The Woodbine Formation is composed largely of terrigenous sediment eroded from Paleozoic sedimentary and weakly metamorphosed sedimentary rocks of the Ouachita Mountains in southern Oklahoma and Arkansas, and subsequently deposited in a complex of nearshore environments along the margins of the broadly subsiding Northeast Texas basin. Three principal depositional systems are recognized in Woodbine rocks--a fluvial system, a high-destructive delta system, and a shelf-strandplain system. Their recognition is based on a regional outcrop and subsurface investigation in which external geometry of framework sandstone was integrated with lithology, sedimentary structures, fossil distribution, and bounding relations.

Two components of the fluvial system, a tributary channel sandstone facies and a meander belt sandstone facies, are developed in the Dexter Member (lower Woodbine) northeast of a line from Dallas to Tyler. On the south and southwest, a high-destructive delta system is persistent throughout the entire Woodbine section. The 3 component facies of the delta system are: progradational channel-mouth bar sands; coastal barrier sands, deposited along shore adjacent to the channel mouth; and prodelta-shelf muds. The Lewisville (upper Woodbine) shelf-strandplain system, developed in the northern third of the basin marginal to principal deltaic facies, is composed of 2 facies: shelf muds and strandplain sands that accumulated along shore.

Near the end of Woodbine deposition, but before transgression by Eagle Ford seas, emergence of the Sabine uplift resulted in erosion of Woodbine sediments, which were subsequently redeposited along margins of the uplift as the Harris sand.

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