Études et Travaux XXX (2017), 339–387 Petrographic Variability of the Fabrics of Wine Jars from Sha‘ar-Ha Ἁmakim as a Refl ection of Diff erences in Their Provenance and Chronology J M, J M Abstract: The aim of the present study is to investigate the relationship between the shape of the Levantine wine jars discovered at Sha‘ar-Ha Ἁmakim and the petrography of their respective fabrics. The majority of sampled ceramic material originates in well-defi ned chronological phases of the settlement at the site, spanning the Persian through to the Middle Roman periods. The obtained results clearly demonstrate a connection between the historical period and the raw materials used in jar production. Specifi cally, the jars of the Phoenician type used in the Persian and Hellenistic periods were made from a fairly homogeneous raw material, the features of which such as the content of the fragments of the coralline alga Amphiroa confi rm the previous results of the investigations of jars whose fabric has been considered as Phoenician. On the other hand the bag-shaped jars, especially those of the Hellenistic period, are characterized by the more diversifi ed petrography of their fabrics, suggesting that they were produced by a number of local workshops to supply the needs of local wineries. Finally, the Roman period brings an abrupt change in the production of wine containers, with the introduction of the common use of the fi ne ferruginous soil rich in quartz silt. Keywords: Sha‘ar-Ha Ἁmakim, wine jars, Persian period, Hellenistic period, Roman period, jars petrography Jacek Michniewicz, Institute of Geology, Adam Mickiewicz University, Poznań;
[email protected] Jolanta Młynarczyk, Institute of Archaeology, University of Warsaw, Warszawa;
[email protected] As is known from written sources and archaeological fi nds, Galilee was a region abounding not only in olive groves, but also in vineyards.1 The wine that came from them was prob- ably an object of regional trade, especially intense in the borderland between western Galilee and southern Phoenicia.