Mineral cleavage can be resolved into two components;cleavability and optical effect. The electrical theory of matterin the solid state leads to a quantitative expression for thecleavability of ionic minerals
C{hkl} = A(hkl)/Σínisicos θ i
Approximate values for s are obtainable by using the electrostaticbond strength. Systematic application to minerals whose constituentatoms have inert-gas cores gives good agreement with observation.