VOLCANO: Final reminder: IAVCEI 2013 Session 3.3a: "Calderas: Context, formation, evolution, structure, unrest, products, hazard, resources"

[Date Prev][Date Next][Thread Prev][Thread Next][Date Index][Thread Index]

 



****************************************************************************************
Final reminder: IAVCEI 2013 Session 3.3a: "Calderas: Context, formation, evolution, structure, unrest, products, hazard, resources"
From: Adelina Geyer Traver <ageyertraver@xxxxxxxxx>
****************************************************************************************

Dear Colleague,

We would like to encourage you to contribute with a presentation to the session on "Calderas: Context, formation, evolution, structure, unrest, products, hazard, resources" (3.3a) at the IAVCEI 2013 Scientific Assembly , 20-24 July 2013 (http://www.iavcei2013.com/) .

Deadline for receipt of abstracts is 31 January 2013.

The conveners are Adelina Geyer (CSIC, Spain), Valerio Acocella (Roma Tre University, Italy) and Nobuo Geshi (Geological Survey of Japan, Japan)

A description of the session is provided below.

Please pass this information on to colleagues and students working in this field.

We apologize for any multiple posting and look forward to meet you in Kagoshima.

Thank you.

Kind regards,

Adelina Geyer
Valerio Acocella
Nobuo Geshi



Calderas: Context, formation, evolution, structure, unrest, products, hazard, resources

Calderas are the most distinctive and dramatic collapse feature of volcanoes. This session aims at providing the state of the art on the main processes accompanying the development of calderas, including their regional tectonic and magmatic context, the conditions for their formation and evolution, their structure and effect on eruptive activity, the role of magma and/or hydrothermal systems on the frequently observed unrest episodes, the impact of unrest and eruptions on hazard and the role of calderas as source for geothermal and ore exploitation.
Ultimate questions, which we will address, include the following. Which are the conditions leading to caldera unrest? How does unrest evolve into an eruption? How caldera formation and structure may affect volcanic activity? Is there any common behaviour or feature in the development and structure of calderas?

--------------------------------------------------------------------------------------
Dr. Adelina Geyer Traver
Institute of Earth Sciences "Jaume Almera" (CSIC)
C/Lluis Solé i Sabaris s/n
08028 Barcelona
Spain

==============================================================

Volcano Listserv is a collaborative venture among Arizona State University (ASU), Portland State University (PSU), the Global Volcanism Program (GVP) of the Smithsonian Institution's National Museum of Natural History, and the International Association for Volcanology and Chemistry of the Earth's Interior (IAVCEI).

ASU - http://www.asu.edu/ PSU - http://pdx.edu/ GVP - http://www.volcano.si.edu/ IAVCEI - http://www.iavcei.org/

To unsubscribe from the volcano list, send the message: signoff volcano to: listserv@xxxxxxx, or write to: volcano-request@xxxxxxx.

To contribute to the volcano list, send your message to: volcano@xxxxxxx. Please do not send attachments.

==============================================================


[Index of Archives]     [Yosemite Backpacking]     [Earthquake Notices]     [USGS News]     [Yosemite Campgrounds]     [Steve's Art]     [Hot Springs Forum]

  Powered by Linux