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A review of past work on the Eocene, Oligocene, and lower Miocene sediments of the Coastal Plain of North Carolina, together with fieldwork in that area, has indicated the necessity of a thorough stratigraphic revision of those beds. The Castle Hayne Formation (middle Eocene) is redefined and divided into three units the New Hanover, the Comfort, and the Spring Garden Members. It is recommended that the name Trent Marl be abandoned. Beds previously assigned to the Trent Marl are placed in the Castle Hayne and in two new formations, herein described as the River Bend Formation (middle and upper Oligocene) and the Belgrade Formation (lower Miocene). The Belgrade Formation is divided into two units the Haywood Landing and the Pollocksville Members. Lithologies, areal distributions, stratigraphic relationships, ages, correlations, and outcrop descriptions are given for the three formations.

Stratigraphic revision of the middle Eocene, Oligocene, and lower Miocene; Atlantic Coastal Plain of North Carolina