I figured more like 40km, but could be wrong. More N-NW.
They seem to be in a different sort of geological setting from Bombora though - analogous with Carouse Dam. Still, very close to the Keith-Kilkenny shear, which seems to be the railroad track between the two.
Look like they have some decent sized targets delined through auger / geochem and magnetics. Possibly applicable to other parts of our tenements (away from the dolerite)? Maybe a question for Tom.
