• Laminated mudstone-sandstone lithofacies- Most common lithofaces on Fish Hill, which is characterised by laterally continuous planar laminations. There are also rare wavy discontinuous laminations and planar cross-bedding towards the top of the sequence. Desiccation cracks are periodically exposed. This bed is interpreted as being characteristic of a low-energy floodplain environment, and is assigned to the Rusophycus ichnocoenosis. Fuersichnus commerfordi isp. n., Sagittichnus lincki, Cruziana problematic, Platicytes lioparadus isp. n, and Rusophycus eutendorfensis, R. jenningsi, and R. biloba were recorded.

•Thin-bedded rippled sandstone lithofacies -Minor beds of fine calcareous and noncalcareous sandstone, with all beds < 200 m in thickness. Beds are laterally continuous with sharp boundaries, and are characterised by uniform fine to very-fine grained sandstone. Small-scale trough cross-bedding often occurs, while small-scale planar cross-bedding and discontinuous wavy lamination is also present. Mudcracks and clasts occur in some of the beds. This bed is interpreted as a moderate energy channel deposit, and assigned to the Margaritichnus ichnocoenosis. Rusophycus isp., Cruziana problematica, Palaeophycus tubularis, and Margaritichnus mansfield isp. n. were recorded.

•Thick-bedded sandstone lithofacies -Consists of very fine to fine grained, red, purple and brown sandstone with small shale lenses. The beds exhibit an over-all coarsening upwards in grain size. Occasional discontinuous wavy lamination, trough cross-bedding and small-scale planar cross-bedding occurs. Represents a high-energy river channel environment. This bed is interpreted as a high energy river channel environment, and assigned to the Cruziana ichnocoenosis. Rusophycus isp. and Cruziana probelmatica were recorded.