This paper is concerned with the question of how to relate laboratory measu
rements of the theology of rocks to the theological assumptions that need t
o be made in geodynamic modelling. First, there is a brief resume of the pr
incipal types of theological behaviour that have been studied in the labora
tory, both pressure-dependent, strain rate-independent and pressure-indepen
dent, strain-rate-dependent. Then, the generalization of the results from t
he relatively simple stress states of the experiments to general stress sta
tes is discussed, followed by consideration of the extrapolation of the exp
erimental results to geological strains and strain rates. Finally, the prob
lems associated with spatial scale are considered, leading to the question
of how to model the theological behaviour of large-scale rock masses, using
the theological measurements of laboratory specimens and taking into accou
nt the heterogeneity of geological-scale rock masses.