Fission Expands Winter Program; Doubles Exploration Drilling - Seite 2

"The expansion of the winter program will allow us to focus to a much greater degree on the numerous regional exploration targets. PLS hosts the world's only major, shallow uranium deposit, where the high-grade mineralization starts at just 50m below the surface. With the recent discoveries of the R840W and R1620E zones, we know that the near-surface, high-grade mineralization at PLS extends along strike well beyond the current defined Triple R deposit resource estimate. In addition, not only does the Patterson Lake Corridor remain very prospective far beyond the 2.63 km mineralized trend but the parallel conductive corridors we've identified are also are very encouraging."

PLS Mineralized Trend & Triple R Deposit Summary

Uranium mineralization at PLS occurs within the Patterson Lake Conductive Corridor and has been traced by core drilling approximately 2.63km of east-west strike length in four separated mineralized "zones". From west to east, these zones are: R840W, R00E, R780E and R1620E. Thus far only the R00E and R780E have been included in the Triple R deposit resource estimate, where-as the R840W and R1620E zones fall outside of the current resource estimate window.

The discovery hole of what is now referred to as the Triple R uranium deposit was announced on November 05, 2012 with drill hole PLS12-022, from what is considered part of the R00E zone. Through successful exploration programs completed to date, it has evolved into a large, near surface, basement hosted, structurally controlled high-grade uranium deposit.

The Triple R deposit consists of the R00E zone on the western side and the much larger R780E zone further on strike to the east. Within the deposit, the R00E and R780E zones have an overall combined strike length validated by a resource estimate of approximately 1.05km with the R00E measuring approximately 105m in strike length and the R780E zones measuring approximately 945m in strike length. A 225m gap separates the R00E zone to the west and the R780E zones to the east, though sporadic narrow, weakly mineralized intervals from drill holes within this gap suggest the potential for further significant mineralization in this area. The R780E zone is located beneath Patterson Lake which is approximately six metres deep in the area of the deposit. The entire Triple R deposit is covered by approximately 50m to 60m of overburden.