Voltage Metals Corp. announced that it has completed a diamond drill program at the Company's 100% owned St. Laurent Nickel-Copper-Cobalt Project, located 160 km northeast of Timmins, Ontario.

The drilling consisted of 2,460 metres in seven holes, with downhole geophysical surveys completed on six of the seven holes.  A total of 570 samples, representing 800 metres of core were split for analysis.  All samples have been shipped to the lab, with results expected periodically over the next eight weeks. The St. Laurent Project has received minimal exploration activity since the initial work in the mid 1960's when nickel-copper mineralization was first identified in a limited number of shallow drill holes.

Subsequent airborne geophysical surveys defined a strong electromagnetic (EM) anomaly with an associated bullseye magnetic response, both of which are coincident with the reported disseminated mineralized zone. Diamond drilling in 2008 and 2019 identified geological characteristics indicative of gabbro breccia/conduit hosted nickel mineralization similar to the Lynn Lake Deposit (28.4 million tons at 0.91% Ni, 0.49% Cu) the Kenbridge deposit (7.5 million tonnes at 0.58% Ni, 0.32% Cu), and the Montcalm Deposit (3.9 million tonnes at 1.3% Ni, 0.67% Cu, 0.05 Co). The recently completed drill program followed up on the results of the 2019 diamond drilling, where the highest nickel grades on the project were intersected with three separate intervals of >1.0% Ni, as well as the widest intersection (113.4 m) of lower grade nickel mineralization. Nickel assays in conjunction with the associated sulphur results indicate a high nickel tenor1 of 5% Ni for massive sulphides (35% S) in the magmatic system.

 Two priority Borehole EM anomalies from the 2019 program and a deeper Heligeotem II Anomaly modelled from a 2007 Survey were also targeted in this drill program. A 285-line km Geotech VTEM survey has been completed on the Jerry Lake Project, situated 57 km northwest of the St. Laurent Project.

The Jerry Lake gabbro represents the only sizeable gabbro body within the Burntbush Assemblage outside of the St. Laurent Gabbro. The Jerry Lake property has never been evaluated with an airborne EM survey, nor has any ground-based exploration been conducted.

A well-defined glacial dispersal fan2 of chalcopyrite and nickel suggests the unrecognized Ni-sulphide potential of the Jerry Lake Gabbro.