Renforth Resources Inc. announced that geologists have returned from the field after completing some follow up fieldwork on Victoria Multi Metals Zone, achieving the following; A review of the mineralized package in several drill holes from across the 2.5 km continuously drilled length to date including detailed review of textures, structure and geochemical identification of pathfinder elements indicating alteration, in an effort to better understand and identify vectors to the mineralization., Samples have been taken from the mineralized zones of several holes in order to test for PGEs. Previous testing of surface samples has confirmed the presence of PGEs in the VMMZ. These have been submitted to the lab., Samples from mineralized and nonmineralized core from each lithology were taken for further petrographic analysis to better understand the alteration and genesis of the mineralization.

Detailed core review from multiple drill holes from the hanging wall in the sediments across the entire width through the mineralized zones and well into the footwall sediments was undertaken. The purpose of this exercise is to identify and better understand the subtle structural and chemical differences in the hydrothermal footprint of the VMS System hosting zinc and copper mineralization as well as the adjacent Nickel-Cobalt bearing calc-silicate alteration zone. Initial core logging has defined several phases or sub-units within the ultramafic bodies - the source of the Ni, Co mineralization.

The company is seeing hydrothermal alteration within the ultramafics leading to Ni, Co enrichment in the contact calc silicate lithology and are working to identify any structural controls on the emplacement of mineralization. This analysis will provide important vectoring data for planning future go forward exploration. Additionally, Renforth will select and submit samples from stored pulps from the entire mineralized package from one drill hole to test for PGEs, both in the presence of nickel and other sulfides and possibly elsewhere in the lithological assembly.