|Region:||Africa and Red Sea|
|Measurement method(s):||No measurements|
|Duration of observation:|
|Inferred cause of deformation:|
|Characteristics of deformation:|
Segererua Plateau is an collection of “a large number” of late-Pleistocene to Holocene basaltic cones, lava flows, and maars. No geodetic measurements have been recorded at this volcano. The date of the last known eruption is unknown.
|Reference:||Smithsonian Institution Global Volcanism Program |