|Region:||Africa and Red Sea|
|Duration of observation:||2005 - 2010|
|Inferred cause of deformation:|
|Characteristics of deformation:|
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 associated with these north-west trending fissures or pyroclastic cones. The most recent confirmed eruption, which consisted of lava flows, was in 1928 or 1929 (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/.]|
The dark-colored lava flows extending diagonally across the center of this Landsat image were erupted from pyroclastic cones of Manda-Inakir volcano. Nasa, 1999.