Massive loess and calcareous paleosols typify the Late Miocene Cerro Azul Formation.
Trace fossils from a large geographic area suggest dominance of insect ichnofossils.
Celliforma, Rosellichnus, Rebuffoichnus, Fictovichnus, and Teisseirei were recorded.
The trace fossil assemblage is comparable with the Celliforma ichnofacies.
Associated uncemented Coprinisphaera ispp. were produced during post-Miocene times.