Abstract
The southern shore of Lake Tanganyika and the country for a distance of 40 miles south of the lake consist of sandstones and conglomerates, dipping north about 10°. These sandstones stretch some little way up the eastern and western shores, and appear to continue away to the south-west. Proceeding further north along the lake shore they get harder, being in places metamorphosed into a pink quartzite.

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