Sierra Colonia Project

Property and Ownership:

The Sierra Colonia property is located in the central part of the Chubut province. It is situated 96 km east-northeast of the Cerro Solo project where the National Commission of Atomic Energy ("CNEA") identified a historical resource of 15 million pounds of contained U308 in the same geological environment (CNEA web site with information dated June 5, 2009. The resource statement is not compliant with National Instrument 43-101).

The property is 100% owned by the Company. Blue Sky has applied for three exploration licenses totalling 300 km2. One exploration license has been fully granted with an environmental impact study approved for prospecting. The approval of the two remaining exploration licenses is pending.

Property Geology and Mineralization:

Uranium mineralization is hosted in sandstones, conglomerates and tuffs of Lower to Upper Cretaceous age of the Chubut Group located in an erosional window at the Mirasol Chico Creek. Petrified wood is commonly associated with uranium mineralization.

Highlights from the prospecting work performed to date are summarized below.

Zone Width (m) Grade % U3O8 Grade % V2O5
Fluo 2 0.14 0.07
1 0.09 1.12
1.5 0.07 0.01
Zone 1 1 0.13 0.5
Zone Caņadon Lillo 0.5 0.53 1.32
Zone 5 1 0.03 0.27

Grab samples from outcrops and hand pits
Anomalous molybdenum values have been detected at Cerro Solo and are also present at Sierra Colonia, including 21 samples ranging from 113 to 671 ppm Mo.

Property History:

The Sierra Colonia project was selected following recommendations by Dr. Jorge Berizzo, Blue Sky's geological consultant, and was based on the proximity of the CNEA's Mirasol uranium occurrence and similar geological setting. The property's history is summarized as follows:Planned Exploration:

Blue Sky is confident that the exploration potential of the Sierra Colonia justifies drilling. Prior to drilling, Blue Sky will complete detailed geological mapping to better define the mineralized horizons and a geophysical survey to establish the depth of the Cretaceous sedimentary rocks.