First Cobalt Acquires Rights to Contiguous Property at Keeley-Frontier

TORONTO, ONTARIO--(Marketwired - Jul 18, 2017) - First Cobalt Corp. (TSX VENTURE:FCC)(FTSSF) (the "Company") is pleased to announce the it has secured an option to acquire 100% rights on a prospective mining claim adjacent to the Keeley-Frontier project in the Cobalt, Ontario mining camp.

Highlights:

  • The property joins First Cobalt's properties to the east and west, further consolidating the land surrounding Keeley-Frontier

  • The property contains known mineralization, which could be associated with a fault structure that also hosts the Wettlaufer silver-cobalt mine

  • Work will commence to determine the continuity of the Wetlaufer fault structure and to test if cobalt-rich veins systems similar to Bellellen and Frontier occur in this area

Frank Santaguida, Vice President, Exploration commented:

"Expansion of First Cobalt's property to the east of the Keeley-Frontier increases the opportunity to explore for the extensions to this silver-cobalt vein system; especially those that are cobalt enriched. This eastern area has largely been forgotten due to the low silver versus high cobalt characteristic. This transaction demonstrates our commitment to consolidate the meaningful property positions within the Camp our strategy to be the first to approach this camp from a bulk mining perspective."

Property Overview

The centre of the claim is over 500 metres west of the Keeley-Frontier deposit (Figure 1) and approximately 1.5 km south of the Bellellen Mine, which boasts an average grade of 9.25% cobalt and 11.55% nickel from over 12 tons of ore that were once shipped (McIlwaine, 1970). This area east of Keeley-Frontier also contains the Haileybury Mine, which is also cobalt- and nickel- rich and relatively low in silver, thus only minor working and drilling has been done here.

The claim itself covers a mineral occurrence with a 64-foot shaft excavated on a series of calcite veins containing cobalt mineralization within Nipissing Diabase rock (McIlwaine, 1970). Material found beside the shaft includes calcite veins approximately 20cm in width. McIlwaine reports samples of the veins returned up to 20 oz per tonne silver. Two holes, both less than 50m, were drilled in 1951 in the southern portion of the claim intersecting minor silver and cobalt veins. The veining is interpreted to be associated with the extension of the Wettlaufer fault structure, which hosts the high grade Wettlaufer silver-cobalt mine that historically produced over 375 ounces per tonne Ag intermittently between 1909 and 1940 (Guindon, 2016). At times, cobalt was also extracted for a total of over 23,000 lbs. The host rock to the Wettlaufer deposit is also Nipissing Diabase.