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The 1805 Molise earthquake occurred on July 26 at 21:01 UTC. It has an estimated magnitude of 6.6 on the equivalent magnitude scale (Me) (calculated from seismic intensity data) and a maximum perceived intensity of X on the
Mercalli intensity scale The Modified Mercalli intensity scale (MM, MMI, or MCS), developed from Giuseppe Mercalli's Mercalli intensity scale of 1902, is a seismic intensity scale used for measuring the intensity of shaking produced by an earthquake. It measures the eff ...
. The area of greatest damage was between the towns of
Isernia Isernia () or, in Pliny and later writers, ''Eserninus'', or in the Antonine Itinerary, ''Serni''. is a town and ''comune'' in the southern Italian region of Molise, and the capital of province of Isernia. Geography Situated on a rocky crest ri ...
and
Campobasso Campobasso (, ; nap, label= Campobassan, Cambuàsce ) is a city and ''comune'' in southern Italy, the capital of the region of Molise and of the province of Campobasso. It is located in the high basin of the Biferno river, surrounded by Sann ...
, while the area of intense damage extended over about 2,000 square kilometres. There were an estimated 5,573 deaths resulting from this earthquake and two of the
aftershock In seismology, an aftershock is a smaller earthquake that follows a larger earthquake, in the same area of the main shock, caused as the displaced crust adjusts to the effects of the main shock. Large earthquakes can have hundreds to thousand ...
s.


Tectonic setting

The Southern
Apennines The Apennines or Apennine Mountains (; grc-gre, links=no, Ἀπέννινα ὄρη or Ἀπέννινον ὄρος; la, Appenninus or  – a singular with plural meaning;''Apenninus'' (Greek or ) has the form of an adjective, which wou ...
originated as northeast moving
fold and thrust belt A fold and thrust belt (FTB) is a series of mountainous foothills adjacent to an orogenic belt, which forms due to contractional tectonics. Fold and thrust belts commonly form in the forelands adjacent to major orogens as deformation propagates ou ...
. Since the Middle
Pleistocene The Pleistocene ( , often referred to as the ''Ice age'') is the geological Epoch (geology), epoch that lasted from about 2,580,000 to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was fina ...
, the tectonics has been dominated by
extension Extension, extend or extended may refer to: Mathematics Logic or set theory * Axiom of extensionality * Extensible cardinal * Extension (model theory) * Extension (predicate logic), the set of tuples of values that satisfy the predicate * E ...
. The axial part of the Apennines is the most seismically active, with a series of damaging historical earthquakes up to about 7 in magnitude. The major
normal fault In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements. Large faults within Earth's crust result from the action of plate tectonic ...
in the epicentral area of the 1805 event is the Bojano fault system.


Earthquake

The earthquake was a result of movement on the NW–SE trending Bojano fault system. A
surface rupture In seismology, surface rupture (or ground rupture, or ground displacement) is the visible offset of the ground surface when an earthquake rupture along a fault affects the Earth's surface. Surface rupture is opposed by buried rupture, where the ...
of 40 km has been attributed to this event, with a maximum displacement of 150 cm. The mainshock was preceded by a series of low intensity
foreshock A foreshock is an earthquake that occurs before a larger seismic event (the mainshock) and is related to it in both time and space. The designation of an earthquake as ''foreshock'', ''mainshock'' or aftershock is only possible after the full sequ ...
s throughout the previous day. The aftershock sequence continued until the following June.


Damage

The damage was particularly intense in the foothills of the
Matese The Matese (Italian: Monti del Matese or Massiccio del Matese) is a chain of mountains in southern Apennines, southern Italy. Geography The Matese mountains straddle two regions (Molise and Campania) and four provinces (Campobasso, Isernia, Ben ...
massif and the Bojano plain, with 30 towns and villages being severely affected. Damage was recorded as far away as
Naples Naples (; it, Napoli ; nap, Napule ), from grc, Νεάπολις, Neápolis, lit=new city. is the regional capital of Campania and the third-largest city of Italy, after Rome and Milan, with a population of 909,048 within the city's adminis ...
and
Salerno Salerno (, , ; nap, label= Salernitano, Saliernë, ) is an ancient city and ''comune'' in Campania (southwestern Italy) and is the capital of the namesake province, being the second largest city in the region by number of inhabitants, after ...
. Landslides and other slope failures were seen over an area of about 5,300 square kilometres. The official number of recorded deaths is given as 5,573, representing nearly 3% of the area's inhabitants, with a further 1,583 injured. Other estimates of the death toll are in the range 4,000 to 6,000.


Aftermath


Response

The most affected area lay within the then
Kingdom of Naples The Kingdom of Naples ( la, Regnum Neapolitanum; it, Regno di Napoli; nap, Regno 'e Napule), also known as the Kingdom of Sicily, was a state that ruled the part of the Italian Peninsula south of the Papal States between 1282 and 1816. It was ...
. The king, Ferdinand IV, took control of the response to this disaster. He sent Gabriele Giannocoli, a tax lawyer, to visit those areas of the countryside that has suffered the most, to evaluate the situation and to do what needed to be done. He was given considerable powers, together with the financial means, to allow him to carry out his task. He concentrated on visiting the most damaged areas, relying on reports from other officials in less affected parts. At his request, soldiers were sent to restore order and to prevent looting in some areas. Only properties in a dangerous state were repaired or demolished. Temporary shelters were provided for the homeless and huts for use as hospitals. Taxes were suspended by the king for all of the countryside around Molise in August.


See also

*
List of earthquakes in Italy This is a list of earthquakes in Italy that had epicentres in Italy, or significantly affected the country. The highest seismicity hazard in Italy was concentrated in the central-southern part of the peninsula, along the Apennine Mountains, Apen ...
*
List of historical earthquakes Historical earthquakes is a list of significant earthquakes known to have occurred prior to the beginning of the 20th century. As the events listed here occurred before routine Seismometer, instrumental recordings, they rely mainly on the analys ...


References

{{Earthquakes in Italy Earthquakes in Italy 1805 earthquakes 1805 in Italy July 1805 events 1805 disasters in Italy 1805 disasters in Europe