Published online by Cambridge University Press: 14 March 2018
Pure samples of the micaceous component of Yorkshire fireclays have been separated. Examination of these by chemical, optical, X-ray, and thermal methods indicates that the material is in all likelihood an intimate mixture (but not an interstratification) of mica and a kaolintype mineral—probably the b/3 disordered kaolinite commonly found in fireclays. The evidence also suggests that this kaolin-type mineral is the end-product of weathering of the mica, and a possible mechanism is suggested.