Deriba Caldera

Deriba Crater is at the highest point of Jebel Marra at an elevation of 3,042 m (9,980 ft), in Darfur in the western part of Sudan. It is between 5 km and 8 km in diameter across the outer crater. The inner crater is filled by a crater lake.

The Marra Mountains are part of a large geologic feature known as the Darfur Dome. The dome appears to be the result of a mantle plume, which is a fixed “hotspot” in the Earth’s mantle (the layer of Earth below the crust). The mantle plume heated the crust from below, leading to uplift of the crust and providing a magma source for the extensive volcanism observed in the region. The 5-kilometer-wide Deriba Caldera was formed by explosive eruption of the Jebel Marra Volcano approximately 3,500 years ago. The volcano is considered dormant, rather than extinct, as hot springs and fumaroles (gas and steam vents) are still present.

The caldera has the classic circular shape: the depression formed as overlying rock and soil collapsed into the magma chamber after it was emptied by powerful eruptions. Following the formation of the main outer crater, a second inner crater (image center) formed, most likely due to later uplift and eruption of fresh magma moving towards the surface. This inner crater is filled with water.

Because the walls of the inner crater are higher than the adjacent caldera floor, precipitation flowing inwards from the outer crater walls does not enter the inner crater lake. White stream bed sediments (image center) show the water pathway around the inner crater to a second lake located along the northeast wall of the outer crater. While Jebel Marra is high enough (3,042 meters) to have a temperate climate and high precipitation, these lakes may be fed by hot springs as well as rainwater.


 This article incorporates public domain material from the National Aeronautics and Space Administration document "Deriba Caldera, Sudan".

  • The Jebel Marra, Darfur, and Its Region: J. H. G. Lebon, V. C. Robertson. The Geographical Journal, Vol. 127, No. 1 (Mar., 1961), pp. 30–45 [1]
  • Notes on Jebel Marra, Darfur: H. F. C. Hobbs. The Geographical Journal, Vol. 52, No. 6 (Dec., 1918), pp. 357–363 [2]
  • Sources of Water in the North-Western Sudan: K. S. Sandford. The Geographical Journal, Vol. 85, No. 5 (May, 1935), pp. 412–431 [3]

External links

  • Location map (small scale) : [10]
  • Satellite image (large scale) : [11]
  • Oblique aerial photo on page 27 (large scale) : [12]
  • Deriba Caldera at NASA Earth Observatory
Listed in the following categories:
Post a comment
Tips & Hints
Arrange By:
There are no tips nor hints for Deriba Caldera yet. Maybe be you will be the first one to post useful information for fellow travellers? :)

Hotels nearby

See all hotels See all
Ledger Plaza Hotel N'Djamena

starting $233

Hilton NDjamena Africa

starting $213

Empires Hotel

starting $48

Mercure N Djamena Le Chari

starting $126

Ibis N'Djamena La Tchadienne

starting $128

Radisson Blu Hotel, N'Djamena

starting $167

Similar tourist attractions

See all See all
Add to wishlist
I've been here
Crater Lake

Crater Lake is a caldera lake located in the U.S. state of Oregon. It

Add to wishlist
I've been here
Mount Rainier

Mount Rainier is an active

Add to wishlist
I've been here

Hallasan is a shield volcano on Jeju Island of South Korea. Hallasan

Add to wishlist
I've been here
Irazú Volcano

The Irazú Volcano (Spanish: Volcán Irazú) is an active volcano in Co

Add to wishlist
I've been here
Poás Volcano

The Poás Volcano, in Spanish Volcán Poás, is an active st

See all similar places