Figure 8. Core photographs, Cape May borehole. A. Lithologic contact and disconformity at 575.7 ft, separating an unnamed Kirkwood sequence (“Kw2c”) above from the Kirkwood 2b sequence below. B. Lithologic contact and disconformity in unrecovered interval between 847 and 850 ft, separating an unnamed Kirkwood sequence (“Kw1c”) above from the Kirkwood 1b sequence below. Silty clays with common shells overlie the unconformity (an indurated zone), and unconsolidated sands of the Highstand Systems Tract (HST) lie below. C. Lithologic contact and disconformity at 1062.3 ft, separating the Kirkwood 1a sequence above from the Kirkwood equivalent (“Kw0”) sequence below. Dark, shelly glauconite sands overlie the unconformity and an indurated zone. D. Lithologic contact and disconformity at 1350.8 ft, separating lower Oligocene (Zone P19) glauconite sands from lowermost Oligocene (Zone P18) glauconitic clay. E. Lithologic contact and disconformity in the unrecovered interval between 1354.5 and 1360 ft, separating lowermost Oligocene (Zone P18) from uniform, laminated upper Eocene (Zone P17) clay.