|Region:||Africa and Red Sea|
|Duration of observation:||2007 - 2010, 2009 - 2010|
|Inferred cause of deformation:||Uncertain|
|Characteristics of deformation:|
At Olkaria 2cm/yr of subsidence is observed between 2007 – 2010 (ALOS) in a small region where flower farms are located on volcanic deposits. No other deformation is observed within the detection limits of 0.3 cm/yr (ENVISAT) and 0.4 cm/yr (ALOS) at Olkaria.
|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.|
|Reference:||Smithsonian Institution Global Volcanism Program|
To the north of this image is Lake Naivasha. Just to the south of the lake is the norther park of the Olkaria complex. Fumarolic activity occurs at the Njorowa Gorge and at the Orengingnai and Orkaria pumice cones.