|Region:||Africa and Red Sea|
|Measurement method(s):||No measurements|
|Duration of observation:|
|Inferred cause of deformation:|
|Characteristics of deformation:|
No geodetic observations have been made at Tosa Sucha.
|Reference:||Ebinger C J, Yemane T, WoldeGabriel G, Aronson J L, Walter R C., (1993). Late Eocene-Recent volcanism and faulting the southern main Ethiopian rift. J Geol Soc London, 150: 99-108.|
Cinder cones, located on the northern shore of Lake Chamo, may have been active in historical time (Ebinger et al., 1993). Many of the volcanological features at this volcano are submerged, or partly-submerged, beneath Lake Chamo.