Rome Resources Ltd. announce further assay results from the recently completed drilling program within the Bisie North Tin Project, including for 3 holes at its Kalayi Prospect and 5 additional holes at its Mont Agoma Prospect. The BTNP is situated in the Walikale District of the North Kivu Province in eastern Democratic Republic of the Congo ("DRC"). Four diamond holes were drilled for a total of 463.5m beneath the artisanal workings at the Kalayi Prospec, where previous channel sampling reported up to 1m at 11% Sn.

Drilling tested 150m of the 600m high grade tin in soil anomaly (>80ppm Sn) within the broader 2,000m soil anomaly (>40ppm Sn). Highly significant intersections included 12.5m at 1.06% Sn from 41.5m including 2.5m at 3.39% Sn from 50m and 0.5m at 11.7% Sn from 51.5m and 3m at 1.92% Sn from 70m including 0.4m at 12.85% Sn from 70.7m. These high-grade intercepts are highly significant as they have potential to develop into zones of substantial width and grade at depth and on strike due to the pinch and swell nature of mineralisation associated with quartz veins and shearing.

Alphamin Resources's Mpama South Prospect has little near surface mineralisation above the bulk of its resource where they have defined 147,900 tonnes of contained tin in the Indicated and Inferred Resource categories. Tin mineralisation is also expected to have a strong shoot geometry as observed elsewhere along the Bisie Ridge which will be confirmed in the future planned drilling programme. KBDD002 reported a best intersection of 2.5m at 2.60% Sn from 79m including 0.5m at 7.15% Sn from 80m.

Initial interpretations suggest that the high-grade tin intersected in KBDD002 forms part of a separate zone of shearing to that in KBDD003 and it is possible that the mineralisation at Kalayi is within a series of en echelon parallel structures which are potentially mineralised along the 2,000m tin in soil anomaly. Mineralisation at Kalayi is clearly within the tin zone with very little copper or base metal support. Tin mineralisation is expected from surface and is interpreted to continue along the ridge to the northwest and southeast of the drilling at Kalayi over the full extent of the 2,000m soil anomaly.

Infill close spaced soil sampling and pitting/trenching programmes have commenced on the ridge and will guide future drilling programmes. Initial focus will be to follow up on the significant tin intercepts in holes KBDD002 and KBDD003 at depth and on strike to identify any potential shoot geometry and continuity of mineralisation within the mineralised structures. The most significant intercept in understanding the model for mineralisation at Mont Agoma was from the deepest intersections reported to date from MADD010A which included 26m at 0.15% Sn from 149m, 41m at 3.52% Cu from 139m including 13.15m at 7.8% Cu from 143.85m and significant silver mineralisation with 8m at >100g/t Ag within a 35m intercept.

These results clearly indicate that drilling at Mont Agoma has been concentrated on the upper levels of mineralisation within tin deposits which typically show a strong zonation with concentrations of copper, zinc, lead and silver typical of tin deposits in the upper levels and tin mineralisation at lower levels. Intersected base metal mineralisation is analogous to the upper levels mined out at San Rafael in Peru where copper, lead, zinc and silver were mined from surface before passing through a transition zone of copper and tin and it is a tin producing mine. San Rafael currently produces 10% of the world's tin.

The 26m tin intercept in MADD010A is the deepest and widest continuous tin intercept reported to date at Mont Agoma and supports a potential increase in width and grade at depth. Tin intercepts of 12m at 0.31% Sn from 29m including 1.75m at 1.14% Sn from 31.75m were also reported from MADD005 and 9m at 0.25% Sn from 122m including 0.5m at 1.2% Sn from 124m and 0.65m at 1.03% Sn from 128.5m from MADD011. Two zones of zinc mineralisation were intersected at Mont Agoma It is not clear whether the eastern zone is a cross-cutting conduit for zinc impregnated mineralised fluids which were deposited along the western shear intersected in MADD002 (90m at 4.01% Zn) or whether it is a localised zone of zinc mineralisation which is not observed on the neighbouring section lines.