Cyntar Ventures Inc. announced that it has received its independent geological report on the Lorn Property prepared by Oliver Friesen, M.Sc., B.Sc. (Hons.) Geology. The report details the work that has been done to date on its 3,957-hectare Lorn Property (the "Property"), located in the Clinton and Lillooet mining divisions of British Columbia, approximately 190 kilometers north of Vancouver. The Company collected 756 soil samples, 12 silt samples and 69 rock samples. Concurrent with the geochemical sampling, geologists prospected and mapped large areas of the Property in detail, covering areas which had not previously been exposed due to glacial ice cover. The 2018 exploration work resulted in the definition of two new mineralized zones on the Property. The Sluice Creek Zone porphyry target covers a widespread soil geochemical anomaly which lies northwest of the historical copper porphyry showings explored by Cominco Ltd. in the 1970's. The anomaly is approximately four km by two km and includes soil values of up to 21.2 g/t Ag, 730 ppb Au, 535 ppm Cu and 190.5 ppm Mo. The anomaly flanks a 1.5 km long magnetic low anomaly, which may be reflecting porphyry style alteration and mineralization below the overburden cover. There is a well-developed, strongly oxidized colour anomaly, with associated pyritic alteration surrounding the target zone. To the west, strong clay-silica alteration typical of epithermal gold systems is widespread. The second anomalous zone lies in the south-central region of the Property. These are brand new exposures revealed by receding glacial ice. Values of up to 1.6% Cu with 22 g/t Ag and 2.7% Cu were returned from samples collected from outcrops trending under the ice, associated with strong silicification and propylitic alteration. Two samples returned values greater than 1 g/t Au in the west area of the Property. The report recommends a Phase 2 program of IP geophysical surveying and detailed mapping over the Sluice Creek Zone budgeted at $150,000, to further define potential drill targets.