Constantine Metal Resources Ltd. announced an agreement to acquire a 100% interest in the 3,016 acres Hornet Creek property (the "Property") located in the Hornet Creek mining district of west-central Idaho, USA. The Hornet Creek property is located within the Blue Mountains region that is host to several gold- enriched volcanogenic massive sulphide ("VMS") prospects and deposits that are considered to be similar in age to Constantine's Palmer project deposits in southeast Alaska. The Property is situated in an area with excellent access and infrastructure, and is amenable to year round exploration. Primary industries within the region currently include logging and ranching, with active mining occurring as recently as the mid-1980s at the nearby Iron Dyke high-grade copper-gold mine. Constantine's 2021-22 plans include staking of 93 additional claims (completed), airborne EM and magnetic survey followed by a diamond drilling program. Constantine previously held the Property under option for a short period. However, the acquisition and review of a more complete data package combined with the October, 2020 site visit, highlighted the drill ready opportunity for its VMS and porphyry copper potential. The Property includes the Peck Mountain copper-gold VMS prospect, where drilling by Conoco Inc. in 1980 and 1981 is reported to have intersected 17 meters (true width) of baritic massive sulphide grading 3 g/t gold and 0.16 % copper. Old pits, trenches and short adits dating from the early 1900s exist on the Property. Grab rock samples collected by Constantine from an area of intense silica and chlorite alteration in the untested, mineralized footwall to the massive sulphide horizon, 1640 feet ("ft") (500 meters ("m")) to the southeast of the Conoco drilling, contained up to 5.67% copper and 0.98 g/t gold. Other grab rock samples collected adjacent to old workings 2.3 miles (3.8 kilometers) to the northwest of the drilled prospect, on a fold repeated or stratigraphically higher horizon, assayed 14.05 g/t gold in iron-oxidized, baritic mineralization, associated with intensely altered volcanic fragmentals and 14.65 g/t gold in an iron rich hanging wall horizon to the previously described sample. The stratigraphic relationships between the Conoco drilling area and the adjacent extensive alteration and mineralization associated with anomalous soil geochemistry and geophysical responses, indicate an excellent exploration environment for VMS mineralization including opportunities to offset the prior drilling.