A Popular Account [81]
another promontory, and bend once more in another chasm towards the east. In this gigantic, zigzag, yet narrow trough, the rocks are all so sharply cut and angular, that the idea at once arises that the hard basaltic trap must have been riven into its present shape by a force acting from beneath, and that this probably took place when the ancient inland seas were let off by similar fissures nearer the ocean.
The land beyond, or on the south of the Falls, retains, as already remarked, the same level as before the rent was made. It is as if the trough below Niagara were bent right and left, several times before it reached the railway bridge. The land in the supposed bends being of the same height as that above the Fall, would give standing- places, or points of view, of the same nature as that from the railway-bridge, but the nearest would be only eighty yards, instead of two miles (the distance to the bridge) from the face of the cascade. 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. Here we see them in a conglomeration, each with a train of pure white vapour, racing down till lost in clouds of spray. A stone dropped in became less and less to the eye, and at last disappeared in the dense mist below.
Charles Livingstone had seen Niagara, and gave Mosi-oa-tunya the palm, though now at the end of a drought, and the river at its very lowest. Many feel a disappointment
The land beyond, or on the south of the Falls, retains, as already remarked, the same level as before the rent was made. It is as if the trough below Niagara were bent right and left, several times before it reached the railway bridge. The land in the supposed bends being of the same height as that above the Fall, would give standing- places, or points of view, of the same nature as that from the railway-bridge, but the nearest would be only eighty yards, instead of two miles (the distance to the bridge) from the face of the cascade. 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. Here we see them in a conglomeration, each with a train of pure white vapour, racing down till lost in clouds of spray. A stone dropped in became less and less to the eye, and at last disappeared in the dense mist below.
Charles Livingstone had seen Niagara, and gave Mosi-oa-tunya the palm, though now at the end of a drought, and the river at its very lowest. Many feel a disappointment