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Former Lake Levels and Climatic Change in the Rift Valley of Southern Ethiopia - 1975

Publisher: 
Blackwell Publishing. The Geographical Journal, Vol. 141, No. 2 (Jul., 1975), pp. 177-194
Full Title: 
Former Lake Levels and Climatic Change in the Rift Valley of Southern Ethiopia - 1975
Abstract: 
Lakes in the Ethiopian rifts are sensitive indicators of Late Quarternary climates. Chew Bahir (Lake Stifanie), which has been dry most of this centery was 20 meters deep about 5660 years ago.
The rift valley of Southern Ethiopia runs NNE from the Kenya frontier for 600km to the Koka Dam ti the Awash River where the rift begins to open out into the Afar and the Danakil depressions. from the Some reslevant information on Koka dam

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