The sequence of Holocene delta development worldwide is indicated as beginning at 6000 BC; by 3000 BC a transgressive sequence of deltaic deposits had developed as shown on the figure. Under conditions of rapid sea level rise these fresh deposits would have been swampy and waterlogged. However, a sudden regression would leave a silty, nutrient-rich floodplain well- drained with a slightly receding (downcutting) river, a condition ideal for irrigated agriculture. Journal of Coastal Research, Special Pub. 27, p. 235. (trans.html)
Copyright 1996 Kirribili Press. Return to Scientific Summary Chronological Index Ignatius Donnelly and the End of the World