Earthquake, Fire, and Water: Destruction Sequence Identified in an 8th Century Early Islamic Harbor Warehouse in Caesarea, Israel
Charles J. Everhardt,
Hendrik W. Dey,
Uzi ‘Ad,
Jacob Sharvit,
Peter Gendelman,
Joel Roskin,
Lotem Robins,
Roy Jaijel,
Ofra Barkai,
Beverly N. Goodman-Tchernov
Affiliations
Charles J. Everhardt
Marine Geoarchaeology and Micropaleontology Laboratory, Dr. Moses Strauss Department of Marine Geosciences, Leon H. Charney School of Marine Sciences, University of Haifa, Haifa 31905, Israel
Hendrik W. Dey
Department of Art and Art History, Hunter College, City University of New York, New York City, NY 10017, USA
Uzi ‘Ad
Israel Antiquities Authority, Caesarea 38900, Israel
Jacob Sharvit
Israel Antiquities Authority, Caesarea 38900, Israel
Peter Gendelman
Israel Antiquities Authority, Caesarea 38900, Israel
Joel Roskin
Laboratory for Geomorphology and Portable Luminescence, Leon Recanati Institute for Maritime Studies, University of Haifa, Haifa 31905, Israel
Lotem Robins
Laboratory for Geomorphology and Portable Luminescence, Leon Recanati Institute for Maritime Studies, University of Haifa, Haifa 31905, Israel
Roy Jaijel
Marine Geoarchaeology and Micropaleontology Laboratory, Dr. Moses Strauss Department of Marine Geosciences, Leon H. Charney School of Marine Sciences, University of Haifa, Haifa 31905, Israel
Ofra Barkai
Israel Antiquities Authority, Caesarea 38900, Israel
Beverly N. Goodman-Tchernov
Marine Geoarchaeology and Micropaleontology Laboratory, Dr. Moses Strauss Department of Marine Geosciences, Leon H. Charney School of Marine Sciences, University of Haifa, Haifa 31905, Israel
An 8th century CE earthquake severely damaged inland cities across the southern-central Levant, but reported evidence of this earthquake along the coastline is scarce. In Caesarea Maritima, archaeologists have found contemporaneous anomalous sand and shelly layers within nearshore structures and interpreted them as construction fill, aeolian accumulation, or abandonment debris. Recently, similar sand deposits were exposed in a Roman-to-Islamic harbor-side warehouse. This presented the first opportunity to directly sample and systematically analyze in situ, undisturbed deposits in order to determine their origin and taphonomic (source and transport) history. Two sediment cores from the deposit as well as comparative reference samples from defined contexts were analyzed for grain size distribution, foraminifera (abundance/taphonomy), and relative age (POSL, archaeochronology). The results support the interpretation that the deposit was formed from the transport of offshore marine sediments during a high-energy inundation event, most likely a tsunami associated with the 749 CE earthquake.