Jefferson Canyon

Why Jefferson Canyon?

Jefferson Canyon Long Section

Long Section Parallel to JF Fault

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Note: The potential quantity and grades are conceptual in nature. There has been insufficient exploration drilling to define a mineral resource and it is uncertain if further exploration will result in the exploration target being delineated as a mineral resource.

Select Historical Drill Results

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Note: The potential quantity and grades are conceptual in nature. There has been insufficient exploration drilling to define a mineral resource and it is uncertain if further exploration will result in the exploration target being delineated as a mineral resource.

“B” Zone Cross Section

From Jefferson Canyon

Note: The potential quantity and grades are conceptual in nature. There has been insufficient exploration drilling to define a mineral resource and it is uncertain if further exploration will result in the exploration target being delineated as a mineral resource.

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Jefferson Canyon’s Large Conductor

CSAMT resistivity data suggests that the Jefferson Canyon fault is a deep structure which likely controls the mineralization and appears to be related to a large conductive feature at depth

This spatial relationship to the gold-silver mineralization supports the potential to expand the mineralized footprint both along strike and depth

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Note: The potential quantity and grades are conceptual in nature. There has been insufficient exploration drilling to define a mineral resource and it is uncertain if further exploration will result in the exploration target being delineated as a mineral resource.