Prosper Gold Corp. provides update the progress of the Phase 1 drill program at the Currie Project (the “Property”) southwest of Matheson, Ontario. 3 holes for a total of 1,002m were drilled, logged, and sampled in December. Assay results will be released when they are received and compiled. The drill is now back on site to complete the remaining 1,500m of Phase 1. The 2,000 hectare Currie Project, 8 km south of the Destor-Porcupine fault, is underlain by altered volcanic and metasedimentary rocks of the Abitibi greenstone belt. The property hosts the Grindstone Creek occurrence, a Gold-Silver-Zinc zone in massive and semi-massive pyrite-sericite schist (GCZ). The sequence strikes ESE and dips steeply southwest as interpreted from drilling. Rocks are strained and especially the felsic volcanic rocks show a strong SW dipping single phase fabric into which any earlier layering would have been transposed. Diabase, a dyke or sill, dips steeply with the strata. Drill intersection modeling shows it is a branching anastomosing unit or swarm with two or three separate arms. The diabase envelope trends ESE, dips steeply, and is about 70m at its thickest. Overburden thickness is consistently about 50 m as shown by the earlier holes and the geology is inferred from drill results to date and from geophysical data, mainly airborne magnetics. Known mineralization is between 120 m to 300 m below surface and occupies a zone about 300 m long, 100 m wide.