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Sparks, R. S. J., Young, S. R., Barclay, J. 
ORCID: https://orcid.org/0000-0002-6122-197X, Calder, E. S., Cole, P., Darroux, B., Druitt, T. H., Harford, C., Herd, R. A., Hoblitt, R., James, M. R., LeJeune, A. M., Robertson, R., Stasiuk, M. V., Stevens, N. F., Toothill, J. and Wadge, G.
(1998)
Magma production and growth of the lava dome of the Soufriere Hills Volcano, Montserrat, West Indies: November 1995 to November 1997.
Geophysical Research Letters, 25 (18).
pp. 3421-3424.
ISSN 1944-8007
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Abstract
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 pyroclastic 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.
| Item Type: | Article |
|---|---|
| Faculty \ School: | Faculty of Science > School of Environmental Sciences |
| UEA Research Groups: | Faculty of Science > Research Groups > Geosciences Faculty of Science > Research Groups > Volcanoes@UEA (former - to 2018) Faculty of Science > Research Groups > Geosciences and Natural Hazards (former - to 2017) |
| Depositing User: | Rachel Snow |
| Date Deposited: | 28 Mar 2011 13:07 |
| Last Modified: | 24 Jul 2024 11:30 |
| URI: | https://ueaeprints.uea.ac.uk/id/eprint/27310 |
| DOI: | 10.1029/98GL00639 |
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