The Roots occurrence is located on a south facing slope, north of Nina Lake.
The area is underlain by rock of the Mississippian to Permian Mount Howell Succession, Nina Creek Group.
It is reported that the first known mineral occurrence in the vicinity was found by the Geological Survey of Canada in the 1940s and described by E.F. Roots as a mineralized zone at least eight feet (2.4 metres) wide, containing malachite, pyrite, and minor azurite (Assessment Report 25532).
The zone occurs in a 60 metre band of sheared, carbonatized, silicified and pyritized interbedded argillite and andesite. The mineralized zone is broken by many faults and is veined by quartz. The showing is exposed in only a few outcrops.
In 1944, a grab sample assayed 4.83 per cent copper (GSC MEM 252-183).
Work History
The Roots showing is described by Gary Lee in 1997 in his prospecting report on his Nina claims (Assessment Report 25532). It is not known if he visited the showing.
Also see Nina (093N 011).