Monitoring the b-value unravels critical stress-changes along magma pathways: results from Etna volcano

<p>The analysis of the <em>b-</em>value, i.e. the slope<em> </em>of the <em>Gutenberg & Richter </em>frequency-magnitude distribution of earthquakes, provides the chance to investigate the local stress conditions with great resolution, especially in active volcanic areas, where seismic productivity is generally high.</p><p>In this work we investigated the seismicity of Mt. Etna between 2005 and 2019, focusing on one of the largest known episodes of unrest in December 2018, when most of the intruding magma aborted its ascent inside the volcano. We found a possible stress concentration zone along magma pathways that may have inhibited the occurrence of a larger, more complete eruption. The <em>b-</em>values time series strongly increase about 19 days before the December 2018 unrest event, while a sharp drop of <em>b </em>started 2 days in advance.&#160;</p><p>Our results suggest that the study of the <em>b-</em>value, in broader correlation with other monitoring measurements, may offer an opportunity to investigate the volcano state and improve the assessment of impending volcanic eruptions.</p>