREAT WESTERN MINING CORPORATION
PLC
("Great Western", "GWM" or the
"Company")
RHYOLITE DOME EPITHERMAL GOLD
TARGET
Great Western Mining Corporation PLC (AIM -
GWMO, Euronext Growth - 8GW) is pleased to report results from
ongoing work on the highly prospective Rhyolite
Dome gold target at its Olympic Gold Project in
Nevada.
HIGHLIGHTS
· Soil sampling results reveal Rhyolite
Dome as a high priority gold target.
· Best grades include 61 ppb, 58 ppb and
51 ppb gold in recent samples and 207 ppb gold in legacy
samples.
· Results include some of the strongest
soil anomalism encountered to date at the Olympic Gold
Project.
· Rhyolite Dome is further enriched with a
suite of indicator elements, including silver, arsenic, and
mercury.
· Rhyolite Dome is located at a crossover
zone between northwest and north-northeast trending major fault
sets.
· The Warrior, Hillside, Cute
Maid and Lou epithermal gold deposits all lie along a 2.2 km trend,
similar to the distance from OMCO to Rhyolite
Dome.
· Other geological features that highlight
prospectivity include a silica sinter, chalcedony veins and a
mapped placer.
Great Western
Chairman Brian Hall commented: "Multiple overlapping lines of evidence
make Rhyolite Dome a high priority gold target for Great Western.
The next step will be to conduct IP surveys over the structure to
narrow down drill targets in three dimensions with the objective of
establishing a discovery intercept. We look forward to updating
shareholders on further progress in
2024".
Introduction
Rhyolite Dome lies within the Olympic Gold
Project, approximately 2 km southeast of the OMCO gold mine site
and 15 km southeast of the Paradise Peak epithermal gold deposits.
It is a rhyolite flow dome structure, surrounded by
clay-altered andesite volcanics and rhyolitic tuffs, with scattered
gold anomalies identified in grabs during 2023 (see RNS
Exploration Update 10 July
2023). The target has never been drilled.
Legacy soil data and new
sampling
Great Western has recently digitised legacy
reconnaissance soil results. The dataset comprises multi-element
results from 115 samples taken from Great Western's claims, arrayed
in four northeasterly traverses. The traverse that crosses Rhyolite
Dome contains some of the strongest soil anomalism encountered at
the Olympic Gold Project, including 207 ppb gold and 1,780 ppb
silver.
In general, the anomalies at Rhyolite Dome
exceed those proximal to the OMCO Mine and Trafalgar Hill where
known mineralisation occurs. This has prompted follow-up sampling
at Rhyolite Dome, with a total of 145 new soil samples taken along
six lines, with 100 m line spacing and 30 m sample spacing
along each line.
Gold results
The gold results are highly positive. Of
the 145 samples taken, 54 are > 10 ppb gold, 9 are > 20 ppb
gold and three outliers contain 51, 58 and 61 ppb gold (values
above 5 ppb have been treated as anomalous for gold). The best gold
results in the new data are clustered near the location of the peak
legacy data sample (at 207 ppb gold). Based on these results, the
northwest side of Rhyolite Dome appears most
prospective.
Multiple prospectivity
indicators
A strong prospectivity picture is developing at
Rhyolite Dome. Additional indicators include:
·
Other metals:
Silver, arsenic and mercury, all of which are also indicative
of low-sulphidation epithermal mineralisation, are enriched in
Rhyolite Dome area and show good correlation with gold and local
structures (Figure 2).
·
Geology:
Rhyolite flow domes are associated with thermal centres in
epithermal systems forming above vertical lava conduits.
·
Textures:
On the southern margin of the dome structure,
chalcedonic stockwork veins were identified during soil sampling.
Stockworks of this type are typically found above the ore zone in
low-sulphidation systems.
·
Hot spring
deposits: Surface deposits of amorphous
silica (sinters) flooding into lake sediments have been identified
by GWM on the northwest flank of the dome structure. Sinters are
another feature typically found above low-sulphidation
centres.
·
Fluid
pathways: Rhyolite Dome area lies at a
crossover zone between northwest and north-northeast trending major
fault sets. These structures may have provided vertical
plumbing for both molten rock and mineralising fluids. Metal
anomalies are aligned along interpreted structures.
·
Placers:
A legacy geological map indicates both outcropping quartz and a
'gold placer', less than 200 m north of the previous best gold
soils results at Rhyolite Dome and topographically lower. Placers
form from the erosion of outcropping gold mineralisation and
subsequent deposition of gold detritus.
·
Neighbouring
deposits: To the east of Olympic, the
Warrior, Hillside, Cute Maid and Lou epithermal gold deposits
all lie along a 2.2 km trend, similar to the distance from OMCO to
Rhyolite Dome. These deposits are each located on north-northwest
trending structures - a matching orientation to the OMCO-RH
trend.
Figure 1. Left: Locations of
Olympic and Rhyolite Dome relative to other mines in the region.
Great Western claims in yellow. Right: Gold distribution across
Rhyolite Dome area, note strongest values in northwest.
Figure 2. Elemental
abundances of silver, arsenic and mercury in soils over Rhyolite
dome area.
Figure 3. Overlapping
geochemical, geological and structural
indicators.
ADDITIONAL
INFORMATION
All soil samples were processed by
Paragon Geochemical Laboratories, Reno, Nevada. Samples were
screened to -80 mesh and analysed by method FSAU-25, aqua regia
digest with ICP-MS finish for a 51-element suite. Quality control
samples were inserted by the company and results reviewed prior to
release.
Note on units - gold, silver and
mercury are quoted in parts per billion (ppb), and arsenic in parts
per million (ppm).
QUALIFIED PERSON
STATEMENT
The information in this announcement
that relates to exploration results is based on information
reviewed by Dr James Blight MGeol PhD MAusIMM who is Exploration
Manager of Great Western Mining PLC. Dr Blight is a "Qualified
Person" as defined in the "Note for Mining and Oil & Gas
Companies" which form part of the AIM Rules for Companies. Dr
Blight has reviewed and consented to the inclusion in the
announcement of the information in the form and context in which it
appears.
For further
information:
Great Western
Mining Corporation PLC
|
|
Brian Hall,
Chairman
|
+44 207
933 8780
|
Max Williams, Finance
Director
|
+44 207
933 8780
|
|
|
Davy (NOMAD,
Euronext Growth Listing Sponsor & Joint
Broker)
Brian Garrahy
|
+353 1 679
6363
|
|
|
SP
Angel (Joint Broker)
Ewan Leggat/Harry
Davies-Ball
|
+44 203
470 0470
|
|
|
Walbrook PR
(PR advisers)
Nick Rome/Joe
Walker
|
+44 207
933 8783
|
Notes to Editors
The Company has a large tract of
acreage in Mineral County, Nevada. The area consists of rugged,
mountainous terrain, which means that large parts of it remain
under-explored. Mineral potential is hosted by the regional Walker
Lane Structural Belt, the largest structural and metallogenic belt
in Nevada, yet one of the least explored in recent times, with
gold, silver and copper currently produced in Mineral County.
Great Western has seven distinct concession areas which offer the
potential for exploiting (1) short term gold and silver deposits
and (2) long-term, world-class copper deposits.
Six of the Company's properties are
in the west of Mineral County and are 100% owned and
operated. The Company has an option to acquire a seventh
property, the Olympic Gold Project, in the east of the
county. Great Western's small exploration team is supported
by locally based consultants and contractors.
The state of Nevada is considered to
be one of the world's most mining friendly jurisdictions.
While tightly regulated and environmentally conscious, Nevada
welcomes the mining industry. Great Western takes care to
ensure that its claims are maintained in good standing and all
regulations observed.
There are numerous gold and silver
prospects on the Company's acreage, including extensive historic
mine workings which offer the opportunity for secondary
recovery. The Company is party to a 50-50 joint venture known
as Western Milling LLC which is constructing a mill to process
pre-mined material for secondary recovery of gold and
silver.
Furthermore, through extensive
drilling over a five-year period, GWM has established a Mineral
Resource on its first target area known as M2, of 4.3 million
tonnes at 0.45% copper, for 19,000 tonnes of contained copper
metal. This resource has been independently reported in accordance
with JORC guidelines.
GWM has also established an Inferred
Resource Estimate of 31,000 tonnes grading 1.6 g/t gold and 3.0 g/t
silver in tailings associated with the OMCO Mine at the Olympic
Gold Project. Additionally, exploration targets have been
independently reported as follows:
·
3,400 - 6,400 tonnes grading between 0.5 and 1.2
g/t Au and 1.2 and 2.1 g/t Ag in the substrate beneath the tailings
volume at the Olympic Mine.
·
9,000 - 12,000 tonnes grading between 0.9 and 2.4
g/t Au and 2.0 and 5.1 g/t Ag in a coarse stockpile at Olympic
Mine.
·
4,200 - 7,700 tonnes grading between 40 and 140
g/t Ag and 0.3 and 0.3 g/t Au in spoil heaps at Mineral
Jackpot.