|Region:||Africa and Red Sea|
|Duration of observation:||May 2006 - July 2010|
|Inferred cause of deformation:|||
|Characteristics of deformation:||
Five stages of deformation have been observed at Paka between 2006 and 2010, identifying two distinct sources (Robertson, 2015).
|References:||'Robertson, E. 2015. Magma storage and transport at Kenyan Rift volcanoes: a remote sensing perspective. Chapter 2. Ph.D Thesis, University of Bristol, UK.', 'Smithsonian Institution Global Volcanism Program