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Hawk Uranium Inc. Toronto, Ont., is a junior Canadian natural resource company listed on the TSX Ventures Exchange (Symbol:HUI) and the Frankfurt Stock Exchange (Symbol: HPM)
Hawk is focused on exploration for:

Gold & Silver
Holdsworth Property, Wawa Area, Northern Ontario (Operator – Hawk)
Uranium
Cluff Lake Property, Athabasca Basin, Northern Saskatchewan
Charlebois Lake Property, Northern Mining District, Northern Saskatchewan
Cortez Property, Ontario
Grand Calumet Property, Quebec
Nickel/Copper/PGM’s
McFauld’s Lake, Hawk/MacDonald-McNugget JV Property, Northern Ontario (Operator – MacDonald Mines)
Additional Holdings:
Wits Basin Precious Minerals Inc.
Directly and through its wholly-owned US subsidiary – Hawk Precious Minerals USA – Hawk owns approx.2.5% (3,482,500 shares) in Wits Basin Precious Minerals Inc. (OTCBB: WITM).
Wits Basin is currently pursuing active projects in the People’s Republic of China, South Africa, Colorado and Mexico.
Additionally, in connection with a loan extended to Wits (see news release 08-11-21), Wits has granted Hawk a security interest over the right of Wits to earn an indirect 65% interest in the company that holds the South African prospecting permits. Wits has also granted Hawk a 5-yr warrant for 250,000 shares, exercisable at $0.125
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Update
2009, A 34-hole, 5,498m drill programme for the gold-mineralized Soocana Vein System on its wholly-owned Holdsworth Gold Property, Hawk Junction-Wawa Area, Northern Ontario.
A total of 2,422 drill core samples were submitted to ActLabs in Thunder Bay for Au, Ag and 36 element ICP analysis.
An additional 90kg (250kg was initially supplied) of Black Sands material from the 4 pit locations in the Black Sands Zone have been shipped to SGS Labs, Lakefield, Ontario for additional metallurgical testing.
The drilling indicated that at surface the more predominant and continuous quartz+ankerite veins are not mineralized over the entire length and gold mineralization appears to be structurally controlled.
The exsolved sugary textured, white, crystalline quartz material occurring at the inflections of fold structures are mineralized with gold. It is believed that deeper drilling is required to test zones at depth where the fold structures flatten out and become more continuous.