DUKE ISLAND PROJECT

Abundance of CU, NI, & PGE sulphide mineralization unlike any known Ural-Alaska complex
Cu, Ni, and Fe are significantly elevated relative to most Ural-Alaska complexes
Surface rock samples with up to 1.95% Cu, 0.25% Ni, and 1 gpt combined PGEs in mafic/ultramafic host rocks

Past drilling has encountered up to 387 feet of disseminated and semi-massive sulphide mineralization with copper and nickel grades
Conductivity highs occur in relation to large ultramafic bodies with four areas of outcropping sulphides
Each of the areas have potential to host several large zones of Cu and Ni enrichment at depth
Only the Marquis target has been tested – partially – by drilling

Airborne TDEM and surface NSAMT have given the Marquis target a new perspective for mineralization
Past drilling was not deep enough to test the potentially Cu-Ni-PGE enriched magmatic sulphide along the bsal contact or within a feeder zone
Each of the areas have potential to host several large zones of Cu and Ni enrichment at depth
A thick interval of semi-massive (15-25%) net textured magmatic sulphide intercepted by drilling appears as only a moderate conductive anomaly

Airborne and surface geophysical surveys indicate a possible feeder dike at depth which has not yet been penetrated