MAX RESOURCE CORP to report high-grade assay results from continuous rock chip channel sampling collected at the recently discovered AM-08 target, located in the AM District of its wholly-owned Cesar Copper-Silver Project, in Northeastern Colombia. Continuous chip channel sampling across the width of the structurally controlled mineralization at the primary outcrop has returned values of: o 2.6% copper and 58 g/t silver over 15.0m including, o 3.5% copper + 77 g/t silver over 10.0m including, o 8.1% copper + 172 g/t silver over 1.0m. In addition, continuous chip channel sampling across mineralized outcrops at several locations west of the primary occurrence has returned values of: o 2.5% copper + 48 g/t silver over 2.0m.

o 1.8% copper + 18 g/t silver over 1.8m. o 1.1% copper + 16 g/t silver over 5.3m. AM-08 is characterized by the presence of two styles of copper-silver mineralization: structurally controlled and stratiform sediment hosted.

Stratiform mineralization at AM-08 has been mapped along strike for 400 metres. Two types of copper-silver mineralization are observed at AM-08, structurally controlled and stratiform: The structurally controlled mineralization is hosted in an NNE striking fault and is thickest where it intersects an NNW striking fault. The primary copper mineral is chalcocite which occurs in multiple veins up to 3 cm thick.

Stratiform mineralization is observed where the mineralized structure comes into contract with sedimentary rocks or lithological contacts. Copper minerals include chalcocite and bornite which form irregular veins that are concordant with the strata. The strike and dip of bedding in the AM-08 area is measured at N30- 60E and 30NE respectively.