Flow-induced Interfacial Deformation Structures (FIDS): polygonal structures & longitudinal ridges and furrows, also with prod and skim marks.
Carboniferous Bude Formation, Upton Beach, North Devon, UK. (50.81612 -4.55666)
The outcrop is c. 2.0m long x 0.45m wide, and the undersides of the beds show: 1 & 2: polygonal structures; 3 & 4: longitudinal ridges and furrows, and 5: prod and skim marks.
Model produced using Scaniverse (https://scaniverse.com/) on an iPhone 13 Pro and processed in MeshLab (https://www.meshlab.net/).
See: Peakall, J. et al. (2024) Flow-induced Interfacial Deformation Structures (FIDS): Implications for the interpretation of palaeocurrents, flow dynamics and substrate rheology, Sedimentology, 71, doi: 10.1111/sed.13219.
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