Yukon · Under Option
A road-accessible gold project near Dawson City with geochemical evidence for an epithermal-style system.
Project Overview
Eureka Dome consists of 76 quartz claims approximately 55 kilometres northeast of the Golden Saddle discovery. The property is accessible by road from Dawson City and is under option to Labrador Gold.
Historical work and Pacific Ridge sampling identified gold and pathfinder-element anomalies around the Eureka Creek fault zone, supporting an epithermal-style exploration model.
76
Quartz claims
55 km
From Golden Saddle
Road
Access from Dawson
14 g/t
Historic float sample
Project Highlights
Placer gold has been reported in many creeks draining the property.
Soil work defined a gold anomaly accompanied by arsenic, antimony and mercury.
The target is interpreted as structurally controlled, epithermal-style gold mineralization near the Eureka Creek fault zone.
Geological Context
Silicified and brecciated rocks, pathfinder-element geochemistry and gold-enriched drainages point toward a high-level alteration system. Detailed mapping, prospecting and trenching are the logical tools for locating the bedrock source.
Complete Project Record
01
Eureka Dome is 100% owned by Pacific Ridge, consists of 76 quartz claims approximately 55 km northeast of Golden Saddle and is road accessible from Dawson City. The property is under option to Labrador Gold Corp. under an agreement announced May 11, 2026.
02
Placer gold occurs in many creeks draining the property. Geochemical anomalies and silicified, brecciated rocks support a high-level epithermal alteration model; reported pathfinder values include arsenic to 3,000 ppb and mercury to 17 ppm.
Historical workers reported breccia float to 14 g/t gold and silt values to 2,190 ppb gold. Pacific Ridge reconnaissance defined a gold-mercury-molybdenum-antimony soil anomaly requiring detailed follow-up.
03
The 2017 soil survey defined a gold anomaly accompanied by arsenic, antimony and mercury. The source is interpreted as structurally controlled epithermal-style gold mineralization associated with the Eureka Creek fault zone.
Historical stream samples downslope of the anomaly ranged from 360 to 2,190 ppb gold. Detailed mapping, prospecting and trenching were identified as the next steps for locating the source.