Roughrock REE Project

100% owned 720 hectare Rare Earth project with bastnaesite and allanite occurrences.

  • 100% owned, 720 hectares, Greenfield Rare Earth Project, No underlying royalties

  • Bastnaesite occurrence within the claim blocks, with Allanite Group minerals (Cerny and Cerna, 1972)

  • Bastnaesite, a cerium fluoride carbonate (CeCO3(F)), found in contact or alteration zones.

  • The Allanite/Bastnaesite minerals, Cesium and Lanthium minerals, were identified within biotitic granite intrusives where sorting by physical flow in a crystal-mush environment occurred. This mineral segregation is commonly referred as a schlieren. Cerny et al 1972 identified Allanite within leucocratic, pegmatitic schlieren along the south shore of Roughrock Lake.

  • Located on the Winnipeg River 9 miles NNW of Minaki, in western Ontario. Geology of this Precambrian area was described by Derry (1930). The bedrock is mostly granitic with a few disseminated bands of amphibolite biotite gneiss and derived migmatites Allanite is fairly common in the pegmatitic bands, attaining up to 10x30 mm in size (Cerny and Cerna, 1972).

  • Rare-earth elements found in bastnaesite can be used to produce magnets in speakers, microphones, and vibration monitors in mobile phones and other high-technology communication devices.

  • In 1949, it was discovered at Mountain Pass, in California, USA

Map showing the occurrence of Bastnasite, Tonalite to Granodiorite, and Granodiorite to Granite near Big Sand Lake and Roughrock Lake, with insets of Kenora and Dryden in Ontario, Canada.

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Map showing designated company project areas outlined in blue, including Harfred, Junior Lake, and other locations, with markers for nearby towns and landmarks such as Sturgeon Falls, Evansville, and Crystal Falls.