A Popular Account Of Dr. Livingstone's Expedition To The Zambesi By David Livingston
































































 -   The tops of the promontories are in general flat, smooth,
and studded with trees.  The first, with its base on - Page 114
A Popular Account Of Dr. Livingstone's Expedition To The Zambesi By David Livingston - Page 114 of 263 - First - Home

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The Tops Of The Promontories Are In General Flat, Smooth, And Studded With Trees.

The first, with its base on the east, is at one place so narrow, that it would be dangerous to walk to its extremity.

On the second, however, we found a broad rhinoceros path and a hut; but, unless the builder were a hermit, with a pet rhinoceros, we cannot conceive what beast or man ever went there for. On reaching the apex of this second eastern promontory we saw the great river, of a deep sea-green colour, now sorely compressed, gliding away, at least 400 feet below us.

Garden Island, when the river is low, commands the best view of the Great Fall chasm, as also of the promontory opposite, with its grove of large evergreen trees, and brilliant rainbows of three-quarters of a circle, two, three, and sometimes even four in number, resting on the face of the vast perpendicular rock, down which tiny streams are always running to be swept again back by the upward rushing vapour. But as, at Niagara, one has to go over to the Canadian shore to see the chief wonder - the Great Horse-shoe Fall - so here we have to cross over to Moselekatse's side to the promontory of evergreens, for the best view of the principal Falls of Mosi-oa-tunya. Beginning, therefore, at the base of this promontory, and facing the Cataract, at the west end of the chasm, there is, first, a fall of thirty-six yards in breadth, and of course, as they all are, upwards of 310 feet in depth. Then Boaruka, a small island, intervenes, and next comes a great fall, with a breadth of 573 yards; a projecting rock separates this from a second grand fall of 325 yards broad; in all, upwards of 900 yards of perennial Falls. Further east stands Garden Island; then, as the river was at its lowest, came a good deal of the bare rock of its bed, with a score of narrow falls, which, at the time of flood, constitute one enormous cascade of nearly another half-mile. Near the east end of the chasm are two larger falls, but they are nothing at low water compared to those between the islands.

The whole body of water rolls clear over, quite unbroken; but, after a descent of ten or more feet, the entire mass suddenly becomes like a huge sheet of driven snow. Pieces of water leap off it in the form of comets with tails streaming behind, till the whole snowy sheet becomes myriads of rushing, leaping, aqueous comets. This peculiarity was not observed by Charles Livingstone at Niagara, and here it happens, possibly from the dryness of the atmosphere, or whatever the cause may be which makes every drop of Zambesi water appear to possess a sort of individuality. It runs off the ends of the paddles, and glides in beads along the smooth surface, like drops of quicksilver on a table.

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