The Bindal project is located in central Norway. Several mineralized outcrops have been discovered with continuous strike lengths of over 100 meters. Multiple vein systems are also located in the project area that spread over many square kilometers.

The Bindal project is an orogenic gold system. At the Reppen prospect host rocks consist of gneiss and mineralization is hosted in quartz lodes. The mineral assemblage consists of quartz-arsenopyrite-pyrite. District scale mica and hornblende schists are common at Kolsvik. Gold is strongly associated with arsenopyrite.

There are still large, un- or under-explored areas in the Bindal project

Note: The nearby mines and deposits in the region provide context for EMX’s Project, which occurs in a similar geologic setting, but this is not necessarily indicative that the project hosts similar mineralization.


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Thick quartz-arsenopyrite veins Click to Enlarge

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