Eastmain Resources Inc. provided results from its summer surface exploration campaign at the Company’s 100%-owned Clearwater Property. Based on the results, a follow-up drill program of up to 20 holes (4,000 m) is underway along the Knight-Serendipity Horizon (“KS Horizon”), including at the Percival Discovery and the newly identified Caradoc Target, located 1.7 km to the east; assay results are expected in September. The Field Exploration Campaign identified additional targets through exploration of the entire 14 km extent of the KS Horizon, beginning at the Knight showing, across the Percival Discovery and for 5 km further east along the southern limb of the KS Horizon, then northward to the Serendipity Target. The campaign was comprised of high-density surface prospecting over VTEM conductors, geological mapping, trenching and channel sampling. Analytical results from the north limb (Serendipity) are pending. Trenching and Channel Sampling of the Percival discovery was completed in June, exposing bedrock above discovery holes ER18-822 and ER18-823. Detailed mapping has identified strong mineralization along a 50 m strike across exposed outcrop. Surface exposures confirm numerous geological observations from discovery drill holes ER18-822 and ER18-823 including the relationship of gold mineralization to sedimentary breccias throughout the Percival area. Where breccias were initially identified in core as weakly to very strongly silicified units of siltstone and mudstone, surface exposures have identified that the main Percival breccia also includes altered and silicified banded iron formation (BIF) and BIF slump breccias where magnetite appears to be replaced by pyrrhotite. Remnant unaltered BIF rafts and smaller blocks have been mapped in the new exposures but were not intersected initially in core at this location. BIF horizons are locally associated to thin layers of garnet amphibolite rock which are part of the iron formation sequence and interbedded with strongly silicified and sericitized schists (altered argillites). Strong alteration is accompanied by sulphide mineralization (1 to 10% pyrrhotite + pyrite) as both replacement of BIF magnetite and as a later hydrothermal sulphide mineralizing event. The BIF and strongly altered BIF/schist package are located within a folded stratigraphic sequence with mafic mudstone and siltstone which also contain sedimentary breccia horizons that can be weakly to moderately silicified, pyrrhotite mineralized, and carry anomalous gold mineralization. Folds seen in sedimentary units in outcrop appear to have NE trending fold plane and a steep axial plunge, however at least 2 phases of deformation are identified which affect the mineralized host rocks. High Density Prospecting and mapping was conducted between May 22 and July 23 using systematic traverse lines spaced 50 m apart along the KS Horizon. The survey targeted GPS locations of soil geochemical and VTEM anomalies obtained in the fall of 2018 with a view to identifying Percival-type pyrrhotite-bearing breccia and silicified breccia units identified in drilling. Shallow overburden permitted the successful use of Beep-Mat™ magnetic susceptibility and EM conductivity instruments to identify occurrences of sulphide mineralisation in bedrock under shallow overburden and prioritize excavation and exploration of buried targets. A total of 1,342 grab samples were taken during the high-density prospecting campaign. Distribution of gold is sporadic in prospecting rock samples along the south limb of the KS Horizon, with anomalous gold values ranging from 300 ppb to 1 g/t Au detected eastwards along strike from the Knight/Percival area for over a distance of 2 km. A second area of similar weak gold mineralization was detected at the eastern end of the southern limb of the KS horizon approximately 3.5 km east of Percival. Arsenic values in rock along the south limb of the KS Horizon present several strong, broad anomalies including a 2 km x 1 km zone centred on the Percival Discovery and a 1 km by 500 m zone associated to the Caradoc Target. Two 500 m x 500 m anomalous areas are located between 1 km and 2 km east of Caradoc. Gold and arsenic anomalies are correlated to structural disruptions of the KS volcano-sedimentary horizon identified from breaks in magnetic and VTEM conductor trends. Mechanical Trenching (excavator) follow-up with detailed mapping and channel sampling has been conducted above traces of several drill holes and over priority targets identified by the prospecting program along the southern limb of the KS horizon. During June and July, 1,844 linear m of trenching were completed and 2,324 channel and grab samples were collected. Analytical results for the Percival area have been received. Other trench analyses are pending. 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.