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Atakor volcanic field

Coordinates: 23°20′N 5°50′E / 23.33°N 5.83°E / 23.33; 5.83
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Atakor Volcanic Field
Landsat satellite image of the Ahaggar with its central volcanic field
Highest point
Elevation2,918 m (9,573 ft)[1]
Coordinates23°20′N 5°50′E / 23.33°N 5.83°E / 23.33; 5.83[1]
Geography
Atakor Volcanic Field is located in Algeria
Atakor Volcanic Field
Atakor Volcanic Field

Atakor volcanic field ("Atakor" in Tuareg means "swollen part, knot at the end of something"[2]) is a volcanic field in Algeria. It lies in the Hoggar mountains and consists of a variety of volcanic features such as lava flows and about 450 individual vents which create a spectacular scenery.

Atakor is one of several large volcanic fields in this mountain range, which sits atop of a domal uplift and has erupted basalt, trachyte and phonolite. Volcanism in Atakor took place in several different phases, beginning 20 million years ago and continuing into the Holocene. Presently there is fumarolic activity.

Geography and geomorphology

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The field lies in the Hoggar[1] and the terrain approaches elevations of 3,000 metres (9,800 ft)[3] although the volcanics form an only superficial cover.[4] The ground has a desert-like appearance.[5] The scenery of the volcanic field is considered to be spectacular,[1] with the lava domes and volcanic necks rising above the surrounding terrain.[3]

The field consists of lava domes, lava flows,[1] maars,[6] scoria cones and volcanic necks[1] which cover an area of about 2,500 square kilometres (970 sq mi)[6] with a volume of about 250 cubic kilometres (60 cu mi) of volcanic rock.[7] Basalts form a 400 metres (1,300 ft) thick plateau,[3] and deep gorges lead up to the volcanic field[8] and split the Hoggar Mountains in a number of segments.[9] Wadis diverge from the Atakor volcanic field;[10] some of them reached Lake Chad in the past,[11] others continued through the Grand Erg Oriental towards Chott Melrhir.[12]

Tahat in the Atakor

There are about 450 recent volcanic centres, of which about 400 are lava domes and 50 small stratovolcanoes,[13] the latter of which include many recent cones[6] which are accompanied by lava flows whose length reaches 20 kilometres (12 mi).[14] Among the older volcanoes of Atakor are the peaks Assekrem and Tahat,[7] the latter of which is the highest summit in the Hoggar.[15] Some of these volcanoes have craters, including double craters, and others are eroded to the point that only volcanic necks remain,[16] while lava domes include shapes from steep pillars to short stubby lava flows[17] and are responsible for much of the field's scenery.[18] Some of these lava domes and necks penetrated older basaltic layers.[19] Among the stratovolcanoes is the Oued Temorte cone, which is 300 metres (980 ft) high, 800 metres (2,600 ft) wide and has erupted an over 10 kilometres (6.2 mi) long lava flow. It has also erupted volcanic ash, lapilli and slag.[20]

Geology

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Atakor is one in a group of volcanic fields of the Hoggar around Tamanrasset which include Adrar N' Ajjer, Eg'ere, Manzaz and Tahalra,[21] and is considered to be part of the Hoggar volcanic province which since 34 million years has covered an area of 11,700 square kilometres (4,500 sq mi) with 1,650 square kilometres (640 sq mi) of volcanic rocks.[22] A low-seismic velocity anomaly underpins the Atakor volcanic field in the mantle[23] but does not appear to reflect the existence of a hotspot.[24]

The basement is formed by Precambrian rocks that form a 1 kilometre (0.62 mi) high swell[21] known as the Hoggar swell,[25] and is further part of the Neoproterozoic Tuareg shield[26] and a metacraton formed during the Eburnean orogeny.[27] The basement crops out in deeply incised valleys,[28] which in general appear to be younger than the Hoggar volcanism.[29] Active faults occur throughout the region.[30]

Atakor has erupted basalts, phonolite and trachyte,[1] the latter two form lava domes.[22] The basalts are characterized by alkali basalts and basanite and form about 80% of all volcanic rocks in Atakor, with less important occurrences of benmoreite, hawaiite, mugearite and rhyolite.[6] Phenocrysts in some volcanic rocks include amphibole, clinopyroxene, olivine and zircon.[20] The Taessa lavas from this volcanic complex[22] have a porphyritic texture.[31] The volcanic rocks appear to ultimately derive from mantle plume melts,[32] although a tectonic origin resulting from the convergence between African and Europe has also been suggested.[33]

Eruptive history

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Volcanic activity in Atakor occurred 20-12 million years ago,[34] 6.7 - 4.2 million years ago and 1.95 million years ago until today,[35] with most volcanic activity taking place during the first episode in the Burdigalian and Serravallian.[34] The second and the third volcanic phases were also accompanied by substantial ground uplift.[7] Phonolite and trachyte erupted first and basalts later,[1] although contrary to initial belief the flood basalts are from the oldest Tertiary,[36] and the phonolitic-trachytic volcanism continued after the basaltic activity.[19] Stratovolcanoes with lava flows are the most recent manifestations of activity in Atakor.[20]

Activity continued in the Holocene, with lava flows covering Holocene features[1] such as 10,000 years old lacustrine sediments,[37] pottery[1] and having a fresh appearance. Tuareg oral tradition of "fire mountains"[14] appears to recount that Tuareg people observed eruptions.[1] Local heat flow anomalies,[38] rare fumaroles and observed seismicity are further evidence of ongoing volcanism.[14]

Climate and history

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Atakor lies within the tropics (south of the Tropic of Cancer) and at high elevation. Precipitation is more common than in the surrounding desert and during winter it can occur in the form of snow;[3] at Assekrem annual precipitation is about 100–150 millimetres (3.9–5.9 in).[8] In the past, precipitation was considerably higher than today,[39] such as during the Villafranchian and the Paleolithic when nivation landforms developed above 2,000 metres (6,600 ft) elevation,[40] as well as moraines[41] such as at Tahat[42] and rock glaciers.[43] A last wet period occurred during the Neolithic.[36]

Vegetation in Atakor is subdivided into several belts, a lower Sudanian belt at 1,700–1,800 metres (5,600–5,900 ft) elevation with bushes and trees,[3] a sub-Mediterranean between 1,800–2,400 metres (5,900–7,900 ft) which includes the olive and a high Mediterranean belt which includes Clematis flammula.[5] The volcanic field is used as a pasture.[8]

References

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  1. ^ a b c d e f g h i j k "Atakor Volcanic Field". Global Volcanism Program. Smithsonian Institution.
  2. ^ Bernus 1991, p. 118.
  3. ^ a b c d e Kubiëna 1955, p. 116.
  4. ^ Capot-Rey 1969, p. 241.
  5. ^ a b Kubiëna 1955, p. 117.
  6. ^ a b c d Dupuy, Dostal & Chikhaoui 1993, p. 132.
  7. ^ a b c Sesiano 1980, p. 74.
  8. ^ a b c Rognon 1963, p. 13.
  9. ^ Büdel 1955, p. 102.
  10. ^ Bernus 1991, p. 118,119.
  11. ^ Pachur & Altmann 2006, p. 27.
  12. ^ Pachur & Altmann 2006, p. 87.
  13. ^ Girod 1963, p. 359,361.
  14. ^ a b c Sesiano 1980, p. 76.
  15. ^ Ayadi et al. 2000, p. 111.
  16. ^ Girod 1963, p. 359.
  17. ^ Girod 1963, p. 363.
  18. ^ Sesiano 1980, p. 75.
  19. ^ a b Büdel 1955, p. 106.
  20. ^ a b c Conquéré, F.; Girod, M. (1 November 1968). "Contribution à l'étude des paragenèses précoces des basaltes alcalins: Les spinelles du volcan de l'Oued Temorte (Massif de l'Atakor, Sahara Algérien)". Contributions to Mineralogy and Petrology (in French). 20 (1): 1–2. Bibcode:1968CoMP...20....1C. doi:10.1007/BF00371063. ISSN 0010-7999. S2CID 130911787.
  21. ^ a b Dupuy, Dostal & Chikhaoui 1993, p. 131.
  22. ^ a b c Benhallou, Megueni & BoussisseIkhlef-Debabha 2019, p. 29.
  23. ^ Ayadi et al. 2000, p. 121.
  24. ^ Ayadi et al. 2000, p. 122.
  25. ^ Ayadi et al. 2000, p. 112.
  26. ^ Bouzid et al. 2015, p. 2.
  27. ^ Bouzid et al. 2015, p. 3.
  28. ^ Sesiano 1980, p. 73.
  29. ^ Büdel 1955, p. 104.
  30. ^ Sesiano 1980, p. 72.
  31. ^ Benhallou, Megueni & BoussisseIkhlef-Debabha 2019, p. 30.
  32. ^ Dupuy, Dostal & Chikhaoui 1993, p. 143.
  33. ^ Benhallou, Megueni & BoussisseIkhlef-Debabha 2019, p. 31.
  34. ^ a b Bouzid et al. 2015, p. 4.
  35. ^ Bouzid et al. 2015, p. 5.
  36. ^ a b Rognon, P.; Mensching, Horst (1969). "Zur Geomorphologie des Hoggargebirges (Zentrale Sahara)". Erdkunde. 23 (1): 61–63. JSTOR 25640889.
  37. ^ Beccaluva, Luigi; Bianchini, Gianluca; Wilson, B. Marjorie; Wilson, Marjorie (2007). Cenozoic Volcanism in the Mediterranean Area. Geological Society of America. p. 324. ISBN 9780813724188.
  38. ^ Lesquer, A.; Bourmatte, A.; Ly, S.; Dautria, J.M. (January 1989). "First heat flow determination from the central Sahara: relationship with the Pan-African belt and Hoggar domal uplift". Journal of African Earth Sciences (and the Middle East). 9 (1): 46. Bibcode:1989JAfES...9...41L. doi:10.1016/0899-5362(89)90006-7. ISSN 0899-5362.
  39. ^ Kubiëna 1955, p. 132.
  40. ^ Capot-Rey 1969, p. 242.
  41. ^ Rognon 1963, p. 25.
  42. ^ Rognon 1963, p. 26.
  43. ^ Reffay, Annie (1982). "L'évolution géomorphologique des dômes volcaniques". Norois (in French). 115 (1): 407. doi:10.3406/noroi.1982.4052. ISSN 0029-182X.

Sources

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Bibliography

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