Crater Lake
The Crater Lake Project is located 200 km northeast of Schefferville, Québec and is accessible via fixed-wing aircraft or helicopter. The property consists of 96 contiguous claims covering 47.0 km2 and are owned 100% by Scandium Canada Ltd.
Crater Lake Geology
The property lies in the Churchill Province in the southwestern region of the Mistastin Batholith (1.4Ga). The Mistastin Batholith covers an area of approximately 5,000 km2. The dominant lithologies are granite and pyroxene-bearing quartz monzonite. It is cut by younger biotite hornblende granite, which is in turn cut by a 6 km diameter olivine quartz syenite, the Crater Lake Intrusive Complex. The dominant exposed lithology is a massive syenite, which contains 1 to 10% of interstitial ferromagnesian minerals. A melanocratic unit, ferrosyenite to alkali pyroxenite, contains more than 50% ferromagnesian minerals, including cumulate fayalite, hedenbergite and ferropargasite, occurs as discontinuous layers, sills and amoeboid-like inclusions or dikes. The unit appears to correspond to several concentric magnetic high features observed at the periphery of the Complex related to a caldera collapse ring-dyke structure.
In 2007, as part of a regional evaluation program, one sample collected in the area that is now the Crater Lake Project returned high concentrations of iron oxide and rare earth elements (REE). This information was inherited by Quest Rare Minerals Ltd (QRM) and lead to the “Discovery Outcrop” in 2009. Since 2009, various geochemical and geophysical programs were conducted followed by numerous prospecting, mapping, and diamond drilling programs.
In 2014, QRM intersected a 225 m long scandium (Sc) and REE bearing zone within a thick ferrosyenite layer at the Boulder Zone with a 27.6 m interval grading 351 g/t Sc2O3 and 1.72% REE. Review of the drilling data also returned a 19 m long interval grading 506 g/t Sc2O3 along the western side of the Crater Lake intrusion.
In 2018, Scandium Canada conducted a field campaign consisting of detailed prospecting and geological mapping over three highly prospective scandium targets, the TGZ, STG and Northern Target areas. All targets are characterized by large, strongly magnetic anomalies of variable strike length up to 750 metres. A strongly magnetic, iron-rich pyroxenitic boulder was found 300 meters north of the STG Target and returned 920 g/t Sc2O3. This iron-rich sample is very similar in composition and texture to a sample that was located to the northeast of the Crater Lake intrusion (up-ice from this target area), which returned up to 2,506 g/t Sc2O3. No ferrosyenite outcrops or boulders were observed near the Northern Target.