Auxiliary material for this article contains descriptions of methods and data used to estimate lava volumes emitted from Soufrière Hills Volcano, Montserrat between 1995 and 2009.

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grl26663-sup-0001-readme.txtplain text document7Kreadme.txt
grl26663-sup-0002-txts01.txtplain text document4KText S1. Dense rock equivalent volumes estimated for the dome.
grl26663-sup-0003-fs01.tifTIFF image100KFigure S1. Cross section of the axisymmetrical lava dome growth model used for volume estimation.
grl26663-sup-0004-txts02.txtplain text document2KText S2. Major dome collapse events.
grl26663-sup-0005-ts01.txtplain text document1KTable S1. Major dome collapses and surveys.
grl26663-sup-0006-txts03.txtplain text document1KText S3. Conduit-derived Vulcanian explosions.
grl26663-sup-0007-ts02.txtplain text document1KTable S2. Characteristics of conduit-derived Vulcanian explosions.
grl26663-sup-0008-txts04.txtplain text document3KText S4. Estimate of the near-shore and fan-delta sediment volumes.
grl26663-sup-0009-fs02.tifTIFF image23909KFigure S2. Contours of the sediment surface around the coast of Soufrière Hills Volcano.
grl26663-sup-0010-ts03.txtplain text document0KTable S3. Submarine sediment volume estimates.
grl26663-sup-0011-txts05.txtplain text document2KText S5. Uncertainties in the estimates.
grl26663-sup-0012-t01.txtplain text document1KTab-delimited Table 1.

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