Engineer Gold Mines Ltd. provided an update on its 100%-owned Engineer District property, which covers 29,593.47 hectares in a 35 km-long contiguous claim grouping near Atlin in northwest British Columbia. The Property includes the historical high-grade Engineer Gold Mine, the TAG developed prospect, and several other high-grade vein and shear-hosted bulk tonnage gold targets. The Company is currently compiling prior owner and historical data to identify opportunities for development and discovery.

Anyox-Rodeo is a massive sulphide showing in an under-explored area within the Wann River drill permit area, where the Company intends to focus its' 2023 exploration efforts. The Anyox-Rodeo showing comprises massive pyrrhotite veins exposed on the southwest bank of the lower Wann River. Reportedly, a 6 m adit was excavated over a copper seam here in 1900 but was subsequently flooded by the Engineer Gold Mine's hydro dam in 1924 (PF810417, BC Minfile).

Historic workings include an adit and two shallow pits, from which a 2008 grab sample of massive pyrrhotite fragments and oxidized spoils returned 0.34% copper, 0.41% nickel, 0.11% cobalt, 0.07 g/t platinum, and 0.2 g/t palladium (Aspinall, 2009; AR 30601). The showing occurs within the Llewellyn fault zone corridor, approximately 1280 m along strike from the extent of known mineralization in the Wann River area, where precious and base-metal enriched veins have been sampled over an area of 800 m x 180 m (Pautler, 2021). Mihalynuk (1999) describes Anyox-Rodeo as a 2 m-wide sulphide pocket where pentlandite and pyrrhotite form a matrix to pegmatitic actinolite in chlorite-actinolite schists of the Boundary Ranges Metamorphic Suite.

Aspinall (2009) describes subvertical, southeast-trending 10 - 20 cm thick massive pyrrhotite veins. The mode of formation of this massive sulphide occurrence is not well understood; its geologic setting, within 200 m of the sheared contact between Stuhini Group volcanics and Boundary Ranges Metamorphic suite in an area where both units are intruded by early Cretaceous foliated diorite to monzodiorite, has prompted comparisons to nearby basaltic copper, volcanogenic massive sulphide ("VMS") and skarn deposits (Mihalynuk et al., 1996; Mihalynuk, 1999; Aspinall, 2011; MINFILE 104M-017).