Aspetti geomorfologici conseguenti all'attività sismica locale sul basso versante orientale del vulcano Etna
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Abstract
Several seismotectonic alignments on the southeastern flank of Mt. Etna are responsible for a high seismic activity with locally shallow earthquakes (h < 2 km). To recognize such alignments may be difficult because of continuous and rapid morphologic changes due to the emplacement of new lava flows and intense anthropic developments. Most seismotectonic alignments are normal faults, which control shoreline features and drainage pattern.
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