|Region:||Africa and Red Sea|
|Measurement method(s):||No measurements|
|Duration of observation:|
|Inferred cause of deformation:|
|Characteristics of deformation:|
No goedetic measurements have ever been made at this very remote small (50 sq km) volcanic field in eastern Mali. The volcanic field is thought to be of Holocene age (Liegeois et al., 2005).
|Reference:||Liegeois J-P, Benhallou A, Azzouni-Sekkal A, Yahiaoui R, Bonin B, 2005. The Hoggar swell and volcanism: reactivation of the Precambrian Tuareg shield during Alpine convergence and West African Cenozoic volcanism. In: Foulger G R, Natland H H, Presnall D C, Anderson D L (eds) Plates, Plumes, and Paradigms, (Geol Soc Amer Spec Pap), 388: 379-400.|
There is no available imagery, or field photographs, available for this volcano.