The Shulaps Mountain asbestos prospect is located at the headwaters of Retaskit Creek, 3.6 kilometres east of Shulaps Peak. The asbestos, intermediate between chrysotile and picrolite, is within serpentinite of the Permian and older Shulaps Ultramafic Complex. The asbestos occurs along fractures in the serpentinite forming fibres up to 15 centimetres long; it's extent is very limited.