|Region:||Africa and Red Sea|
|Duration of observation:||1997-2000, 2003-2006|
|Inferred cause of deformation:|
|Characteristics of deformation:|
Geodetic studies of Namarunu, a shield volcano in the Kenyan Rift, have shown no deformation between 1997-2000 and 2003-2006 (Biggs et al. 2009).
|Reference:||Biggs, J., E. Y. Anthony, and C. J. Ebinger. "Multiple inflation and deflation events at Kenyan volcanoes, East African Rift." Geology 37, no. 11 (2009): 979-982.|
|Reference:||Smithsonian Institution Global Volcanism Program |
Namarunu is composed of several basaltic lava cones and tuffs. This photograph was taken looking south from the Tirr Tirr margin escarpment. Photo by Martin Smith, 1993 (copyright British Geological Survey, NERC).