In this Questions contribution, I consider some of the accepted methods of
measuring viscosity ratios in rocks, and pose a new one. For a wide range o
f strain and orientations, it can be shown that the bedding normal is immea
surably close to the XY plane, and this has applications to the relationshi
p between cleavage and strain. I therefore propose that with some limitatio
ns, cleavage refraction can provide a measure of effective viscosity ratios
in layered rocks. Examples show that cleavage refraction across competence
contrasts yields surprisingly small viscosity ratios. This method might al
so provide a way of distinguishing Newtonian from non-Newtonian behaviour o
f rocks over time and space. (C) 1999 Elsevier Science Ltd. All rights rese
rved.