The Binding of the Nile And the New Soudan

nd forming small deltas like the plain of Kom- Ombos. On the sea - bottom were laid down deposits of sand and gravel, and then the land began to rise. Meantime the volcanic movements of East Central Africa had shaped the country into its present configuration, and the rivers which drained from the great lakes and swamps of the south, and those which flowed down from the high plateau on the east, combining their waters somewhere about Khartoum, pushed their marvellous course northwards, and began the creation of the fertile soil of Egypt. From this time onwards the climatic conditions must have continued very much what they are to-day. Changes, of course, there have been in the level of the land; but the sea- valley had become a river-valley, and year by year the annual flood increased the cultivable soil, and refreshed it with moisture, just as it would bedoing to-day if left untrammelled by the devices of man. Late in the history of the river-valley, but very early in the history of humanity, this favoured strip of country became the home of men, who doubtless cast their seed upon the slime left by the retreating waters, and reaped their crops long before the dawn of history. It is remarkable and characteristic of the conditions of the country that tradition ascribes to the earliest King of Egypt, Menes, the first King of the First Dynasty, the first attempts to regulate the flow of the liver?in other words, the first scheme of irrigation proper. If it were...