The Hebecourt property straddles the boundary between the Quebec and Ontario provinces and is underlain by volcanic rocks that are at the base of the prolific Blake River Group of the Abitibi Subprovince.

The property is also located about 4 km south of the regional Destor-Porcupine Break which controls many world class gold deposits, including the Timmins gold camp.__The core of the Hébécourt property is marked by a 200-300m thick rhyolite unit that is found across the center of the property. The rhyolite is locally weakly to strongly altered to sericite and chlorite with local carbonate. The property encloses a series of VMS-style zinc and copper showings that are found mostly in felsic rocks but also locally in mafic flows. Previous work has been focused mostly on footwall-type stringer mineralization but no systematic exploration has targeted the top of the felsics where massive sulphides are more likely to occur.

In 2005, Cogitore drilled four holes specifically targeting the top of the felsic unit. Encouraging mineralization was obtained in hole HEB-02 which yielded 1.2% Zn over 7.2 metres, including 3.58%Zn over 1.0 metre. The mineralization in HEB-02 consists of "classic" stringer-style mineralization with chlorite alteration such as is typically found around VMS deposits. Drilling is scheduled at Hebecourt in 2007.

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