Alicanto Minerals report that it has intersected a thin semi-massive sulphide skarn mineralisation with visual chalcopyrite in the first hole drilled at The Swamp Thing target within its Greater Falun copper-gold project in Sweden. The Company has also intersected intense biotite-amphibole-garnet alteration footprint in all recently drilled holes at the Wolf Mountain Prospect, proving the area has hosted a larger active alteration system than previously demonstrated. Greater Falun is located in the Bergslagen region, which hosts world-class base and precious metals projects such as the Garpenberg mine operated by Boliden and the Zinkgruvan mine operated by Lundin. One drill hole has been completed at The Swamp Thing (Enmyregruvan), ST20-01, targeting areas below the historical workings. Samples show zoned garnet-skarn alteration and pure limestone. Grab samples at waste piles from historical workings have previously assayed up to 1.81% Cu (ASX 18/07/2020). The drillhole also intersected a thick sequence of limestone between 17.60-204.95m, 226.40-254.00m and 323.40-344.30m. The limestone is locally intruded by granite and feldspar porphyry apophyses likely emanating from a Causative Intrusion. Between 58.30-58.62m, the drillhole intersects a semi-massive sulphide skarn mineralisation with visual Chalcopyrite at the contact zone between limestone and a feldspar-porphyry apophysis. Overall, the intersected limestone varies between unaltered to completely skarn replaced near intrusive contacts. Traces of sphalerite occur at 113-135m and disseminated magnetite at 159-200m. Between 255.40-323.40m intense skarn alteration overprints what is interpreted as volcanic ash-silt- sandstones and granite. The hole was stopped in an undeformed, magnetite bearing intermediate intrusion, interpreted to post-date mineralisation formation. The thickness of the intersected limestone stratigraphy was significantly larger than expected, with a structural thickening process likely taking place. The strength of the endoskarn in the granite at 255.40-323.40m is intriguing as primary rock textures are in parts completely obliterated. The chalcopyrite mineralised skarn contact of the feldspar porphyry apophysis at 58.30-58.62 (ca. 30m from surface) shows what the potential target mineralisation could look like within this environment. This drillhole is the best example of Skarn zonation within limestone that has so far been drilled in the Greater Falun project.