1962 Irpinia earthquake

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1962 Irpinia earthquake
Italy relief location map.jpg
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UTC  time1962-08-21 18:19:33
ISC  event 875196
USGS-ANSS ComCat
Local date21 August 1962 (1962-08-21)
Local time18:19 CET [1]
Magnitude6.15 Mw  [2]
Depth9.0 km (5.6 mi) [3]
Epicenter 41°13′N15°01′E / 41.22°N 15.01°E / 41.22; 15.01 [3]
Type Strike-slip
Areas affected Italy
Max. intensity IX (Violent)
Casualties≤20 dead

The second shock in the 1962 Irpinia earthquake (terremoto dell'Irpinia del 1962) sequence was the largest and most destructive in a series of earthquakes in the southern Apennines. It occurred on 21 August at 18:19 CET, [1] measuring Mw 6.15 and assigned a maximum intensity of IX (Violent). [2] It was preceded by an Mw  5.68 foreshock, and followed by a 5.34 aftershock. The earthquakes resulted in nearly 20 fatalities and significant property losses.

Contents

Tectonic setting

The central Italian Peninsula is dominated by active extensional tectonics, forming the Apennine Mountains. One explanation is that slab rollback is occurring within the Adriatic Plate as it subducts beneath the Tyrrhenian Sea. Another explanation is because the back-arc basin in the Tyrrhenian Sea opening at a faster rate than the African Plate is colliding with the Eurasian Plate. [4] Extensional tectonics in the region have been active since the since the Pliocene epoch, mainly accommodated by northwest–southeast striking normal faults. [5] The faults associated with large earthquakes on the peninsula are geologically young in age, and rarely rupture the surface. Occasionally, strike-slip events like the 1456 Central Italy earthquakes, as well as the 1971 (Mw  5.0) and 2012 (Mw  4.6) moderate earthquakes in the southern Apennine region suggest the dominant style of faulting is not limited to normal dip-slip. [3] Strike-slip faults on the Italian Peninsula are oriented east–west.

Geology

Prior to the occurrence of the large foreshock at 18:09, a series of foreshocks were already present in the afternoon that same day. The mainshock struck at 18:19 with a moment magnitude of 6.15 Mw  and Richter scale magnitude of 6.1 ML . Very few aftershocks were instrumentally recorded; the largest measured 5.4 ML . Both the foreshock and mainshock occurred at a depth of 8 km, based on waveform analysis, [1] but this result is still controversial and unreliable. The lack of documented surface ruptures further instigated controversy into the mechanism of the earthquakes. The seismology community debated between strike-slip and normal faulting as the cause. [6]

A study in 2016 reevaluated its depth to 9 km, and generated a reliable strike-slip focal mechanism. [6] The epicenters are located between the zone of northwest–southeast trending normal faults and east–west striking strike-slip faults. The earthquake sequence represent strike-slip faulting with small normal components along either east–west or north–south trending faults. The location of the 1962 earthquakes is close to the faults that triggered the 1456 earthquakes. [3]

Impact

The first of three severe shocks occurred at 18:09 local time. While it did not cause any damage, it was felt strong enough to frighten residents in Benevento and Avellino. Many residents were driven out of their homes in fear of further shocks. The second shock was the most destructive and violent. It damaged 68 municipalities across the provinces of Benevento and Avellino. A maximum intensity of IX was assigned in the towns of Melito Irpino, Molinara, Reino, and Sant'Arcangelo Trimonte. These towns sustained heavy damage, with at least 90% of all structures affected. More than 50% of the total buildings affected were a total loss due to the severity of damage or complete destruction. Nearly twenty people died and 16,000 were made homeless. [7]

Aftermath

The town of Apice, abandoned after the earthquake. Apice vecchio - strada.jpg
The town of Apice, abandoned after the earthquake.

The Council of Ministers, allocated 2 billion Italian liras for first responders and 400 million for assistance. More than 20,000 tents were erected over a period of next ten days for the homeless. Significant quantities of medical supplies, food and clothing were distributed. More than 2,000 barracks were constructed by civil and military engineers to house homeless. [7]

After the earthquakes, there were concerns about the potential for landslides as the shocks had destabilized ground conditions on the nearby hills. As a result, authorities decided to evict the residents of Melito Irpino and Apice. [7] The old medieval Melito Irpino is currently a ghost town. [8]

See also

Related Research Articles

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References

  1. 1 2 3 Rob, Westaway (1987). "The Campania, southern Italy, earthquakes of 1962 August 21". Geophysical Journal International. 88 (1). Oxford University Press: 1–24. Bibcode:1987GeoJ...88....1W. doi: 10.1111/j.1365-246X.1987.tb01366.x .
  2. 1 2 Rovida A.; Locati M.; Camassi R.; Lolli B.; Gasperini P. (2020). "The Italian earthquake catalogue CPTI15". Bulletin of Earthquake Engineering. 18 (7): 2953–2984. Bibcode:2020BuEE...18.2953R. doi:10.1007/s10518-020-00818-y. S2CID   212732483.
  3. 1 2 3 4 Paola Vannoli; Fabrizio Bernardi; Barbara Palombo; Gianfranco Vannucci; Rodolfo Console; Graziano Ferrari (2016). "New constraints shed light on strike-slip faulting beneath the southern Apennines (Italy): The 21 August 1962 Irpinia multiple earthquake". Tectonophysics . 691. Elsevier: 375–384. Bibcode:2016Tectp.691..375V. doi:10.1016/j.tecto.2016.10.032.
  4. ↑ D'Agostino N.; Mantenuto S.; D'Anastasio E.; Avallone A.; Barchi M.; Collettini C.; Radicioni F.; Stoppini A.; Fastellini G. (2009). "Contemporary crustal extension in the Umbria–Marche Apennines from regional CGPS networks and comparison between geodetic and seismic deformation" (PDF). Tectonophysics. 476 (1–2): 3–12. Bibcode:2009Tectp.476....3D. doi:10.1016/j.tecto.2008.09.033.
  5. ↑ Akinci, A.; Galadini, F.; Pantosti, D.; Petersen, M.; Malagnini, L.; Perkins, D. (6 April 2009). "Effect of Time Dependence on Probabilistic Seismic-Hazard Maps and Deaggregation for the Central Apennines, Italy". The Bulletin of the Seismological Society of America. 99 (2A). Seismological Society of America: 585. Bibcode:2009BuSSA..99..585A. doi:10.1785/0120080053. Archived from the original on 10 April 2009. Retrieved 6 April 2009.
  6. 1 2 Aldo Piombino; Filippo Bernardini; Gregorio Farolfi (2021). "Assessing Current Seismic Hazards in Irpinia Forty Years after the 1980 Earthquake: Merging Historical Seismicity and Satellite Data about Recent Ground Movements". Geosciences. 11 (4): 168. Bibcode:2021Geosc..11..168P. doi: 10.3390/geosciences11040168 .
  7. 1 2 3 "I terremoti del '900: Il terremoto del 21 agosto 1962 nell'Appennino campano" (in Italian). National Institute of Geophysics and Volcanology. 20 August 2012. Retrieved 2 March 2022.
  8. ↑ (in Italian) Melito Irpino on paesifantasma.it (Italian ghost towns website)
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