EMX’s Ringerike/Ertelien project is located just north of Oslo and is situated along the Langdalen mineralized trend. Ni-Cu-(Co) mineralization occurs as remobilized semi-massive to massive sulfide within mafic dykes.

Nearby magnetic highs could potentially be the causative mafic intrusive body and is potentially a large intrusion with a bottom loaded sulfide cumulate. There are historic Ni-Cu-Zn Co mines and prospects on EMX land position and surrounded properties.

EMX believes that application of modern and updated mineral deposit models and new exploration technologies will likely result in new discoveries at Ringerike/Ertelien.

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 tonnages or grades of mineralization.



Ringerike/Ertelien project geology and minerals occurrences Click to Enlarge