Developments in Volcanology Series
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About this series
- How do collapse calderas form?
- What are the conditions to create fractures and slip along them to initiate caldera collapse and when are these conditions fulfilled?
- How do these conditions relate to explosive volcanism?
- Most products of large caldera-forming eruptions show evidence for pre-eruptive reheating. Is this a pre-requisite to produce large volume eruptions and large calderas?
- What are the time-scales behind caldera processes?
- How long does it take magma to reach conditions ripe enough to generate a caldera-forming eruption?
- What is the mechanical behavior of magma chamber walls during caldera collapse? Elastic, viscoelastic, or rigid?
- Do calderas form by underpressure following a certain level of magma withdrawal from a reservoir, or by magma chamber loading due to deep doming (underplating), or both?
- How to interpret unrest signals in active caldera systems?
- How can we use information from caldera monitoring to forecast volcanic phenomena?
In the form of 14 contributions from various disciplines this book samples the state-of-the-art of caldera studies and identifies still unresolved key issues that need dedicated cross-boundary and multidisciplinary efforts in the years to come.
* International contributions from leading experts
* Updates and informs on all the latest developments
* Highlights hot topic areas and identifies and analyzes unresolved key issues
Titles in the series (3)
- Melt Inclusions in Volcanic Systems: Methods, Applications and Problems
5
Melt inclusions provide a unique record of the physical and chemical processes operating in active magma chambers associated with volcanic systems. This book includes a summary of modern techniques used to study and interpret melt inclusions in volcanic rocks, as well as descriptive studies of specific volcanoes. These various studies document the enormous potential for melt inclusions to provide a window into the dynamics of active magma chambers. 'Melt Inclusions in Volcanic Systems' gives the most up-to-date summary of research on the application of melt inclusions in studies of active and fossil volcanic systems, as well as suggestions for future research in this area.
- Vesuvius: Education, Security and Prosperity
8
VESUVIUS 2000 is an interdisciplinary project aimed at producing a safe and prosperous habitat for the people living around Vesuvius. To produce this environment requires an effective collaboration between the experts and the public, whereby the danger from the volcano is used to reorganize the territory and thus produce new opportunities for the people surrounding the volcano. As an all inclusive physico-mathematical-computer model of the volcano, the Global Volcanic Simulator is a key tool for determining the effects of different eruption scenarios and thus for urban planning of the territory. Unlike the evacuation plans which tend to manage emergencies, VESUVIUS 2000 aims at preparing the Vesuvius area to confront future eruptions with minimal socio-economic and cultural consequences. * Addresses volcanic risk mitigation in densely populated area surrounding Vesuvius * Provides education about volcanos * Displays physical modeling of eruption processes and integration of models
- Caldera Volcanism: Analysis, Modelling and Response
10
This volume aims at providing answers to some puzzling questions concerning the formation and the behavior of collapse calderas by exploring our current understanding of these complex geological processes. Addressed are problems such as: - How do collapse calderas form? - What are the conditions to create fractures and slip along them to initiate caldera collapse and when are these conditions fulfilled? - How do these conditions relate to explosive volcanism? - Most products of large caldera-forming eruptions show evidence for pre-eruptive reheating. Is this a pre-requisite to produce large volume eruptions and large calderas? - What are the time-scales behind caldera processes? - How long does it take magma to reach conditions ripe enough to generate a caldera-forming eruption? - What is the mechanical behavior of magma chamber walls during caldera collapse? Elastic, viscoelastic, or rigid? - Do calderas form by underpressure following a certain level of magma withdrawal from a reservoir, or by magma chamber loading due to deep doming (underplating), or both? - How to interpret unrest signals in active caldera systems? - How can we use information from caldera monitoring to forecast volcanic phenomena? In the form of 14 contributions from various disciplines this book samples the state-of-the-art of caldera studies and identifies still unresolved key issues that need dedicated cross-boundary and multidisciplinary efforts in the years to come. * International contributions from leading experts * Updates and informs on all the latest developments * Highlights hot topic areas and identifies and analyzes unresolved key issues
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