|Region:||Africa and Red Sea|
|Duration of observation:||1997-2000, 2003-2010|
|Inferred cause of deformation:||Uncertain|
|Characteristics of deformation:|
Biggs et al. (2011) processed InSAR data from Tullu Moje (called Tulla Moje within Biggs et al. (2011)) between 1997-2000 and 2003-2010. They found no evidence of surface deformation until 2009-2010, but no deformation mechanism is given.
|Reference:||Biggs, J., I. D. Bastow, D. Keir, and E. Lewi (2011), Pulses of deformation reveal frequently recurring shallow magmatic activity beneath the Main Ethiopian Rift, Geochem. Geophys. Geosyst., 12, Q0AB10, doi:10.1029/2011GC003662.|
|Reference:||Siebert, L., and T. Simkin (2002), Volcanoes of the World: An Illustrated Catalogue of Holocene Volcanoes and Their Eruptions, Global Volcanism Program Digital Inf. Ser., GVP‐3, Smithsonian Inst., Washington, D. C. [Available at http://www.volcano.si.edu/world/.]|
Interferograms used in the analysis of deformation. Each fringe represents 2.8 cm of displacement in the satellite line-of-sight (Biggs et al., 2011), no deformation is observed at this volcano. The summit of the volcano is shown by a black dot, as reported by the Smithsonian Database (Siebert and Simkin, 2002).