Ethiopia - Melka Kunture and Bachilt Archaeological Site

Melka Kunture, as it can be seen today, is part of a gently undulating landscape of the Upper Awash Valley, in the highlands of Ethiopia, at c. 2000m asl. All over the Upper Pliocene and the Pleistocene, tectonic activity led to the deepening of the demi-graben depression where the meandering paleo-Awash deposited alluvia. Through time, parts of the paleo-landscape were buried again and again, blanketed both by alluvial deposits, and by volcanic deposits produced by the nearby volcanoes. Accordingly, past surfaces, littered with archaeological implement and prehistoric animal remains, were covered by sediments and escaped destruction. There is now evidence by natural erosion on the banks of the little gullies of the local tributaries of the Awash.