Griffith's criterion for the fracture stress of a cracked plate is \[ \sigma_f = \sqrt{\frac{2E\gamma_s}{\pi a}} \] where \( \gamma_s \) is the surface energy per unit area and \( a \) is the half crack length.
So the pure Griffith energy balance is valid only for perfect brittle materials.
Griffith validated his theory experimentally using fine glass fibres, a nearly ideal brittle material, and the historical basis of the theory tells us a lot about where it does and doesn't apply.
The experimental basis of Griffith's work confirms it is restricted to perfectly brittle materials.
Therefore, the correct answer is Perfect brittle materials.
