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Explosive volcanic history and hazard zonation maps of Boquerón Volcano (San Salvador volcanic complex, El Salvador)

By
D. Ferrés
D. Ferrés
Departamento de Vulcanología, Instituto de Geofísica, Universidad Nacional Autónoma de México, México D.F., México
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H. Delgado Granados
H. Delgado Granados
Departamento de Vulcanología, Instituto de Geofísica, Universidad Nacional Autónoma de México, México D.F., México
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R.E. Gutiérrez
R.E. Gutiérrez
Dirección General del Observatorio Ambiental (DGOA), Ministerio de Medio Ambiente y Recursos Naturales, San Salvador, El Salvador
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I.A. Farraz
I.A. Farraz
Terracon Ingeniería S.A. de C.V., México D.F., México
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E.W. Hernández
E.W. Hernández
Dirección General del Observatorio Ambiental (DGOA), Ministerio de Medio Ambiente y Recursos Naturales, San Salvador, El Salvador
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C.R. Pullinger
C.R. Pullinger
Independent Consultant, San Salvador, El Salvador
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C.D. Escobar
C.D. Escobar
Dirección General del Observatorio Ambiental (DGOA), Ministerio de Medio Ambiente y Recursos Naturales, San Salvador, El Salvador
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Published:
November 01, 2013

Boquerón Volcano, formed on the old San Salvador Volcano, is the youngest and active central edifice of the San Salvador volcanic complex, which also includes 25 secondary vents. The San Salvador volcanic complex is located in the vicinity of the San Salvador metropolitan area and is considered one of the most hazardous volcanic centers in El Salvador and Central America. Boquerón Volcano has a long record of effusive and explosive eruptions spanning 36,000 yr; the most recent eruption was in 1917. We reviewed and updated its eruptive history through detailed fieldwork, allowing the recognition of up to 25 different eruptions. Lava flows, ash-fall, and ballistic projectile deposits produced by Strombolian or violent-Strombolian eruptions are the most recurrent events preserved in the stratigraphic record of Boquerón Volcano. Pyroclastic-flow, and especially pyroclastic-surge, deposits are also present, indicative of explosive subplinian and Plinian eruptions, some of which had significant phreatomagmatic components.

We define three hazard scenarios regarding ash fall, ballistic projectiles, and pyroclastic density currents for Boquerón Volcano and constrain them using its documented explosive eruptive history, fieldwork, and computer simulations. Each scenario is characterized by a likelihood of occurrence (high, medium, low), assigned to eruptive events of small, intermediate, or large magnitude, which are mainly characterized for the areal distribution of the related volcanic products. Resulting hazard maps show areas likely to be affected by future eruptions, enabling decision makers and the general public to consider volcanic hazards in land development and risk mitigation planning.

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GSA Special Papers

Understanding Open-Vent Volcanism and Related Hazards

William I. Rose
William I. Rose
Geological Engineering & Sciences, Michigan Technological University, Houghton, Michigan 49931, USA
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José Luis Palma
José Luis Palma
Departamento de Ciencias de la Tierra, Universidad de Concepción, Victor Lamas 1290, Concepción, Chile
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Hugo Delgado Granados
Hugo Delgado Granados
Instituto de Geofísica, Universidad Nacional Autónoma de México Circuito Científico, C.U. Coyoacán 04510, México, D.F.
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Nick Varley
Nick Varley
Facultad de Ciencias, Universidad de Colima, Avenida Universidad 333, Colonia Las Víboras, C.P. 28040, Colima, México
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Geological Society of America
Volume
498
ISBN print:
9780813724980
Publication date:
November 01, 2013

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