The Shaker limestone occurrence is located west of Atlin Lake about 30 kilometres north-northwest of the community of Atlin.
A large area of Upper Mississippian to Permian Cache Creek Complex (Horsefeed Formation) limestone occurs between the upper reaches of Atlin Lake and Tagish Lake to the west. This formation consists mainly of limestone that ranges in thickness from 900 to 1500 metres and includes local bodies of mafic flow, diabase, and lithic tuff.
The rock is a massive, medium to pale grey, bioclastic limestone that has a faint brownish tinge. It is a typically crinoidal, fusulinid calcarenitic limestone that is generally recrystallized, producing either a fine-grained porcelaneous appearance or a fine crystalline rock with light and dark mottles (Geological Survey of Canada Paper 74-47).