Fission Hits Off-Scale on Land, 555m West of Triple R - Seite 2

R600W High-Grade Zone:

PLS15-343 (line 615W) is the 6^th hole defining the R600W zone and represents a very significant upgrade to the strength and width of mineralization of the R600W zone. The hole was collared as an angled hole collared 10m south of PLS13-124 (strongest interval returning 0.29% U3O8 over 6.5m, see new release Feb 05, 2014). Due to technical difficulties completing the hole, the hole was terminated at 368.0m. A down-hole gamma survey could only be completed to 129.7m depth, ending within a strongly mineralized interval. Overburden continues to 99.2m, immediately underlain by Devonian sandstone to a depth of 108.6m which overlies basement rock. The basement lithologic sequence from 108.6m to 156.0m is comprised primarily of pelitic gneiss becoming graphitic from 142m to 156m. From 156m to 368m, basement lithology is predominantly a semi-pelitic gneiss. A total composite of 69.5m of mineralization within 2 discrete intervals of variably weak to strong radioactive mineralization was intersected from 105.5m to 346.0m. Weak mineralization extends into the overlying Devonian sandstone. The strongest mineralization is present from 118.0m - 134.0m which includes 9.31m of >10,000 cps, including 8.85m of continuous >10,000 cps with peaks up to 52,900 cps. A lower zone of strong mineralization is present from 141.5m - 150.5m which includes 0.46m of >10,000 cps in 4 narrow discrete intervals.

Hole ID	Zone	Collar			* Hand-held Scintillometer Results On Mineralized Drillcore (>300 cps / >0.5M minimum)				Sandstone From - To (m)	Basement Unconformity Depth (m)	Total Drillhole Depth (m)
		Grid Line	Az	Dip	From (m)	To (m)	Width (m)	CPS Peak Range
PLS15-343	R600W	615W	349	-64.7	105.5	171.0	65.5	<300 - 52900	99.2 - 108.6	108.6	368.0
					342.5	346.5	4.0	<300 - 550

Natural gamma radiation in drill core that is reported in this news release was measured in counts per second (cps) using a hand held RS-121 Scintillometer manufactured by Radiation Solutions, which is capable of discriminating readings to 65,535 cps. The reader is cautioned that scintillometer readings are not directly or uniformly related to uranium grades of the rock sample measured, and should be used only as a preliminary indication of the presence of radioactive materials. The degree of radioactivity within the mineralized intervals is highly variable and associated with visible pitchblende mineralization. All intersections are down-hole. All depths reported of core interval measurements including radioactivity and mineralization intervals widths are not always representative of true thickness and thus true thicknesses are yet to be determined.