Benton Resources Inc. announced that it has discovered wide zones of mineralization at the Company's Far Lake IOCG project ("Far Lake") including 0.15% Cu and 0.15 g/t Ag over 60.4 m, including 0.35% Cu and 0.51 g/t Ag over 15.6 m and 1.08% Cu and 1.63 g/t Ag over 2.6 m in drill hole FL-20-11. Drill hole FL-20-11 is located approximately 1,800 m NW along the same structure as the Far Lake discovery zone where surface sampling produced Cu grades up to 22% over 0.7 m. Drill holes FL-20-01 to FL-20-05 completed in the discovery zone yielded results including 0.19% Cu and 0.34 g/t Ag over 33.6 m, including 1.11% Cu and 1.33 g/t Ag over 3.1 m (FL-20-03). The Far Lake project, pursuant to which the Company currently holds under option from White Metal Resources Corp., is located 80km west of Thunder Bay, Ontario. FL-20-01 to FL-20-05 were shallow holes and mineralized targets were interrupted by a series of diabase dykes and sills. Future drilling in this area will therefore be deeper to avoid intersecting these younger mafic intrusions. The Company is very encouraged by the Cu mineralization intersected in almost every hole and confirms that there is a direct correlation between Cu-sulphides and the two NW trending structures that cross the property. In December 2020, the Company hired Abitibi Geophysics ("Abitibi") to complete a 3D DasVision IP survey which is nearing completion. Preliminary data has identified chargeability targets between 350- 800 m in depth that coincide with the FL#1 and FL#2 structures which contain and appear to be controlling the Cu mineralization discovered to-date. The DasVision, distributed array survey, is designed for deep mineral exploration, up to 1,000m depth. Benton will rely on this new dataset to expand its exploration at depth. Drill holes FL-20-01 to FL-20-05 were shallow holes drilled over a 200m strike length into the Far Lake discovery zone and were all interrupted by diabase dykes/sills. Drill hole FL-20-06 intersected a silicified breccia in and E-W interpreted structure with no significant Cu results. FL-20-07 was drilled approximately 2 km south of the main Far Lake copper zone. The hole was designed to test two parallel EM conductive anomalies on the northern edge of the Shebandowan greenstone belt. Alteration and pyrite mineralization were abundant, but no significant results were received. Drill hole FL-20-08 was drilled to test a new gold occurrence (trace to 970 ppb Au) which was identified by Benton along the north shore of Kabaigon Lake. Drill results included 0.23g/t Au over 1.6m. Drill hole FL-20-09 and FL-20-10 were drilled as a fence to test a 250-300 m width of the Two-Pond structural zone that contains chalcopyrite and abundant silicification on surface. Both holes intersected intense epidote alteration and fine chalcopyrite, mineralized in small quartz veinlets flooded throughout a metasediment over several metres. Drill hole FL-20-11 was designed to test Cu mineralization below the trenches dug by Benton in 2020, along strike of the discovery zone. This area contained the highest Cu-in-soil assay values with coincident anomalous Cu in trench sampling. The hole was drilled approximately 100m south of the widest soil anomaly and intersected large, silicified zones, breccias, epithermal style veining and intense sericite and epidote alteration. Highlights include 0.15% Cu and 0.15g/t Ag over 60.4m, including 0.35% Cu and 0.51 g/t Ag over 15.6 m and 1.08% Cu and 1.63 g/t Ag over 2.6m. Drill hole FL-20-12 was drilled below the highest Cu-in-soil anomaly on the property located along the FL#1 structure plus outcrop containing chalcopyrite (with malachite and azurite). This hole was the deepest of the drill program which ended at 297 m in a rusty red highly magnetic granite. Abundant magnetite is often associated with fine-grained, disseminated chalcopyrite.