|Region:||Africa and Red Sea|
|Duration of observation:||2005 - 2010|
|Inferred cause of deformation:|
|Characteristics of deformation:|
This collection of fissure vents sits in the Manda Gargori rift, the youngest riting segment in this region. Pagli, et al. (2014), for the purposes of investigating regional velocity fields, has looked at Envisat InSAR data covering this volcano. They report no deformation. No historical activity has been officially reported, but human footprints in ashfall deposits suggests a historical-age eruption (Siebert and Simkin, 2002).
|Reference:||Pagli, C. et al., 2014. Current plate boundary deformation of the Afar rift from a 3-D velocity field inversion of InSAR and GPS. Journal of Geophysical Research: Solid Earth, 119(11), pp.8562-8575.|
|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/.]|