Eastmain Resources Inc. announced channel sampling assay results and final high density prospect sampling results from its summer exploration campaign at the Company’s 100%-owned Clearwater Property. A 20-hole (4,000 m) drill program is now underway at Percival, Caradoc and the new target areas, with 13 holes (2,800 m) complete, with assays pending. The final results from the summer campaign include channel sample and grab sample assays from 12 of 14 trenches. The sampling targeted a 2.5 km segment of the south limb of the Knight-Serendipity Volcano-sedimentary Horizon (“KS Horizon”) from the Knight showing to the Caradoc showing, over the Percival Discovery. The complete program comprised high-density surface prospecting and rock sampling over VTEM conductors, geological mapping, mechanized trenching and channel sampling over the entire KS Horizon. Caradoc and KS Horizon Trenching – Gold values up to 1.23 g/t Au over 27.2 m have been sampled in iron formation related stratigraphy. Exposed significant silicified breccias with mineralization adding to the potential for an iron formation related gold host. KS Horizon North Limb High-Density Surface Prospecting - Sampling results from the north limb of the volcano-sedimentary belt have returned anomalous geochemical arsenic (As) in rock samples that coincide with previously selected VTEM geophysical anomalies. Additional field follow-up will be completed in advance of trenching and drill target selection. Trenching and Channel Sampling has exposed bedrock along the KS horizon over a strike length of 2.5 km, allowing for detailed mapping of the geology and mineralization initially identified using VTEM followed by high density prospecting. New exposures at Caradoc (TR19-02) and Percival (TR19-06) and elsewhere along the belt have enhanced Eastmain’s understanding of this complex stratigraphy. Surface exposures confirm the relationship of gold mineralization to sedimentary breccias throughout this portion of KS Horizon. These breccias are interpreted as sedimentary slump breccias in siltstones, mudstones and banded iron formation (BIF) which form part of the KS Horizon stratigraphy. These breccias are weakly to very strongly silicified and display sericite, chlorite and biotite alteration. Breccia matrices may display the presence of graphite and sulphide (pyrrhotite +/- pyrite). Magnetite is seen to be replaced by pyrrhotite within silicified sequences. Gold mineralization increases with the degree of silicification and may also be re-concentrated by deformation and folding along the KS Horizon. In addition to sedimentary breccia zones, anomalous (100 – 200 ppb) gold mineralization over widths of tens of metres is also seen in units of graphitic siltstones. BIF horizons are locally associated to thin layers of garnet amphibolite rock at the Percival Discovery, which are part of the iron formation sequence, and with interbeds of strongly silicified and sericitized schists (altered argillites). The predominant BIF horizon at Caradoc does not display significant brecciation in trench exposure, although soft sediment deformation is evident. Alteration mineralogy in BIF is strong at this location and takes the form of bedding parallel and joint controlled alteration of bedded magnetite to grunerite. Iron formation amphibole-garnet interbeds at this location are altered by sericite accompanied by grunerite (or anthophyllite) and sulphide mineralization (5-7% Po+Py). The strongest gold mineralization related to BIF at the Caradoc exposures is located in these amphibole-garnet-grunerite units, including the discovery sample of 10.3 g/t Au. At the north end of the Caradoc trench exposure, channel sampling cut gold mineralization in mudstone breccia (1.16 g/t Au over 2.89 m). Based on the results and lithology at this location the trench has been extended and additional results are pending. Near the Percival Discovery, Trench TR19-06 has exposed a complex sequence of slump breccias composed of Banded iron formations and mudstones with varying degrees of silicification. Gold mineralization, including 1.23 g/t Au over 27.2 m is found in all sampled lithologies at this location. The structural and stratigraphic relationship between the Percival Trench and Trench TR19-06 is being studied to provide more insight into the impact of deformation on breccias and gold mineralization. High Density Prospecting: The High Density Prospecting program comprised of 1,342 grab samples using systematic traverse lines spaced 50 m apart along the KS Horizon, targeting soil geochemical and VTEM anomalies obtained in the fall of 2018. Prospecting was enhanced by the use of Beep-MatTM magnetic susceptibility and EM conductivity instruments. The survey results present strong arsenic (As) (a gold related trace element in the region) soil geochemical anomalies which correspond to VTEM anomalies identified and selected as possible mineralized targets. Today’s results identified 6 VTEM targets with As anomalies and were distributed along the northern limb of the KS Horizon. Additionally, a strong 1 km long As anomaly was identified along a section of the KS horizon bridging two selected targets. New ground follow-up for these zones is planned for selection of trench and drill targets.