late Santonian to Maastrichtian rudist frameworks.
See reef 1935 for remarks.
Patch reef with low mounds of radiolitid clusters that were successively overlain by 0.5 m of cobbly limestones with abundant corals, a thin, reddish soil, 0.5m of in-situ rudists, another reddish soil zone, and a highly fragmented zone with radiolitid rudist fragments followed by a small diversity of rudists.
