Fire Eye Project

The area northeast of Woodward Lake is underlain by the Middle Lake granite portion of the Archean Johnson River Inlier. Unit Wfn consists of a sheared granite which contains local inclusions of pelitic schist, amphibole, and/or metadiorite. The granite is, locally overlain by basal Wollaston Group unit Wpsn of a series of fine- to medium-grained, graphitic, pelitic to semipelitic biotite gneiss with intercalated intervals of meta-arkose and meta quartzite. The showing was described by prospectors as outcrops of felsic and mafic metasediments and boulders of poorly mineralized (pyritic) gabbro.

• SMDI 0606 – Woodward Lake showing area is underlain by the Middle Lake granite portion of the Archean Johnson River Inlier. Unit Wfn consists of a sheared granite which contains local inclusions of pelitic schist, amphibole, and/or metadiorite.
• SMDI 0606 – Woodward Lake showing area is underlain by the Middle Lake granite portion of the Archean Johnson River Inlier. Unit Wfn consists of a sheared granite which contains local inclusions of pelitic schist, amphibole, and/or metadiorite. The granite is, locally overlain by basal Wollaston Group unit Wpsn of a series of fine- to medium-grained, graphitic, pelitic to semipelitic biotite gneiss with intercalated intervals of meta-arkose and meta quartzite.
• SMDI 1710 – Middle Lake Uraniferous Pegmatite Anomalies 1, 3, 4, and 5 showing area is underlain by basal Wollaston Domain pelitic to semipelitic biotite gneiss with intercalated quartzite. These supracrustal rocks have been intruded by a series of pegmatite and aplite dykes.
• SMDI 1832 – Fire Eye Lake Uranium Occurrence is in an area underlain by Archean Johnson River Inlier cream to white quartz monzonite to granite. Locally, the Archean granites are unconformably overlain by a series of basal Wollaston Group graphitic pelitic to semipelitic biotite gneisses with significant intercalated meta-arkose, calc-silicate, impure marble, and metadiorite horizons.