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
































































 -   The natives who followed the dead hippopotamus caught
it a couple of miles below, and, having made it fast to - Page 272
A Popular Account Of Dr. Livingstone's Expedition To The Zambesi By David Livingston - Page 272 of 505 - First - Home

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The Natives Who Followed The Dead Hippopotamus Caught It A Couple Of Miles Below, And, Having Made It Fast To A Rock, Were Sitting Waiting For Us On The Bank Beside The Dead Animal.

As there was a considerable current there, and the rocky banks were unfit for our beds, we took the hippopotamus in tow, telling the villagers to follow, and we would give them most of the meat.

The crocodiles tugged so hard at the carcass, that we were soon obliged to cast it adrift, to float down in the current, to avoid upsetting the canoe. We had to go on so far before finding a suitable spot to spend the night in, that the natives concluded we did not intend to share the meat with them, and returned to the village. We slept two nights at the place where the hippopotamus was cut up. The crocodiles had a busy time of it in the dark, tearing away at what was left in the river, and thrashing the water furiously with their powerful tails. The hills on both sides of Kariba are much like those of Kebrabasa, the strata tilted and twisted in every direction, with no level ground.

Although the hills confine the Zambesi within a narrow channel for a number of miles, there are no rapids beyond those near the entrance. The river is smooth and apparently very deep. Only one single human being was seen in the gorge, the country being too rough for culture. Some rocks in the water, near the outlet of Kariba, at a distance look like a fort; and such large masses dislocated, bent, and even twisted to a remarkable degree, at once attest some tremendous upheaving and convulsive action of nature, which probably caused Kebrabasa, Kariba, and the Victoria Falls to assume their present forms; it took place after the formation of the coal, that mineral having then been tilted up.

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