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The tenement application is centered approximately 600km northeast of Perth and 38 kilometres south east of Lake Mason homestead in Western Australia.

The 91km2 tenement covers greenstones and granites along the western margin of the Archaean Booylgoo Range greenstone belt. The greenstone sequence is tightly folded into the Mt Anderson syncline, and comprises a layered succession of metamorphosed mafic igneous rocks, minor felsic volcanics with Banded Iron Formation (BIF) and other sedimentary rocks. Metamorphic grades are believed to be lower greenschist facies.

There are 20km of mapped BIF on the tenement, but in the non-outcrop areas these need to be drill tested for potential hematite/goethite deposits.

It is considered that potential exists in the area for substantial deposits of iron ore, and possibly gold, and base metals.