The Sligo and Hosston Formations of Aptian age occur over thousands of square miles in the subsurface of South Texas. These two formations consist of three major coeval parts, Hosston, lower Sligo, and upper Sligo, all three of which were deposited contemporaneously to produce a time-transgressive wedge of sediment. Superimposed on the overall transgressive sequence are numerous progradational cycles composed of shoaling-upward sequences.