| Jebel Marra | |
|---|---|
&sq=Qlik&lang=&file=File:Jebel_Marra_Volcano,_Sudan_by_Planet_Labs.jpg) Deriba caldera, with the two lakes visible | |
| Highest point | |
| Listing | Country high point Ultra |
| Coordinates | 12°57′N 24°16′E / 12.95°N 24.27°E[1] |
| Geography | |
&sq=Qlik&lang=&file=File:Sudan_relief_map.svg)  Deriba caldera | |
Deriba is a Pleistocene or Holocene caldera in Darfur, Sudan. Part of the volcanoes of the Marra Mountains, it lies on the Darfur dome and like the Tagabo Hills and Meidob Hills volcanism may be the product of a mantle plume. After the separation of South Sudan, the highest point of Sudan is on the margin of the caldera.
The caldera lies atop a shield volcano or ash cone in the southern Marra Mountains, which developed first as a pile of basaltic lava flows and later as layers of volcanic ash and tuff, including the eruptions that formed the caldera. A large eruption occurred about 3,520 ± 100 years before present, and hot springs and fumaroles are active to the present day.
Deriba contains two lakes, one in the northeastern side of the main caldera and the other in a cone in the southwestern sector of the Deriba caldera. The fresher southwestern lake is smaller but considerably deeper than the saltier northeastern lake; in the late Pleistocene the caldera was filled with a larger lake.