Deposits from dome-collapse and fountain-collapse pyroclastic flows at Soufrière Hills Volcano, Montserrat

P.D. Cole; E.S. Calder; R.S.J. Sparks; C.L. Harford; A.B. Clarke; T.H. Druitt; S.R. Young; R.A. Herd; G.E. Norton

doi:10.1144/GSL.MEM.2002.021.01.11

Deposits from dome-collapse and fountain-collapse pyroclastic flows at Soufrière Hills Volcano, Montserrat

P.D. Cole, E.S. Calder, R.S.J. Sparks, C.L. Harford, A.B. Clarke, T.H. Druitt, S.R. Young, R.A. Herd, G.E. Norton

School of Geosciences

Research output: Contribution to journal › Article › peer-review

Abstract

Pyroclastic flows were formed at Soufrière Hills Volcano by lava-dome collapse and by fountain collapse associated with Vulcanian explosions. Major episodes of dome collapse, lasting tens of minutes to a few hours, followed escalating patterns of progressively larger flows with longer runouts. Block-and-ash flow deposit volumes range from

Original language	English
Pages (from-to)	231-262
Number of pages	32
Journal	Memoirs
Volume	21
Issue number	1
DOIs	https://doi.org/10.1144/GSL.MEM.2002.021.01.11
Publication status	Published - 1 Jan 2002

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AU - Cole, P.D.

AU - Calder, E.S.

AU - Sparks, R.S.J.

AU - Harford, C.L.

AU - Clarke, A.B.

AU - Druitt, T.H.

AU - Young, S.R.

AU - Herd, R.A.

AU - Norton, G.E.

PY - 2002/1/1

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AB - Pyroclastic flows were formed at Soufrière Hills Volcano by lava-dome collapse and by fountain collapse associated with Vulcanian explosions. Major episodes of dome collapse, lasting tens of minutes to a few hours, followed escalating patterns of progressively larger flows with longer runouts. Block-and-ash flow deposit volumes range from

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Deposits from dome-collapse and fountain-collapse pyroclastic flows at Soufrière Hills Volcano, Montserrat

Abstract

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