|Region:||Africa and Red Sea|
|Measurement method(s):||InSAR, No measurements|
|Duration of observation:||2004 - 2007|
|Inferred cause of deformation:|
|Characteristics of deformation:|
An InSAR study of volcanoes in the Kenyan Rift looked at deformation at Ol Doinyo Eburru between 2004 -2007 using ALOS data. Ol Doinyo Eburru, however, was consistently incoherent, and as such no information on deformation at this volcano can be reported (Robertson, 2015).
|Reference:||Smithsonian Institution Global Volcanism Program|
|Reference:||NASA Landsat image, 1999|
|Reference:||Robertson, E. 2015. Magma storage and transport at Kenyan Rift volcanoes: a remote sensing perspective. Chapter 2. Ph.D Thesis, University of Bristol, UK.|
Ol Doinyo Eburru has an E-W elongated rhyolitic edifice. Lake Naivasha can be seen to the south-east of the photograph.