The Pimaco occurs at or near the contact between rusty-weathering argillites, siltstone and quartzite of the Middle Proterozoic lower Aldridge Formation (Purcell Supergroup), and turbidite wackes and laminated siltstone of the middle Aldridge Formation.
Cassiterite, scheelite and wolframite bearing quartz-greissen veinlets occur in Moyie diorite sills within the Aldridge rocks.
The contact is a favourable horizon to Sullivan-type mineralization on the property.