Teuton Drills Ram Property in BC’s Active Golden Triangle
TEUTON RESOURCES CORP.
2130 Crescent Road
Victoria, BC V8S 2H3
Phone: (778) 430-5680
Website: www.teuton.com
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Teuton Drills Ram Property in BC’s Active Golden Triangle
• Porphyry style copper-gold mineralization identified (2024) in surface zone 150m wide by
450m long
• Gold grades up to 7.01 g/t and copper up to 8.24% in separate VMS system
Victoria, British Columbia, Canada, August 26, 2025. Teuton Resources Corp. (“Teuton” or “the
Company”) (“TUO”-TSX-V) (“TEUTF”-OTC:QB) announces it is currently drilling targets at its
Ram property in British Columbia’s Golden Triangle, focusing on two newly discovered (2024)
mineralized zones that exhibit characteristics of both porphyry copper-gold and VMS (volcanogenic
massive sulfide) systems. The Ram is jointly owned with Silver Grail Resources Ltd. Following the
conclusion of the drill program at the Ram, an IP geophysical survey at the Clone property is tentatively
scheduled for September, should weather and personnel conditions allow. [Refer to the end of the release
for URLs for various maps]
Key Highlights
• Strategic location within the active southern Golden Triangle, surrounded by Goliath
Resources’ expanded claim block following their Golddigger discovery
• Multiple deposit types identified in 2024: porphyry copper-gold (Malachite zone) and VMS
copper-gold-silver (Mitch zone)
• Drilling is proceeding well, about 900m drilled to date
Market Context and Regional Significance
The Ram property sits in the heart of one of Canada’s most active exploration regions, where recent
discoveries by Goliath Resources and Dolly Varden Silver have renewed focus on the southern Golden
Triangle. Teuton’s legacy land position, with many claims staked over 30 years ago, now appears as
strategic “islands” within Goliath’s expanded holdings, potentially benefiting from the regional
exploration momentum and geological understanding.
Discovery Details
Malachite Porphyry Zone
The Malachite zone represents a 450m x 150m porphyritic outcrop with widespread malachite staining
and magnetite veinlets. Surface sampling in 2024 has identified gold-copper mineralization at many
points within the zone.
Selected Results
• Sample C009921—Grab*: 2.33 g/t Au, 5.78% Cu in porphyritic diorite with chalcopyrite
• Sample Q310429—Grab*: 1.27 g/t Au, 2.94% Cu in malachite-chalcopyrite mineralization
Statistical Summary (35 grab* samples)
• Gold: trace to 2.33 g/t (average 0.35 g/t)
• Copper: 0.002% to 5.78% (average 0.59%)
Sawcut Channel Sampling (14 samples, 1m average)
• Gold: trace to 1.05 g/t (average 0.23 g/t)
• Copper: 0.01% to 1.91% (average 0.39%)
*Grab samples are by their nature selective and are not indicative of the overall grades of mineralized
areas.
Mitch VMS Zone
Located 500m southwest of the Malachite zone, the Mitch zone contains en-echelon massive sulfide
stringers up to 7cm wide, exhibiting classic VMS characteristics with robust precious metal grades:
Selected Results
• Sample 711540—Grab*: 7.01 g/t Au, 3.58 g/t Ag, 0.11% Cu (pyrite-rich vein)
• Sample H226985--0.5m channel sample: 0.75 g/t Au, 117 g/t Ag, 8.24% Cu
• Sample Q310447—Grab*: 1.95 g/t Au, 58.63 g/t Ag, 5.03% Cu (pyrite-chalcopyrite vein)
Statistical Summary (25 grab* samples):
• Gold: trace to 7.01 g/t (average 0.82 g/t)
• Silver: 0.12 to 58.63 g/t (average 5.90 g/t)
• Copper: 0.006% to 5.02% (average 0.30%)
*Grab samples are by their nature selective and are not indicative of the overall grades of mineralized
areas.
Geological Model and Exploration Rationale
The Ram property hosts Upper Triassic Stuhini rocks and Lower Jurassic Hazelton volcano-sedimentary
sequences intruded by early Jurassic porphyries, potentially correlative with the productive Goldslide
Intrusive suite. This geological setting is favourable for both porphyry and VMS-style mineralization.
It is also favourable for Red Mountain type, precious metal mineralization described as high-grade (3 g/t
to 20 g/t) gold mineralization in semi-tabular pyrite + pyrrhotite stockworks 5m to 29m thick with intense
sericite alteration surrounded by disseminated sphalerite + pyrrhotite.
The Mitch zone sits within a discrete north-south trending magnetic anomaly on the edge of a 1km-long
oval magnetic feature, consistent with porphyry-related alteration signatures.
Select Sample of Core from Mitch Zone
Exploration Timeline and Strategy
Current Activities
Drilling is now underway at the Ram property targeting both the Malachite and Mitch zones.
• Contractor: Hy-Torque Drilling Ltd. with helicopter support from Kestrel Helicopters and
Tseax Aviation/Yellowhead Helicopters
• Likely September 2025 IP Geophysical Survey: Four 1km lines on Clone property testing
porphyry copper-gold potential.
Strategic Approach
The exploration program follows a systematic approach to test both near-surface high-grade VMS targets
and deeper porphyry potential, maximizing discovery probability across multiple deposit models.
Clone Property—An Additional Opportunity
Recent surface work at the Clone property (2023-24), jointly owned with Silver Grail Resources Ltd.,
has identified encouraging gold-copper values in an area distinct from the historic Main zone where
several million dollars were spent on high-grade gold discoveries in the 1990’s. The new target area, as
is the case with the Ram property, sits near the critical Triassic-Jurassic contact and exhibits:
• Wide-spread copper rock geochemical anomalies suggesting buried porphyry potential
• Gold values ranging to 93.7 g/t in cross-cutting structures
• Anomalous bismuth (up to and exceeding 10,000 ppb), molybdenum, and tungsten signatures
suggesting a nearby intrusive source
• Tertiary age porphyritic and felsic dykes similar in description as those carrying gold values at
Goliath’s Golddigger discovery
• Tertiary age Intrusions
The new zone of interest is slated for 4 kms of IP survey lines, weather permitting, likely to be carried
out in mid -September of 202 5. The presence of pervasive anomalous copper values on surface as
indicated by a number of samples taken in 2023-24 suggests this area could be in the vicinity of a buried
porphyry deposit, however at this stage of exploration it is only conjecture. More work is necessary to
prove the hypothesis and positive results from an IP survey could be a large step in that direction.
Another possible theory derives from recent exploration work at Goliath Resources’ Golddigger property
(southeast of the Clone, refer to map) where overlooked Eocene age dykes have been shown to contain
gold values with associated bismuth, molybdenum and tellurium values . The prospective area on the
Clone has been sampled with gold values ranging from trace to 93.7 g/t (see Clone Compilation Map).
Anomalous to extremely anomalous values in bismuth have also been recorded in this area along with
many anomalous values in molybdenum as well as tungsten. One sample taken in 1995 registered values
in excess of 10,000 ppb bismuth.
Mapping in 1996 on the Clone was completed by personnel from Homestake Mining, then owners of the
Eskay Creek mine. All of this work was done while the property belonged to Teuton and Silver Grail,
and although it would now be termed “historical” under th e auspices of National Policy 43 -101, it is
believed to be reliable. Dykes as found on the Clone property in this area have been described as felsic
and porphyritic, the same general type as at Goliath Resource’s Golddigger property. Plans are to age
date the dykes on the Clone this year to see if they are actually from the Eocene (the Eo cene is a
subdivision of the Tertiary). Note: Readers are cautioned that mineralization described on Goliath
Resources Golddigger property is not necessarily indicative of mineralization on the Clone property.
URLs For Maps
https://teuton.com/SEPropertiesMap
https://teuton.com/RamCompilationMap
https://teuton.com/CloneCompilationMap
QA/QC
All samples were crushed and pulverized at the MSA laboratory in Langley, BC using technique
PREP910. The pulps were dropped delivered to MSA at their laboratory where Au was tested on 30 g
nominal samples by fire assay (MSA method FAS-111). An additional 51 elements were tested on 0.5 g
splits using Aqua Regia digestion and ultra trace level ICP -AES analysis (MSA method IMS -130).
Samples with overlimit Ag, Cu, Zn were reanalyzed using ore-grade Aqua Regia digestion and ICP-ES
analysis (MSA methods ICF-6x). MSA is an accredited facility.
Qualfied Person
D. Cremonese, P. Eng., is the QP for Teuton Resources Corp.; as President and CEO of Teuton he is
not independent of the Company.
About Teuton
Teuton owns interests in more than twenty properties in the prolific “Golden Triangle” area of
northwest British Columbia and was one of the first companies to adopt what has since become known
as the “prospect generator” model.
Teuton was the original staker of the Treaty Creek property assembling the core land position in 1985.
It presently holds a 20% carried interest in Treaty Creek (carried until such time as a production
decision is made) as well as a 0.98% NSR in the claims covering the Goldstorm gold -silver-copper
deposit. A 0.49% NSR is owned in the peripheral claims. Neither of the NSRs is subject to a buy -
back. Teuton also owns many other royalties in claim packages south of Seabridge Gold’s KSM
property and Newmont Mining’s Brucejack property. Interested parties can access information about
Teuton at the Company’s website, www.teuton.com.
ON BEHALF OF THE BOARD OF DIRECTORS OF TEUTON RESOURCES CORP.
"Dino Cremonese"
Dino Cremonese, P. Eng.,
President and Chief Executive Officer
For further information, please visit the Company's website at www.teuton.com or contact:
Barry Holmes
Director Corporate Development and Communications
Tel. 778-430-5680
Email: [email protected]
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