|Region:||Africa and Red Sea|
|Duration of observation:||1997-2000, 2004-2010|
|Inferred cause of deformation:||Uncertain|
|Characteristics of deformation:|
Between June and December 2007 3-5 cm of uplift was observed at Halebeti, a volcanic edifice names in Biggs et al. (2011), located ~10 km south of Hertali.
|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.|
Time series of deformation at Hertali (Haledebi) volcano, as well as other nearby volcanoes, from Envisat interferograms between 2004 and 2010. Orange highlights show periods of uplift, green highlights subsidence (Biggs et al., 2011).