Contoured Cu-in-soil data across the Liberty property, highlighting the extensive property scale area of high mineral potential. High-grade Cu-bearing grab and chip samples in the southwestern area occur along a structural break (dashed lines are inferred faults are based on regional magnetic data) between ultramafic rocks to the northeast and argillites to the southwest. Wetland conditions defined by areas of deeper organic material and of high, near-surface groundwater content are outlined in the central and northern portions of the surveyed area. These soil conditions may result in locally subdued geochemical responses.
Contoured Cu-in-soil data across the Liberty property, highlighting the extensive property scale area of high mineral potential. High-grade Cu-bearing grab and chip samples in the southwestern area occur along a structural break (dashed lines are inferred faults are based on regional magnetic data) between ultramafic rocks to the northeast and argillites to the southwest. Wetland conditions defined by areas of deeper organic material and of high, near-surface groundwater content are outlined in the central and northern portions of the surveyed area. These soil conditions may result in locally subdued geochemical responses.