Útdráttur
Ascent of magma through Earth's crust is normally associated with, among other effects, ground deformation and gravity changes. Geodesy is thus a valuable tool for monitoring and hazards assessment during volcanic unrest, and it provides valuable data for exploring the geometry and volume of magma plumbing systems. Recent decades have seen an explosion in the quality and quantity of volcano geodetic data. New datasets (some made possible by regional and global scientific initiatives), as well as new analysis methods and modeling practices, have resulted in important changes to our understanding of the geodetic characteristics of active volcanism and magmatic processes, from the scale of individual eruptive vents to global compilations of volcano deformation. Here, we describe some of the recent developments in volcano geodesy, both in terms of data and interpretive tools, and discuss the role of international initiatives in meeting future challenges for the field.
| Upprunalegt tungumál | Enska |
|---|---|
| Síður (frá-til) | 1-12 |
| Síðufjöldi | 12 |
| Fræðitímarit | Journal of Volcanology and Geothermal Research |
| Bindi | 344 |
| DOI | |
| Útgáfustaða | Útgefið - 15 sep. 2017 |
Athugasemd
Funding Information: Research by JF has been supported by the Spanish Ministry of Economy and Competitiveness research project ESP2013-47780-557 C2-1-R and the EU 7th FP MED-SUV project (contract 308665 ), and is a contribution to the Moncloa Campus of International Excellence. Eugenio Sansosti provided the data and images for Fig. 2 . Marco Bagnardi contributed the image used to make Fig. 3 . We are grateful to Dan Dzurisin and Jurgen Neuberg for their thorough and constructive reviews. Publisher Copyright: © 2017 Elsevier B.V.Fingerprint
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