It preserves fossils dating back to the early Cretaceous period.

[1] The formation consists of gray shale with some interbedded siltstone and silty limestone, with some fine grained sandstone towards the top of the formation.

C. Loeblichi Miller and Harris has been recovered from the formation,[2] as have fossil ophiuroids (brittle stars).

[3] The formation is also the type location for the bryozoan Reptomulticava texana.

The distribution of foram fossils in the formation (planktonic species more common towards the bottom and benthic species more common towards the top) suggests that the sea in the area was shallowing during deposition of the formation.