A Popular Account of Dr. Livingstone's Expedition to the Zambesi and its tributaries eBook

This eBook from the Gutenberg Project consists of approximately 474 pages of information about A Popular Account of Dr. Livingstone's Expedition to the Zambesi and its tributaries.

A Popular Account of Dr. Livingstone's Expedition to the Zambesi and its tributaries eBook

This eBook from the Gutenberg Project consists of approximately 474 pages of information about A Popular Account of Dr. Livingstone's Expedition to the Zambesi and its tributaries.

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 on first seeing the great American Falls, but Mosi-oa-tunya is so strange, it must ever cause wonder.  In the amount of water, Niagara probably excels, though not during the months when the Zambesi is in flood.  The vast body of water, separating in the comet-like forms described, necessarily encloses in its descent a large volume of air, which, forced into the cleft, to an unknown depth, rebounds, and rushes up loaded with vapour to form the three or even six columns, as if of steam, visible at the Batoka village Moachemba, twenty-one miles distant.  On attaining a height of 200, or at most 300 feet from the level of the river above the cascade, this vapour becomes condensed into a perpetual shower of fine rain.  Much of the spray, rising to the west of Garden Island, falls on the grove of evergreen trees opposite; and from their leaves, heavy drops are for ever falling, to form sundry little rills, which, in running down the steep face of rock, are blown off and turned back, or licked off their perpendicular bed, up into the column from which they have just descended.

The morning sun gilds these columns of watery smoke with all the glowing colours of double or treble rainbows.  The evening sun, from a hot yellow sky, imparts a sulphureous hue, and gives one the impression that the yawning gulf might resemble the mouth of the bottomless pit.  No bird sits and sings on the branches of the grove of perpetual showers, or ever builds its nest there.  We saw hornbills and flocks of little black weavers flying across from the mainland to the islands, and from the islands to the points of the promontories and back again, but they uniformly shunned the region of perpetual rain, occupied by the evergreen grove.  The sunshine, elsewhere in this land so overpowering, never penetrates the deep gloom of that shade.  In the presence of the strange Mosi-oa-tunya, we can sympathize with those who, when the world was young, peopled earth, air, and river, with beings not of mortal form.  Sacred to what deity would be this awful chasm and that dark grove, over which hovers an ever-abiding “pillar of cloud”?

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A Popular Account of Dr. Livingstone's Expedition to the Zambesi and its tributaries from Project Gutenberg. Public domain.