A geologic fault system in central Italy that produced a deadly earthquake in 2016 is also responsible for a fifth-century earthquake that damaged many Roman monuments, including the Colosseum, according to new research.
Scientists had thought the Mount Vettore fault system was dormant until it ruptured in 2016. They knew it could produce earthquakes, but as far as anyone knew, this was the first time the fault had ruptured in recorded history.
But a new study in the AGU journal Tectonics combining geologic data with historical records shows the fault produced a major earthquake in 443 A.D. that damaged or destroyed many well-known monuments from Roman civilization.
Among the damaged buildings were the Colosseum, made famous by the Roman Empire’s gladiator contests, as well as Rome’s first permanent theater and several important early Christian churches.
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| The surface of the Mount Vettore fault system, where it ruptured in 2016 [Credit: Paolo Galli] |
Reconstructing Italy’s geologic past
Italy lies on the southern end of the Eurasian tectonic plate, close to where it meets the Adriatic, African, and Ionian Sea plates. The movement of these plates relative to each other created the Apennine mountains millions of years ago, and makes Italy seismically and volcanically active today.
Hundreds of kilometers of geologic faults snake through the Apennine Mountains. Seismologists consider some of these faults to be silent or dormant because they haven’t been linked to any known historical earthquakes.
Scientists thought Mount Vettore was one of these silent fault systems until it ruptured in 2016. After Galli and his colleagues mapped the fault’s rupture in 2016, they decided to look for evidence of it having ruptured in the past.
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| A recently reassembled epigraph, or stone inscription, of the prefect Rufius Caecina Felix Lampadius, describing restorations for the Colosseum after the 443 AD earthquake [Credit: Paolo Galli] |
In the new study, Galli and his colleagues analyzed the sediment layers in the trenches and found the Mount Vettore system ruptured five other times in the past 9,000 years, in addition to 2016. One of those ruptures occurred in the middle of the fifth century, at the very end of the Roman period. Averaging the time between ruptures, they found the Mount Vettore system produces major earthquakes every 1,500 to 2,100 years.
Combining science and history
Using data from past archaeological digs in Italy and historical records from the Roman Empire, Galli and his colleagues matched the fifth-century rupture of Mount Vettore to an earthquake that rocked central Italy in 443 A.D., just three decades before the final Roman emperor was deposed.
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| A timeline of past earthquakes that have damaged Roman ruins during the common era (AD) [Credit: GeoSpace] |
The new study’s results suggest the 2016 earthquake was not as unexpected as scientists thought, and other Apennine faults considered dormant by scientists may in fact pose a seismic hazard to central Italy. Considering the immense historical and cultural value of Roman ruins in this region, Galli’s priority is to better understand the rest of the silent faults on the Italian peninsula.
Author: Lauren Lipuma | Source: American Geophysical Union [March 05, 2019]
from The Archaeology News Network https://ift.tt/2EPNMWf
Breaking News: Seemingly dormant geologic fault damaged famous Roman buildings 1,500 years ago - News Paper




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