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.

In October 2021, a trench was completed southeast of the 2019 VLF survey line L 300N. The anomaly showed a width of 25 m (southwest/northeast). Work for 2022 consisted of trenching (4 x 25m trenches), VLF grid extension and survey, and geochemistry (30 soil samples collected and analysed). The 2023 work program consisted of trenching (3) and geochemical sampling and analyses. See appended maps and tables.