Quaternary | |
Seismic Activity in the Celje Basin (Slovenia) in Roman Times—Archaeoseismological Evidence from Celeia | |
article | |
Miklós Kázmér1  Petra Jamšek Rupnik2  Krzysztof Gaidzik3  | |
[1] MTA-ELTE Geological, Geophysical and Space Science Research Group, Department of Palaeontology, Eötvös University;Geological Survey of Slovenia;Institute of Earth Sciences, University of Silesia in Katowice | |
关键词: paleoseismology; Periadriatic fault system; active tectonics; Southern Alps; Pannonian Basin; Dinarides; | |
DOI : 10.3390/quat6010010 | |
学科分类:自然科学(综合) | |
来源: mdpi | |
【 摘 要 】
Searching for unknown earthquakes in Slovenia in the first millennium, we performed archaeoseismological analysis of Roman settlements. The Mesto pod mestom museum in Celje exhibits a paved Roman road, which suffered severe deformation. Built on fine gravel and sand from the Savinja River, the road displays a bulge and trench, pop-up structures, and pavement slabs tilted up to 40°. The city wall was built over the deformed road in Late Roman times, supported by a foundation containing recycled material (spolia) from public buildings, including an emperor’s statue. We hypothesize that a severe earthquake hit the town before 350 AD, causing widespread destruction. Seismic-induced liquefaction caused differential subsidence, deforming the road. One of the nearby faults from the strike-slip Periadriatic fault system was the seismic source of this event.
【 授权许可】
CC BY
【 预 览 】
Files | Size | Format | View |
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RO202307010002649ZK.pdf | 4126KB | download |