An area of abundant rubble to sub-crop of felsic volcanic to hypabyssal rocks containing base metal sulphides was identified along a tributary of the Jacquet River. The area was previously thought to be underlain exclusively by fine-grained clastic sedimentary rocks of the Jacquet River Formation.

On October 14, 2021, a trench was completed southeast of the 2019 VLF survey line L 300N. The anomaly showed a width of 25 m (southwest/northeast). At this time, analytical results for samples taken from the trench are pending.

Work for 2022 consisted of trenching (4 x 25m trenches), VLF grid extension and survey, and geochemistry (30 soil samples collected and analysed).