|Region:||Africa and Red Sea|
|Measurement method(s):||No measurements|
|Duration of observation:|
|Inferred cause of deformation:|
|Characteristics of deformation:|
No geodetic measurements have ever been made at the Tahalra Volcanic Field. It is thought that this region was active between the Miocene and Holocene.
|Reference:||NASA Landsat7 image (worldwind.arc.nasa.gov).|
The blue-green areas across the centre of this image is the Tahalra Volcanic Field. Approximately 100 strombolian basaltic cones can be found in the area. Nasa n.d.