1930 Senigallia earthquake

1930 Senigallia earthquake
Date October 30, 1930
Magnitude 5.8 Ml
Epicenter 43°40′01″N 13°16′01″E / 43.667°N 13.267°ECoordinates: 43°40′01″N 13°16′01″E / 43.667°N 13.267°E[1]
Areas affected Italy, Senigallia
Casualties 18

The 1930 Senigallia earthquake struck the city of Senigallia in central Italy on October 30. It occurred just a few months after the destructive 1930 Irpinia earthquake, which had caused over 1400 casualties in the southern part of the country.

Geology

The coastline in the area around Senigallia is controlled by active thrust faulting at the leading edge of the North Apennines fold and thrust belt. Movement on a blind thrust, the Senigallia Fault, has caused folding in the area around the port forming an anticline that extends about 10 kilometres (6.2 mi) parallel to the coast. The rupture area for the 1930 earthquake is thought to have measured about 12 kilometres (7.5 mi) along strike and 6.9 kilometres (4.3 mi) down dip.[2][3][4]

Earthquake

A foreshock preceded the main event by a few minutes. Its loud boom was heard by many, despite the shock causing little damage. After hearing the rumble, people fled the buildings and flooded into the streets. Shortly after the main shock came at 8:10 a.m.,[5] with a magnitude of 5.9 on the Richter magnitude scale.[6]

The earthquake affected the whole central and northwestern part of the Italian peninsula, with its epicenter near the city of Senigallia. Other major cities, such as Ancona and Fano, were damaged too, as were other settlements such as Montemarciano, Mondolfo, San Costanzo and 40 other minor towns. It was assessed as level VIII to IX on the Mercalli Intensity Scale.

The earthquake was felt from Istria to Puglia, throughout the whole Adriatic shoreline, and up to Naples on the opposite side of Italy. The following aftershocks lasted for over a month. A small tsunami struck Ancona's harbor, but damage was limited to a moored steamship.[6]

Casualties

The earthquake took only 18 lives (14 in Senigallia, 4 in Ancona), but many more were injured. Thanks to the foreshock alerting the people, casualties were quite low, but many were wounded by debris falling from the damaged buildings.

Many families became refugees, and had to live in tents and makeshift shelters. The region's tourist industry experienced much trouble in the following years, despite government assistance.

Whole districts of Ancona, such as Capodimonte and San Lazzaro, were abandoned; the residents left for the countryside. People from Senigallia built encampments in the town's outskirts and occupied summer camps and rail coaches.[6]

Damages

Many towns reported severe damage. In San Costanzo, 25 houses collapsed, and twice as much were damaged beyond repair. 450 buildings needed restoration work, but luckily no one perished, and only one inhabitant was wounded.

In Mondolfo, the damage was worse. The 15 second shock destroyed 60 houses, and 39 were severely damaged. Another 540 displayed cracks in the walls, while 20 people were injured.[6]

In Fano, the shock was much shorter (due to the different composition of the ground), about five seconds, but 86 houses suffered critical, 1197 severe and 2880 light damage, while six people required medical assistance.[6]

Marotta, Mombaroccio, Cartoceto, Saltara, Candelara, Sant'Ippolito, Sorbolongo, Urbino, Fossombrone and Sant'Andrea di Suasa all reported some damage. More severely affected were Monteporzio, Fratte Rosa, Serrungarina and Urbania.[6]

The old town of Senigallia, rich in monuments and businesses, was practically destroyed: the city lost its importance as a harbor and trade hub of the Adriatic Sea, along with its cultural heritage. The stone building decorations were mostly replaced by concrete or plaster fillings, compromising the look of the city center. The Misa River, used as an harbor channel, had to have new concrete embankments and lost its scenic attractiveness. Rebuilding worsened the damage; most repairable buildings were demolished to make way for new construction. The outcome was a decline in city population, importance and tourist appeal. The population shrank 70% over the next five decades.[7]

See also

References

  1. ↑ Guidoboni, Emanuela; Ferrari G., Mariotti D., Comastri A., Tarabusi G. & Valensise G. (2007). "CFTI4Med, Catalogue of Strong Earthquakes in Italy (461 B.C.-1997) and Mediterranean Area (760 B.C.-1500)". INGV-SGA. Archived from the original on 22 July 2011. Retrieved 22 July 2011.
  2. ↑ Pessina, V.; Scandella L., Franceschina G. & Lai C.G. (2008). "Seismic Risk assessment of Italian seaports: the case of Ancona (Italy)" (PDF). The 14 th World Conference on Earthquake Engineering October 12–17, 2008, Beijing, China. Retrieved 24 July 2011.
  3. ↑ Basili, R.; Mirabella F., Vannoli P. & Valensise G. (2004). "Identifying Blind Seismogenic Faults at the Apennine Thrust Front: Implications for the Seismic Hazard of the Northern Marche (Central Italy) Coastal Belt". American Geophysical Union, Fall Meeting 2004, abstract #T14C-07. Retrieved 24 July 2011.
  4. ↑ Favali, P.; Frugoni F., Monna D., Rainone M.L., Signanini P. & Smriglio G. (1995). "The 1930 earthquake and the town of Senigallia (Central Italy): an approach to seismic risk evaluation" (PDF). Annali di Geofisica 38 (5-6). Retrieved 24 July 2011.
  5. ↑ "Earthquake chronicle according to a student of Senigallia Seminary". Retrieved 25 July 2011.
  6. ↑ 6.0 6.1 6.2 6.3 6.4 6.5 "Terremoto del 30.10.1930, Marche settentrionali (Senigallia)". Retrieved 22 July 2011.
  7. ↑ "Piano di recupero del centro storico" (PDF). Comune di Senigallia. Retrieved 22 July 2011.

External links