Published online by Cambridge University Press: 01 May 2009
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.
page 368 note 1 Scott-Elliot, & Gregory, : Quart. Journ. Geol. Soc., 1895, li, p. 674.Google Scholar
page 368 note 2 Scott-Elliot & Gregory, l.c.
page 369 note 1 Quart. Journ. Geol. Soc., 1900, lvi, p. 205.Google Scholar