Quaternary glaciation of the Bale Mountains, Ethiopia
(2005)
Journal Article
Osmastom, H., Mitchell, W., & Osmaston, J. (2005). Quaternary glaciation of the Bale Mountains, Ethiopia. Journal of Quaternary Science, 20(6), 593-606. https://doi.org/10.1002/jqs.931
Central Ethiopia comprises a high plateau at 2000-3000 m, formed from Tertiary lava flows and bisected by the Eastern African Rift. Ten volcanic mountains rise to altitudes of just over 4000 m, but on only three has Quaternary glaciation been substan... Read More about Quaternary glaciation of the Bale Mountains, Ethiopia.