Fig. 4.  View of the end of Perachora Peninsula looking west from St. Nicholas Church. The proposed MIS 7a/c terrace of Leeder et al. (2005) is shown and the location of the uppermost eroded coralline-dominated mound is 50 m east of the lighthouse. The NE–SW fault mentioned in the text lies directly in front of and below the area shown in the photograph. This fault controls the eastern end of the mini-graben structure in which the Heraion archaeological site lies. The minor fault mapped by Leeder et al. (2005, fig. 6a) supposedly passes through the far edge of the archaeological site and cuts the prominent east–west fault that dissects the end of the peninsula. It should be noted also that the sharp margins of the triangular end of the peninsula are defined by coastal-bounding faults. Other faults, especially the Xylokastro Fault, are interpreted in submarine rocks between the end of the peninsula and the south coast of the Gulf of Corinth visible in the distance.