Get in Touch

Unlisted Syracuse Gold - Private property. Patented mineral rights & surface rights. Copious past production from proximity mines make this a high potential, tier one, Canadian brownfield opportunity.

 

The surrounding cluster of quartz carbonate vein systems within 4km of Syracuse has produced a staggering 53 million gold ounces since 1910. (compare with entire State of Alaska total ounces mined 40m oz. and entire State of Nevada 155m oz. since 1835)

 

Gold Veins at Syracuse were first discovered in 2008 representing the only new vein system discovered in nearly a century within the core mining complex. The footprint at surface is now very similar in all aspects to the cluster's largest mines.

 

Presently seven continuous parallel vein sets of different age and composition are exposed and trac able on outcrop. Several sets are exposed and trac able for 700 feet each and continue into overburden on each end. Combined, thousands of feet of vein exposure have been revealed. The shear sequence comprised from central series basalt hosting these veins is minimum 100m wide striking strategically on the property for approx. 600m.

Syracuse Geology represents some of the most impressive high strain events in Central Timmins. This transcurrent tectonic intersection with it's deformation intensity should be directly correlated to vein widths at depth, degree of porosity, flow volume and the non ability for the system to seal, resulting in repeated reactivations within these zones of permanent weakness. Syracuse is a major conduit in the core mining cluster, a root of the Central Timmins plumbing system and primary target for additional high potential ore.