Max Resource Corp. announced new assay results that support the continuity of the AM-1 stratabound copper-silver mineralization, within the AM South zone at the Company’s wholly-owned CESAR sediment-hosted copper-silver project, located 420-km north of Bogota, Colombia. Highlights: New copper-silver outcrops demonstrate the AM-1 horizon extends for 2.4-kilometres; this horizon remains open both strike and down and up dip. New rock chip results include: 2.1% copper + 30 g/t silver over 8-metre by 1-metre panel; 1.7% copper + 13 g/t silver over 8-metre by 3-metre panel; 1.7% copper + 26 g/t silver over 1-metre channel; 2.1% copper + 30 g/t over 2-metre (composite grab); 4.7% copper + 34 g/t silver grab sample; and 4.5% copper + 40 g/t silver grab sample. Max considers composite grab sampling as representative, but cautions investors that grab samples are selective and may not represent in-situ mineralization. Field work is now testing the continuity and lateral extend of several horizons within the AM South zone, which currently extends over an area of 4-kilometre x 3-kilometre, and remains open laterally. The open-ended AM-1 horizon is presently interpreted to be offset and up lifted equivalent of the AM-2 horizon (assays pending). The AM South zone copper-silver mineralization is interpreted to be of stratabound/Kupferschiefer type hosted in fine-grained sediments. The principal minerals are chalcocite, a copper sulphide, and the copper oxides, malachite and azurite. The Max technical team continues to build its geological model on KGHM’s Kupferschiefer, Europe’s largest copper mine, with production in 2018 of 30 million tonnes grading 1.49% copper and 48.6 g/t silver from a mineralized zone of 0.5 to 5.5-metre thickness. The Kuperschiefer is also the world’s leading silver producer, yielding 40 million ounces in 2019, almost twice the production of the world’s second largest silver mine, according to the World Silver Survey 2020. Max cautions investors that using the Kuperschiefer as a geological model and mineralization hosted at Kuperschiefer is not necessarily indicative of mineralization at CESAR.