TY - CHAP
T1 - Analysis of magma flux and eruption intensity during the 2021 explosive activity at La Soufrière, St Vincent, West Indies
AU - Sparks, R. J. Steve
AU - Aspinall, Willy P.
AU - Barclay, Jenni
AU - Renfrew, Ian
AU - Contreras-Arratia, Rodrigo
AU - Stewart, Robert
N1 - Issue: The 2020-21 Eruption of La Soufrière Volcano, St Vincent
PY - 2024/4/1
Y1 - 2024/4/1
N2 - Real-time Seismic Amplitude Measurement signals and eruption cloud height measurements were used to estimate peak intensities of 40 explosive events during the 8–22 April 2021 activity of La Soufrière vol-cano. We estimated magma supply rates and erupted volumes in each explosion, characterized uncertainty by stochastic modelling and identified four eruptive stages. Stage 1 included an intense period of 9.5 hours with 11 explosive events with peak eruption intensity between 2000 and 4000 m
3 s
−1 and magma supply rate reaching 828 m
3 s
−1. Twelve high-intensity explosions (c. 4000 m
3 s
−1) occurred in Stage 2 with average magma supply rate of 251 m
3 s
−1. Stage 3 involved both declining intensity and magma supply rate and lengthening repose periods between explosions. Stage 4 involved three much weaker explosions. The total erupted volume of magma is estimated at 38.5 × 10
6 m
3 (90% credible interval: [22.0.. 61.9] × 10
6 m
3) consistent with indepen-dent estimates from analysis of tephra deposits and volcano subsidence sourced at c. 6 km depth. The 150-fold increase in magma supply rate, from the preceding effusive phase to Stage 1 of the explosive phase, is attributed to replacement of very high-viscosity degassed magma occupying the shallow conduit system with new, lower-viscosity, volatile-rich magma from the magma chamber.
AB - Real-time Seismic Amplitude Measurement signals and eruption cloud height measurements were used to estimate peak intensities of 40 explosive events during the 8–22 April 2021 activity of La Soufrière vol-cano. We estimated magma supply rates and erupted volumes in each explosion, characterized uncertainty by stochastic modelling and identified four eruptive stages. Stage 1 included an intense period of 9.5 hours with 11 explosive events with peak eruption intensity between 2000 and 4000 m
3 s
−1 and magma supply rate reaching 828 m
3 s
−1. Twelve high-intensity explosions (c. 4000 m
3 s
−1) occurred in Stage 2 with average magma supply rate of 251 m
3 s
−1. Stage 3 involved both declining intensity and magma supply rate and lengthening repose periods between explosions. Stage 4 involved three much weaker explosions. The total erupted volume of magma is estimated at 38.5 × 10
6 m
3 (90% credible interval: [22.0.. 61.9] × 10
6 m
3) consistent with indepen-dent estimates from analysis of tephra deposits and volcano subsidence sourced at c. 6 km depth. The 150-fold increase in magma supply rate, from the preceding effusive phase to Stage 1 of the explosive phase, is attributed to replacement of very high-viscosity degassed magma occupying the shallow conduit system with new, lower-viscosity, volatile-rich magma from the magma chamber.
UR - http://www.scopus.com/inward/record.url?scp=85180593699&partnerID=8YFLogxK
U2 - 10.1144/SP539-2022-286
DO - 10.1144/SP539-2022-286
M3 - Chapter (peer-reviewed)
VL - 539
T3 - Geological Society Special Publications
SP - 63
EP - 79
BT - Geological Society Special Publication
PB - Geological Society of London
ER -