Results of first ever seven-days reconnaissance program on CLARKIE following up proprietary data from a gold glacial dispersal train are significantly positive.

Main objective was to investigate Natel volcanic contact with Clarkie sediments (stratigraphic equivalent of those hosting world-class Goldcorp Eleonore gold mine), and adjacent diorite intrusions and porous conglomerates and tuffs.

On DIOS wholly-owned CLARKIE (no royalties), the Clarkie sedimentary Basin is dominated by folded wacke/ conglomerates with minor mafic volcanics and silicate iron formations. Dominant lithic wackes are locally silicified with traces to 3% disseminated pyrite/pyrrhotite particularly near contacts with mafic units and iron formations. Silicate iron formations (rusty orange gossans over a 2 km strike length) vary from one to forty meters thick. A (100-300 m thick) lapilli (block) felsic/intermediate volcaniclastic unit topped that mixed sequence. From 160 visited outcrops up to now on CLARKIE (114 claims for 70 sq. km), 88 samples were collected and assayed at ALS Global laboratory, Val d'Or, for gold (Au-AA23), incl. six blanks for quality control, supervised by Harold Desbiens, VP, M.Sc. Geo 43-101 QP.

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