Max Resource Corp. report new assay results expanding the URU zone from 12-km² to over 48-km², located along the CESAR North 80km-long belt, within the wholly-owned CESAR project in NE Colombia. Visible mineralization reports the presence of chalcocite, native copper and copper oxides. Two types of mineral events have been observed. On type is hosted in a stockwork within igneous host rock and is associated with the presence of epidote and the second type is sediment-hosted stratiform copper silver mineralization of Kupferschiefer type. The stratiform type is cross cut by the mineralized stockwork associated with igneous rocks. Max interprets the sediment-hosted stratabound copper-silver mineralization in the Cesar basin to be analogous to both the Central African Copper Belt (CACB) to the south and the Polish Kupferschiefer to the north. Almost 50% of the copper known to exist in sediment-hosted deposits is contained in the CACB, including Ivanhoe Mines Ltd. 95-billion-pound Kamoa-Kakula copper deposits in the Congo.