2001
DOI: 10.1046/j.0956-540x.2001.01518.x
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Faulting and earthquake triggering during the 1783 Calabria seismic sequence

Abstract: Summary Between the 1783 February 5 and 1783 March 28, five earthquakes struck the southern part of Calabria. The main shock (February 5) and the first aftershock (February 6) devastated the region ENE of the Messina Strait. The greatest damage occurred along the foot of the Aspromonte Mountains south of San Giorgio Morgeto, and along the Tyrrhenian coast south of Palmi. A surface break about 18 km long, with several feet of downthrow to the west, formed along the Cittanova (Santa Cristina) Fault as a result o… Show more

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Cited by 140 publications
(201 citation statements)
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“…Since the Middle Pleistocene, active faulting has contributed to continuous extensional deformation from eastern Sicily to western Calabria (Siculo-Calabrian Rift Zone, see inset in Fig. 1(a); Monaco and Tortorici, 2000;Jacques et al, 2001). In eastern Sicily the SSW-NNE striking normal faults are mostly located offshore and control the Ionian coast from Messina to the eastern lower slope of Mt.…”
Section: Geological and Geomorphological Settingmentioning
confidence: 99%
“…Since the Middle Pleistocene, active faulting has contributed to continuous extensional deformation from eastern Sicily to western Calabria (Siculo-Calabrian Rift Zone, see inset in Fig. 1(a); Monaco and Tortorici, 2000;Jacques et al, 2001). In eastern Sicily the SSW-NNE striking normal faults are mostly located offshore and control the Ionian coast from Messina to the eastern lower slope of Mt.…”
Section: Geological and Geomorphological Settingmentioning
confidence: 99%
“…Geographical setting of the area of Gioia Tauro, Italy (above). Simplified geological cross-section of the basin (below), modified from Jacques et al [15]. …”
Section: Geological and Geomorphologic Settingmentioning
confidence: 99%
“…The marine sequence is unconformably overlain by the most superficial layers of the plain (up to a depth of 50-70 m from the ground level), that is prevalently constituted by granular saturated soils consisting of Middle-Upper Pleistocene alluvial conglomerates and sands, truncated by a wide planation surface [13,15]. Geographical setting of the area of Gioia Tauro, Italy (above).…”
Section: Geological and Geomorphologic Settingmentioning
confidence: 99%
See 1 more Smart Citation
“…The cumulative effects of all these earthquakes was devastating and great changes were produced even in the environment morphology: diffuse landsliding led to heavy changes to the hydrogeological system (more than 200 lakes formed as a consequence of stream damming caused by slides). The most extraordinary effects were chiefly due to the 5 February earthquake (Vivenzio, 1788;Hamilton, 1783;Dolomieu, 1784;Baratta, 1901;Jacques et al, 2001). On the 5 February, at about 12:00, a catastrophic tsunamigenic earthquake abruptly opened the seismic period.…”
Section: The 1783-1785 Calabrian Seismic Sequencementioning
confidence: 99%