Bayuda volcanic field

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Bayuda volcanic field (also spelled Bayiuda[1]) is a volcanic field in Sudan, within the Bayuda Desert. It covers a surface of about 11 by 48 kilometres (6.8 mi × 29.8 mi) and consists of a number of cinder cones as well as some maars and explosion craters. These vents have erupted aa lava flows.

Bayuda volcanic field
Bayuda Vulkanfeld.jpg
The volcanic field from space
Highest point
Elevation670 m (2,200 ft) [1]
Coordinates18°20′N 32°45′E / 18.33°N 32.75°E / 18.33; 32.75Coordinates: 18°20′N 32°45′E / 18.33°N 32.75°E / 18.33; 32.75[1]
Bayuda volcanic field is located in Sudan
Bayuda volcanic field
Bayuda volcanic field
Last eruption1,102 +- 48 years ago

The field rises above a Precambrian-Paleozoic basement that may be a domal uplift. There is little known about the occurrence of volcanic eruptions, but the last eruption has been dated to 1,102 ± 48 years before present.

Geography and geomorphologyEdit

The volcanic field is located in the Bayuda Desert within the great bend of the Nile,[1] 300 kilometres (190 mi) north of Khartoum.[2] It lies 80 kilometres (50 mi) away from Merowe; there are wells at Abu Khorit and Sani[3] north of the volcanic field.[4] The field was discovered by aerial photography in 1920.[3]

Bayuda is an elongated volcanic field[1] with fresh volcanic features[3] extending over an area of 11 by 48 kilometres (6.8 mi × 29.8 mi) in northwesterly direction. Within this area, a number of volcanic vents within a narrow space have formed a continuous volcanic surface.[5] Some individual lava fields cover over 20 square kilometres (7.7 sq mi) of surface,[6] but surfaces of about 10 square kilometres (3.9 sq mi) are more typical.[7] There are usually only a few flows per vent, although they often have lobate structures. The surface of the lava flows has varying textures and often contains hills or ridges,[8] generally corresponding to aa lava.[9] Some flows reach lengths of 10 kilometres (6.2 mi).[10]

Cinder cones make up the bulk of the field,[1] of which there are about one hundred.[11] Usually the cones reach heights of over 400 metres (1,300 ft)[7] and are formed by volcanic ash, lapilli, lava bombs and scoria.[12] Many of these aside from pyroclastics also erupted lava flows[5] which then broke the crater rims.[1] Explosion craters[1] and sporadic maars are also found,[2] they are surrounded by tephra deposits which form low rims of pyroclastic material[13] and which also cover neighbouring volcanoes.[4] Individual vents form two separate alignments.[10]

Hosh ed Salam ("dark enclosure"[14]) crater is 500 metres (1,600 ft) deep and 1,300 metres (4,300 ft) wide,[1] other craters are Jebel Hebeish and El Muweilih which have formed shallow rises above the surrounding terrain and have cut into the basement rocks.[9] El Muweilih contains a salt lake after which it is named and which was used as a source of salt,[6] while Jebel El Abour contains a secondary cone. The Sergein hills and Jebel Azrub are composite volcanoes.[5] Angalafib, Goan and Jebel El Abour are also quite high.[6]

Lava and scoria from Bayuda

Pumice blocks from the field were found in Wadi Abu Dom,[3] and scoria downstream in the Nile.[14] Tephra identified in deposits on Mograt Island in the Nile most likely comes from this volcanic field.[15] The volcanic field is a potential site for geothermal power development, with temperatures underground of about 200 °C (392 °F).[16]


Volcanic activity has been taking place in Sudan since the Cretaceous, with most recent manifestations documented in the Bayuda volcanic field, Marra Mountains and Meidob volcanic field[3] both in Darfur,[17] and elsewhere in the form of small basaltic outcrops.[18] Bayuda is a small volcanic field in comparison to other African volcanic fields.[4] Volcanism at Bayuda may be associated with the Central African Shear Zone[19] and of Precambrian faults,[20] perhaps together with a mantle plume.[21]

The basement consists of granites of Precambrian and Paleozoic age[1] that belong to the Bayuda terrane,[2] which together with gneisses form a gentle pedeplain away from rougher landscape along the Nile.[22] Later on during the Cretaceous the Nubian Formation was laid down and there are hints of a domal uplift in the Bayuda area,[3] which probably predates the onset of volcanism and may have influenced the course of the Nile.[22] The existence of such a dome has been questioned, however.[23]


Bayuda has erupted basaltic rocks,[5] with most collected rocks belonging to an alkali basalt suite[24] although basanite, melabasanite, hawaiite and trachybasalt have been identified as well.[2][25] Phenocrysts include clinopyroxene and olivine.[24] Various xenoliths have been found, including garnet-containing clinopyroxenite, harzburgite, garnet hornblendite, amphibole-containing peridotite, olivine and spinel pyroxenite and websterite.[26]

In general the composition resembles that of other Sudanese-Egyptian volcanoes,[2] about two different magma families have been identified which originate from disparate mantle domains.[10] The total volume of the volcanic rocks is about 18 cubic kilometres (4.3 cu mi),[27] the rocks reach thicknesses of about 200 metres (660 ft) maximally.[4]

Eruptive historyEdit

Volcanic activity has been dated to 1.7 - 0.9 million years ago,[28] but it continued after the end of the latest wet period 5,000 years ago[1] as indicated by the uneroded state of some of the volcanoes[4] such as Hosh ed Salam.[29] The presence of maars and volcanoes with signs of phreatomagmatic activity may indicate activity during pluvials.[30] Volcanism at Bayuda commenced with isolated volcanoes. After a while, new edifices were constructed atop the older ones, influencing the morphology of the new volcanoes.[27]

The most recent lava flow was dated to less than 1,100 years before present,[1] with radiocarbon dating producing an age of 1,102 ± 48 years before present.[7] Aside from this date, however, there is little information on the timing of recent volcanic activity in the Bayuda volcanic field.[30] The volcanic field may be a potential source for geothermal energy.[16]


  1. ^ a b c d e f g h i j k l "Bayuda Volcanic Field". Global Volcanism Program. Smithsonian Institution.
  2. ^ a b c d e Lenhardt et al. 2018, p. 2.
  3. ^ a b c d e f Almond, Ahmed & Khalil 1969, p. 550.
  4. ^ a b c d e Almond 1974, p. 346.
  5. ^ a b c d Almond, Ahmed & Khalil 1969, p. 557.
  6. ^ a b c Almond, Ahmed & Khalil 1969, p. 561.
  7. ^ a b c Almond, Kheir & Poole 1984, p. 235.
  8. ^ Almond, Ahmed & Khalil 1969, p. 558.
  9. ^ a b Almond, Ahmed & Khalil 1969, p. 559.
  10. ^ a b c Klitzsch & Thorweihe 1999, p. 129.
  11. ^ Almond, Ahmed & Khalil 1969, p. 556.
  12. ^ Lenhardt et al. 2018, p. 4.
  13. ^ Lenhardt et al. 2018, p. 7.
  14. ^ a b Grabham 1920, p. 134.
  15. ^ Dittrich, Annett; Neogi, Sayantani (27 January 2017). "Holocene Lake and Shallow Water Sediments at Mograt Island, Sudan". Studia Quaternaria. 34 (1): 17. doi:10.1515/squa-2017-0001.
  16. ^ a b Khadam, A. M. A.; Ramadan, K.; Hamouda, E. A. (August 2018). "Geothermal Mainstream Adoption through Risk Mitigation in Sudan". 2018 International Conference on Computer, Control, Electrical, and Electronics Engineering (ICCCEEE): 1–11. doi:10.1109/ICCCEEE.2018.8515898. ISBN 978-1-5386-4123-1.
  17. ^ Grabham 1920, p. 135.
  18. ^ Almond, Kheir & Poole 1984, p. 233.
  19. ^ Pachur & Altmann 2006, p. 266.
  20. ^ Pachur & Altmann 2006, p. 97.
  21. ^ Klitzsch & Thorweihe 1999, p. 109.
  22. ^ a b Almond, Ahmed & Khalil 1969, p. 551.
  23. ^ Almond, Kheir & Poole 1984, p. 242.
  24. ^ a b Almond, Ahmed & Khalil 1969, p. 564.
  25. ^ Almond 1974, p. 350.
  26. ^ Klitzsch & Thorweihe 1999, p. 132.
  27. ^ a b Almond, Ahmed & Khalil 1969, p. 563.
  28. ^ Almond, Kheir & Poole 1984, p. 234.
  29. ^ Pachur & Altmann 2006, p. 398.
  30. ^ a b Lenhardt et al. 2018, p. 12.


  • Almond, D. C. (1 March 1974). "The composition of basaltic lavas from Bayuda, Sudan and their place in the cainozoic volcanic history of north-east Africa". Bulletin Volcanologique. 38 (1): 345–360. Bibcode:1974BVol...38..345A. doi:10.1007/BF02599411. ISSN 0366-483X.
  • Almond, D. C.; Ahmed, Farouk; Khalil, Badr Eldin (1 June 1969). "An excursion to the Bayuda volcanic field of Northern Sudan". Bulletin Volcanologique. 33 (2): 549–565. Bibcode:1969BVol...33..549A. doi:10.1007/BF02596524. ISSN 0366-483X.
  • Almond, D.C.; Kheir, O.M.; Poole, S. (January 1984). "Alkaline basalt volcanism in northeastern Sudan: a comparison of the Bayuda and Gedaref areas". Journal of African Earth Sciences. 2 (3): 233–245. doi:10.1016/S0731-7247(84)80018-X. ISSN 0731-7247.
  • Grabham, C. W. (1920). "The Bayuda Volcanic Field". Sudan Notes and Records. 3 (2): 133–136. JSTOR 41715760.
  • Klitzsch, Eberhard; Thorweihe, Ulf (1999). Nordost-Afrika : Strukturen und Ressourcen : Ergebnisse aus dem Sonderforschungsbereich "Geowissenschaftliche Probleme in ariden und semiariden Gebieten" (in German) ([Online-Ausg.]. ed.). Weinheim: Wiley-VCH. ISBN 978-3-527-27724-7.
  • Lenhardt, Nils; Borah, Suranjana B.; Lenhardt, Sukanya Z.; Bumby, Adam J.; Ibinoof, Montasir A.; Salih, Salih A. (March 2018). "The monogenetic Bayuda Volcanic Field, Sudan – New insights into geology and volcanic morphology". Journal of Volcanology and Geothermal Research. 356: 211–224. Bibcode:2018JVGR..356..211L. doi:10.1016/j.jvolgeores.2018.03.010. ISSN 0377-0273.
  • Pachur, Hans-Joachim; Altmann, Norbert (2006). Die Ostsahara im Spätquartär (in German). SpringerLink. doi:10.1007/978-3-540-47625-2. ISBN 978-3-540-47625-2.