Rua Gold Inc · TSX:RUA
Rua Gold — Investor Presentation (December 2025)
11 slides from Rua Gold's investor presentation, December 2025
Slide 1: The Glamorgan Epithermal Gold Project
The Glamorgan Epithermal Gold Project 1055 West Georgia Street, Suite 1500, Vancouver BC, V6E 4N7 www.ruagold.com
Slide 2: Hauraki Goldfield Major Epithermal Gold District
Hauraki Goldfield Major Epithermal Gold District Hauraki Goldfield >50 epithermal gold-silver deposits Mined since 1860’s, largest mined deposits in the south >15 Moz gold and >60 Moz silver produced Auckland Rua Gold Glamorgan Permit 2.8 km from WKP next big epithermal deposit? Martha Goldmine, Wai
Slide 3: Epithermal Gold Characteristics
Epithermal Gold Characteristics • Formed in active volcanic regions within fossilized geothermal cells of 3-5 km diameter with magnetically destructive fluids → Regional and Local Magnetics • Quartz veins and silicification are highly resistive → CSAMT Resistivity • Gold-silver deposited with and in
Slide 4: Glamorgan magnetic low
Glamorgan magnetic low All regional large-scale gold deposits Sutcliff (incl. WKP and Waihi) lie along an 18 km NNW-SSE chain of magnetic lows (in blue) that correspond to epithermal Wires alteration cells Sutcliff 2.5 km Ultra-detailed UAV 2.8 km WKP magnetics Rua identified 18 km two adjacent 2.5-
Slide 5: Structures from magnetic data
Structures from magnetic data Sutcliff UAV magnetics also reveal orientation of underlying large-scale regional structures that are quartz vein hosts Wires Rua-owned UAV and magnetometer 5.5 km Structures in Glamorgan UAV data are Glamorgan permit parallel to mineralised quartz veins boundary at WKP
Slide 6: Soil Geochemistry
Soil Geochemistry Au-As soil Soil geochemistry highlights high-grade geochemistry gold and arsenic enveloping outcropping quartz veins paralleling north-northeast Sutcliff (Sutcliff and Tairua) and north-south (Wires) prospects 2.5 km Sutcliff Wires Si-clay mineralisation identified from TerraSpec T
Slide 7: Geological mapping
Victoria Drill Geological Program: mapping Lode confirmed 80m below historic mine Regional volcanic geology dominated by ignimbrites covering andesite basement rocks Sutcliff 2.6 km 2.5 km Detailed geological mapping identifies Wires hydrothermally altered andesites (alteration cells) with silicific
Slide 8: High-grade gold in rock chips
Victoria Drill Geological Program: mapping Lode confirmed 80m below historic mine High-grade gold in rock chips from Sutcliff, Tairua, and Wires 43.1 g/t sample from the Sutcliff 7.3 g/t Au prospect displays colloform- crustiform banded quartz and lattice-bladed quartz after calcite, indicative of h
Slide 9: CSAMT – Resistivity at depth
CSAMT – Resistivity at depth Extensively used at WKP and Waihi to identify deeply rooted resistors/quartz veins CSAMT at Glamorgan revealed several similar deeply rooted A resistors at Sutcliff and Wires host to high-grade gold on Sutcliff surface and enveloped by highly Wires anomalous soil gold ge
Slide 10: Glamorgan Summary
Glamorgan Summary • Significant epithermal gold prospect in a major gold producing district, Hauraki Goldfield, New Zealand • Adjacent to Wharekirauponga (WKP) epithermal gold-silver project • 3-5 km diameter alteration cells typical of neighbouring Au deposits • Magnetic lineations highlight deep s
Slide 11: Rua Gold Inc. Strategic Advantage
Rua Gold Inc. Strategic Advantage • Very experienced Board and Management Contact • Proven record of bringing gold mines into production Robert Eckford CEO • Board and Management own 20% of the company email: reckford@ruagold.com • Exploring in two major gold districts (Hauraki and Reefton, Zeenat L