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A retrospective study of the pre-eruptive unrest on El Hierro (Canary Islands): implications of seismicity and deformation in the short-term volcanic hazard assessment

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Figure

Figure 1. IGN monitoring network during the unrest period at ElHierro. The top left inset displays the location of El Hierro withinthe Canary Archipelago.
Table 1. Indicators during the unrest period. NA indicates not available.
Figure 2. Structural data of El Hierro (vents and fissure onshore andoffshore, as in Becerril et al., 2013, 2014) and the evolution of theseismicity during the unrest period (average location of the seismicswarm).
Figure 3. Susceptibility maps obtained from (a) the volcano-structural data; (b) the first days of unrest; (c) the middle of the unrest; (d) thedays before the submarine eruption.
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