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Updated: May 23, 2025
The banks of the Chobe, like those of the Zouga, are of soft calcareous tufa, and the river has cut out for itself a deep, perpendicular-sided bed. Where the banks are high, as at the spot where the wagons stood in 1851, they are covered with magnificent trees, the habitat of tsetse, and the retreat of various antelopes, wild hogs, zebras, buffaloes, and elephants.
The angular blocks of trachyte imbedded in the stratum Number 5 in section are exactly the same in composition as the great bed below, and in them I think we see the fragments of the rocks that once filled the perpendicular-sided hollow now occupied by the lake.
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