Titlebook: Landscapes and Landforms of Ethiopia; Paolo Billi Book 2015 Springer Science+Business Media Dordrecht 2015 Ethiopia.Geomorphology.Horn of

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Geomorphology of the Adwa Districtterm landscape evolution from the Late Proterozoic to the Quaternary. Two landscape features of the Adwa district exemplify the control of tectonic uplift and erosion, often in a feedback loop: the plateau landscape and river incision. The plateau landscape developed upon metamorphic, sedimentary an

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Gully Development in the Tigray Highlandsment, where intense rainfalls challenge the physical integrity of the landscape. Over the last two centuries, three major phases in the hydrological regime of the region could be distinguished. In the first phase, between 1868 (or earlier) and ca. 1965, the relatively stable gully channels showed an

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Sediment Yield Variability at Various Spatial Scales and Its Hydrological and Geomorphological Impacile River Basin. SY data collected using reservoir sediment surveys or runoff and suspended sediment concentration (SSC) measurements at river gauging stations in the framework of different programs were compiled, screened, and used for our analysis. A large spatial variation in area-specific SY (SS

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Climatic and Hydrologic Changes in Northern Ethiopia in the last 3,500 Years: Evidence from the Geomrved along the lake margins provide a detailed archive of the climate history of East Africa over the past 3,500 years. These successions are represented by colluvial/stromatolitic deposits and palustrine, deltaic, and fluvial sediments along the northern and southern coasts, respectively. During th

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