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Cedartree Property

The Cedartree Lake gold property is located approximately 80 km southeast of the town of Kenora, Northwestern Ontario, about 15 km east of Sioux Narrows, a small village along paved highway #71, between the towns of Kenora and Fort Frances. From Sioux Narrows the claims are easily accessible by heading east, 12 kilometres, on the Cameron Lake Road.

At first glance the most striking aspect of this property might be its high grade gold zone that occurs within 15m of surface and less than 200m from the main Cameron Lake Road. But the property is much larger. It is comprised of 198 claim units which cover approximately 8,000 acres and is host to numerous gold showings, shear zones, sulfide-rich areas that have never been drilled. With only a shoe-string budget in 2013, exploration resulted in both the discovery of a zinc and copper zone associated with the Stephen Lake intrusion, and the extension of the main gold zone to the south. A sizeable trenching and drilling program is necessary to systematically develop this severely under-explored property, which overall has only experienced limited activity. With a proper budget, significant growth to the main gold resource is expected since several structural extensions have been identified through examination of cross-sections in 2016.

Earlier exploration work by the Company confirmed the presence of gold mineralization along fracture and shear zones which transect an intermediate composition (granodiorite-quartz diorite) dyke/sill possibly related to the Stephen Lake intrusion. Alteration associated with these fracture and shear zones is comprised of ankerite, sericite, silica, chlorite and pyrite.

Gold occurs within all three rock types found on the property (gabbro, intermediate intrusive, and volcanic tuffs). Silica flooding and the presence of gray quartz veins and veinlets is typically evident of higher grade gold mineralization; at least two generations of quartz veining are found in drill core: gray quartz which usually carries fine to course grained (remobilized?) gold and white fracture-fill veining. Multi-metre wide zones of <1cm-5cm of banded pyrite occur throughout the felsic-intermediate intrusive and typically contain higher gold values particularly when hydrothermally altered.

Several east-west trending steeply dipping shear zones which truncate the granodiorite intrusive contain impressive gold values.  The main shear zone has been given an Initial Resource Estimate (see March 12 2012 NI 43-101 Technical Report) as summarized in the table below:

+ Gold Channel: Plan View & Long Section


On June 1, 2018 following meetings and discussions with local indigenous community members, Metalore launched an exploration program in the area shown below:

2018 exploration along the gold corridor resulted in the discovery of an altered and mineralized granodiorite which yielded surface values. Observations of a dioritic to granodioritic intrusive to the southwest shows a possible connection between this intrusive and the main, gold enriched granodiorite to the northwest. This newly discovered intrusive network adds great potential for additional gold resources at Cedartree.

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