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1962 Irpinia Earthquake
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 August 21 at 18:19 CET, measuring 6.15 and assigned a maximum intensity of IX (''Violent''). It was preceded by an 5.68 foreshock, and a 5.34 aftershock. The earthquakes resulted in nearly 20 fatalities and significant property losses. 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. Extensional tectonics in the region have been active since the since the Pliocene epoch, mainly accommodated by northwest–southeast striking norma ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fault (geology)
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 forces, with the largest forming the boundaries between the plates, such as the megathrust faults of subduction zones or transform faults. Energy release associated with rapid movement on active faults is the cause of most earthquakes. Faults may also displace slowly, by aseismic creep. A ''fault plane'' is the plane that represents the fracture surface of a fault. A ''fault trace'' or ''fault line'' is a place where the fault can be seen or mapped on the surface. A fault trace is also the line commonly plotted on geologic maps to represent a fault. A ''fault zone'' is a cluster of parallel faults. However, the term is also used for the zone of crushed rock along a single fault. Prolonged motion along closely spaced faults can blur the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
1456 Central Italy Earthquakes
On December 5, the largest earthquake to occur on the Italian Peninsula struck the Kingdom of Naples. The earthquake had an estimated moment magnitude of 7.19–7.4 , and nucleated near the town of Pontelandolfo in present-day Province of Benevento, central Italy. Earning a level of XI (''Extreme'') on the Modified Mercalli intensity scale, the earthquake caused widespread destruction in central and southern Italy. An estimated 30,000–70,000 people were killed. It was followed by two strong 7.0 and 6.0 earthquakes to the north on December 30. Tectonic setting The central Italian Peninsula is dominated by active extensional tectonics, forming the Apennine Mountains. The mountain range formed during the Miocene and Pliocene due to the subduction of the Adriatic Plate beneath the Eurasian Plate. The resulting subduction formed a fold and thrust belt. During the Quaternary, thrust tectonics gave way to extensional tectonics, with the development of a zone of normal faulting runn ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Council Of Ministers (Italy)
, border = , image = , caption = Logo of the Italian Government , date_established = (Kingdom of Italy) (Italian Republic) , state = Italy , address = Palazzo Chigi , leader_title = President of the Council , appointed = President of the Republic , responsible = Italian Parliament , url Official website The Council of Ministers ( it, Consiglio dei Ministri, CdM) is the principal executive organ of the Government of Italy. It comprises the President of the Council (the Prime Minister of Italy), all the ministers, and the undersecretary to the President of the council. Deputy ministers ( it, viceministri) and junior ministers ( it, sottosegretari) are part of the government, but are not members of the Council of Ministers. History The Council of Ministers' origins date to the production of the Albertine Statute by the Kingdom of Sardinia in 1848. The Statute, which subsequently became the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
National Institute Of Geophysics And Volcanology
The National Institute of Geophysics and Volcanology ( it, Istituto Nazionale di Geofisica e Vulcanologia, INGV) is a research institute for geophysics and volcanology in Italy. INGV is funded by the Italian Ministry of Education, Universities and Research The Ministry of Education, University and Research (in it, Ministero dell'Istruzione, dell'Università e della Ricerca, italic=no or MIUR) is the ministry of the Italian government for the national education system, the Italian universities and .... Its main responsibilities within the Italian civil protection system are the maintenance and monitoring of the national networks for seismic and volcanic phenomena, together with outreach and educational activities for the Italian population. The institute employs around 2000 people distributed between the headquarters in Rome and the other sections in Milan, Bologna, Pisa, Naples, Catania and Palermo. INGV is amongst the top 20 research institutions in terms of scientific publi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sant'Arcangelo Trimonte
Sant'Arcangelo Trimonte is a ''comune'' (municipality) in the Province of Benevento in the Italian region Campania, located about 70 km northeast of Naples and about 13 km east of Benevento. Sant'Arcangelo Trimonte was part of Province of Avellino until 1978; its territory borders the following municipalities: Apice, Buonalbergo, Paduli Paduli is a ''comune'' (municipality) in the Province of Benevento in the Italian region Campania. It is located on a rocky spur between the Calore and Tammaro rivers, about 60 km northeast of Naples and about 9 km northeast of Benevent .... References Cities and towns in Campania {{Campania-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Reino, Campania
Reino is a ''comune'' (municipality) in the Province of Benevento in the Italy, Italian region Campania, located about 70 km northeast of Naples and about 15 km north of Benevento. As of 31 December 2004, it had a population of 1,344 and an area of 23.6 km2.All demographics and other statistics: Italian statistical institute National Institute of Statistics (Italy), Istat. Reino borders the following municipalities: Circello, Colle Sannita, Fragneto l'Abate, Pesco Sannita, San Marco dei Cavoti. References Cities and towns in Campania {{Campania-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Molinara
Molinara is a ''comune'' (municipality) in the Province of Benevento in the Italian region Campania, located about 80 km northeast of Naples and about 20 km northeast of Benevento. Molinara borders the following municipalities: Foiano di Val Fortore, San Giorgio La Molara, San Marco dei Cavoti San Marco dei Cavoti () is a ''comune'' (municipality) in the Province of Benevento in the Italian region Campania, located near the Fortore The Fortore (Latin: ''Fertor'' or ''Frento'') is a river which flows through the provinces of Benevento, .... References External links Official website {{Authority control Cities and towns in Campania ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Melito Irpino
Melito Irpino (Irpino: ) is a town and ''comune'' in the province of Avellino, in the Campania region of south-western Italy. History The remains of the ancient Melito were found in 1880. According to some theories, it could be a suburban village belonging to Aeclanum, but the prevailing theory suggests that it was the ancient village of ''Melae'' (or ''Melas''). In ''Ab Urbe Condita'' (book XXIV, chapter X), Titus Livius wrote that Melae was destroyed in 215 BC by the troops of Claudius Marcellus and Quintus Fabius, during the Second Punic War.History of Melito Irpino (municipal website) Geography The municipality is located in the northern area of its province, next to that of Benevento. C ...[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Province Of Avellino
The Province of Avellino ( it, Provincia di Avellino) is a province in the Campania region of Southern Italy. The area is characterized by numerous small towns and villages scattered across the province; only two towns have a population over 20,000: its capital city Avellino (in the west) and Ariano Irpino (in the north). Geography It has an area of and a total population of 401,028 per 30.9.2021. There are 118 ''comuni'' in the province, with the main towns being Avellino and Ariano Irpino. See Comuni of the Province of Avellino. It is an inner province, with no connection to the sea. History The ancient inhabitants of the area were the Hirpini, whose name stems from the Oscan term ''hirpus'' ("wolf"), an animal that is still present in the territory, though in greatly reduced numbers. In the province of Avellino there are many archaeological Roman sites, with Aeclanum being the most important. In the Middle Age, the was the first political body established in 1022 by the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Province Of Benevento
The Province of Benevento ( it, Provincia di Benevento) is a province in the Campania region of Italy. Its capital is the city of Benevento. Geography The province has an area of 2,071 km2, and, , a total population of 279,308. There are 78 ''comuni'' in the province (for the full list, see comuni of the Province of Benevento). The biggest municipalities, the only ones over 10,000 inhabitants, are Benevento, Montesarchio, Sant'Agata de' Goti and San Giorgio del Sannio. The territory of the province of Benevento closely approximates that of the Principality of Benevento in the mid and late eleventh century. It borders Molise (province of Campobasso) on the North, Apulia (province of Foggia) on the East, the province of Avellino and the metropolitan City of Naples on the South, and the province of Caserta on the West. The lowest point is in the comune of Limatola (44 meters above sea level), while the highest point is Monte Mutria (1822 meters), one of the mountains of the M ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oxford University Press
Oxford University Press (OUP) is the university press of the University of Oxford. It is the largest university press in the world, and its printing history dates back to the 1480s. Having been officially granted the legal right to print books by decree in 1586, it is the second oldest university press after Cambridge University Press. It is a department of the University of Oxford and is governed by a group of 15 academics known as the Delegates of the Press, who are appointed by the vice-chancellor of the University of Oxford. The Delegates of the Press are led by the Secretary to the Delegates, who serves as OUP's chief executive and as its major representative on other university bodies. Oxford University Press has had a similar governance structure since the 17th century. The press is located on Walton Street, Oxford, opposite Somerville College, in the inner suburb of Jericho. For the last 500 years, OUP has primarily focused on the publication of pedagogical texts and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Richter Scale
The Richter scale —also called the Richter magnitude scale, Richter's magnitude scale, and the Gutenberg–Richter scale—is a measure of the strength of earthquakes, developed by Charles Francis Richter and presented in his landmark 1935 paper, where he called it the "magnitude scale". This was later revised and renamed the local magnitude scale, denoted as ML or . Because of various shortcomings of the original scale, most seismological authorities now use other similar scales such as the moment magnitude scale () to report earthquake magnitudes, but much of the news media still erroneously refers to these as "Richter" magnitudes. All magnitude scales retain the logarithmic character of the original and are scaled to have roughly comparable numeric values (typically in the middle of the scale). Due to the variance in earthquakes, it is essential to understand the Richter scale uses logarithms simply to make the measurements manageable (i.e., a magnitude 3 quake factors ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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