Soda Lakes of East Africa 2016
DOI: 10.1007/978-3-319-28622-8_2
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Genesis of the East African Rift System

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Cited by 11 publications
(5 citation statements)
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“…An analogous tectonic scenario can currently be observed in the Great Rift Valley of East Africa, resulting from the fracturing of the African Plate. The tectonic depressions are occupied by elongated and narrow lakes and river systems, reflecting the rift morphology that extends regionally (> 3000 km) from Mozambique to Ethiopia 47 , 48 .…”
Section: Discussionmentioning
confidence: 99%
“…An analogous tectonic scenario can currently be observed in the Great Rift Valley of East Africa, resulting from the fracturing of the African Plate. The tectonic depressions are occupied by elongated and narrow lakes and river systems, reflecting the rift morphology that extends regionally (> 3000 km) from Mozambique to Ethiopia 47 , 48 .…”
Section: Discussionmentioning
confidence: 99%
“…Faults in the SMER show a dominant N–S to N20° trend and age of faulting is estimated to be around ∼18 Ma [ 37 , [41] , [42] , 43 , 44 , 45 , 46 ]. Beginning in early Pleistocene (about 1.6 Ma ago), the youngest faults (Wonji Fault Belt -WFB) began to form on the rift floor [ 18 , [47] , [48] , [49] , [50] , [51] , [52] , [53] ]. Despite the MER's general NE-SW trend, the WFB is characterized by active extension fractures and normal faults that have an NNE-SSW trend.…”
Section: Geological Settingmentioning
confidence: 99%
“…In addition to these works, the broad review of 300 million years of Rift Valley Lakes in central and east Africa (Benvenuti et al, 2002), the Paleoenvironment of Lake Abijata, Ethiopia, during the past 2000 years by Bonnefille et al (1986), the study on the Late Quaternary lacustrine sediments of the Zeway-Shala Basin by Balemwald (1998), the research on Late Quaternary Lake Levels in the Rift Valley of Southern Ethiopia and elsewhere in Tropical Africa by Grove and Goudie (1971) and Grove et al (1975), examined the paleolake environment which is a key to understand the present hydrological dynamics in the CRV. The study on the evolution of the northern part of the Ethiopian Rift by Kazmin et al (1980) and the work of that of Giday et al (2016) and related the structural and geomorphic features of the EARS with the genesis of the rift valley lakes.…”
Section: Geological and Structural Setup Of The Crvmentioning
confidence: 99%