Members of the Passaic, Lockatong, and Stockton formations shown on a composite section derived from the NBCP and ACE cores. This diagram shows the color and grain size of the units, the formations, and members. In the Passaic and Lockatong formations, the members consist of individual McLaughlin cycles (i.e., 400,000-year eccentricity cycles). Modified from Olsen et al. (2018) based on Olsen et al. (1996a) and the NBCP website.