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Magma production and growth of the lava dome of the Soufriere Hills Volcano, Montserrat, West Indies: November 1995 to November 1997

  • R. S. J. Sparks
  • , S. R. Young
  • , J. Barclay
  • , E. S. Calder
  • , P. Cole
  • , B. Darroux
  • , T. H. Druitt
  • , C. Harford
  • , R. A. Herd
  • , R. Hoblitt
  • , M. R. James
  • , A. M. LeJeune
  • , R. Robertson
  • , M. V. Stasiuk
  • , N. F. Stevens
  • , J. Toothill
  • , G. Wadge

Research output: Contribution to journalArticlepeer-review

152 Citations (Scopus)
14 Downloads (Pure)

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.
Original languageEnglish
Pages (from-to)3421-3424
Number of pages4
JournalGeophysical Research Letters
Volume25
Issue number18
DOIs
Publication statusPublished - 15 Sept 1998

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