2013/03/01 by Vera Pessina, Andrea Tertulliani, Romano Camassi +2 · 1 citation
Earth and Planetary Sciences · #earthquake and tectonic studies #Earthquake Detection and Analysis #Seismic Waves and Analysis
paper · doi:10.4430/bgta0083
openalex publication_date 2013/03/01 · openalex created_date 2025/10/10 · openalex updated_date 2026/06/11
On November 24, 2004 an earthquake (Mw= 5.0) struck the west side of Lake Garda (northern Italy), producing moderate but widespread damage. It provided the opportunity of reviewing the seismicity of all the area over the past two centuries, whose former most significant event is the October 30, 1901 earthquake (Mw= 5.5), while other minor but damaging events are the January 5, 1892 (Mw=5.0) and November 16, 1898 (Mw=4.6) earthquakes. On the reviewing we found common similarities in ground shaking distribution as recurrent damaged spots, amplification zones due to local site condition or energy radiation. We believe that these findings are suitable to provide information for provisional purposes in low hazard level area hampered by the lack of knowledge about the seismic sources. New data are provided both in MCS scale and EMS. The sensitivity of a source parameters estimation technique was evaluated for the major event.