Figure 6
A synthesis of river activity in the Mediterranean at the Early–Mid-Holocene transition, including the main flood periods in SE Italy, Iberia, eastern Mediterranean, Tunisia, and Morocco16, the sedimentary gap in NE Moroccan rivers from 8700 to 7300 cal. BP25, indices of aggradation in Iberia21, the braided phases identified at Lalo-Espeluche18, the aggradation phases identified at Sidari19, and the base-level variations of the Charef River with the I-1 and I-2 incision phases and the four aggradation phases.
