The panoramic photo above is the roadcut which parallels Coral Way. Note the large clasts in this conglomerate on the upper left of the outcrop, and the cross-bedding on the right, with a distinct rubble zone separating the two. These clasts, some very angular, came from eroding sea cliffs. According to Halley and Evans (1983) this outcrop is indicative of a shoreline, with the presence of islands in the area.
On the outcrops below the Metro Mover numerous bivalves and corals were observed, as well as coarse shell lag deposits.
