Seismically induced liquefaction structures in La Magdalena archaeological site, the 4th century AD Roman Complutum (Madrid, Spain)

The ancient Roman city of Complutum (Alcalá de Henares, Madrid), founded in the 1st century AD, was one of the most important cities of Hispania. The old Roman city was destroyed, abruptly abandoned, relocated close by and rebuilt during the late 4th century AD. Destruction of the city and its reloc...

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Bibliographic Details
Published in:	Sedimentary geology Vol. 344; pp. 34 - 46
Main Authors:	Rodríguez-Pascua, M.A., Silva, P.G., Perucha, M.A., Giner-Robles, J.L., Heras, C., Bastida, A.B., Carrasco, P., Roquero, E., Lario, J., Bardaji, T., Pérez-López, R., Elez, J.
Format:	Journal Article
Language:	English
Published:	Elsevier B.V 01-10-2016
Subjects:	4th century AD Complutum Cracks Craters Earthquake Earthquake Archaeological Effects (EAEs) Grounds Historic sites Liquefaction Roman Sand Seismic phenomena ANE, Spain Earthquake Archaeological Effects (EAEs) 4th century AD Earthquake Liquefaction Complutum
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Summary:	The ancient Roman city of Complutum (Alcalá de Henares, Madrid), founded in the 1st century AD, was one of the most important cities of Hispania. The old Roman city was destroyed, abruptly abandoned, relocated close by and rebuilt during the late 4th century AD. Destruction of the city and its relocation has not yet been explained by archaeologists. In this paper, with our multidisciplinary approach, we identify and characterize earthquake archaeological effects (EAEs) affecting the archaeological site, the La Magdalena, an agricultural holding 4km from the core of Complutum. The most important EAEs in the site are liquefactions (sand dikes and explosive sand-gravel craters) affecting Roman structures, such as water tanks (cisterns), houses and graves. Ground liquefaction generated significant ground cracks, explosive craters and folds in foundations of buildings. Several other Roman sites throughout the valley were also abandoned abruptly during the 4th century AD, in some cases with EAEs of similar origin. This suggests the occurrence of a 5.0–6.6Mw seismic event in the zone, in accordance with the minimum empirical limit of seismically-induced liquefaction and the maximum surface rupture length of the Henares fault.
Bibliography:	ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23
ISSN:	0037-0738
DOI:	10.1016/j.sedgeo.2016.01.025