Original metadata (https://open.yukon.ca) (English, HTML)

View metadata and access the original English HTML file: Original metadata (https://open.yukon.ca).

Format

HTML

Access

file-only

Publisher-reported update

2026-08-26

Galena and pyrrhotite occur in manganese-stained quartz-carbonate breccia beneath rusty limestone. Surface geology of the area suggests that the mineralization is a replacement of brecciated limestone in the footwall of a low-angle fault. Results from previous exploration have proved disappointing but the host structure is probably regional in extent and larger deposits may exist along strike.

Access original file