Frontline Gold Corporation announced that following the completion of its 2022 field program, it has staked an additional 134 claim units at its Epworth Property (Property), Nunavut. The 2022 exploration program was designed to follow up on the discovery of a new 1.1 km trend of high- grade Cu-Zn-Pb-Ag mineralization and strongly anomalous Au & Co mineralization during the 2021 field season. The new claims cover the southern strike extension of the Metallic Trend.

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) and 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 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. 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); and 1700 ppm Co (with 201 ppb Au, 6090 ppm Cu, 8.93% Zn, 1.78% Pb & 154 ppm Ag). The recently completed exploration program consisted of prospecting and rock and soil sampling across and along strike of the Metallic Trend, and at a few regional targets on claims staked in February 2022.

Lake sediment sampling was also conducted on the lake beside which the exploration team was camped. A total of 58 rock, 66 soil and 12 lake sediment samples were collected during the current program. Assays will be reported as they become available.

The Epworth Project is part of a broad platform-type clastic-carbonate sequence belonging to the early Proterozoic Coronation Supergroup that extends from the north shore of Takijuq Lake to the Coronation Gulf for over 130 km. Polymetallic sulphide mineralization occurs as disseminations in the matrix of coarse clastic quartzites or as concordant zones of cherty replacements and veins within permeable dolomite . The stratigraphy, diagenetic evolution and rift-related tectonic setting of the Coronation Supergroup compare favourably to the African Copperbelt where large (>100mt) high-grade (3-4% Cu) sediment-hosted stratiform Cu-Co-Ag deposits are frequent, and to stratabound Mississippi Valley Type (MVT) sediment-hosted Pb-Zn deposits worldwide.

The gold-rich nature of the system further increases the economic potential of this area.