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Pattern and mechanism of volcanic activity at the Santiaguito Volcanic Dome, Guatemala

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Abstract

Santiaguito volcano has shown a continuous slow extrusion of dacite lava since 1922. In the 50 years of activity there have been four periods of abnormally high extrusion rates, interspersed by periods of little magma production. The type of activity shown by the volcano has been varied and crudely cyclic. Dome extrusion periods are accompanied by pyroclastic activity and followed by lava flows. There are now 16 time stratigraphic units delineated on the dome. Activity since 1967 has been especially closely observed. Dome extrusion at the west end of the complex has been accompanied by pyroclastic cruptions and plug dome extrusion at the east end. The eurrent extrusion rate has remained essentially constant since 1967 at about 5×106 m3/yr, far below Santiaguito’s 1922–71 average of 14×106 m3/yr. The active vent at the east end of the volcano (Caliente vent) has been the principal vent of the volcano since the creation of the explosion crater in 1902. After its initial period of dome extrusion (1922–25), the Caliente vent has chiefly produced pyroclastic eruptions as well as at least 95% of the dome’s lumarolic activity, while lateral vents have continued to give rise to lavas. Lava flows at Santiaguito have effective viscosity values of about 106 poises, while dome lavas are significantly more viscous. The differences in viscosity are in part related to volatile content of the lava when it reaches the surface. During dome extrusion, lavas lose their volatiles through pyroclastic activity before they reach the surface. Lava flows at Santiaguito occur when lava reaches the surface with higher volatile content. Obstruction of either the central (pyroclastic) vent or the lateral (dome extrusion) vent or both vents has an important influence on succeeding activity. In June 1972, at the time of this writing, the outbreak of new lava flows at both the Caliente and lateral El Brujo vents has just occurred, resulting from obstruction of pyroclastic activity by a large plug dome at the Caliente vent.

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References

  • Alvarado, J. A., 1936,Fratado de Caficultura Practica. Guaternala, 262 pp.

  • Bohnenbergur, O. H., Bengoechea, A. J., Dondoll, C., andCastro, A. M., 1969,Report on active volcanoes in Cemral America during 1957–1965. Bull. Volc. Eruptions (Volc. Suciety of Japan) No. 9–1, p. 2–19.

  • Deger, E., 1931,Chemische Umersuchung der bei den Ausbruchen des Vulkans Santa Maria, Guatemala, im Jahre 1929 viedergegungenen Auswurfsmarcrialen. Chemic der Erde,6, p. 376–380.

    Google Scholar 

  • Friedman, I., Long, W., andSmith, R. L., 1963,Viscosity and water contem of thyolue glass. J. Geophys. Res.,68, p. 6523.

    Article  Google Scholar 

  • Hantke, G., 1955,Ubersicht über the vulkanische Tätigkeit 1951–1953. Bull. Volc.,16, p. 71–113.

    Article  Google Scholar 

  • Kalser, W., 1930,Notiz über einen Besuch des Sama Maria, Guatemala. Z. Vulk.,12, p. 236.

    Google Scholar 

  • Meyer-Abich, H., 1956,Los volcanes activos de Guatemala y El Salvador. Anales del Servicio Geológico Nacional de El Salvador,3, p. 1–102.

    Google Scholar 

  • Minakaml, T., 1939,Geophysical studies of Asama I olcano. Proc. 6th Pacific Sci. Congo., Berkeley,2, p. 2859–873.

    Google Scholar 

  • Morris, R. C., 1963,La Cupula de Lava Samiagnito. Prensa Libre, Guatemala, December 11–19 (series in five parts).

  • Nichols, R. L., 1939,Viscosity of lava. J. Geol.,47, p. 290.

    Article  Google Scholar 

  • Pough, F. H., andMuiford, J. W., 1957,The Cranbrook Central American Volcanic Expedition. Granbrook (Mich.) Inst. Sci. Newslettet, Oct. 1957, p. 25–28.

  • Reck, H., andVon Tulrckheim, O. G., 1936,Der Zustand der Vulkans Fuego Atitlan und Sama Maria in Guatemala Ende 1934. Z. Vulk.,14, p. 259–263.

    Google Scholar 

  • Ruse, W. I., Jr., 1970,The Geology of the Santiaguito Volcanic Dome. Guatemala. Ph. D. Thesis, Dartmouth College, 253 p.

  • —————, 1972a,Notes on the 1902 eruption of Santa Maria Volcano, Guatemala. Bull. Volc.,36, No. 1, p. 29–45.

    Article  Google Scholar 

  • —————, 1972b,Santiagnito Voleanic Dome, Guatemala. Geol. Soc. Amer. Bull.,83, p. 1413–1434.

    Article  Google Scholar 

  • —————,Sronber, R. E., andBonis, S. B., 1970,Volcanic Activity at Samiaguito Volcano, Guatemala, June 1968–August 1969. Bull. Vole.,34, No. 1, p. 295–307.

    Article  Google Scholar 

  • Sapper, Karl, 1904,Die vulkanischen Ereignisse in Mittelamerika in Jahre 1902. Neues Jahrbuch f. Miner., Geol. u. Palaont., p. 39–90.

  • -----, 1913,Die Mittelamerikanischen Vulkane. Petermanns Geographische Mitteilungen, Erg. 178, 173 p.

  • —————, 1926,Die Vulkanische Tätigkeit in Mittelamerika im 20 Jahrhundert, I Teil, Z. Vulk.,9, p. 156–203.

    Google Scholar 

  • —————, andTermer, F., 1930a,Vulkanische Ereignisse; Santa Maria. Z. Vulk.,13, p. 57.

    Google Scholar 

  • —————, 1930b, Der Ausbruch des Vulkans Santa María in Guatemala vom 2–4 November 1929. Z. Vulk.,13, p. 73–101.

    Google Scholar 

  • —————, 1932,Einige Bemerkungen über tätige vulkane von Guatemala und El Salvador. Z. Vulk.,14, p. 273–287.

    Google Scholar 

  • Stoiber, R. E., andRose, W. I., Jr., 1969,Recent Volcanic and Fumarolic Activity at Santiaguito Volcano, Guatemala. Bull. Volc.,33, No. 2, p. 475–502.

    Article  Google Scholar 

  • —————, 1970,The Geochemistry of Central American Volcanic Gas Condensates. Geol. Soc. Amer. Bull.,81, p. 2891–2912.

    Article  Google Scholar 

  • Termer, F., 1929,Ausbruch des Vulkans Santa María in Guatemala am 14 Mai 1928. Z. Vulk.,12, p. 231–235.

    Google Scholar 

  • —————, 1930,Vulkanische Ereignisse; Santa María. Z. Vulk.,13, p. 25.

    Google Scholar 

  • —————, 1934,Die Tätigkeit des vulkans Santa María in Guatemala in den Jahren 1931–1933. Z. Vulk.,16, p. 43–50.

    Google Scholar 

  • —————, 1964,Die Tätigkeit der Vulkane von Guatemala in den Jahren 1960–1963. Petermanns Geographysche Mitteilungen,108, p. 261–268.

    Google Scholar 

  • von Tuerckheim, Otto Gunter, 1923,Ascension al crater del Volcan de Santa María, Guatemala. Memoires de la Societe « Antonio Alzate »,41, p. 343–351.

    Google Scholar 

  • —————, 1935,Nachrichtendienst über vulkanische Ereignisse 1934–1935; Santa María. Z. Vulk.,16, p. 263.

    Google Scholar 

  • Yokoyama, I., 1957,Energetics in active volcanoes, 1st, 2nd and 3rd paper. Bull. Earthquake Research Institute,35, p. 75–97.

    Google Scholar 

  • Zies, E. G., 1941,Temperatures of volcanoes, fumaroles and hot springs. InTemperature: its Measurement and Control in Science and Industry. Am. Inst. Phys. Symp., New York, Nov. 1939, p. 372.

    Google Scholar 

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  1. Department of Geology and Geological Engineering, Michigan Technological University, 49931, Houghton, Michigan, USA

    W. I. Rose Jr.

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Rose, W.I. Pattern and mechanism of volcanic activity at the Santiaguito Volcanic Dome, Guatemala. Bull Volcanol 37, 73–94 (1973). https://doi.org/10.1007/BF02596881

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