LaSalle Exploration Corp. announced assay results for seven holes drilled as part of the maiden drill program on the 100% owned Radisson Property located in the Eeyou Istchee ? James Bay Territory, Qu?bec. These holes tested both the Goldhawk and Goldfang zones, discovered late in the 2020 field season by surface prospecting, and which occur within an extensive, gold enriched structural corridor that extends more than 8 kilometres to the east/southeast onto the neighbouring Serpent property, that is actively being explored by Harfang Exploration Inc. Goldhawk Zone: Three drill holes totaling 763 metres tested the Goldhawk Zone over 100 metres of strike length. All three holes intersected the 10 to 25 metre wide Goldhawk Main Shear Zone. In addition, a 3 to 6 metre wide shear zone was intersected at shallow depths in each of the drill holes. Both shears consist of 1-3% laminated sheared quartz veins with 1 to 3% pyrite. The diorite host wallrock locally contains up to 5% pyrite. The shears are also characterized by intense alteration along with iron oxide staining and pyrite mineralization. The main shear intersections ranged from 1.37 to 1.64 g/t over 10 to 22 metres, with higher grade intersections up to 15.85 g/t over 0.50 metres. The shallow shear intersections ranged from 1.09 to 2.13 g/t over 3 to 6 metres. Both well mineralized shear zones are hosted within a 50 to 75 metre wide gold anomalous (i.e., >0.050 g/t gold) zone. There is strong assay support for the high-grade intersections with gold grades in the adjacent sheared diorite wallrock ranging from 1.10 to 6.37 g/t over 1 to 3 metres. Ongoing prospecting discovered the Goldhawk Extension 1 km west-northwest of the current Goldhawk drilling. This discovery is characterized by a 1 to 3 metre wide shear zone hosted in altered diorite with 5-10% laminated quartz veins. Mineralization in the quartz veins consists of 0.5 to 2% pyrite and locally up to 5% pyrite in the host diorite with occurrences of visible gold noted. Goldfang Zone: Four drill holes totaling 408 metres tested the Goldfang Zone over 100 metres of strike length. Gold mineralization was intersected in one of these drill holes. The intersection consists of quartz veins with 1-2% pyrite and pyrrhotite hosted in altered amphibolite that returned 7.74 g/t over 1.13 metres. Silver and base metal mineralization was intersected in two of these drill holes. These intersections contain anomalous to high grade silver, up to 219 g/t, anomalous copper, with values up to 1,040 ppm and anomalous to high grade molybdenum, with values up to 4,910 ppm. This mineralization is hosted in narrow quartz veins and irregular fractures with 1-2% disseminated chalcopyrite, pyrite, pyrrhotite and molybdenite within altered amphibolite and felsic dykes. These metre scale intersections are part of wider (i.e., 2 to 7 metres) zones with anomalous values.