The Gracias Formation is a sedimentary unit, consisting of sandstone, siltstone, claystone and a few conglomeratic beds. The formation crops out in western Honduras and ranges from 200 to 300 metres (660 to 980 ft) in thickness. The formation overlies the Padre Miguel Group, while it is overlain by Pleistocenebasalts.[2] The Padre Miguel Group provided the provenance for the sedimentary material for the Gracias Formation. The clasts in the formation are largely composed of rhyolite, rhyodacite, pumice, vitric ash, quartz, feldspar, and minor biotite fragments.[3]