[A Popular Account of Dr. Livingstone’s Expedition to the Zambesi and Its Tributaries by David Livingstone]@TWC D-Link bookA Popular Account of Dr. Livingstone’s Expedition to the Zambesi and Its Tributaries CHAPTER II 2/45
The lofty range of Kebrabasa, consisting chiefly of conical hills, covered with scraggy trees, crosses the Zambesi, and confines it within a narrow, rough, and rocky dell of about a quarter of a mile in breadth; over this, which may be called the flood-bed of the river, large masses of rock are huddled in indescribable confusion.
The drawing, for the use of which, and of others, our thanks are due to Lord Russell, conveys but a faint idea of the scene, inasmuch as the hills which confine the river do not appear in the sketch.
The chief rock is syenite, some portions of which have a beautiful blue tinge like _lapis lazuli_ diffused through them; others are grey.
Blocks of granite also abound, of a pinkish tinge; and these with metamorphic rocks, contorted, twisted, and thrown into every conceivable position, afford a picture of dislocation or unconformability which would gladden a geological lecturer's heart; but at high flood this rough channel is all smoothed over, and it then conforms well with the river below it, which is half a mile wide.
In the dry season the stream runs at the bottom of a narrow and deep groove, whose sides are polished and fluted by the boiling action of the water in flood, like the rims of ancient Eastern wells by the draw-ropes.
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