Projects

• The Pearl claims cover 1,475 hectares encompassing multiple untested inferred pegmatites identified though LiDAR imagery¹.

• The inferred pegmatites have the same orientation and similar outcrop to historically mapped pegmatites² in the north and east of the property.

• Proximal to waterbodies where lake sediments are recorded as having anomalous or highly elevated results^3,4 for lithium and elements associated with LCT pegmatites⁵.

1: Ontario Ministry of Natural Resources and Forestry, accessed 24 March 2025, Forest Resources Inventory leaf-on LiDAR, Ontario GeoHub <https://geohub.lio.gov.on.ca/

2: Fenwick, K.G., 1967, Whitemud Lake area (Fredart-Whitemud lakes area), District of Kenora (Patricia Portion), Ontario Geological Survey, P0412

3: Ontario Geological Survey, 2001, Lake Sediment Analytical Data for the Sioux Lookout-Bamaji Lake Area: Operation Treasure Hunt, MRD088

4: Ontario Geological Survey, 2002, Lake Sediment Geochemical Data from the Perrault Falls Survey Area, Northwestern Ontario: Operation Treasure Hunt, MRD106

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

• 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.

• White Pine is supportive of intrusive-type uranium (an example is Rössing in Namibia) with two granitic rock batholiths intruded into an area of gneiss¹.

• Statistical analysis completed over a lake sediment sampling study containing more than 4,000 samples² and covering approximately 15,000 km² delineates White Pine as a prospective uranium target when plotting the 99.5% percentile uranium assay data.

• Very highly anomalous and extremely anomalous uranium in lake sediments compared with regional data, including values of up to 149 ppm uranium and nine samples with uranium values in excess of five standard deviations above mean.

• Radiometric survey results³ indicate an intense radiometric signature over the property, extending at least 14 km. This area aligns closely with the anomalous uranium-in-lake sediments described above.

• Minimal fieldwork to date, with no systematic or modern sampling.

1: Breaks, F.W. 1980, Sioux Lookout-Armstrong, Geological Compilation Series, Kenora and Thunder Bay Districts, Ontario Geological Survey: 2000 Series Map, NTS Number: 52.

2: Jackson, J.E. 2003, Lake Sediment Geochemical Data from the Ignace Survey Area, Northwestern Ontario: Operation Treasure Hunt, MRD118 & Russel, D.F., 2004, Lake Sediment and Water Data for the Sturgeon Lake-Wabigoon Lake Area, MRD130 & Felix, V.E., 2005, Lake Sediment and Water Analytical Data for the Eagle Lake Area, Northwestern Ontario, MRD 145.

3: Goldak Airborne Surveys 2008, Technical report on a radiometric survey, Basket Lake Block, Northwestern Ontario, Takara Resources Inc.

• The Burrows Projects comprise three under-explored properties covering 2,400 hectares in an area outlined by the Ontario Survey as a target for grassroots lithium exploration¹.

• Elevated lithium and caesium are known from deep lake sediment assays and the local geology is recognised as having potential to host lithium-bearing pegmatites².

• Historic drilling in the 1970s^3,4 within 2 km of the projects hit 5 metre-thick pegmatites that were never assayed for lithium.

1: Paju, G.F. 2019. Beardmore to Geraldton: A grassroots look for lithium in a prolific gold camp; in Report of Activities 2018, Resident Geologist Program, Thunder Bay North Regional Resident Geologist Report: Thunder Bay North District; Ontario Geological Survey, Open File Report 6352, p.55-71.

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

3: Hudson Bay Exploration & Development Co Ltd, 1973, Hudson Bay Exploration And Development Company Limited, Final Report On Exploration, Exploration Assistance Agreement. Geraldton - Beardmore Area, Thunder Bay Mining Division - Ontario, Longlac Project; Contract No. Gb-25 (Assessment Report Number: 42E15NE8354 ).

4: Moly-Ore Mines Ltd, 1965, Report on Diamond Drilling Program on Moly Ore Mines Limited, Burrows Lake Property, Area of Burrows Lake, Port Arthur Mining Division, (Assessment Report Number: 42E15NW0002).

• Bay Road covers 425 hectares directly south of the fertile White Otter Batholith.

• The property is centred on 6 km of felsic intrusive rock¹ mapped by the Ontario Geological Survey.

• The intrusive feature has a spatial relationship with highly anomalous REEs^2,3,4 in lake sediment assays, specifically “magnet metals” dysprosium and neodymium – used in the manufacture of modern permanent magnets.

1: Santaguida, F., 2001, Ontario Geological Survey,. Precambrian Geology Compilation Series - Quetico Sheet, 2000 Series Map (M2663).

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

3: Jackson, J.E. 2003, Lake Sediment Geochemical Data from the Ignace Survey Area, Northwestern Ontario: Operation Treasure Hunt (MRD118).

4: Dyer, R.D., Burke, H.E. 2012, Lake Sediment and Water Geochemical Data from the Mine Centre Area, Northwestern Ontario (MRD296).

• Ellie covers 530 ha along trend from a felsic dyke¹, with highly anomalous lithium in lake sediment results^2,3 immediately to the northeast.

• Anomalous lithium, beryllium and niobium in lake sediment results are evident in other nearby lakes.

• Located on the south-western flank of the Eye-Dashwa Intrusion – an Archean granodiorite – and a gabbroic intrusion.

• Kenorland Mineral’s (TSXV: KLD) Algoman gold and lithium project lies adjacent to the south.

1: Santaguida, F., 2001, Ontario Geological Survey,. Precambrian Geology Compilation Series - Quetico Sheet, 2000 Series Map (M2663).

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

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

• 1,175 hectare property located within a large 90 km x 40 km felsic intrusion.

• Multiple pegmatites were mapped¹ by the Ontario Geological Survey in the late 1970s but never tested or evaluated.

• The pegmatite occurrences are located in the vicinity of highly anomalous lithium, caesium and beryllium in lake sediment values².

1: Siragusa, G.M. 1977,  Esnagi Lake, Algoma District - 2000 Series Map, M2382.

2: Jackson, J.E. 2002, Lake Sediment and Water Geochemical Data from the Kabinakagami Lake Area, Northern Ontario (MRD110).

• The three Wapesi properties (Mining Creek, Altimeter Bay and Sunlight Bay) cover 2,109 hectares and are associated with the Wapesi Batholith in the English River Sub-Province, an area of intense lithium exploration.

• The Wapesi Batholith is considered fertile and prospective for the generation of LCT-type deposits, and the batholith is known to contain multiple mapped but untested pegmatites.

• The properties are located in areas of anomalous or very high lake sediment^1,2 assays resulting from elements associated with LCT pegmatites³.

• Mining Creek and Sunlight Bay lie at the interface between the granitic intrusion and the metasedimentary country rocks, a prospective location for LCT³ pegmatites.

• Altimeter Bay is in the centre of the intrusion over elevated lithium in lake sediments.

1: Ontario Geological Survey, 2001, Lake Sediment Analytical Data for the Sioux Lookout-Bamaji Lake Area: Operation Treasure Hunt, MRD088.

2: Ontario Geological Survey, 2002, Lake Sediment Geochemical Data from the Perrault Falls Survey Area, Northwestern Ontario: Operation Treasure Hunt, MRD106.

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