Camino Minerals Corp. announced results and preliminary interpretation of the geological mapping survey conducted at the Atajo zone on its 22,000-hectare Chapitos copper-gold project, near Chala, Southern Peru. The detailed geological mapping has identified a north-south oriented structural corridor that is up to 150 metres wide, 450 metres long, and is comprised of a series of steeply dipping normal faults and associated pervasive fracture network. The bounding fault structures juxtapose copper mineralized and altered porphyritic andesites and breccias against unaltered, bedded volcaniclastics. The mineralization is typically fracture and fault controlled and in places the mineralizing fluids have also exploited the shallow north-dipping bedding to form stratigraphically controlled mantos. Additionally, during the mapping program follow-up work was conducted on a number of soil and rock anomalies in the surrounding Atajo region. Positive visual results from limited outcrops in these anomalous areas warranted further work and have resulted in an ongoing trenching and bedrock sampling program. Results will be released and disseminate as they are received from the laboratory and interpreted.