Discovery­Corp Enterprises Inc. and Scramble Resources Corp. announced encouraging results from the confirmation drill program completed at the NewFind Gold Project. The 500 metre (m) Clifford target was confirmed to host high grade gold mineralisation within a multi-metre anomalous gold-bearing halo associated with increasing silica, sericite and disseminated sulphide mineral content.

The Clifford target was evaluated across three drill fences roughly spaced 250 m apart and evaluated to an average depth of approximately 50-60 m below surface; the target is open along strike and down dip. Exploration Summary: The initial drill program on the NewFind Gold Project was a confirmation or due-diligence-type program on the most advanced target, the historic Mt Clifford Mine, a 500 m long section of the Clifford Structure. This work was undertaken to determine the style(s) and tenure of mineralization that could be expected within large scale gold-in-soil anomalies on major structures in the area associated with mapped folds.

Previous work at Clifford included small scale underground mining, and rotary air blast (RAB) and reverse circulation (RC) drilling. As this is a structurally controlled gold target, diamond drilling (DD) was used to better identify lithology, alteration, structure, and mineralization styles controlling the values in the historical results. The confirmation drill program evaluated three fences across the Clifford Target each separated by approximately 250 m. The program, designed to test and step-out from select historical drillhole locations, was successful in its objective; returning consistent, and in some cases, better results than previous drilling, and providing confidence in continuity of mineralization.

Additional drilling will be required to follow-up the potential extent of the Clifford Target mineralization, as well as drill testing of the full pipeline of targets that were developed, based on thorough geological investigation using field mapping, geophysical surveys and geochemical surveys across the core area of the tenements. The Clifford Mid confirmation drill fence consisted of three holes, 21LNDD005-006, and 010. All holes cut a strongly deformed, folded and sheared, package of mixed sedimentary units and ultramafic rocks.

Elevated gold values (up to 57.75g/t Au) are associated with quartz- carbonate veined, carbonate- albite- silica- sericite altered volcaniclastics interfolded with pyritic black shales within or adjacent to parasitic fold hinges in high strain zones. In this section, an ~3.5 m interval of disseminated sulphide (pyrite- arsenopyrite- pyrrhotite) bearing porphyry cut by late extensional quartz- carbonate veining yielded a section grading 3.60 g/t Au. 21LNDD005 confirmed the high-grade interval in WILRC9712 and identifies continuity of two other zones in historic drill hole RC055.

21LNDD006 confirmed the intervals within historic hole RC055 and 21LNDD010 stepped approximately 40 m down dip and intercepted the target zone and the upper sections of the drill hole indicate potential for a new mineralized zone developing. The Clifford South confirmation drill section consisted of three holes, 21LNDD007-009, all cutting the corridor of strongly deformed mixed sedimentary and ultramafic rock units. As with the other sections, the best grades are associated with quartz-carbonate veining and disseminated sulphides within an alteration zone of in silica- carbonate- sericite- (±albite).

More specifically the best intervals are closely associated with the high strain zones exhibiting inferred mylonitic breccia and parasitic fold hinges. Hole 21LNDD008 confirmed the mineralization in historical hole WILRC9709; however, the diamond drilling indicates the mineralized zones are more discreet. Hole 21LNDD009, an approximate 25 m undercut of 21LNDD008, intercepts a wider section of anomalous gold bearing stratigraphy; the mineralization appears to be down dip and trending to the southeast.

The Clifford North confirmation drill section consisted of four drill holes, 21LNDD001 ­ 004. Three of four holes intersected the structural zone of interest. Elevated gold values appear to be associated with very fine-grained disseminated pyrite and arsenian pyrite within strong silica- sericite- carbonate altered and stockwork veined folded volcaniclastic sedimentary sequence with local sheared quartz-carbonate veining.

This alteration and mineralization appears to be spatially associated with porphyritic intrusive units and associated with folds within higher strain portions of the structural corridor.