The Second International Symposium on the East African Lakes was held from 10-15
January 2000 at Club Makokola on the southern shore of Lake Malawi. The symposium was …

Blocked‐valley lakes are formed when tributaries are impounded by the relatively rapid
aggradation of a large river and its floodplain. These features are common in the landscape …

Reconstructions of lake-level variations in Lake Malawi, East Africa, indicate the lake was
about 200 to 300 m below present during most of the period from~ 40,000 to 28,000 years …

Kalahari Group sediments accumulated in the Kalahari basin, which started forming during
the breakup of Gondwana in the early Cretaceous. These sediments cover an extensive part …

This study of the Recent sediments of northern Lake Tanganyika is based on high‐
resolution seismic profiling and 43 Kullenberg cores, made by Elf‐Aquitaine (project Georift) …

The pans, or small dry or ephemeral lakes, of the southern Kalahari in Botswana are
contained in shallow, sub-circular to sub-elliptical, enclosed depressions in the surface …

This work considers new evidence for palaeo-environmental change taking place during the
Pleistocene in northern Botswana. Duricrusted strandlines along the northeastern margin of …

Abstract The eastern Sahara Desert of Africa is one of the most climatically sensitive areas
on Earth, varying from lake-studded savannah woodland to hyperarid desert over the course …

Diatom analysis of core M98-2P from the northern basin of Lake Malawi shows changes in
lake level and mixing during the last 24,000 calendar years. Fluctuations between the major …

The Nachukui Formation lies between present day Lake Turkana and the Murua Rith and
Labur Ranges to the west. Sedimentary deposits in the area consist of patchy Miocene strata …