Torr Metals is chasing high-quality porphyry targets with strong similarities to New Afton in southern BC – Beragampengetahuan

beragampengetahuan (www.beragampengetahuan.com
Newswire) New Gold’s (TSX:NGD) New Afton mine is Canada’s
only underground block caving operation, located about 10 kilometers
outside of Kamloops, in south-central British Columbia.

New Gold began construction of the New Afton mine in 2007 and reached
commercial production in 2012. The operation is on the site of the
historic Afton open pit mine, which operated from 1977 until 1997.

In March 2020 New Gold incorporated the C-Zone development that
extended the mine life to 2030.

The mineral resource estimate as of Dec. 31, 2024, consists of
81,643,000 tonnes of ore in the measured and indicated categories. At
grades of 0.51 grams per tonne gold, 1.69 g/t silver and 0.61% copper,
the New Afton deposit contains 1,352,000 ounces of gold, 4,431,000
ounces of silver and 1.1 billion pounds of copper.

In 2024 New Afton produced 72,609 gold ounces and 54 million pounds of
copper, beating gold guidance and meeting copper guidance for the
year.

According to a Feb. 10 2025, technical report,

The New Afton deposit is classified as a silica-saturated alkalic
copper-gold porphyry deposit. Copper-gold alkalic porphyry
mineralization results from late-stage hydrothermal activity driven
by remnant heat from the porphyry intrusion. Thermal gradients
within these systems give rise to broadly concentric, although often
complexly intermingled, zones of alteration and mineralization. At
New Afton, copper-gold mineralization typically occurs as east-west
subvertical tabular zones of disseminations, stringers, and
fracture-filling sulphides within rocks of the volcanic Nicola Group
and the diorite. The deposit consists of three principal zones:

• 
  The Main zone, located on the western edge of the Pothook diorite
  is subdivided into Lift 1 East, Lift 1 West (both mined out), B3,
  C-Zone, and D-Zone mining zones; mining is currently focused on
  the B3 and C-Zone. 
• 
  The Hangingwall (HW) zones are smaller satellite zones located
  along the southern margin of the Pothook diorite.
  
• 
  The Eastern zones include two separate areas located on the
  northern margin of the Pothook diorite: East Extension and K-Zone.
  East Extension is currently in the mine planning phase and KZone
  is currently being explored.

Mineralization is subdivided into three types: hypogene (either
chalcopyrite- or bornite-dominant), secondary hypogene (sometimes
referred to as mesogene) (overprint of tennantite-enargite +
tetrahedrite and bornite + chalcocite rims), and supergene (native
copper and chalcocite).

I have been evaluating copper-gold deposits in the southern and
northern Quesnel Trough for over 20 years. While no one has yet
discovered another deposit like New Afton, Torr’s ongoing
exploration efforts may yield promising results, though there are no
guarantees.

The Quesnel Trough, or Quesnel Terrane, is a Cordilleran volcanic and
magmatic island-arc assemblage that was accreted onto the continental
margin of North America during the Late Triassic to Early Jurassic
periods; it is British Columbia’s primary copper-producing belt.

Torr Metals

Torr Metals started out exploring the Latham copper-gold project in
the Golden Triangle of northwestern BC but pivoted to the Kolos
copper-gold project after CEO Malcolm Dorsey and his brother, Cameron
Dorsey, both structural geologists (Cameron is an advisor to the
company) staked the claims based on an exploration model they have
developed over the past several years of working in the region.

Torr’s third property is the Filion gold project in Ontario.

Kolos Copper-Gold Project

The 332-square-kilometer Kolos copper-gold project (including the
57-square-kilometer Bertha Property strategically optioned in March
2025 for full ownership) contains Nicola Belt geology along trend and
with similar attributes to alkaline and calc-alkaline copper ±
gold ± molybdenum porphyry mines at Copper Mountain, Highland
Valley, and New Afton.

The project is adjacent to Highway 5, the Coquihalla Highway, with
year-round access and operation potential via forestry service roads
and substantial infrastructure provided by the city of Merritt located
23 km to the south. The project contains sixteen historical copper and
gold occurrences, majority never drill tested including the main
target areas. Through its own exploration, Torr has vectored four main
copper-gold porphyry targets covering 11.8-square-kilometers of
surface geochemical anomalism, three of those are permitted for
drilling.

Geology

The project lies within the Quesnel Terrane, a prolific porphyry belt
in British Columbia that is host to major deposits and long-lived
mines that within the region largely consist of Late Triassic
calc-alkaline and alkaline intrusions, including Highland Valley (30
km to the northwest), New Afton (30 km to the north), and Copper
Mountain (106 km to the south) deposits.

The Coquihalla Highway separates the two main lithologies encountered
on the Kolos project. West of the highway and in the northeast section
of the property andesitic rocks of the Late Triassic Nicola Group
predominate, consisting of andesite hornblende porphyry as well as
andesitic tuff, lapilli tuff, agglomerate and volcanic breccias.
Within the northern portion of the property Nicola Group volcanics are
intruded by a fine-grained diorite that is apparently a subvolcanic
equivalent of the andesite.

A major north-trending structural corridor, the Fanta Fault, is
exposed along the Coquihalla Highway and for the most part separates
Nicola Group volcanic and sedimentary rocks to the west from the
batholith to the east. The fault is characterized by brecciation,
pyritization, carbonate and epidote alteration, local clay alteration
and variable silicification.

Highly prospective mineralization consists of locally abundant pyrite
that is disseminated within host volcanics as well as concentrated
within north-trending fault structures that separate the underlying
Late Triassic Nicola Group rocks from Late Triassic granodiorite to
quartz monzonite intrusions.

Elsewhere throughout the project area, localized occurrences of
malachite with rare chalcopyrite also occur within host Nicola Group
volcanics, associated with increased fracturing together with
carbonate alteration and quartz-carbonate veinlets. These veinlets
carry malachite, pyrite ± chalcocite that together with
observed alterations styles is suggestive of the upper level of a
large-scale copper porphyry system with near-surface exposure.

As shown on the map below, there are at least nine major or mid-tier
mining companies operating within the Late Triassic-Alkaline Cu-Au
Porphyry Belt, including Taseko (Gibraltar mine), Boliden (Gjoll
project), Teck (Highland Valley mine), Hudbay Minerals (Copper
Mountain mine), Imperial Metals (Mount Polley mine), New Gold (New
Afton mine), KGHM (Ajax project), and Glencore’s shuttered
Brenda mine.

Regional exploration

Regional exploration occurred in the area starting in the 1960’s
through to the late 1980’s as a result of the porphyry
copper-molybdenum discoveries at Highland Valley. There have been at
least 10 operators within the Kolos project area since the
1960’s that defined six significant copper and gold occurrences:
Ace, Kirby, Lodi, Rea, Helmer and Clapperton. Intermittent historical
work at these occurrences includes rock and soil geochemical sampling,
trenching and electromagnetic (EM) geophysical surveys. 

Kolos copper and gold occurrences. What Torr started with

Ace

Historical geological mapping from 1988 identified older trenches with
exposures of andesite tuff, andesite feldspar porphyry,
quartz-sericite schists, phyllites and a quartz monzonite hosting
quartz-carbonate veins and variable amounts of malachite, chalcocite
and chalcopyrite.

Kirby

A rock sample taken from the discovery of the Kirby occurrence in 2014
assayed 4.24 grams per tonne gold, 11.3 g/t silver and 0.516% copper.

Another zone of historical mineralization is noted ~500 meters
east-southeast of the Kirby occurrence near the Coquihalla Highway,
with exposures of andesite tuff and diorite hosting quartz-carbonate
veins with pyrite, chalcopyrite and malachite. In 1988, four rock
samples taken from this outcrop exposure yielded 0.14, 0.60, 0.89,
0.22 grams per tonne gold across a 400-meter north-south trend.

Lodi

The Lodi occurrence contains andesite hosting crosscutting fracture
zones along the north-trending Fanta fault with narrow quartz
carbonate veins, up to a quarter-meter wide, and weak to trace
malachite ± chalcocite, chalcopyrite and pyrite mineralization.
Magnetite is also reported in the area with a rock sample collected in
1988 yielding 0.60 grams per tonne gold, 4.8 g/t silver and 0.233%
copper. Another zone of mineralization is located ~1 kilometer east of
the main occurrence, near the Coquihalla Highway, where another
outcrop rock grab sample from 1988 yielded 0.425 g/t gold, 1.8 g/t
silver and 0.415% copper.

Rea

The only known historical work consists of a rock grab sampling
program in 1988 with one sample taken from a rare outcrop that yielded
4.75 g/t gold, 144.0 g/t silver, 0.52% zinc and greater than 1% lead
and copper, whereas another sample taken approximately 900 meters west
of the previous sample yielded 0.63 g/t gold.

In 2004, a rusty diorite boulder (float) sample, located approximately
1.1 kilometers west-southwest of the occurrence, yielded 4.84 g/t
gold, 14.3 g/t silver, 0.202% copper and 0.126% lead.

Helmer

Historical trenching has exposed narrow, up to 1-meter-wide silicified
zones and/or quartz calcite veins in altered and sheared andesitic and
tuffs hosting pyrite, minor galena, chalcopyrite, and sphalerite
mineralization together with limonite and malachite oxidation. The
veins trend northwest with a steep dip. Historical rock grab sampling
from a trench-exposed outcrop yielded up to 1.425 g/t gold and 11.4
g/t silver. In 2007, a chip sample of mineralized outcrop yielded 1.26
g/t gold, 7.0 g/t silver, 0.178% copper, 0.410% lead and 1.450% zinc
over 0.4 meters, whereas a grab sample from another historical trench
assayed 0.37 g/t gold, 163.0 g/t silver, 1.860% lead and 6.50% zinc.

Clapperton

Scattered quartz veins up to 15 centimeters wide contain minor
calcite, epidote, chlorite and hornblende hosted within a chloritized
and kaolinized biotite-hornblende diorite. The veins parallel the
shear direction, trending approximately 20 and 120 degrees, and
contain minor amounts of chalcocite, chalcopyrite, bornite, malachite
and rare molybdenite as disseminated blebs.

In 1975, other zones of chalcopyrite and malachite mineralization were
reported several hundred meters north-northwest, 600 meters northeast,
400 meters south, and 1 km east-southeast of the main zone. This
indicates a multi-kilometer scale to copper porphyry-style
mineralization.

Recent exploration

In September 2023 Torr Metals announced the staking of the Kolos copper-gold project totaling 13,957 hectares. The news release mentions the six
copper and gold occurrences with the highlighted grades, and the
initiation of a 2023 field program composed of up to 2,300 soil
samples as well as rock sampling, with a focus on testing potential
extensions to historical geochemical anomalies.

The field program was completed that November, and Torr announced that it collected 47 rock and 3,348 soil samples, within about a 48 km² area. The program included the
first-ever surface geochemical and ZTEM airborne geophysical surveys
conducted over known historical copper-gold occurrences that have
never been drill-tested.

President and CEO Malcolm Dorsey compared what was found at Kolos to
Kodiak Copper’s (TSXV:KDK) proximal MPD project:

“These highly pronounced geophysical and geological features in
addition to the coincident historical occurrences are what first
attracted our attention to the area, as we know that similar
geophysical patterns have proven to be highly prospective within the
region, such as at Kodiak Copper Corp’s West and Gate Zones ~60
km to our south.”

The following May, 2024, Torr Metals expanded the project by 75% through staking, upsizing it from 140 km² to 240 km². The northerly
expansion followed an extension of the Fanta Fault, an orientation
identified by the company as a major structural control on copper and
gold mineralization in the area.

Torr was also the first to identify and sample a new mineralized
outcrop exposure it named the Vik Zone. New exploration targets were
identified in the northern and eastern portions of the expanded
project, including two large-scale low magnetic geophysical anomalies
that exhibit the same signature as the nearby Ram soil anomaly, which
is defined by a footprint of >200 ppm Cu measuring 900m by 500m.

“While our main focus remains on the more advanced drill-ready
Lodi, Kirby, Ace, Rea, and Clapperton Zones, the new discovery of the
Vik Zone demonstrates the effectiveness of our exploration model in
finding highly anomalous mineralization in unexplored areas,”
Dorsey said.

The next month, Torr announced the final assay results from the 2023 rock sampling
program and delineation of a robust ZTEM geophysical anomaly at the Vik
Zone, which it described as “a new discovery of copper (Cu)
and molybdenum (Mo) mineralization in outcrop, on the margins of one
of three highly prospective and untested moderate to high resistivity
anomalies identified across a >2.5 kilometer (km) trend.”

Of the 47 rock grab samples taken, 22 yielded >100 ppm Cu, with
five samples exceeding 500 ppm. The highest value returned 4,240 ppm
(4.24%) Cu within the Clapperton Zone.

A total of 10 grassroots targets were identified in the
southern and central portions of the project, with comparable
prospective geology and ZTEM geophysical signatures to the six
significant mineralized zones, which now comprised Vik, Lodi, Kirby,
Ace, Rea and Clapperton.

Sonic Zone discovery

In August 2024 Torr Metals made a discovery that both confirmed the exploration methodology, and introduced
a fascinating analog.

Final assay results from a total of 33 rock grab samples collected
during 2024 reconnaissance programs revealed additional high-grade
rock grab assays within the Kirby, Rea and Clapperton zones, as well
as a new copper-gold discovery in the northern portion of the project
that Torr termed the Sonic Zone.

Initial rock grab samples from the Sonic Zone revealed anomalous
copper and gold values in outcrop within a 1,000- by 2,000-meter
footprint of strong magmatic-hydrothermal alteration that aligns
with the margins of a high magnetic geophysical signature, identified
as a potential source for a monzodiorite intrusion.

The discovery reinforced Torr’s exploration model and suggested
the potential for another large-scale cluster of anomalies comparable
in scale to the already established Kirby, Lodi, Ace and Rea targets
to the south.

New Afton comparison

CEO Malcolm Dorsey for the first time referenced New Afton as a
potential comparable to the Kolos copper-gold project:

“The discovery of the Sonic Zone is particularly promising, as
it opens up a new area of mineralization that bears geological
similarities to the high-grade New Afton copper-gold porphyry deposit,
located just 27 km to the north,” he said.

More details on the proposed analog were provided in the next
paragraph:

“Key surface indicators within the Sonic Zone suggest
significant potential for a silica-saturated porphyry system with
similar geological characteristics to the nearby high-grade New
Afton copper-gold deposit. New Afton is characterized by monzonite
to monzodiorite intrusions and alteration patterns that include
potassic alteration (dominated by biotite, with K-feldspar and
magnetite) and propylitic alteration (chlorite, epidote, and
calcite).

Surface features such as these, along with narrow quartz veins,
silicification (increased silica content in the rock), and location
along the margins of a high magnetic geophysical anomaly are strong
indicators of underlying mineral potential. Similar parallels have
been observed at the Sonic Zone, underscoring the high degree of
prospectivity for this area to host a substantial mineralizing
system.”

Fast forward to January 2025, when Torr announced a high-grade rock grab sample of 1.10% Cu from the Sonic Zone, as well as new mapping that significantly
expanded Sonic’s footprint from 2 km² to 12 km². The
zone now spans approximately 3 km by 4 km, “characterized by
pervasive alteration and mineralization in surrounding Nicola Group
volcanics and altered monzonite-monzodiorite intrusive bodies
comparable to regional alkalic copper-gold porphyry systems such as
New Afton and Copper Mountain.”

“The geological and geophysical similarities to the nearby
high-grade New Afton deposit underscore the immense potential for
substantial discoveries in this area,” said Dorsey.

Bertha discovery

In March 2025 Torr Metals made another move to expand the Kolos
property, this time by signing an option agreement for the Bertha property, which is contiguous to Kolos on its northern portion. Along with
gaining the 57-square-km Bertha, the company also staked an additional
35 km² of highly prospective ground surrounding the new target.

According to Torr, unexplored Bertha hosts nine significant copper and
gold occurrences along an epithermal and porphyry trend extending
northwest from the Sonic Zone. Through this acquisition and claim
staking, the Kolos project now covers 332 km².

Supergene enrichment

“At Bertha, fieldwork confirmed structurally controlled
supergene copper mineralization composed primarily of chalcocite,
where historical rock grab samples have returned up to 8.48% Cu in
outcrop. The upcoming IP survey will be the first to test for
subsurface extensions of this undrilled zone, which shares key
structural and mineralogical features with the upper supergene zone of
the high-grade New Afton copper-gold deposit, located just 28
kilometres to the north-northeast.”

“We’re excited to launch this next phase of exploration
across our 332 km² land package, where recent work at the Bertha
target has revealed compelling geological similarities to the nearby
high-grade New Afton deposit,” Dorsey stated on June 26. “A new copper-gold porphyry discovery at Kirby, Bertha, or
Sonic would be highly meaningful.”

The following three paragraphs are from the July 8, 2025 news release:

“The Bertha Zone represents a highly prospective, underexplored
high-grade copper target where recent fieldwork has confirmed
supergene-style copper mineralization, primarily sooty chalcocite,
native copper, and malachite nodules hosted within brecciated volcanic
rocks. This style and setting are geologically significant and
comparable to the supergene enrichment zone at New Afton, located just
28 km to the north.”

“Supergene mineralization happens when copper-rich fluids from
deeper underground move up through cracks in the rock, usually helped
by rainwater or groundwater. As these fluids rise closer to surface,
they interact with oxygen and other elements. This chemical reaction
causes high-grade copper minerals, like chalcocite, native copper, and
malachite, to form near surface.”

“At New Afton, the presence of a well-developed supergene
blanket, characterized by abundant native copper and sooty chalcocite,
was critical to the early economic success of the mine. This zone
accounted for approximately 80% of the initial orebody, enabling low
strip ratios, enhanced metal recoveries, and early cash flow. It
overlies a deeper primary hypogene copper-gold porphyry system hosted
within the Cherry Creek intrusion of the Iron Mask batholith, where
brecciation and hydrothermal fluid pulses played a key role in both
metal deposition and alteration zoning.”

On Aug. 13, 2025, Torr Metals announced results from the induced polarization (IP) survey and
rock grab sampling program at Bertha.

Selected rock grab sampling returned up to 16.9% copper and 8.48 grams
per tonne silver from a series of parallel quartz-carbonate veins
along a 30-meter strike length. According to TMET, these results
validate the high-grade nature of the historical exploration pit,
which reported past production of 30 tonnes averaging 2.14% Cu
and 27.43 g/t Ag. Additionally, mineralization continues along a
>450m west-southwest strike between the Bertha and Bertha
South showings.

Importantly, the high-grade copper mineralization is situated
along the margins of a newly defined IP chargeability anomaly
exceeding 900 meters in strike length and over 500 meters in width,
which remains open at depth, down-plunge, and to the east.

“The confirmation of high-grade copper at-surface and
identification of a large 0.7 km2 IP geophysical anomaly at
Bertha represent a major step forward in defining the untested
potential of this area,” Dorsey said. “The signature
strength and dimensions are highly promising for targeting a midsize
high-grade porphyry system perhaps similar to the New Afton system,
with a broad moderate chargeability overlapping resistivity along the
margins of a magnetic anomaly, together with nearby evidence of
high-grade supergene copper mineralization. We now have the
geochemical and geophysical data needed to plan drill targets in
preparation for an inaugural drilling program at Bertha, the first to
test this previously untouched target.”

Torr’s latest news release on Sept. 3 announced results from the compilation of historical soil and
rock grab sampling covering the adjoining 57-square-km Bertha
property.

The data set highlights a 4.5-square-km copper-gold soil anomaly north
of the Sonic Zone, reporting up to 4,510 ppm (4.51%) copper and 590
parts per billion gold (0.590 g/t). The anomaly has a strike length of
3.7 km with a width of 1.2 km.

Meanwhile, 2025 field reconnaissance at the Sonic Zone copper-gold
porphyry target area identified a new mineralized outcrop
approximately 1 km northeast of Torr’s 2024
discovery, which returned 1.1% Cu in a magnetite-rich grab
sample along the margins of a highly prospective high magnetic
anomaly. The newly identified outcrop yielded 0.42% Cu from
a strongly sheared quartz-carbonate vein hosted in Nicola Group
volcanics, proximal to a pyritized monzonite intrusion and
silica-apatite dyke: further supporting vectors toward a potential
alkalic Cu-Au porphyry center.

The historical data set also defined a more than 4-km gold-silver
epithermal corridor, extending northwest from the Sonic Zone porphyry
target through the Plug and Meadow Creek occurrences (March 11, 2025 news release) with up to 700 ppb Au in soil and 2.24 g/t Au over 4.4 meters,
20.78 g/t Au over 0.56m, and 6.24 g/t Au with 1,715 g/t Ag over 0.36m
in trenching.

Four porphyry targets

In total, Torr has identified four undrilled copper-gold porphyry
targets at Kolos — Sonic, Bertha, Kirby and Lodi —
with surface geochemical anomalies covering a combined 11.8
km². Bertha, Kirby, and Lodi are fully drill-permitted, while
Sonic is in the permitting phase.

“The combination of historical data and our recent fieldwork
continue to highlight the significant discovery potential at the
highway-accessible Kolos Project,” Dorsey stated. “We are
advancing the drill permit for the Sonic Zone and plan to fully
evaluate the highly prospective 4 km² “Gap” area this
year.

Our inaugural Phase 1 drill program will begin at the Bertha target,
where surface outcrop rock samples returned up to 16.9% copper,
supported by a strong chargeability anomaly suggesting mineralization
may extend beyond 500 vertical metres. These efforts mark the
beginning of a broader strategy to unlock four high-impact
opportunities within Canada’s most productive copper
belt.”

Conclusion

The average copper grade in BC is .40% CuEq. If a large part of Kolos
exhibits higher-grade mineralization it could potentially support a
starter pit and the tonnage required for an economic mine would be
smaller. Also, it will attract more investor attention which makes
financing easier.

And it might be something TMET could handle by itself without blowing
out the share structure, which is mostly what happens with juniors
with porphyries (Because it takes so many drill holes to come up with
a resource). On the other hand, it could attract deep-pocketed majors
to fund exploration/development.

I have been looking at these types of deposits in the southern Quesnel
Trough for over 20 years. But no one has ever found another Afton. A
well-developed supergene enrichment blanket superimposed on the
hypogene mineralization is a target well worth chasing; Kolos appears
to have it (although it is very early stage and needs to have more
work), strengthening the potential comparison to New Afton. And
let’s not forget at least three other large already identified
targets.

Torr Metals
TSXV:TMET
2025.09.12 Share
Price: Cdn$0.16
Shares Outstanding: 31.8m
Market Cap:
Cdn$6.7m
TMET website

Richard (Rick) Mills
aheadoftheherd.com

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