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Book Chapter

Volcanic hazards in Nicaragua: Past, present, and future

By
Armin Freundt
Armin Freundt
SFB 574 at Kiel University, Wischhofstr. 1-3, D-24148 Kiel, Germany, and IFM-GEOMAR (Leibniz Institute of Marine Sciences), Wischhofstr. 1-3, D-24148 Kiel, Germany
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Steffen Kutterolf
Steffen Kutterolf
SFB 574 at Kiel University, Wischhofstr. 1-3, D-24148 Kiel, Germany
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Hans-Ulrich Schmincke
Hans-Ulrich Schmincke
SFB 574 at Kiel University, Wischhofstr. 1-3, D-24148 Kiel, Germany, and IFM-GEOMAR (Leibniz Institute of Marine Sciences), Wischhofstr. 1-3, D-24148 Kiel, Germany
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Thor Hansteen
Thor Hansteen
SFB 574 at Kiel University, Wischhofstr. 1-3, D-24148 Kiel, Germany, and IFM-GEOMAR (Leibniz Institute of Marine Sciences), Wischhofstr. 1-3, D-24148 Kiel, Germany
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Heidi Wehrmann
Heidi Wehrmann
SFB 574 at Kiel University, Wischhofstr. 1-3, D-24148 Kiel, Germany
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Wendy Pérez
Wendy Pérez
SFB 574 at Kiel University, Wischhofstr. 1-3, D-24148 Kiel, Germany
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Wilfried Strauch
Wilfried Strauch
Instituto Nicaragüense de Estudios Territoriales (INETER), Apdo. 2110, Managua, Nicaragua
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Martha Navarro
Martha Navarro
Instituto Nicaragüense de Estudios Territoriales (INETER), Apdo. 2110, Managua, Nicaragua
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Published:
January 01, 2006

We review the most important types of volcanic hazards that have occurred in Nicaragua during the past ∼40,000 yr and that are expected to occur in the future. Population density within the potential hazard area is clearly essential in defining and understanding volcanic hazard and risk. There are three main groups of volcanic events that pose major hazards: Group 1 comprises several types of explosive volcanic eruptions that impact society (people and infrastructure) directly. The most hazardous types are pyroclastic surges, particularly those generated by water-magma interaction, pyroclastic fallout, and pyroclastic flows, as well as tsunamis generated by volcanic eruptions within and close to Nicaragua's large lakes. Group 2 includes nonexplosive volcanic activity such as lava flows and the permanent or episodic emission of volcanic gases from open vents. Group 3 comprises chiefly lahars generated by mixing of volcanic debris with water and volcano flank collapses (landslides) sometimes unrelated to synchronous volcanic eruptions but being conditioned chiefly by the stability of a volcanic edifice. We discuss the present database on the age and type of the most recent eruptions emphasizing those that potentially pose major hazards to the populated areas. These include volcanogenic tsunamis in Lake Managua and Lake Nicaragua, scoria cone and maar formation chiefly in the western part of Managua, and major explosive eruptions of Chiltepe and Masaya volcanoes, a large eruption from Masaya volcano having devastated the entire area of present Managua only ∼2000 yr ago. We discuss the most important techniques for monitoring volcanoes to detect unrest and predict the time and magnitude of upcoming eruptions, emphasizing techniques presently employed in Nicaragua. Finally, we address the subjects of risk assessment, including hazard and risk maps, and the importance of long-term development plans to reduce vulnerability.

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Contents

GSA Special Papers

Volcanic Hazards in Central America

William I. Rose
William I. Rose
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Gregg J.S. Bluth
Gregg J.S. Bluth
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Michael J. Carr
Michael J. Carr
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John W. Ewert
John W. Ewert
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Lina C. Patino
Lina C. Patino
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James W. Vallance
James W. Vallance
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Geological Society of America
Volume
412
ISBN print:
9780813724126
Publication date:
January 01, 2006

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