Seismic risk in Malta

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Seismic risk in Malta is considered to be low with little historic damage noted and no known victims. The archipelago is however in a potentially significant seismic zone and the risk to the population is probably undervalued.

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Tectonics

Map of tectonic plates in the Eastern Mediterranean Aegean Sea and Anatolian Plates map-fr.png
Map of tectonic plates in the Eastern Mediterranean

The Maltese Archipelago rests on an underwater plateau, a relatively stable part of the African Plate. The islands are situated around 200 km to the south of the subduction fault between the African Plate and the Eurasian Plate. The pelagic plate forms a shallow platform separating the Ionian basin from the Western Mediterranean Basin, situated roughly under the Strait of Sicily. The plate is crossed by a rift zone formed of three grabens: the Pantelleria graben, that of Malta, and that of Linosa. These grabens are linked by a system of north–south orientation faults (sometimes west–east) with dextral cavities that are responsible for most of the earthquakes that can affect the archipelago. [1]

The islands themselves are made up of limestone rocks from the Oligocene and Miocene geological epochs, belonging to the Cenozoic era.

List of major earthquakes

Prior to the 20th century and the first seismic recordings in the region, information on Maltese earthquakes was researched in archives. These range mostly from the arrival of the knights of the Order of St John of Jerusalem in 1530 to the British colonisation of Malta. After this period, the localisation of the epicentres of earthquakes in the Sicilian Channel has been relatively limited, mostly due to an inadequate network of seismic stations, particularly before 1980.

Summary table of earthquakes since 1500

YearDateLocalisation of the epicentreCoordinatesMaximum intensity in MaltaEarthquake intensity Earthquake magnitude (Mw)
154210 December at around 15:15 [2] East of Sicily 37°12′N14°54′E / 37.20°N 14.90°E / 37.20; 14.90
7
10
6.6
15628 March, morning
5 ?
16361 September
5 ?
169311 January, around 13:30East of Sicily 37°11′N15°01′E / 37.18°N 15.02°E / 37.18; 15.02
7–8
9
7.4
174320 February, around 16:30 Ionian Sea 39°52′N18°47′E / 39.87°N 18.78°E / 39.87; 18.78
7
9
6.9
178919 January, morning Sicilian Channel  ?
5 ?
179326 February, morning Sicilian Channel  ?
5 ?
184811 January, around middayEast of Sicily 37°12′N15°12′E / 37.2°N 15.2°E / 37.2; 15.2
5
8–9
5.5
185612 October, around 00:45 Crete 37°12′N15°12′E / 37.2°N 15.2°E / 37.2; 15.2
7
7.7
18568 February, around 23:45 Sicilian Channel  ?
5 ?
188615 August, around 02:45 Sicilian Channel  ?
5 ?
188627 August, around 22:00 Aegean Sea  ? 36°24′N27°12′E / 36.4°N 27.2°E / 36.4; 27.2  ?
6–7
11
7.3
191130 September, around 09:25 Sicilian Channel  ? 36°24′N13°30′E / 36.4°N 13.5°E / 36.4; 13.5  ?
7
192318 September, at 07:30 Sicilian Channel  ? 35°30′N14°30′E / 35.5°N 14.5°E / 35.5; 14.5  ?
6
192626 June at 19:46 Aegean Sea 36°30′N27°30′E / 36.5°N 27.5°E / 36.5; 27.5  ?
5
7.6
197221 March at 23:06 Sicilian Channel 35°48′N15°00′E / 35.8°N 15°E / 35.8; 15  ?
5
4.5
202222 NovemberSicilian Channel4.6
202322 April at 12.20am [3] 35.026°N 15.219°E5.3

Details of major earthquakes

Earthquake of 10 December 1542

The Sicilian Chronicle of the 16th century reports that the earthquake of 10 December 1542 was strongly felt in Malta where some houses were knocked down.

Earthquake of 11 January 1693

German copper engraving dating from 1696 on the Sicilian earthquake 1693 Sicily earthquake.jpg
German copper engraving dating from 1696 on the Sicilian earthquake

The earthquake of 11 January 1693 in Val di Noto is the most significant earthquake felt in Malta since the 16th century. In Sicily, it caused the death of around 60,000 individuals. With a magnitude of 7.4, it is considered to be the most powerful earthquakes in Italian history. [2] The earthquake was preceded on 9 January by a precursory earthquake of a magnitude of around 5.9 which was strongly felt but did not cause damage.

In Malta, the earthquake provoked panic among the population, with many Maltese refusing to go back to their homes in the nights that followed, seeking refuge in tents or underground shelters. No victims were reported. The Order delegated its head engineer, Mederico Blondel to assess the damage. At Valletta, no building escaped unharmed by the earthquake, from simple cracks to complete demolition. The other towns of the Grand Harbour were considerably less affected. However, the old city of Mdina suffered more greatly as many of the buildings were older and were poorly maintained. Notably St. Paul's Cathedral was part destroyed – but the cathedral was already badly damaged before the earthquake, and so a reconstruction had already been planned. The Banca Giuratale in Mdina was equally damaged, and would be rebuilt in 1726 by Charles François de Mondion. At Rabat, the bell tower and the apse of the church of St. Paul came down. The Tal-Virtù Church suffered considerable damage, it was situated at a high altitude which was particularly susceptible to earthquakes. [4]

St. Paul's Cathedral, Mdina, rebuilt after the 1693 earthquake, damaged by the 1743 earthquake St Paul's Cathedral Mdina.jpg
St. Paul's Cathedral, Mdina, rebuilt after the 1693 earthquake, damaged by the 1743 earthquake

At Gozo, the walls of the Cittadella were damaged, but Blondel notes that the damage were more likely caused by years of neglect. The Cathedral of the Assumption, Gozo lost its bell tower. [1]

The considerable damage material in Malta has been attributed to the maximum earthquake intensity of 7–8.

Earthquake of 20 February 1743

Local historian Gian Pietro Francesco Agius de Soldanis recounts 20 February 1743 earthquake in his magnum opus Il Gozo Antico-Moderno e Sacro-Profano, a two-volume manuscript dealing with the history of Gozo completed in 1746: [5]

...At 5 pm, a violent earthquake shook the Maltese isles. It lasted for seven minutes. It left great damage on the two isles. At Gozo, the church of Saint George, Saint James and the chapel of Notre-Dame at Qala were greatly damaged. In Malta, the church of St John at Valletta, the cathedral of Mdina and many other churches were also effected. At Wardija, near Qala, people are said to have seen the earth rise and fall with such force that the soil seemed to remain floating in the air, creating a dust cloud that remained for a long time. Many of the hills in Gozo crumbled.

A document in the archives of the cathedral of Mdina described how the coppolino (the little dome) of the cathedral fell into the church, the back end of the choir was destroyed and the bell tower heavily damaged. The cathedral was so cracked in all areas that:

...Even the sound of the bell didn't dare to enter for fear of seeing the building fall.

An account by six architects described three large cracks of around 3 cm in width on each side of the cupola, revealing most of the stones in the cupola and the terrible damage to the walls of the choir. [1]

Earthquake of 12 October 1856

Ghajn Hadid Tower, which collapsed in the 1856 earthquake Ghajn Hadid Tower closer view.JPG
Għajn Ħadid Tower, which collapsed in the 1856 earthquake

The epicentre situated near Crete was very seriously hit by the particularly violent earthquake of 12 October 1856. Certain seismic registers attribute it with a magnitude of 8.2. It claimed numerous victims in Crete. Despite being at a distance of more than 1000 km from the epicentre, the earthquake was violently felt in Malta, as the newspapers of the era testify. People were woken in the middle of the night by a deafening growl and a movement of the earth that lasted between 22 and 60 seconds. Nearly all the houses in Valletta were damaged, as were houses in Gozo, notably on the upper floors. Numerous churches were affected, and in particular the cathedral of Mdina. The belltower of the church of the Carmelites at Mdina was so cracked that it needed to be rebuilt. The chapel on the islet of Filfla was destroyed. [1] The 17th-century Għajn Ħadid Tower collapsed in this earthquake and has remained in ruins ever since. [6]

Earthquake of 27 August 1886

This was probably the earthquake on the same day that struck the SW Peloponnese. Once again, the local papers reported a general panic in the population that rushed outside dwellings, awoken by the earthquake on 27 August 1886. Some buildings were affected, including the ceiling of the Palace of Justice in Valletta. For once, the cathedral in Mdina was not greatly affected. [1]

Earthquake of 30 September 1911

Fort Chambray in Gozo Fort Chambray 0001.jpg
Fort Chambray in Gozo

30 September 1911 earthquake was more distinctly felt in Gozo than in Malta. Newspapers reported the appearance of deep cracks in the domes and the belltowers of many churches, in particular at Nadur, Għarb, and Ir-Rabat, Gozo, where many public buildings were affected. Numerous rural buildings were completely destroyed. Fort Chambray was badly hit. Many landslides were reported on the isle of Gozo. In Malta, damage was limited to a few cracks. [1]

Earthquake of 18 September 1923

18 September 1923 earthquake was the first to follow the installation of a Milne seismograph at Valletta. It seems not to have worked and gave no useful information; the seismologic data is therefore not clear. The shock seems to have been most felt around the Grand Harbour. Some damage was reported, such as the falling of the stone crosses on churches or cracks in the domes. The greatest ravages seem to have been those exerted on the church of St Paul in Rabat, Malta. The Tal-Virtù Church was badly damaged and remained unused for more than 70 years. [1]

Details of major tsunamis

Tsunami of 16 January 1693

The tsunami of 16 January 1693 occurred contemporaneously with the strong earthquake. Agius de Soldanis recounts how the sea at Xlendi turned a thousand times before returning with force. [7]

Tsunami of 28 December 1908

The tsunami of 28 December 1908 corresponds to the earthquake in the Strait of Messina. [2] At least three large waves caused significant damage and took a number of victims in the east of Sicily. The waves of this tsunami hit the shores of Malta an hour later, causing flooding at Msida, where part of the old town was damaged. At Marsaxlokk a foaming wave crossed the main road hitting the church of St. Peter. At Sliema, the sea came and went with force. The sea level was registered as abnormally high in the Grand Harbour. Many fishing boats were damaged or destroyed, but no deaths were reported. [7]

Evaluation of seismic risk

Seismic risk was evaluated at an event of intensity 8 happening every 1000 years and an event at intensity 6 happening every 92 years. Historically, since 1530, an earthquake of 7–8 intensity has been reported, as well as at least four events of intensity 7. [1]

The risk of a tsunami wave between 4 m and 7 m high is estimated as a possibility every 600 to 1500 years. The occurrence of an event comparable to that of 1603, could have grave social and economic consequences as areas near the sea are largely built up, in particular for tourist activity in the region of Sliema. [7]

Integration of risk in building standards

Despite a proposed bill, no seismic building standards have been imposed as the rate of construction accelerates and numerous buildings are completed. The risk is increased further by building in unreinforced masonry, incorporating heavy floors and concrete roofs with often large cellars used as garages. This type of construction is particularly sensitive to earthquakes. [1]

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This page list topics related to Malta.

<span class="mw-page-title-main">St Paul's Cathedral, Mdina</span> Church in Mdina, Malta

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<span class="mw-page-title-main">Lorenzo Gafà</span>

Lorenzo Gafà (1639–1703) was a Maltese Baroque architect and sculptor. He designed many churches in the Maltese Islands, including St. Paul's Cathedral in Mdina and the Cathedral of the Assumption in Victoria, Gozo. He was the younger brother of the sculptor Melchiorre Cafà.

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The 1912 Maymyo earthquake or Burma earthquake struck Burma on the morning of May 23, with an epicentre near Taunggyi and Pyin Oo Lwin in Shan State. The earthquake was initially calculated at 8.0 on the surface wave magnitude scale (Ms ) by Beno Gutenberg and Charles Francis Richter, and described by them as being one of the most remarkable seismic events in the early 1900s. Recent re-evaluation of the earthquake, however, have revised the magnitude to 7.6–7.9. It was preceded by two foreshocks on May 18 and 21 with respective intensities V and VII on the Rossi–Forel scale, while the mainshock was assigned IX. Shaking was felt throughout most of Burma, parts of Siam and Yunnan; an area covering approximately 375,000 square miles. It was one of the largest earthquakes in the country.

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The 1856 Heraklion earthquake, also known as the Crete earthquake or Rhodes earthquake, occurred on the morning of October 12 at 02:45 am local time. This extremely catastrophic earthquake had an estimated magnitude of 7.7 to 8.3 at a depth of approximately 61 to 100 km. The earthquake was felt over a very wide area extending from Sicily, Italy to the Levant and North Africa. On the Greek island of Crete, the effects of the earthquake were cataclysmic, over 500 bodies were recovered in the city of Heraklion. Shockwaves from the earthquake were felt intensely, covering all of the Ottoman Empire; present-day Turkey, Cyprus and the Middle East where damage and human losses were reported. In Malta, the earthquake collapsed the Għajn Ħadid Tower—a coastal watchtower built around the year 1638. In Cairo, Egypt, the earthquake destroyed buildings, created seiches in canals, and killed several people. Off the Egyptian and Italian coasts, sailors reported feeling a seaquake.

The 1743 Salento earthquake affected the Apulian region of southwestern Italy on 20 February at 23:30 IST. The ~7.1 Mw  earthquake had an epicenter in the Adriatic and Ionian seas, off the coast of modern-day Lecce and Brindisi provinces in Salento. It had a maximum Modified Mercalli intensity of IX (Violent), causing heavy damage in Nardò. Damage was also reported across the sea, in the Balkans. The earthquake also generated a tsunami of up to 11 meters in run-up. Between 180 and 300 people were killed in the disaster.

The 1804 Almería earthquake was a highly destructive seismic event in the Province of Almería, southern Spain. It occurred on August 25 at 8:25 pm local time. The mainshock had a maximum intensity assigned VIII–IX on the European macroseismic scale (EMS), and an estimated moment magnitude of 6.2–6.4 Mw . At least 400 people were reported killed.

References

  1. 1 2 3 4 5 6 7 8 9 Galea, Pauline (2007). "Seismic history of the Maltese islands and considerations on seismic risk: Earthquakes in Malta". Annals of Geophysics. 50 (6): 725–740. Retrieved 5 June 2015.
  2. 1 2 3 Boschi, E.; Guidoboni, G.; Mariotti, D.; Valensise, G.; Gasperini, P. (2000). "Catalogue of Strong Italian Earthquakes from 461 B.C. to 1997". Annals of Geophysics. 43 (4): 609–868.
  3. "Tremor of 5.3 magnitude hits Malta". Times of Malta. 22 April 2023. Retrieved 20 May 2023.
  4. Buhagiar, Mario (1979). "The Crypt and Church of S. Marija tal-Virtù at Rabat". Elita Historica: A Journal of Maltese History. 7 (4): 326–345. Archived from the original on 3 March 2016.
  5. Agius de Soldanis, Gian Pietro Francesco (1746). Il Gozo Antico-Moderno e Sacro-Profano (in Italian). PLG, Biblioteca ms. 243.
  6. Mifsud, Simon (24 December 2012). "Għajn Ħadid Tower and Aħrax Tower". MilitaryArchitecture.com. Archived from the original on 23 August 2017.
  7. 1 2 3 Camilleri, Dennis (2005). "Tsunami Risks in the Mediterranean – Part 2" (PDF). The Architect. 34 (4): 18–19.