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Detailed Reference Information |
Sparks, R.S.J., Young, S.R., Barclay, J., Calder, E.S., Cole, P., Darroux, B., Davies, M.A., Druitt, T.H., Harford, C., Herd, R., James, M., Lejeune, A.M., Loughlin, S., Norton, G., Skerrit, G., Stasiuk, M.V., Stevens, N.S., Toothill, J., Wadge, G. and Watts, R. (1998). Magma production and growth of the lava dome of the Soufriere Hills Volcano, Montserrat, West Indies: November 1995 to December 1997. Geophysical Research Letters 25: doi: 10.1029/98GL00639. issn: 0094-8276. |
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From November 1995 to December 1997 a total volume of 246¿106 (DRE) m3 of andesite magma erupted, partitioned into 93¿106 m3 of the dome, 125¿106 m3 of pyroelastic flow deposits and 28¿106 m3 of explosive ejecta. In the first 11 weeks magma discharge rate was low (0.5 m3/s). From February 1996 to May 1997 discharge rates have averaged 2.1 m3/s, but have fluctuated significantly and have increased with time. Three pulses lasting a few months can be recognised with discharge rates reaching 3 to 8 m3/s. Short term pulsations in growth lasting a few days reach discharge rates of over 10 m3/s and there are periods of days to a few weeks when dome growth is <0.5 m3/s. Discharge rate increased from May 1997 with an average rate of 7.5 m3/s to December 1997. The observations indicate an open magmatic system. ¿ 1998 American Geophysical Union |
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BACKGROUND DATA FILES |
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Abstract |
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Keywords
Volcanology, Volcanology, Magma migration, Volcanology, Eruption mechanisms, Volcanology, Eruption monitoring |
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Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
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