The Meziadin showing is located near the headwaters of Del Norte Creek approximately 75 kilometres east of Stewart. The area was initially explored prior to 1913, again in 1922 and in 1938-39.

The area is underlain by siltstone, greywacke, sandstone, calcarenite, argillite, conglomerate and minor limestone of the Middle-Upper Jurassic Bowser Lake Group. The showing comprises a fissured and partly silicified zone, 0.4 to 0.9 metre wide, in argillite. Along the footwall, a layer of quartz is interbanded with argillite. The quartz is locally copper stained (inferred to be malachite) and contains pyrite, galena and sphalerite with high values in gold and silver reported. Two other zones occur in the vicinity, 0.9 to 6.1 metres wide. These strike northwest, dip vertically and locally contain small, silicified sections which contain small patches of sphalerite and chalcopyrite.

A 1.46 metre sample from one of these two other zones, assayed 4.8 grams per tonne gold, 27.4 grams per tonne silver, 1.6 per cent copper, 1.6 per cent zinc and nil lead (Mandy, 1939 in Special Report 3). This was the best assay result from the program, most samples contained only trace gold and silver.