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Bulletin of Volcanology

, Volume 55, Issue 8, pp 571–587 | Cite as

Late Pleistocene to Holocene eruptive activity of Pico de Orizaba, Eastern Mexico

  • Armann Hoskuldsson
  • Claude Robin
Article

Abstract

The Late Pleistocene to Holocene eruptive history of Pico de Orizaba can be divided into 11 eurptive episodes. Each eruptive episode lasted several hundred years, the longest recorded being about 1000 years (the Xilomich episode). Intervals of dormancy range from millenia during the late Pleistocene to about 500 years, the shortest interval recorded in the Holocene. This difference could reflect either changes in the volcano's activity or that the older stratigraphic record is less complete than the younger. Eruptive mechanisms during the late Pleistocene were characterized by dome extrusions, lava flows and ash-and-scoria-flow generating eruptive columns. However, in Holocene time plinian activity became increasingly important. The increase in dacitic plinian eruptions over time is related to increased volumes of dacitic magma beneath Pico de Orizaba. We suggest that the magma reservoir under Pico de Orizaba is stratified. The last eruptive episode, which lasted from about 690 years bp until ad 1687, was initiated by a dacitic plinian eruption and was followed by effusive lava-forming eruptions. For the last 5,000 years the activity of the volcano has been gradually evolving towards such a trend, underlining the increasing importance of dacitic magma and stratification of the magma reservoir. Independent observations of Pico de Orizaba's glacier early this century indicate that some increase in volcanic activity occurred between 1906 and 1947, and that it was probably fumarolic.

Key words

Volcanism Mexico Holocene History Pico Citlaltepetl Volcano 

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References

  1. Bardinzeff JM, Bonin B (1987) The amphibole effect: A possible mechanism for triggering explosive eruptions. J Volcanol Geotherm Res 33:255–262Google Scholar
  2. Calvin EM, Kodo AM, Brookins DG, Ward DB (1989) Strontium isotope and trace element geochemistry of Pico de Orizaba, Trans-Mexican Volcanic Belt, Mexico. Comparison of phase II and III. IAVCEI, Santa Fe, (abstr.), 38 ppGoogle Scholar
  3. Cantagrel JM, Robin C (1979) K-Ar dating on eastern Mexican volcanic rocks — relations between the andesitic and alkaline provinces. J Volcanol Geotherm Res 5:99–114Google Scholar
  4. Cantagrel JM, Gourgaud A, Robin C (1984) Repetitive mixing events and Holocene pyroclastic activity at Pico de Orizaba and Popocatepetl (Mexico). Bull Volcanol 47-4(1):735–748Google Scholar
  5. Fisher RV, Schmincke H-U (1984) Pyroclastic rocks. Springer Berlin Heidelberg, New York, 472 ppGoogle Scholar
  6. Flint RF (1949) Glacial and quanternary geology. (Third printing) John Wiley & Sons, New York, 525 ppGoogle Scholar
  7. Gourgaud A (1985) Melange de magmas dans les series alcalines et calco-alkaline: leur role dans la genese des laves intermediaires et leur influence sur les mecanismes eruptifs. Exemple pris dans le Massif Central Francais (Mont-Dore, Chaine des Puys), à la Martinique (Montagne Pelee, Fissure Burgas-Diamant) et au Mexique (Pico de Orizaba). These de doctorat d'état, University of Clermont-Ferrand II, 522 ppGoogle Scholar
  8. Heine K (1989) Late Quaternary glacial chronology of the Mexican volcanoes. Die Geowissenschaften, 6th Jahrgang 7:197–205Google Scholar
  9. Hildreth W (1981) Gradients in silicic magma chambers: implications for lithospheric magmatism. J Geophys Res 86:10153–10192Google Scholar
  10. Hoskuldsson A (1986) Porosity and alteration in the Tjornesbeds (in Icelandic). Report, University of Iceland, 62 ppGoogle Scholar
  11. Hoskuldsson A (1992) Le complexe volcanique Pico de Orizaba-Sierra la Negra-Cerro las Cumbres (Sud-Est Mexicain): Structure, dynamismes eruptifs et evaluations des aleas. These de doctorat d'University Blaise Pascal, University of Blaise Pascal, 210 ppGoogle Scholar
  12. Hoskuldsson A, Robin C, Cantagrel JM (1990) Repetitive debris avalanche events at volcan Pico de Orizaba, Mexico. IAVCEI Mainz, (abstr.), 47 ppGoogle Scholar
  13. Le Maitre RW (ed) (1989) A classification of igneous rocks and glossary of terms, Recommendations of the International Union of Geological Sciences Subcommission and the Systematics of Igneous Rocks, Blackwell Scientific Publications, London, 193 ppGoogle Scholar
  14. Mooser F, Maldonado-Koerdell M (1961) Tectonica penecontemporanea a lo largo de la costa mexicana del Oceano Pacifico. Gefis Intern I:3–20Google Scholar
  15. Mooser F, Meyer AH, McBirney AR (1958) Catalogue of active volcanoes of the world, part VI, Central America. Interna Volc Assoc, pte. 6:36 ppGoogle Scholar
  16. Negendank JFW, Emmermann R, Krawcyk R, Mooser F, Tobschall H, Werle D (1985) Geological and geochemical investigation on the eastern Trans-Mexican Volcanic Belt. Geofis Intern 24:477–575Google Scholar
  17. Nixon GT (1982) The relationship between Quaternary volcanism in Central Mexico and the seismicity and structure of subducted oceanic lithosphere. Geol Soc Am Bull 93:514–523Google Scholar
  18. Ordonez E (1906) De Mexico a jalapa (Excursion de l'est). Congres Geologique International X, Guide des excursions, 11 ppGoogle Scholar
  19. Robin C (1981) Relations Volcanologie-Magmatologic-Geodynamique: application au passage entre volcanism alcalin et andesitique dans le sud Mexicain (Axe trans-mexicain et provence alcaline oriental) These Doctorat d'etat Universite Clermont-Ferrand II, 503 ppGoogle Scholar
  20. Robin C, Cantagrel JM (1982) Le Pico de Orizaba (Mexique). Structure et evolution d'un grand volcan andesitique complexe. Bull Volcanol 45-4:99–315Google Scholar
  21. Rose WI Jr, Pearson T, Bonis S (1976) Nuee ardente eruption from the foot of a dacite lava flow, Santiaguito volcano Guatemala. Bull Volcanol 40-1:23–38Google Scholar
  22. Siebe C, Adams M, Sheridan M (1991) Holocene age of major block-and-ash-flow fan at the western slopes of Pico de Orizaba volcano. Primer Congreso Mexicano de mineralogia, Mexico, (abstr.), 203 ppGoogle Scholar
  23. Simkin T, Siebert L, McCelland L, Bridge D, Newhall C, Latter JH (1981) Volcanoes of the World. A regional directory, gazetteer, and chronology of volcanism during the last 10000 years. Smithsonian Institution, Stroudsbourg, Pennsylvania, Hutchinson & Ross, 333 ppGoogle Scholar
  24. Smith AL, Roobol MJ (1991) Mt Pelee, Martinique. A study of an active island arc volcano. Geol Soc Am Mem 175, 114 ppGoogle Scholar
  25. Waitz P (1910) Observaciones geologicas acerca del Pico de Orizaba. Bolletin de la Sociedad Geologica Mexicana, VII:67–80Google Scholar
  26. Wright JV, Smith AL, Self S (1980) A working terminology of pyroclastic deposits. J Volcanol Geotherm Res 8:315–336Google Scholar

Copyright information

© Springer-Verlag 1993

Authors and Affiliations

  • Armann Hoskuldsson
    • 1
  • Claude Robin
    • 1
  1. 1.University Blaise Pascal, C.R.V., and C.N.R.S., 5 rueClermont FerrandFrance

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