Eastmain Resources Inc. reported the completion of its fall 2019 20-hole drill program (5,152 m in total) with results from 13 (thirteen) holes (3,654 m) at the Company’s 100%-owned Clearwater Property. The 13 reported holes tested targets eastwards along 4.5 km of the Knight Serendipity meta-sedimentary horizon (KS Horizon) beginning in the Caradoc area. The holes tested trenched geological features as well as soil, rock and VTEM anomalies obtained over the 2019 exploration campaign. Holes ER19-856 to ER19-858 and ER19-865 to ER19-868 did not intersect significant results includes drilling to the east of the Percival discovery focused initially on the Caradoc showing area with 7 holes testing approximately 1 km of strike length along the southern limb of the KS Horizon, including the previously reported hole ER19-855 (0.26 g/t Au over 26.9 m including 0.45 g/t Au over 10.5 m). Holes ER19-856 to ER19-861 targeted stratigraphy comprising banded iron formation (BIF), mafic epiclastics, mudstone and graphitic mudstone rocks with exposures of sedimentary breccia and silicified sedimentary breccia, identified through mapping and trenching. Holes ER19-855, ER19-856 and ER19-860 were drilled on a single drill section, intersecting parallel east-west units of locally brecciated iron formation within a package of variably graphitic mudstones which are also locally brecciated and silicified. Hole ER19-860, drilled below hole ER19-855 intersected a continuation of silicified breccia in BIF returning an anomalous interval of gold mineralization (0.13 g/t Au over 5.0 m). A section drilled immediately adjacent to the main Caradoc trench comprising holes ER19-857 and ER19-858 intersected a 32 m interval of iron formation flanked on the north by variably graphitic mudstones intruded by narrow felsic dykes and on the south by mafic epiclastic sediments underlain by basalts. Strong gold mineralization related to BIF at the Caradoc exposure, including the discovery sample of 10.3 g/t Au were not repeated in these drill holes. Holes ER19-859 and ER19-861 tested the KS Horizon sequence approximately midway between the Caradoc and Percival showings. Hole ER19-859 drilled beneath trench TR19-09 and hole ER19-861 drilled beneath trench TR19-12 where strongly folded BIF units were uncovered. Both holes returned anomalous mineralization in silicified and brecciated BIF intervals. Drill holes ER19-862 to ER19-868 were drilled along the eastern extension of the KS Horizon beyond the Caradoc showing, over a strike length of 2.5 km, testing VTEM, soil and rock sample anomalies along the metasedimentary package. Results obtained from the three holes closest to Caradoc, ER19-862 to ER19-864, returned narrow anomalous gold intervals in silicified breccias typical of the KS Horizon to the west from Percival to Caradoc. As drilling progressed further east, the KS Horizon lithologies persist, including sedimentary breccias, however intensity of silicification and sulphide mineralization is reduced. Only one anomalous interval was intersected in these holes. Hole ER19-868 intersected a 10.9 m interval grading 0.22 g/t Au in graphitic mudstone located in a mapped fold zone in the KS Horizon. With the discovery of Percival breccia gold mineralization, 2019 exploration at the Clearwater property has targeted silicified breccias within the KS metasedimentary horizon. Soft sediment deformation and slumping have affected BIF, siltstone, mudstone and graphitic mudstones creating sedimentary breccia units within the KS metasedimentary package. These different breccias have been silicified and altered (sericite +/- carbonate) to varying intensities and locally strong silicification and alteration is accompanied by sulphide mineralization (1 to 10% pyrrhotite + pyrite) as replacement mineralization, likely sourced from metamorphism of magnetite-bearing BIF and by remobilization into breccia matrices as well as through a later hydrothermal sulphide mineralizing event. Slump breccias within stratigraphic units present unique orientations relative to their host lithology. The very silicified Percival slump breccias and similar nearby occurrences are also affected by regional scale folding and deformation related to the Cannard deformation zone. The identification of well mineralized locally brecciated graphitic metasediments along the southern limb of the KS horizon and to the north at the Serendipity showing suggest that gold mineralization is distributed in graphitic sediments and may persist throughout the 14 km long KS stratigraphy, presenting an attractive formational target for exploration. The design of the Eastmain Resources’ drilling programs, Quality Assurance/Quality Control and interpretation of results is under the control of Eastmain’s geological staff, including qualified persons employing a strict QA/QC program consistent with NI 43-101 and industry best practices. The Clearwater project is supervised by Eastmain’s Project Geologist, Michel Leblanc P. Geo. Drill core is logged and split with half-core samples packaged and delivered to ALS Minerals laboratory. Samples are dried and subsequently crushed to 70% passing a 2 mm mesh screen. A 1,000 grams subsample is pulverized to a nominal 85% passing 75-micron mesh screen. The remaining crushed sample (reject) and pulverized sample (pulp) are retained for further analysis and quality control. All samples are analysed by Fire Assay with an Atomic Absorption (AA) finish using a 50 g aliquot of pulverized material. Assays exceeding 5 g/t Au are re-assayed by Fire Assay with a Gravimetric Finish. Eastmain regularly inserts 3rd party reference control samples and blank samples in the sample stream to monitor assay performance and performs duplicate sampling at a second certified laboratory. Approximately 10% of samples submitted are part of the Company’s laboratory sample control protocols.