The Gord Ridge showing is located on the Unuk 12 claim. A northeast-trending silicified shear or vein zone up to 2 metres wide is hosted in phyllitic sediment or tuff in the lower part of the Betty Creek Formation (Hazelton Group). The structure can be traced for approximately 100 metres and is sporadically mineralized with sphalerite, pyrite and galena.
See Tarn Creek (104B 344) and AP (104B 083) for details of common work history on the Unuk property.