The Nile Tributaries Of Abyssinia And The Sword Hunters Of The Hamran Arabs By Sir Samuel W. Baker
 -  Nothing remained but the bones and skull of
the elephant, the flesh and the ivory had been stolen. The tracks - Page 223
The Nile Tributaries Of Abyssinia And The Sword Hunters Of The Hamran Arabs By Sir Samuel W. Baker - Page 223 of 290 - First - Home

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Nothing Remained But The Bones And Skull Of The Elephant, The Flesh And The Ivory Had Been Stolen.

The tracks of a great number of men were left upon the ground, and the aggageers were fortunate to return without an attack from overwhelming numbers.

After hunting and exploring for some days in this neighbourhood, I determined to follow the bed of the Royan to its junction with the Settite. We started at daybreak, and after a long march along the sandy bed, hemmed in by high banks, or by precipitous cliffs of sandstone, we arrived at the junction; this was a curious and frightful spot during the rainy season. The entire course of the Royan was extremely rapid, but at this extremity it entered a rocky pass between two hills, and leapt in a succession of grand falls into a circular basin of about four hundred yards diameter. This peculiar basin was surrounded by high cliffs, covered with trees; to the left was an island formed by a rock about sixty feet high; at the foot was a deep and narrow gorge through which the Settite river made its exit from the circle. This large river entered the basin through a rocky gap, at right angles with the rush of water from the great falls of the Royan, and as both streams issued from gorges which accelerated their velocity to the highest degree, their junction formed a tremendous whirlpool: thus, the basin which was now dry, with the exception of the single contracted stream of the Settite, was in the rainy season a most frightful scene of giddy waters. The sides of this basin were, for about fifty feet from the bottom, sheeted with white sand that had been left there by the centrifugal force of the revolving waters; the funnel-shaped reservoir had its greatest depth beneath the mass of rock that formed a barrier before the mouth of the exit. From the appearance of the high-water mark upon the rock, it was easy to ascertain the approximate depth when the flood was at its maximum. We pitched our camp on the slope above the basin, and for several days I explored the bed of the river, which was exceedingly interesting at this dry season, when all the secrets of its depths were exposed. In many places, the rocks that choked its bed for a depth of thirty and forty feet in the narrow passes, had been worked into caverns by the constant attrition of the rolling pebbles. In one portion of the river, the bottom was almost smooth, as though it had been paved with flagstones; this was formed by a calcareous sediment from the water, which had hardened into stone; in some places this natural pavement had been broken up into large slabs by the force of the current, where it had been undermined. This cement appeared to be the same that had formed the banks of conglomerate, which in some places walled in the river for a depth of ten or fifteen feet, with a concrete of rounded pebbles of all sizes from a nutmeg to a thirty-two pound shot.

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