IMC International Mining Corp. reported additional results from the 2020 exploration program undertaken on the company’s 100% owned Thane Property located in north-central British Columbia, Canada. The Property comprises 206.58 sq. kilometers of contiguous claims that were privately owned until acquired by IMC in March 2020. The Property is located within the Quesnel Terrane, a north-south linear volcano-sedimentary belt of rocks intruded by multi-phase intrusive rocks, which hosts multiple porphyry style deposits. To the south of the Property is the currently producing Mt. Milligan copper-gold alkalic porphyry mine and to the north is the past producing Kemess calc-alkalic porphyry copper- gold mine. During the summer of 2020, exploration fieldwork completed an 8-week field program that included Induced Polarization (“IP”) surveying, petrographic studies, geological mapping, rock, soil and silt sampling with the objective of identifying prospective drill targets for the 2021 exploration season. The results reported in this release are from the Cirque Area, which comprises approximately 5 sq. kilometers of the 206.58 sq. km Property. Work at the Cirque Area consisted of approximately 1.6 sq. kilometers of geological mapping, collection of 74 rock samples in support of the geological mapping program, 1.5 line-kilometers of IP surveying, collection of 29 soil samples along a single IP line and 8 samples submitted for petrographic study. Sample 3103 was collected from a north-south trending fault zone and sample 3110 was collected from a north-south trending sulphide vein. The 77.80 g/t Au, returned from sample 3110, is the highest gold value returned to date from the Thane Property. This vein appears to have been sampled during the British Columbia Geological Survey mapping program of the Hogem Batholith in 2019. Sample GJ019-6-2 returned 8980 ppm Cu, 3330 ppb Au and 11.4 ppm Ag (Paper 2020-01, Geological Field Work 2019) and has been named the Ootes Showing. The highest copper grade of the 2020 work program was returned from sample 2319 (8.70% Cu, 1.83g/t Au and 29.8g/t Ag), located at the original Cirque Showing. This showing was discovered by IMC’s predecessor company (Thane Minerals Inc. “TMI”) but was never sampled in outcrop. It is a pervasively silicified diorite with abundant sub-vertical northwest-southeast trending quartz-epidote-chalcopyrite-pyrite veins and fractures. Very little molybdenite is associated with this orientation of veining within the Cirque Area. To the east of the Cirque Showing, potentially deep seated, structurally controlled, north-south trending sub-vertical quartz-epidote-chalcopyrite-molybdenite veins are observed cutting the diorite, quartz monzodiorite and granodiorite. These veins are noticeably absent in the area of the Cirque Showing. They appear to post-date both potassic and albite porphyry related alteration as they are noted to cut these alteration types within the area. These veins return significant levels of molybdenum, with the highest value returned from sample 3312 of 5,320 ppm Mo. The single IP survey line was established with an a-spacing of 100 metres and was oriented in a north-easterly direction due to topographic constraints. The north-easterly direction was not optimal for picking up the narrow north-south trending structures discovered during the 2020 work program.