Landscapes and Landforms of Ethiopia — illustration 1, PDF page 303
Source record
- Source
- Habesha History book corpus — Landscapes and Landforms of Ethiopia
- Book
- Landscapes and Landforms of Ethiopia
- Source reference
- Landscapes and Landforms of Ethiopia; PDF page 303; embedded illustration 1, exact source rectangle 53.86, 59.53, 541.54, 257.77
- Page
- 303
- Publication year
- 2015
- Type
- Book illustration
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Source-page captions
Fig. 17.13 Palaeohydrography north of Lake Ziway. a The regional drainage during the Late Reduced Lakes phase (latest Pleistocene) toward the desiccated lake basin, a condition that dominated also during the Megalake phase and ensured high water supply to the lakes. The Abosa fault may have been active during these stages making the central portion of the basin actively subsiding. WFB Wonji Fault Belt; SDZFZ Silti-Debre Zeyt Fault Zone. Present Lake Ziway and Koka Reservoir for reference. b Around the Pleistocene–Holocene transition, the possibly concurrent activity of the Abosa fault and of the transverse
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