The largest is probably more than a hundred feet square, and something more in height. It presents a singularity in its construction worthy of notice. It is a pyramid within a pyramid; i.e. the inner pyramid has been cased over by a larger one; one of its sides being in ruins makes this peculiarity visible. By climbing up the ruined side, it is easy to reach its summit. No remains of a city or any traces of temples are visible in the immediate vicinity of this place, which is called by the natives “Turboot.”
On the 23d we came in view of the lower end of the rapids of the Third Cataract; those hereabouts are called “the rapids of Oula” We were obliged to consume thirty-nine days in getting as far as the island of Kendi, (which is not above fifty miles from Meroe.) As the direction of the river continued almost the same, coming from about the north-east, and the wind being almost invariably ahead, the difficulties attending advancing the boats by the cordel were very great, as the river here is spotted by an infinity of islands and rocks. In some of the passages where the water was deep, the current was as swift as a mill-sluice, which made it necessary to employ the crews of perhaps twenty boats to drag up one at a time. In other passages, where the water was very shallow, it was sometimes necessary to drag the boats by main force over the stones at the bottom. The camp of the Pasha remained during all this time about eight hours march above Meroe, on the right bank of the river, waiting till the boats should have passed the rapids. No military movements took place, except detaching the Divan Effendi with four hundred cavalry, to join the detachment already in Berber, where all was quiet and friendly. The country on the rapids of the Third Cataract is sterile, being composed, for the most part, of black granite and sand, excepting some of the islands, which contained good ground, and a few spots on the shores, where the floods of the river had deposited some fertile soil. The rocks by the shore presented indications which proved that the river had risen in some of its floods about twenty feet above its present level. Ostriches