Active continental rifting in Ethiopia has led to formation of numerous volcanoes and geothermal sys
Silicic volcanic complexes in the Main Ethiopian Rift (MER) system host long-lived shallow magma res
The Main Ethiopian Rift is accompanied by extensive volcanism and the formation of geothermal system
The Ziway-Shala Lakes Basin is a structural depression found in the Main Ethiopian rift being associ
In the Main Ethiopian Rift (MER) area, rural populations often use water that exceeds the World Heal