Extensive in-situ and laboratory-based experimental work formed the basis f
or an assessment of the stability of an abandoned panel of Winsford salt mi
ne, Cheshire, England, conducted by numerical modelling with the finite-dif
ference code FLAC. The final model is composed of a Burger rheological comp
onent to represent the time-dependent deformation of the salt sequences and
a Mohr-Coulomb constitutive model to simulate the behaviour of the non-cre
eping marl strata. The results of the creep model are compared with actual
convergence monitoring data for validation purposes. The results indicate t
hat the section of the mine is stable and confirm the presence of an inhere
ntly stable core in each of the internal pillars within the panel.