1703 Apennine earthquakes
ML | |
Epicenter | 42°42′N 13°04′E / 42.7°N 13.07°E (first event) |
---|---|
Areas affected | Italy |
Casualties | 10,000 deaths |
The 1703 Apennine earthquakes were a sequence of three
Tectonic setting
The central part of the Apennines has been characterised by
The Norcia earthquake
The earthquake occurred at 18:00
Damage
There was extensive damage in the area around Norcia, with
Casualties
Estimates of the death toll vary from 6,240[8] to 9,761.[5]
The Montereale earthquake
The earthquake occurred at 13:30 UTC on 16 January with an estimated magnitude of 6.2.[5] It is thought to have been caused by movement on the Montereale Fault.[1] Damage was recorded in Montereale, Cittareale, Accumoli and Amatrice. Although of lower magnitude than the other two events, this earthquake was still felt in Rome.[6] The estimated intensity for this event is VIII (Severe).[7] No separate casualty figures are available for this event.
The L'Aquila earthquake
The earthquake occurred at 11:05 UTC on 2 February with an estimated magnitude of 6.7.[5] It was caused by movement on the Mt. Marine Fault.[1]
Damage
Most of the buildings in L’Aquila were badly damaged or completely destroyed. Damage was reported from as far away as Rome.
Casualties
Estimates of the death toll vary from 2,500[7] to 5,000.[9]
Summary of earthquakes
Details taken from Catalogue of Strong Earthquakes in Italy (461 BC – 1997) and Mediterranean Area (760 B.C. – 1500)[10]
Name | Date | Time | Coordinates | Magnitude | Intensity |
---|---|---|---|---|---|
Norcia | 14 January | 18:00 | 42°42′N 13°04′E / 42.70°N 13.07°E | 6.7 | XI |
Montereale | 16 January | 13:30 | 42°37′N 13°06′E / 42.62°N 13.10°E | 6.2 | VIII |
L'Aquila | 2 February | 11:05 | 42°26′N 13°18′E / 42.43°N 13.30°E | 6.7 | X |
Relationship between the events
Some seismologists interpret these events as related. It has been suggested that the Norcia earthquake led directly to the Montereale event, which had the effect of further loading the fault at Aquila, thus triggering the final event.[1] Such sequential adjacent events are examples of coulomb stress transfer.
See also
- 2009 L'Aquila earthquake
- 1706 Abruzzo earthquake
- 1461 L'Aquila earthquake
- List of earthquakes in Italy
- List of historical earthquakes
References
- ^ .
- ^ "Seismically Induced Ground Ruptures and Large Scale Mass Movements: Field Excursion and Meeting 21–27 september 2001" (PDF). Archived from the original (PDF) on 17 July 2011. Retrieved 25 September 2009.
- from the original on 10 April 2009. Retrieved 6 April 2009.
- ^ "Magnitude 6.3 – CENTRAL ITALY 2009 April 06 01:32:42 UTC". United States Geological Survey. 6 April 2009. Archived from the original on 9 April 2009. Retrieved 6 April 2009.
- ^ a b c d "IISEENET (Information Network of Earthquake disaster Prevention Technologies) – Search Page". Archived from the original on 21 July 2010. Retrieved 25 September 2009.
- ^ a b c "Description of the effects in Rome caused by the three earthquakes". Legacy.ingv.it. Retrieved 21 May 2012.
- ^ a b c d "Geological effects induced by the L'Aquila earthquake (6 April 2009, Ml = 5.8) on the natural environment: preliminary report" (PDF). Archived from the original (PDF) on 17 February 2012. Retrieved 21 May 2012.
- ^ "Davison, C. 1912–1913. The death-rate of earthquakes, Science progress in the twentieth century, A quarterly journal of Scientific work & thought". Retrieved 21 May 2012.
- OCLC 316760617.
- ^ Guidoboni, E.; Ferrari, G.; Mariotti, D.; Comastri, A.; Tarabusi, G.; Sgatoni, G.; Valensise, G. "Catalogue of Strong Earthquakes in Italy (461 BC – 1997) and Mediterranean Area (760 B.C. – 1500)". INGV-SGA. Retrieved 31 March 2022.
Further reading
- Galli, P.; Messina, P.; Peronace, E; Galderisi, A.; Ilardo, I.; Polpetta, F. (2023), "Paleoseismic evidence of five magnitude 7 earthquakes on the Norcia fault system in the past 8,000 years (Central Italy)", Frontiers in Earth Science, 11, ISSN 2296-6463