|Region:||Africa and Red Sea|
|Duration of observation:||2005-2010|
|Inferred cause of deformation:|
|Characteristics of deformation:|
Gufa is a collection of basaltic scoria cones alines E-W. 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 at this rhyolitic stratovolcano.
|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.|
The Gufa volcanic field can be seen in the upper right of this image (Nasa, 1999).