Cruse Formation – Papelon Point

Slumped sands on alternating sand and claystone interval

Abundant Ophiomorpha, mostly parallel to the bedding

Alternating sand, siltsone, claystone and lignite beds, mostly parallel bedding. This is the only locality that I have seen lignite in place within the Cruse

The outcrop consists of a mix of parallel bedded sands and claystones and slumped sands and claystones