The property is located southeast of Amos, in the eastern part of the Abitibi Greenstone Belt.

It is dominantly underlain by quartz-phyric rhyolites, rhyolitic lapilli to block-size tuffs, agglomerates, dacites, narrow bands of clastic sediments and argillites. Compilation of data revealed that the large (250 m x 3km) and strong hydrothermal system associated with Cu-Zn mineralization qt the Landome VMS deposit is but one part of an 8 km long alteration zone that continues to the east into the whole Landrienne property. Numerous drill intersections showing elevated copper and zinc values are found at Landrienne and, significantly, the chemical signature of rhyolites at Landrienne is typical of that found in highly prospective VMS mining camps of the Abitibi belt (such as at as Kidd Creek).

Deep penetrating TDEM surveys have now been completed over most of the property and surface conductors have all been tested either by Cogitore or by former property owners. A limited amount of field work is proposed in the vicinity of the last two holes of the 2005 campaign in order to assess the significance and strength of alteration observed in the recent (2005) drilling. Surface showings around the drilling area will be examined to better understand the volcanic facies. Pending the results of this work, a decision will be made as to whether to continue or terminate the project.

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