Transition from steady to unsteady Plinian eruption column: the VEI 5, 4.6 ka Fogo A Plinian eruption, Sao Miguel, Azores

Alessandra Pensa, Raymond Cas, Guido Giordano, Massimiliano Porreca, Nicolau Wallenstein

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6 Citations (Scopus)

Abstract

The 4.6ka Fogo A trachytic Plinian eruption on São Miguel Island, Azores, Portugal, is composed by four main phases: 1) Initial phreatomagmatic activity which emplaced thin surge deposits with accretionary lapilli; 2) fully buoyant steady Plinian activity which generated a prominent trachytic basal fall-out deposit; 3) partial collapsing activity, which led to the emplacement of two trachytic-trachydacitic intra-plinian ignimbrites (pink and black ignimbrites) and associated surge deposits, inter-stratified within two fall-out deposits; 4) vent widening and fully collapsing activity which caused the emplacement of the climactic brown trachydacitic ignimbrite. The deposits of these four main phases have been organised into three members FGA1, FGA2 and FGA3, sub-divided into 15 stratigraphic or emplacement units. The fluctuations from a steady to unsteady Plinian eruption column parallel the change in composition of the magma from trachytic to trachydacitic. Although minimal, the change in composition resulted in a marked change in colour of the juvenile clasts from white at the base (first phase) to pink and light-dark grey banded and black (second and third phases) and to dark brown (fourth phase). Density analysis of juvenile clasts revealed that the change in composition did not significantly affect the density of the juvenile pumice pyroclasts, the vesicularity of which increases from 70% to 85% up through the sequence. The pink and the black intra-plinian ignimbrites were emplaced only, within the narrow paleo-valleys of the southern flank with maximum thicknesses of 9m and 5m respectively, transitioning onto adjacent topographic highs where thin veneer surge layers were deposited. The fall-out deposits inter-bedded between the ignimbrites lack basal reverse grading, indicating that the eruption column continued to be sustained during the partial collapses generating the intra-plinian ignimbrites. The climactic dark brown ignimbrite was emplaced radially with a maximum thickness of >40m. The absence of oxidation surfaces or evidence of reworking within the Fogo A deposits, indicates that there were no time breaks during the different phases of the eruption. The on-land bulk volume of the three ignimbrites has been estimated around 3.2km3, while the volume of the intra-plinian fall-out deposits is ~0.003km3. These bulk volume estimations, summed with the basal fall-out volume calculated by Walker and Croasdale (1970), makes a total bulk volume for the Fogo A deposits of 4.4km3 indicating a Volcanic Explosively Index of 5, higher than previously estimated. This result is fundamental for the forecasting a possible scenario for a future eruption.
Original languageEnglish
Pages (from-to)1-18
Number of pages18
JournalJournal of Volcanology and Geothermal Research
Volume305
DOIs
Publication statusPublished - 2015

Keywords

  • Fogo A eruption sequence
  • Fogo volcano
  • Intra-plinian ignimbrite
  • Unsteady plinian eruption

Cite this

@article{14ee306fadf34ac591ac6ed60eeb7d15,
title = "Transition from steady to unsteady Plinian eruption column: the VEI 5, 4.6 ka Fogo A Plinian eruption, Sao Miguel, Azores",
abstract = "The 4.6ka Fogo A trachytic Plinian eruption on S{\~a}o Miguel Island, Azores, Portugal, is composed by four main phases: 1) Initial phreatomagmatic activity which emplaced thin surge deposits with accretionary lapilli; 2) fully buoyant steady Plinian activity which generated a prominent trachytic basal fall-out deposit; 3) partial collapsing activity, which led to the emplacement of two trachytic-trachydacitic intra-plinian ignimbrites (pink and black ignimbrites) and associated surge deposits, inter-stratified within two fall-out deposits; 4) vent widening and fully collapsing activity which caused the emplacement of the climactic brown trachydacitic ignimbrite. The deposits of these four main phases have been organised into three members FGA1, FGA2 and FGA3, sub-divided into 15 stratigraphic or emplacement units. The fluctuations from a steady to unsteady Plinian eruption column parallel the change in composition of the magma from trachytic to trachydacitic. Although minimal, the change in composition resulted in a marked change in colour of the juvenile clasts from white at the base (first phase) to pink and light-dark grey banded and black (second and third phases) and to dark brown (fourth phase). Density analysis of juvenile clasts revealed that the change in composition did not significantly affect the density of the juvenile pumice pyroclasts, the vesicularity of which increases from 70{\%} to 85{\%} up through the sequence. The pink and the black intra-plinian ignimbrites were emplaced only, within the narrow paleo-valleys of the southern flank with maximum thicknesses of 9m and 5m respectively, transitioning onto adjacent topographic highs where thin veneer surge layers were deposited. The fall-out deposits inter-bedded between the ignimbrites lack basal reverse grading, indicating that the eruption column continued to be sustained during the partial collapses generating the intra-plinian ignimbrites. The climactic dark brown ignimbrite was emplaced radially with a maximum thickness of >40m. The absence of oxidation surfaces or evidence of reworking within the Fogo A deposits, indicates that there were no time breaks during the different phases of the eruption. The on-land bulk volume of the three ignimbrites has been estimated around 3.2km3, while the volume of the intra-plinian fall-out deposits is ~0.003km3. These bulk volume estimations, summed with the basal fall-out volume calculated by Walker and Croasdale (1970), makes a total bulk volume for the Fogo A deposits of 4.4km3 indicating a Volcanic Explosively Index of 5, higher than previously estimated. This result is fundamental for the forecasting a possible scenario for a future eruption.",
keywords = "Fogo A eruption sequence, Fogo volcano, Intra-plinian ignimbrite, Unsteady plinian eruption",
author = "Alessandra Pensa and Raymond Cas and Guido Giordano and Massimiliano Porreca and Nicolau Wallenstein",
year = "2015",
doi = "10.1016/j.jvolgeores.2015.09.012",
language = "English",
volume = "305",
pages = "1--18",
journal = "Journal of Volcanology and Geothermal Research",
issn = "0377-0273",
publisher = "Elsevier",

}

Transition from steady to unsteady Plinian eruption column: the VEI 5, 4.6 ka Fogo A Plinian eruption, Sao Miguel, Azores. / Pensa, Alessandra; Cas, Raymond; Giordano, Guido; Porreca, Massimiliano; Wallenstein, Nicolau.

In: Journal of Volcanology and Geothermal Research, Vol. 305, 2015, p. 1-18.

Research output: Contribution to journalArticleResearchpeer-review

TY - JOUR

T1 - Transition from steady to unsteady Plinian eruption column: the VEI 5, 4.6 ka Fogo A Plinian eruption, Sao Miguel, Azores

AU - Pensa, Alessandra

AU - Cas, Raymond

AU - Giordano, Guido

AU - Porreca, Massimiliano

AU - Wallenstein, Nicolau

PY - 2015

Y1 - 2015

N2 - The 4.6ka Fogo A trachytic Plinian eruption on São Miguel Island, Azores, Portugal, is composed by four main phases: 1) Initial phreatomagmatic activity which emplaced thin surge deposits with accretionary lapilli; 2) fully buoyant steady Plinian activity which generated a prominent trachytic basal fall-out deposit; 3) partial collapsing activity, which led to the emplacement of two trachytic-trachydacitic intra-plinian ignimbrites (pink and black ignimbrites) and associated surge deposits, inter-stratified within two fall-out deposits; 4) vent widening and fully collapsing activity which caused the emplacement of the climactic brown trachydacitic ignimbrite. The deposits of these four main phases have been organised into three members FGA1, FGA2 and FGA3, sub-divided into 15 stratigraphic or emplacement units. The fluctuations from a steady to unsteady Plinian eruption column parallel the change in composition of the magma from trachytic to trachydacitic. Although minimal, the change in composition resulted in a marked change in colour of the juvenile clasts from white at the base (first phase) to pink and light-dark grey banded and black (second and third phases) and to dark brown (fourth phase). Density analysis of juvenile clasts revealed that the change in composition did not significantly affect the density of the juvenile pumice pyroclasts, the vesicularity of which increases from 70% to 85% up through the sequence. The pink and the black intra-plinian ignimbrites were emplaced only, within the narrow paleo-valleys of the southern flank with maximum thicknesses of 9m and 5m respectively, transitioning onto adjacent topographic highs where thin veneer surge layers were deposited. The fall-out deposits inter-bedded between the ignimbrites lack basal reverse grading, indicating that the eruption column continued to be sustained during the partial collapses generating the intra-plinian ignimbrites. The climactic dark brown ignimbrite was emplaced radially with a maximum thickness of >40m. The absence of oxidation surfaces or evidence of reworking within the Fogo A deposits, indicates that there were no time breaks during the different phases of the eruption. The on-land bulk volume of the three ignimbrites has been estimated around 3.2km3, while the volume of the intra-plinian fall-out deposits is ~0.003km3. These bulk volume estimations, summed with the basal fall-out volume calculated by Walker and Croasdale (1970), makes a total bulk volume for the Fogo A deposits of 4.4km3 indicating a Volcanic Explosively Index of 5, higher than previously estimated. This result is fundamental for the forecasting a possible scenario for a future eruption.

AB - The 4.6ka Fogo A trachytic Plinian eruption on São Miguel Island, Azores, Portugal, is composed by four main phases: 1) Initial phreatomagmatic activity which emplaced thin surge deposits with accretionary lapilli; 2) fully buoyant steady Plinian activity which generated a prominent trachytic basal fall-out deposit; 3) partial collapsing activity, which led to the emplacement of two trachytic-trachydacitic intra-plinian ignimbrites (pink and black ignimbrites) and associated surge deposits, inter-stratified within two fall-out deposits; 4) vent widening and fully collapsing activity which caused the emplacement of the climactic brown trachydacitic ignimbrite. The deposits of these four main phases have been organised into three members FGA1, FGA2 and FGA3, sub-divided into 15 stratigraphic or emplacement units. The fluctuations from a steady to unsteady Plinian eruption column parallel the change in composition of the magma from trachytic to trachydacitic. Although minimal, the change in composition resulted in a marked change in colour of the juvenile clasts from white at the base (first phase) to pink and light-dark grey banded and black (second and third phases) and to dark brown (fourth phase). Density analysis of juvenile clasts revealed that the change in composition did not significantly affect the density of the juvenile pumice pyroclasts, the vesicularity of which increases from 70% to 85% up through the sequence. The pink and the black intra-plinian ignimbrites were emplaced only, within the narrow paleo-valleys of the southern flank with maximum thicknesses of 9m and 5m respectively, transitioning onto adjacent topographic highs where thin veneer surge layers were deposited. The fall-out deposits inter-bedded between the ignimbrites lack basal reverse grading, indicating that the eruption column continued to be sustained during the partial collapses generating the intra-plinian ignimbrites. The climactic dark brown ignimbrite was emplaced radially with a maximum thickness of >40m. The absence of oxidation surfaces or evidence of reworking within the Fogo A deposits, indicates that there were no time breaks during the different phases of the eruption. The on-land bulk volume of the three ignimbrites has been estimated around 3.2km3, while the volume of the intra-plinian fall-out deposits is ~0.003km3. These bulk volume estimations, summed with the basal fall-out volume calculated by Walker and Croasdale (1970), makes a total bulk volume for the Fogo A deposits of 4.4km3 indicating a Volcanic Explosively Index of 5, higher than previously estimated. This result is fundamental for the forecasting a possible scenario for a future eruption.

KW - Fogo A eruption sequence

KW - Fogo volcano

KW - Intra-plinian ignimbrite

KW - Unsteady plinian eruption

UR - http://goo.gl/84SuDa

U2 - 10.1016/j.jvolgeores.2015.09.012

DO - 10.1016/j.jvolgeores.2015.09.012

M3 - Article

VL - 305

SP - 1

EP - 18

JO - Journal of Volcanology and Geothermal Research

JF - Journal of Volcanology and Geothermal Research

SN - 0377-0273

ER -