Iva

• Iva is a 642 hectare property centred on anomalous lithium, caesium and beryllium lake sediment^1,2 assay results.

• Positioned at the interface between granite and metasedimentary lithologies³, a favourable setting for LCT pegmatites⁴.

• Nearby lithium projects highlight regional potential: Patriot Lithium's Bull Project sits 11 km to the east, and the Niobe-Nym Lakes LCT pegmatites lie 20 km away – both are associated with the same intrusion as Iva.

1: Dyer, R.D., 1999, Lake Sediment and Water Geochemistry Data from the Atikokan-Lumby Lake Area, Northwestern Ontario (MRD043)

2: Jackson, J.E., 2001, Lake Sediment and Water Geochemical Data from the Shebandowan Lake Area, Northwestern Ontario (MRD076)

3: Pirie, J. 1978, Ontario Geological Survey Crooked Pine Lake, Rainy River District Geological Map #M2405

4: Bradley, D.C., McCauley, A.D., Stillings L.M., 2017, Mineral-Deposit Model for Lithium-Cesium-Tantalum Pegmatites, USGS.