The Ike 14 area is underlain by the Triassic Brooklyn Formation, intruded by bodies of diorite possibly related to the Cretaceous Antsey plutonic bodies mapped in the area.

In 1972, Ryslo Silver Mines had a grid over their Ike 12 and 14 claim area where they reported it to be underlain by massive and bedded limestone, gritty limestone (with some skarn fractions) and diorite. The formations arround the diorite contains disseminations of pyrite, chalcopyrite and magnetite. Malachite occurs north of the diorite.

See the Seattle occurrence (082ESE158) for details of the area which was held and worked as a single property at various periods in history.