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A geoelectrical investigation of a slow moving earth slide–earth flow in Lower Jurassic Lias Group rocks of the Cleveland Basin, UK, is described. These mudrock slopes are particularly prone to failure and are a major source of lowland landslides in the UK, but few attempts have been made to spatially or volumetrically characterise the subsurface form of these slides. The primary aim of this study was to consider the efficacy of fully three-dimensional geoelectrical imaging for landslide investigation with reference to a geological setting typical of Lias Group escarpments. The approach described here included a reconnaissance survey phase using two-dimensional electrical resistivity tomography (ERT), resistivity mapping, self-potential (SP) profiling and mapping, followed by a detailed investigation of an area of the landslide using three-dimensional (3D) ERT and self-potential tomography (SPT). Interpretation of the …