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dc.contributor.authorCarracedo, Juan Carlos-
dc.contributor.authorTroll, Valentín R.-
dc.contributor.authorPérez Torrado, Francisco José-
dc.contributor.authorRodríguez Badiola, Eduardo-
dc.contributor.authorHansen Machín, Álex-
dc.contributor.authorParis, Raphael-
dc.contributor.authorGuillou, Hervé-
dc.contributor.authorScaillet, Stéphane-
dc.identifier.citationEos, Trans. AGU, Vol. 87, No. 43, 462-465en_US
dc.descriptionInsightful reviews by Robert I. Tilling and Chris Stillman greatly improved this contri-bution and are gratefully acknowledged.en_US
dc.description.abstractWhen a volcano that has been dormant for many centuries begins to show possible signs of reawakening, scientists and civil authorities rightly should be concerned about the possibility that the volcanic unrest might culminate in renewed eruptive activity. Such was the situation for Teide volcano, located on Tenerife in the Canary Islands, when a mild seismic swarm during April-July 2004 garnered much attention and caused public concern. However, that attention completely ignored the fact that the seismic recordings of the swarm were due to a much improved monitoring system rather than due to an actual event of alarming magnitude or extent.en_US
dc.format.extent6739 bytes-
dc.publisherAmerican Geophysical Unionen_US
dc.subjectVolcanic hazards and risksen_US
dc.subjectVolcano monitoringen_US
dc.subjectVolcano/climate interactionsen_US
dc.subjectTeide Volcanoen_US
dc.subjectCanary Islandsen_US
dc.titleRecent Unrest at Canary Islands’ Teide Volcano?en_US
dc.description.peerreviewedPeer revieweden_US
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