• "Concordant, well-bedded white-grey limestone layers, with bed-thicknesses varying between 0.1 and 0.5 m...the track-bearing exposure comprises the upper bedding plane of a 12-cm-thick limestone layer...Two carbonate lithofacies can be discerned. White, massive, micritic limestones predominate on the western side while the eastern side is characterized by a grey rudist biostrome between 2 and 2.5 m wide and oriented N-S. Radiolitid rudistis occur in dense thickets or agglomerations, lithified in vertical to subvertical positions. Interstices between the shells are filled with fine skeletal detritus. The dinosaur trackways occur on the upper surface of the biostrome, suggesting it was dead and at least temporarily emergent during trackway formation...the massive limestone is a bioclastic wackestone...Geopetal fabrics are common within the limestones. The lower part of these fabrics is infilled with vadose crystal silt and the upper part with sparry calcite cement."