Pilley’s Island Project
Overview
The Pilley’s Island Project hosts high-grade VMS mineralization with a rich mining history and strong exploration potential
Geology and Mineralization
Geology
- Pilley’s Island is located within the Notre Dame Subzone of the Dunnage Tectonostratigraphic Zone
- Most of the Project is underlain by Ordovician submarine volcanic rocks of the Roberts Arm Group which is regionally identified as part of a mature arc sequence referred to as the Buchans-Roberts Arm Belt that also hosts the historic Buchan’s mine.
- Mineralization occurs as low grade (Spencer’s Dock); medium grade (Old Mines); and high grade (3B-Zone/Clifford Jones).
- The deposits that are of both sub-seafloor replacement and exhalative varieties. The deposits are often flanked by extensive chlorite, sericite, silica, K-feldspar and epidote alteration often observed in bimodal-felsic VMS systems.
The Spencer’s Dock area displays sericite/silica alteration that generally increases in intensity near mineralized zones, while the 3B / Old Mine areas display sericite/silica alteration that is abundant but less widespread and is more intense when proximal to mineralized zones.
Mineralization
From north to south this Project is underlain by:
Newfoundland, a World-Class Jurisdiction
Tier-1 Mining Jurisdiction
- Established mining ecosystem with strong government support
- Mining sector contributes ~32% to GDP
- Readily available, skilled labor force
- Friendly and transparent mine permitting
- Rated top 6 globally in 2024 by Fraser Institute
- Hydro power abundant throughout Newfoundland
Pilley’s Island
- Project is accessible 365 days a year by road, air and sea
- ~45min drive from Springdale via Hwy 380N
- Excellent infrastructure, hosts past producing mines
- ~150km from Pine Cove Mill and Port by way of major roads
Why VMS (Volcanogenic Massive Sulphide)?
VMS Deposits are Polymetallic, High-grade and Understood Geologically
Polymetallic Revenue Streams
• Copper, zinc, lead, gold, silver (± cobalt) in a single asset
• Diversified exposures reduces reliance on a single commodity and provides a natural hedge against price volatility
High Grades & Strong Economics
• VMS deposits are known for compact footprints with robust grades in copper/zinc
• By-products (gold/silver) lower effective cash costs
Geological Predictability & Camp Scale
• Well-understood geological model; exploration is de-risked
• VMS deposits occur in clusters - one discovery often leads to several
Strategic Alignment
• Supplies critical metals for electrification (copper, zinc, cobalt)
• Governments and majors increasingly prioritizing securing supply, VMS systems are
a priority given multiple commodities present
M&A & Exit Potential
• Juniors advance discoveries, natural acquisition targets for mid-tiers/majors
• Track record of premium takeouts in established VMS camps (Noranda, Kidd Creek, Flin Flon, Iberian Pyrite Belt)
