Possible coupling between climatically induced lake level change, volcanic eruptions and seismotectonic activation in the Rukwa-Rungwe-Nyasa rift, SW Tanzania

The Rukwa rift basin is presently a closed hydrogeological depression containing a shallow lake (max 20 me deep) with its surface at an altitude around 810 m above sea level. Lacustrine terraces and paleo-shorelines are known up to 980 m above sea level, an altitude at which it reach the overflow si...

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Veröffentlicht in:	Geophysical research abstracts 2007-01
Hauptverfasser:	Delvaux, D, Macheyeki, A S, Kervyn, F, Fontijn, K, Ernst, G, Temu E.B., EB
Format:	Artikel
Sprache:	eng
Schlagworte:	Freshwater
Online-Zugang:	Volltext
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