Broadway Gold Mining Ltd. provided an update on its Phase III surface drilling program at the company's 100%-owned Madison copper-gold project in the legendary Butte-Anaconda mining region of Montana, USA. Key highlights to date from the recently documented, well-mineralized, two-mile-long geological, geophysical and geochemical trend include: Latite porphyry discovered in holes C17-24 and C17-27; Anomalous gold, silver, manganese, lead, sulfur, strontium and zinc identified in the phyllically altered latite; Porphyry body appears to be of significant size with intercepts to date measuring up to 234 metres and open in all directions; and new discovery in regional trend near Butte region. Seven holes totaling 2,323 meters have been drilled to date, as Broadway aggressively and systematically tests IP targets highlighted during the property-wide survey completed in 2017. As expected, some of the holes have encountered excellent indications of a deeper porphyry, while others intersected skarn similar to that encountered in earlier drilling at the Madison mine to the north. Initial areas tested include: The North Central area, where some of the strongest IP responses throughout the survey identified a prominent northwest-striking IP anomaly; The Mise-a-la-Masse target, where a northward extension of a skarn and massive sulfide ore body intercepted in C17-20 (23.8 meters of 1.247% copper and 1.843 grams per tonne gold) was indicated; and the southeast chargeability area, where two copper-gold porphyry targets have been identified and IP located several anomalies. The quartz latite porphyry is light grey to dark green in color and fine grained. It is moderately to strongly altered with zones of propylitic, silicic and phyllic alteration increasing in intensity with depth. Mineralization in C17-24 consists of porphyry-style disseminated and microveinlet pyrite with lesser sphalerite and galena. A 12.74-meter interval returned positive values of 0.228 g/t Au, 7.69 g/t Ag, 570 ppm Pb and 1205 ppm Zn, confirming the latite is mineralized. Mineralization in C17-27 consists of fine disseminations, microveinlets and coarse blebs of pyrite. Samples for C17-27 will be submitted to the lab as soon as the core is logged and split. C17-22, where a seven-meter interval of pyrite-rich carbonaceous dolomite returned values of 243 ppm Mo, 188 ppm Cu and 390 ppm vanadium, apparently explaining the northwest trending IP anomaly along the Green Campbell Fault Zone. C17-25 failed to explain a strong IP anomaly in the southeast corner of the property indicating an additional hole on a different azimuth is warranted.