Other Projects:

Run Lake

Key Points of Interest

  • Host to a number of uranium and base metal mineral showings.
  • Trench samples returned up to 5.43% Cu and 6.36% U3O8, while historic drilling returned 1.24% U3O8 over 6.7 metres (Cons. Van-Tor Resources Ltd DDH VT-20 1968).

A regional northeast-trending structural lineament termed the Charlot Fault, that was active during deposition of the Fair Point sediments and is host or very near to the Maurice Bay uranium deposit, continues through the Run Lake property.  One of the more interesting occurrences within the property demonstrates copper and pitchblende mineralization within faults/fractures in a mylonitic rock that are splays off of the Charlot Fault. Other mineral occurrences to the west include trench samples assaying up to 4.83% Cu in sheared, hematitic paragneisses and conglomerates, and pitchblende and uraninite as fracture fillings (North American Rare Metals Ltd. 1969 Saskatchewan Mineral Deposit Index record# 1495).

The Run Lake property consists of 14 mineral claims totaling 26,183 ha.  The property is located just outside the north-west margin of the Athabasca Basin, 20km northwest of Uranium City, within the Zemlak geological domain of the Hearne Province.
Qualified Person: The technical information in this website has been prepared in accordance with the Canadian regulatory requirements set out in National Instrument 43-101 and reviewed by Ross McElroy, P.Geol. ,President and COO for Fission 3.0 Corp., a Qualified Person.

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