Frontline Gold Corporation announced the discovery of a new 1.1 km trend of high-grade Cu-Zn-Pb-Ag mineralization and strongly anomalous Au & Co mineralization on its Epworth Project (the `Property') located in Nunavut. As a result of the very encouraging 2021 prospecting results, Frontline has staked an additional 202 claim-units resulting in a 306 claim-unit/4835-hectare property. The Epworth Project is located 85km south of the village of Kugluktuk (Coppermine), containing three main previously known areas of high-grade polymetallic mineralization from 1-25m wide occurring for more than 15km along strike.

Historical surface grab samples have reported spectacular high-grade mineralization including: 61.2% Cu & 5600 gpt Ag (Payback Showings); 19.22% Zn with 810 gpt Ag, 3% Cu & 1.86 gpt Au (Metallic Showing). The newly discovered trend was identified while investigating the historical Metallic Showing (formerly named `Dead Showing') in the northern part of the property, consisting of dolomite with sulphide-rich quartz-carbonate veining in outcrop. Mineralized angular float boulders, subcrop and outcrop were found to extend much further to the south than previously identified, along a well- defined north-northwest-south-southeast-trending corridor.

A total of 84 rock grab samples were sent to Activation Labs (Actlabs) in Thunder Bay, Ontario for Au, Ag and trace element geochemical analysis. Samples along the Metallic Trend returned strongly anomalous to high-grade Cu-Zn-Pb as well as consistently anomalous Au, locally high-grade Ag and anomalous Co with values up to: 37.8% Cu (with 184 ppb Au, 2970 ppm Zn, 449 ppm Pb & 45 ppm Ag). 3.01 gpt Au (with 7860 ppm Cu).

19.3% Zn, 10% Pb & 1130 ppm Ag (with 1.85 gpt Au & 3.01% Cu). 1700 ppm Co (with 201 ppb Au, 6090 ppm Cu, 8.93% Zn, 1.78% Pb & 154 ppm Ag). En-echelon quartz-carbonate veins within the dolomite are a common feature in this landscape; however, sulphide mineralization occurs only in discrete north-northwest-south-southeast- trending corridors.

The trend appears to be offset locally by northeast-trending faulting and may continue further to the north and to the south. In the northeast part of the property, a new lead showing was discovered (Northeast Showing), again in dolomite, with galena-rich quartz-carbonate stringers. Samples returned up to 19.4% Pb (with 7720 ppm Cu & 3100 ppm Zn).