Romios Gold Resources Inc. reported that field work in 2022 has expanded the known extent of mineralization at the TOE Zone on Romios' Trek Property in the Golden Triangle of NW British Columbia and continues to support an Eskay Creek or Kuroko VMS model for this untested high-grade Cu-Au-Ag-Sb target. The geology and style of the high-grade mineralization at the TOE Zone are both very similar to the world class Eskay Creek Au-Ag deposit. The known extent of this mineralization was increased by 75% in 2022 and it is believed that there is room for substantial expansion as many of the showings trend off under overburden. Three (3) styles of related mineralization occur: 1) A series of narrow, high-grade Cu-Au-Ag-Pb-Zn-Sb sulphide horizons up to 1 m wide are found within the andesite /basalt units. The cores of these zones have returned assays from trace to highs of 2.2 g/t Au, 809 g/t Ag, 3.9% Cu, 2.7% Zn, 0.9% Pb, 539 ppm As, and 0.28% Sb (antimony) over widths of 15 to 25 cm. 2) Thick units of gossanous felsic volcanics occur in a belt NW of the mafic volcanics and the widest of these returned assays of 1.5 g/t Au, 65 g/t Ag, 480 ppm As and 0.13% Cu over 4.0 m A 1.0 m wide sample collected from the centre of this aforementioned zone in 2021 assayed 2.3 g/t Au, 82 g/t Ag, 556 ppm As and 1.24% Cu with no visible copper mineralization. This zone is highly weathered at surface and the grades may well be higher in fresher rock at depth. 3) A highly mineralized quartz vein near the felsic volcanics assayed 3.0 g/t Au, 373 g/t Ag, 2.3% Cu, 0.25% Pb, 0.23% Sb, 0.96% Zn across 0.25 m. Scattered veins of coarse-grained massive pyrite are also mineralized; one 0.1 m vein assayed 0.85% Cu, 0.27 g/t Au and 17 g/t Ag. Mineralization has now been located in outcrops scattered over a 175 m x 65 m NE-trending area (see Map 1). The full extent of these outcrops is obscured to the NW and SE by glacial till cover. A >30 m wide unit of gossanous, pyritic argillite lies within the volcanic sequence and is somewhat anomalous in copper (311-535 ppm), gold (23-49 ppb), zinc (407 to 1160 ppm), silver (3 ppm), and manganese (2910 to 5520 ppm), suggesting that the mineralizing event continued to some degree throughout both volcanism and sedimentation. The presence of Cu-Au-Ag-Sb-Zn-Pb mineralization in a bimodal sequence of felsic and mafic volcanics interbedded with pyritic argillite is similar to the geology of the Eskay Creek deposit 66 km to the SE. The age of the rocks hosting the Toe Zone has not been determined yet but rocks similar in age to Eskay Creek occur 11 km to the NE on Romios' North East claim block. The full extent of the Toe Zone mineralization is unclear due to glacial till cover. A program of geophysical surveys (IP) and further detailed mapping will be designed in order to define the most favourable drill sites. The samples discussed in this document were grab and chip samples considered representative of the outcrops and veins being sampled. They were submitted to the ISO/IEC 17025 accredited ALS Canada Ltd. laboratories in Terrace and Vancouver, BC for assay and multi-element analyses. As a matter of
procedure, a rigorous quality assurance and quality control program was implemented to ensure reliable assay results by inserting alternating blanks and commercial assay standards at every 10th position in the sample series.