“…Following the Cretaceous-Eocene arching and a period of quiesence, the Baringo-Saguta graben was formed during the Miocene as part of the Turkana depression (Saggerson and Baker, 1965;Berry and Whitman, 1968; Fitch and Vondra, 1976). The Lake Rudolf basin formed in the Baringo-Saguta graben and has been a sediment trap from the Miocene to the present (Walsh and Dodson, 1969;Patterson e^ , 1970;Butzer, 1971;de Heinzelin £1»» 1971;Vondra and Bowen, 1976).…”