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Journal articles on the topic 'Cameroon Volcanic Line'

Author: Grafiati

Published: 4 June 2021

Last updated: 26 July 2025

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1

Nemzoue, P. N. N., N. A. K. Keutchafo, and J. P. Tchouankoue. "GEOTHERMAL DEVELOPMENT IN CAMEROON." Revista de Engenharia Térmica 19, no. 1 (2020): 32. http://dx.doi.org/10.5380/reterm.v19i1.76428.

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Africa is currently experiencing a period of economic growth. Its population is growing rapidly and its economies grow and diversify. To be sustainable, such growth requires a large investment in the energy sector. In the case of Cameroon hydroelectric energy is the main source of electrical power whereas the analysis of the geological point of view shows that Cameroon is unique in west-northern of Africa for its active volcanic line (with the last eruption of Mount Cameroon that last erupted in 1999 and 2000) that is a favorable zone for the production of power from geothermal resources. The

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2

Ngounouno Yamgouot, Fadimatou, Isaac Bertrand Gbambie Mbowou, Ismaïla Ngounouno, Azizi Abdoul Youpoungam, Isaac Daama, and Bernard Déruelle. "Insight into geochemistry of basaltic rocks from Mt Cameroon and characterization of the mantle source." International Journal of Advanced Geosciences 6, no. 2 (2018): 151. http://dx.doi.org/10.14419/ijag.v6i1.10738.

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Alkaline volcanic activities occurred in the Mt Cameroon at the ocean-continent boundary of the Cameroon Line. It is characterized by a volcanic association of alkali basalts and hawaiites extruded during the late Miocene to Recent times. The major and trace element geochemistry of the Mt Cameroon are consistent with the fractional crystallization of olivine ± clinopyroxene ± plagioclase (± amphibole). Petrographical and mineralogical study reveals the presence of xenocryts (olivine, clinopyroxene and spinel) in Mt Cameroon basalts. Their composition are similar to xenoliths and rocks crystals

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3

Ubangoh, R. U., I. G. Pacca, J. B. Nyobe, J. Hell, and B. Ateba. "Petromagnetic characteristics of Cameroon Line volcanic rocks." Journal of Volcanology and Geothermal Research 142, no. 3-4 (2005): 225–41. http://dx.doi.org/10.1016/j.jvolgeores.2004.11.006.

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4

Aminatou, Fagny Mefire, Nkouandou Oumarou Faarouk, Temdjim Robert, et al. "New K–AR ages of tchabal mbabo alkaline volcano massif, Cameroon volcanic line and adamawa plateau (central Africa)." International Journal of Advanced Geosciences 4, no. 2 (2016): 62. http://dx.doi.org/10.14419/ijag.v4i2.6516.

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Tchabal Mbabo in Central Africa is a voluminous volcano massif composed of alkali lava series. K-Ar geochronology data obtained from three samples of basanite - trachyandesite composition defined at least two volcanic activities. The first at end Eocene (38.22 ± 0.80 Ma) and the second during Oligocene (28.88 ± 0.61 and 28.60 ± 0.60Ma). The distribution of different ages along the Cameroon Volcanic Line is difficult to council with any migration of magmatic activity, as previously suggested. The most realistic scenario for the formation of Cameroon Line is that the ascent of lavas has been fav

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5

Tabod, C. T., J. D. Fairhead, G. W. Stuart, B. Ateba, and N. Ntepe. "Seismicity of the Cameroon Volcanic Line, 1982–1990." Tectonophysics 212, no. 3-4 (1992): 303–20. http://dx.doi.org/10.1016/0040-1951(92)90297-j.

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6

Tanyileke, G. Z., M. Kusakabe, and W. C. Evans. "Chemical and isotopic characteristics of fluids along the Cameroon Volcanic Line, Cameroon." Journal of African Earth Sciences 22, no. 4 (1996): 433–41. http://dx.doi.org/10.1016/0899-5362(96)00025-5.

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7

Hlaváč, Peter, Petr Baňař, and Eric Bertrand Fokam. "Pselaphinae of the Cameroon Volcanic Line. Part 3. A new genus of Goniacerini (Coleoptera: Staphylinidae: Goniaceritae) from Mount Cameroon." Zootaxa 5323, no. 2 (2023): 255–67. https://doi.org/10.11646/zootaxa.5323.2.5.

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Hlaváč, Peter, Baňař, Petr, Fokam, Eric Bertrand (2023): Pselaphinae of the Cameroon Volcanic Line. Part 3. A new genus of Goniacerini (Coleoptera: Staphylinidae: Goniaceritae) from Mount Cameroon. Zootaxa 5323 (2): 255-267, DOI: 10.11646/zootaxa.5323.2.5, URL: http://dx.doi.org/10.11646/zootaxa.5323.2.5

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8

Fagny, A. M., O. F. Nkouandou, J. M. Bardintzeff, et al. "Petrology and geochemistry of the Tchabal Mbabo volcano in Cameroon volcanic line (Cameroon, Central Africa): An intra-continental alkaline volcanism." Journal of African Earth Sciences 170 (October 2020): 103832. http://dx.doi.org/10.1016/j.jafrearsci.2020.103832.

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9

Milelli, L., L. Fourel, and C. Jaupart. "A lithospheric instability origin for the Cameroon Volcanic Line." Earth and Planetary Science Letters 335-336 (June 2012): 80–87. http://dx.doi.org/10.1016/j.epsl.2012.04.028.

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10

Hlaváč, Peter, and Petr Baňař. "Pselaphinae of the Cameroon Volcanic Line. Part 1. New Pselaphinae (Coleoptera, Staphylinidae) from the island São Tomé." Zootaxa 5222, no. 3 (2022): 267–76. https://doi.org/10.11646/zootaxa.5222.3.4.

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Hlaváč, Peter, Baňař, Petr (2022): Pselaphinae of the Cameroon Volcanic Line. Part 1. New Pselaphinae (Coleoptera, Staphylinidae) from the island São Tomé. Zootaxa 5222 (3): 267-276, DOI: 10.11646/zootaxa.5222.3.4

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11

Nkouathio, D. G., J. J. Ménard, P. Wandji, and J. M. Bardintzeff. "The Tombel graben (West Cameroon): a recent monogenetic volcanic field of the Cameroon Line." Journal of African Earth Sciences 35, no. 2 (2002): 285–300. http://dx.doi.org/10.1016/s0899-5362(02)00031-3.

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12

Aziwo, Bertrand Tatoh, Jules Tamen, Boris Chako-Tchamabé, et al. "Tephrostratigraphy and morphometry of Wum Maar Volcano (Oku Volcanic Group- Cameroon Volcanic line): Implications for complex monogenetic volcanoes." Journal of African Earth Sciences 188 (April 2022): 104470. http://dx.doi.org/10.1016/j.jafrearsci.2022.104470.

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13

Dedzo, M. Gountie. "Mapping and Assessment of Volcanic Hazards Related to the Ignimbritic Eruption by AMS in Bambouto Volcano (Cameroon Volcanic Line)." Open Geology Journal 7, no. 1 (2013): 1–13. http://dx.doi.org/10.2174/1874262901307010001.

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14

Pierre, Wotchoko, Tita Margaret Awah, Kouankap Nono Gus Djibril, et al. "Hydrochemistry of springs in the bambui-sabga volcanic area (north west region, Cameroon volcanic line)." International Journal of Advanced Geosciences 3, no. 2 (2015): 42. http://dx.doi.org/10.14419/ijag.v3i2.5355.

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<p>This study was carried out in the Bambui-Sabga volcanic area in Tubah Sub-Division, North West Region, Cameroon. This research was aimed at carrying out a hydrochemical characterization of springs in the area. Chemical analysis were done using a DR 2010 Hach Spectrophotometer. The analysed spring samples were close to neutral (pH 6.9-7.6) with a high electrical conductivity ranging from 1,400 - 11,400 µS/cm and TDS from 750 - 7,960 mg/l. The FS01 spring recorded the highest average temperature of 34oC, yellowish-brown in colour and rusty odour, while the FS02 spring had a salty taste

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15

Atanga, M. B. S., Anita vd Merve, M. S. Njome, W. Kruger, and C. E. Suh. "Health System Preparedness for Hazards Associated with Mount Cameroon Eruptions: A Case Study of Bakingili Village." International Journal of Mass Emergencies & Disasters 28, no. 3 (2010): 298–325. http://dx.doi.org/10.1177/028072701002800301.

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Mount Cameroon, the only active volcano along the Cameroon Volcanic Line (CVL) and most active in equatorial West Africa, erupted seven times in the last century. The 1999 eruption prompted evacuation of over 600 inhabitants of Bakingili village on the south western slopes – the first in the history of this volcano. Besides destruction from flowing lava, associated health hazards resulted from fine ash and poisonous gases that accompanied explosions. This eruption revealed a lack of preparedness on the part of the communities and the Cameroonian administration to such phenomena, as a National

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16

Yamgouot, Fadimatou Ngounouno, Bernard Déruelle, Isaac Bertrand Gambie Mbowou, and Ismaïla Ngounouno. "Petrology of the Volcanic Rocks from Bioko Island (“Cameroon Hot Line”)." International Journal of Geosciences 06, no. 03 (2015): 247–55. http://dx.doi.org/10.4236/ijg.2015.63019.

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17

Itiga, Zénon, Jacques-Marie Bardintzeff, Pierre Wotchoko, Pierre Wandji, and Hervé Bellon. "Tchabal Gangdaba massif in the Cameroon Volcanic Line: a bimodal association." Arabian Journal of Geosciences 7, no. 11 (2013): 4641–64. http://dx.doi.org/10.1007/s12517-013-1126-8.

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18

Aka, Festus T., Keisuke Nagao, Minoru Kusakabe, et al. "Symmetrical Helium isotope distribution on the Cameroon Volcanic Line, West Africa." Chemical Geology 203, no. 3-4 (2004): 205–23. http://dx.doi.org/10.1016/j.chemgeo.2003.10.003.

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19

Azinwi Tamfuh, Primus, Djibril Gus Kouankap Nono, Pierre Wotchoko, et al. "Geochemistry of a lateritic mantle developed on basalt in the Cameroon Western Highlands (Cameroon Volcanic Line)." Geoderma 376 (October 2020): 114569. http://dx.doi.org/10.1016/j.geoderma.2020.114569.

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20

Gountié Dedzo, Merlin, Djamilatou Diddi Hamadjoda, Eric Martial Fozing, et al. "Petrology and geochemistry of ignimbrites and associated enclaves from Mount Bambouto, West-Cameroon, Cameroon Volcanic Line." Geochemistry 80, no. 4 (2020): 125663. http://dx.doi.org/10.1016/j.chemer.2020.125663.

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21

Kamgang, Pierre, Emmanuel Njonfang, Alexandre Nono, Merlin Gountie Dedzo, and Félix M. Tchoua. "Petrogenesis of a silicic magma system: Geochemical evidence from Bamenda Mountains, NW Cameroon, Cameroon Volcanic Line." Journal of African Earth Sciences 58, no. 2 (2010): 285–304. http://dx.doi.org/10.1016/j.jafrearsci.2010.03.008.

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22

Gonmadje, Christelle, Charles Doumenge, Terry Sunderland, Michael Balinga, and Bonaventure Sonké. "Analyse phytogéographique des forêts d'Afrique Centrale: le cas du massif de Ngovayang (Cameroun)." Plant Ecology and Evolution 145, no. (2) (2012): 152–64. https://doi.org/10.5091/plecevo.2012.573.

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Phytogeographical analysis of Central African forests: the Ngovayang massif (Cameroon) <b>Background and aims</b> – The Ngovayang massif, in southern Cameroon, is part of a group of small hills along the Atlantic coast of the Gulf of Guinea. This area is known for its floristic richness and its high level of endemism. We conducted a phytogeographical analysis of this massif and evaluated its floristic affinities with other forested sites in Central Africa. <b>Methods</b> – Phytogeographical analysis was based on a comparison of lists of tree species with dbh ≥ 10 cm, inventoried in 1-ha perman

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23

Konfor, Njilah, Robert Temdjim, Charles Richard, Nzolang Ghogomu, Rose Tchuitchou, and Humphery Ajonina. "Geochemistry of tertiary-quaternary lavas of Mt. Oku Northwest Cameroon." Revista Facultad de Ingeniería Universidad de Antioquia, no. 40 (July 31, 2014): 59–75. http://dx.doi.org/10.17533/udea.redin.20149.

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The Oku massif occupies the central position amongst the continental sector volcanoes of the Cameroon Volcanic Line (CVL). Field observations, petrographic major, trace and REE geochemistry show that lavas are basanite/alkali basalt-trachyte/rhyolite suited with a distinct compositional gap within the benmoreite field. This gap, which cannot be explained by sampling bias, may therefore reflect density filtration within the magmatic plumbing system. However, accumulation and fractionation of major mineral phases: pyroxenes, olivines and plagioclases appear to have controlled magma evolution. Fr

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24

Reusch, Angela Marie, Andrew A. Nyblade, Rigobert Tibi, et al. "Mantle transition zone thickness beneath Cameroon: evidence for an upper mantle origin for the Cameroon Volcanic Line." Geophysical Journal International 187, no. 3 (2011): 1146–50. http://dx.doi.org/10.1111/j.1365-246x.2011.05239.x.

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25

Reusch, A. M., A. A. Nyblade, D. A. Wiens, et al. "Upper mantle structure beneath Cameroon from body wave tomography and the origin of the Cameroon Volcanic Line." Geochemistry, Geophysics, Geosystems 11, no. 10 (2010): n/a. http://dx.doi.org/10.1029/2010gc003200.

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26

Ubangoh, R. U., I. G. Pacca, and J. B. Nyobe. "Palaeomagnetism of the continental sector of the Cameroon Volcanic Line, West Africa." Geophysical Journal International 135, no. 2 (1998): 362–74. http://dx.doi.org/10.1046/j.1365-246x.1998.00635.x.

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27

Schmidt, Christoph, Jean Pierre Tchouankoue, Peguy Noel Nkouamen Nemzoue, Félicité Ayaba, Siggy Signe Nformidah-Ndah, and Emmanuel Nformi Chifu. "New thermoluminescence age estimates for the Nyos maar eruption (Cameroon Volcanic Line)." PLOS ONE 12, no. 5 (2017): e0178545. http://dx.doi.org/10.1371/journal.pone.0178545.

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28

Pouclet, André, Armand Kagou Dongmo, Jacques-Marie Bardintzeff, et al. "The Mount Manengouba, a complex volcano of the Cameroon Line: Volcanic history, petrological and geochemical features." Journal of African Earth Sciences 97 (September 2014): 297–321. http://dx.doi.org/10.1016/j.jafrearsci.2014.04.023.

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29

Chenyi, Marie-Louise Vohnyui, David Guimollaire Nkouathio, Pierre Wotchoko, et al. "Volcanology and geochemical study of the volcanic rocks of the Bafmeng area (Mount Oku, Cameroon Volcanic Line)." International Journal of Biological and Chemical Sciences 11, no. 2 (2017): 941. http://dx.doi.org/10.4314/ijbcs.v11i2.25.

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30

Dili-Rake, Jacques, Sahabo Aboubakar Abdoulaye, Joseph Legrand Tchop, et al. "Magmatism of the Beka Volcanic Massifs (Cameroon Volcanic Line, West-Central Africa): New Petrographical and Mineralogical Data." Journal of Geoscience and Environment Protection 10, no. 07 (2022): 198–228. http://dx.doi.org/10.4236/gep.2022.107013.

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31

Asaah, Asobo N. E., Tetsuya Yokoyama, Festus T. Aka, et al. "Geochemistry of lavas from maar-bearing volcanoes in the Oku Volcanic Group of the Cameroon Volcanic Line." Chemical Geology 406 (June 2015): 55–69. http://dx.doi.org/10.1016/j.chemgeo.2015.03.030.

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32

Dongmo A, Kagou, Guedjeo C .S, Primus A.T, et al. "Geochemical and geotechnical characterization of soils developed on volcanic rocks on the Bamenda mountain (Cameroon volcanic line)." International Journal of Advanced Geosciences 6, no. 2 (2018): 184. http://dx.doi.org/10.14419/ijag.v6i2.13505.

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The weathering mechanism of rocks exposed under the same conditions on the Bamenda Mountain is not well understood. The aim of this study is to characterize basalt, trachyte and rhyolite and their products on the geochemical and geotechnical aspect. Here three wells were hand dug on rocks developed on basalt, trachyte and rhyolite and studied. The results showed that, Ki values (0.34-6.57) indicate SiO2 are more leached on soils developed on basalt than those on trachyte and rhyolite. CIA (72.62-97.8) and CIW (72.76-98.8) indicate an advanced to extreme chemical weathering in this environment,

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33

Ngwa, Caroline N., Bless N. Shu, Benoît J. Mbassa, Festus T. Aka, and Pauline N. Wokwenmendam. "Olivine chemistry from Cameroon: evidence of carbonate metasomatism along the ocean-continental boundary of the Cameroon volcanic line." Mineralogy and Petrology 114, no. 1 (2019): 57–70. http://dx.doi.org/10.1007/s00710-019-00689-5.

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34

Ako, Andrew Ako, Gloria Eneke Takem Eyong, Jun Shimada, et al. "Nitrate contamination of groundwater in two areas of the Cameroon Volcanic Line (Banana Plain and Mount Cameroon area)." Applied Water Science 4, no. 2 (2013): 99–113. http://dx.doi.org/10.1007/s13201-013-0134-x.

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35

Wandji, Pierre, Dieudonné Tchokona Seuwui, Jacques-Marie Bardintzeff, Hervé Bellon, and Bernard Platevoet. "Rhyolites of the Mbépit Massif in the Cameroon Volcanic Line: an early extrusive volcanic episode of Eocene age." Mineralogy and Petrology 94, no. 3-4 (2008): 271–86. http://dx.doi.org/10.1007/s00710-008-0013-6.

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36

Shellnutt, J. G., T. Y. Lee, P. K. Torng, C. C. Yang, and Y. H. Lee. "Late Cretaceous intraplate silicic volcanic rocks from the Lake Chad region: An extension of the Cameroon volcanic line?" Geochemistry, Geophysics, Geosystems 17, no. 7 (2016): 2803–24. http://dx.doi.org/10.1002/2016gc006298.

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37

Tchamabé, Boris Chako, Takeshi Ohba, Issa , et al. "Temporal Evolution of the Barombi Mbo Maar, a Polygenetic Maar-Diatreme Volcano of the Cameroon Volcanic Line." International Journal of Geosciences 05, no. 11 (2014): 1315–23. http://dx.doi.org/10.4236/ijg.2014.511108.

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38

Kemgang Ghomsi, Franck Eitel, Janvier Domra Kana, Zakari Aretouyap, et al. "Main structural lineaments of the southern Cameroon volcanic line derived from aeromagnetic data." Journal of African Earth Sciences 186 (February 2022): 104418. http://dx.doi.org/10.1016/j.jafrearsci.2021.104418.

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39

Pierre, Wotchoko, Takojio Nguemo Rose Eugenie, Kouankap Nono Gus Djibril, et al. "The Twin Bambili Maars (Bamenda Mountains, Cameroon Volcanic Line): Simulative Model of Formation." Open Journal of Geology 07, no. 04 (2017): 443–56. http://dx.doi.org/10.4236/ojg.2017.74030.

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40

Meyers, Jayson B., and Bruce R. Rosendahl. "Seismic reflection character of the Cameroon volcanic line: Evidence for uplifted oceanic crust." Geology 19, no. 11 (1991): 1072. http://dx.doi.org/10.1130/0091-7613(1991)019<1072:srcotc>2.3.co;2.

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41

C. S, Guedjeo, Kagou Dongmo A., Wotchoko P., et al. "Landslide Susceptibility Mapping and Risk Assessment on the Bamenda Mountain (Cameroon Volcanic Line)." Journal of Geosciences and Geomatics 5, no. 4 (2017): 173–85. http://dx.doi.org/10.12691/jgg-5-4-2.

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42

Okereke, C. S. "Contrasting modes of rifting: The Benue Trough and Cameroon Volcanic Line, West Africa." Tectonics 7, no. 4 (1988): 775–84. http://dx.doi.org/10.1029/tc007i004p00775.

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43

Marcel, Jean, Jean Marcel Abate Essi, Jorelle Larissa Meli’i, Philippe Njandjock Nouck, Abakar Mahamat, and Eliezer Manguelle-Dicoum. "Geodynamic insights of the Cameroon Volcanic Line (Western Africa) from isostatic gravity anomalies." Journal of Geodynamics 121 (November 2018): 36–48. http://dx.doi.org/10.1016/j.jog.2018.07.002.

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44

Caldeira, R., and J. M. Munhá. "Petrology of ultramafic nodules from São Tomé Island, Cameroon Volcanic Line (oceanic sector)." Journal of African Earth Sciences 34, no. 3-4 (2002): 231–46. http://dx.doi.org/10.1016/s0899-5362(02)00022-2.

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45

Asaah, Asobo N. E., Tetsuya Yokoyama, Festus T. Aka, et al. "A comparative review of petrogenetic processes beneath the Cameroon Volcanic Line: Geochemical constraints." Geoscience Frontiers 6, no. 4 (2015): 557–70. http://dx.doi.org/10.1016/j.gsf.2014.04.012.

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46

Prigent, Stéphane R., Philippe Le Gall, Shay Wilfred Mbunda, and Michel Veuille. "Seasonal and altitudinal structure of drosophilid communities on Mt Oku (Cameroon volcanic line)." Comptes Rendus Geoscience 345, no. 7-8 (2013): 316–26. http://dx.doi.org/10.1016/j.crte.2013.08.001.

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47

Prigent, S.R., Gall P. Le, S.W. Mbunda, and M. Veuille. "Seasonal and altitudinal structure of drosophilid communities on Mt Oku (Cameroon volcanic line)." Comptes Rendues Geosciences 345 (June 5, 2013): 316Ð326. https://doi.org/10.1016/j.crte.2013.08.001.

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48

Yiika, Lemnyuy Prosper, Adze Rene Meniemoh, Emmanuel Eseya Mengu, Chin Thierry Berinyuy, and Kouankap Nono Gus Djibril. "Geochemistry and source area weathering of soils around Mount Bamboutos (Cameroon Volcanic Line)." Advances in Analytic Science 6, no. 1 (2025): 3670. https://doi.org/10.54517/aas3670.

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<p class="MsoNormal" style="text-align: justify; text-justify: inter-ideograph; line-height: 120%; layout-grid-mode: char; mso-layout-grid-align: none; punctuation-wrap: simple; margin: 12.0pt 0cm 6.0pt 0cm;"><span lang="EN-US" style="font-size: 10.0pt; mso-bidi-font-size: 11.0pt; line-height: 120%; font-family: 'Times New Roman',serif; mso-fareast-language: ZH-CN;">This study aimed at investigating the weathering of the source area and the geochemistry of the soils around Mount Bamboutos, West Region, Cameroon. In this study, soil samples were collected from a depth of 0&ndash

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49

Gvoždík, Václav, Tadeáš Nečas, Matej Dolinay, Breda M. Zimkus, Andreas Schmitz, and Eric B. Fokam. "Evolutionary history of the Cameroon radiation of puddle frogs (Phrynobatrachidae: Phrynobatrachus), with descriptions of two critically endangered new species from the northern Cameroon Volcanic Line." PeerJ 8 (March 3, 2020): e8393. http://dx.doi.org/10.7717/peerj.8393.

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The Cameroon Volcanic Line, a mountain chain located between West and Central Africa, is a region of numerous endemic diversifications, including of puddle frogs (Phrynobatrachus). This study reviews the phylogeny and taxonomy of puddle frogs of the “Cameroon radiation,” which is a clade containing mainly montane but also at least three lowland species. Molecular data revealed a novel evolutionary lineage from high altitudes in the northern part of the mountains. Puddle frogs from the new, minute-sized (SVL < 20 mm) lineage are identified using molecular, morphological and acoustic data and

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50

Mouzong, Marcelin Pemi, Inoussah Moungnutou Mfetoum, Simon Koumi Ngoh, Prosper Gopdjim Noumo, and Jean Gaston Tamba. "Current Status, Future Prospects, and the Need for Geothermal Energy Exploration in Cameroon: Comprehensive Review." Geofluids 2023 (August 24, 2023): 1–13. http://dx.doi.org/10.1155/2023/6168519.

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Cameroon is a country in Central Africa that relies heavily on hydropower, fossil fuels, solar, and biomass for its energy needs. However, the unstable and intermittent nature of these energy sources makes them unreliable, and there is a pressing need for a more secure and sustainable energy supply. Geothermal energy, which is abundant in Cameroon due to its favorable geological characteristics, has not been fully explored as a potential energy source. This study is aimed at providing a comprehensive review of the current status and future prospects of geothermal energy in Cameroon, based on p

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