|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.
|References:||'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.'|