Summary
A detailed topographic analysis and hydrological modeling of the Melka Kunture archaeological site in Ethiopia's Upper Awash Valley reveals significant geohazards and paleo-landscape features. The study identifies active flooding, erosion, and sedimentation processes threatening the site, while also uncovering evidence of past tectonic activity and a shifted drainage pattern. Notably, it suggests the presence of an ancient lake or palustrine environment upstream, with water likely draining via the Atabella tributary—a theory supported by the valley's unusually large cross sections. This research demonstrates how morphometric terrain analysis can provide critical insights for archaeological and environmental studies, bridging gaps between disciplines.
Citation
Maerker, M., Schillaci, C., & Kropáček, J. (2018). Morphometric terrain analysis to explore present day geohazards and paleolandscape forms and features in the surroundings of the Melka Kunture prehistoric site, Upper Awash Valley, Central Ethiopia. Auc Geographica, 53(1), 10–19. https://doi.org/10.14712/23361980.2018.2