This puddingstone is a distinctive, Late Devonian, grayish-purple to grayish-red, thin to very thick-bedded, cross–bedded, conglomerate.
This puddingstone is a distinct geological formation from the Late Devonian period, characterized by its grayish-purple to grayish-red color and layered structure. It can be found in various thicknesses, ranging from thin to very thick.