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Acoustic attenuation in Lake Tanganyika
Nature, 1979THE Lake Tanganyika acoustic attenuation experiment of April 1970 (ref. 1) was the second of two lake experiments designed to help identify the cause of the low-frequency attenuation anomaly in seawater by providing comparative freshwater data. Although the Lake Tanganyika results showed no evidence of the anomaly, the attenuation was unaccountably ...
R. H. MELLEN +2 more
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Nature, 2003
Warming of surface waters and declining fish catches in Lake Tanganyika have been linked to global climate change. The impact of global warming on natural ecosystems may be starting to affect local economies.
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Warming of surface waters and declining fish catches in Lake Tanganyika have been linked to global climate change. The impact of global warming on natural ecosystems may be starting to affect local economies.
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The Prosobranchs of Lake Tanganyika
Nature, 1938WHEN Sir Richard Burton discovered Lake Tanganyika in 1858 his companion, Speke, collected a number of shells from the shores. These proved to be Prosobranchs of types hitherto unknown in fresh water. Later investigations, notably those of the three Tanganyika expeditions, the first two under the leadership of J. E. S.
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Chlorinated hydrocarbon residues in the fish of lake Tanganyika
Bulletin of Environmental Contamination and Toxicology, 1976The use of chlorinated hydrocarbon pesticides for the control of tropical diseases and the treatment of agricultural crops in Central Africa has [ncreased tremendously since it was started in 1954 (LAMBRECHT, 1954; BRION, 1962). Even though the levels of residues from such pesticides have been studied extensively in many parts of the world, there are ...
Deelstra, H., Power, J.L., Kenner, C.T.
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Variable extension in Lake Tanganyika
Tectonics, 1988Lake Tanganyika is part of the east African rift system. The amount of extension along 22 dip section seismic lines in the lake has been measured. The maximum extension observed is 4.5 km (approximately 10%) at the central part of the rift and decreases to about 0.5 to 1‐km extension at the north and south ends of the rift.
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The Fisheries of Lake Rukwa, Tanganyika
2021This survey of the fisheries of Lake Rukwa, Tanganyika, describes results obtained during 1963-1964, and includes comparative material given by previous workers, in particular surveys conducted in 1936 by Ricardo and, in 1946 by Swynnerton. Data is given on the general hydrology of the Lake including chemical analyses, seasonal and annual fluctuations ...
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A Floating Pharmacy on Lake Tanganyika
Journal of Pharmacy Practice, 2011Elias B, Chahine, Adwoa O, Nornoo
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Dagaa Fisheries in Lake Tanganyika
The East African Agricultural Journal, 1954(1954). Dagaa Fisheries in Lake Tanganyika. The East African Agricultural Journal: Vol. 19, No. 4, pp. 251-252.
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The Rise and Fall of Lake Tanganyika
Quarterly Journal of the Geological Society of London, 1892After alluding to certain observations of Cameron, Livingstone, and Stanley on the changes of level of Lake Tanganyika, the writer states that the most interesting point in connexion with the rise and fall of the lake is the question:—How is it possible for a great lake to rise 30 feet above its normal level by the blocking up of its outlet ...
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