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Excavation

  • San Giovanni (Tornareccio)
  • Val di Sangro
  •  
  • Italy
  • Abruzzo
  • Province of Chieti
  • Tornareccio

Tools

Credits

  • The Italian Database is the result of a collaboration between:

    MIBAC (Ministero per i Beni e le Attività Culturali - Direzione Generale per i Beni Archeologici),

    ICCD (Istituto Centrale per il Catalogo e la Documentazione) and

    AIAC (Associazione Internazionale di Archeologia Classica).

  • AIAC_logo logo

Summary (English)

  • The Sangro Valley Project completed its second and final year of excavations in San Giovanni di Tornareccio during the 2013 season. Work focused on three areas of the villa complex: the drain in SG 2000 was reopened to explore its relationship with Structure C and its associated run-off zone to the south; SG 3000 was expanded to determine the extent, function and phasing of Structure D; and exploratory trenches SG 5000 and SG 6000 were placed in the environs of the villa complex. The 2013 discovery of a lime kiln is proof that the villa complex was recycled, explaining why only the lower foundations of the walls of the complex remain and the overall lack of material evidence at the site.

    Structures A-D comprise a villa/bath complex adjacent to a reliable and abundant source of water for use in its bath and agricultural production activities. The room with the cocciopesto basin and drain (Structure C) is not part of the bath complex, but likely shared its water source and was used for work activities associated with Structure D, in a manner similar to the cocciopesto basin found in ACQ 10000, a rural Roman farm site, described in the 2009 season report. Based on ceramic and C-14 evidence, the villa complex was likely constructed in the late Republican or early Imperial period, enjoying a significant prosperity throughout the 1st century C.E. that ended in the second century C.E. with a thorough dismantling and recycling. Later phases of Structure D are less securely dated due to the lack of ceramic evidence and badly damaged stratigraphy. Current thinking is that Structure D was significantly modified during the recycling activities and experienced a second peak of activity that continued into the 3rd – 4th centuries C.E.

  • Susan Kane - Oberlin College 

Director

Team

  • Alexander Ekserdijan - Oxford University
  • Aran Schultz - Oberlin College
  • Ashley Ratigan - Oberlin College
  • Emily Flach - Durham University
  • Emma Mack - Oxford University
  • Fergus Morgan - Oxford University
  • Gillian De Boer - University of Edinburgh
  • Helen Sanford - Durham University
  • Jasmine Clark - Oxford University
  • Jerome Luchese Smith - Oxford University
  • Kirk Pearson - Oberlin College
  • Margaret Miller - Oberlin College
  • Margaret Saunders - Oberlin College
  • Mark Loughbridge - University of Edinburgh
  • Phoebe Anderson-Kline - Oberlin College
  • Rachel Backshall - Oxford University
  • Tinni Bhattacharyya - Oberlin College
  • Uxue Eguilaz - Oxford University
  • Will Austin - Oberlin College
  • Zachary Evans - Oberlin College
  • Zuzana Jurisova - University of Edinburgh
  • Kristen Wroth - Boston University
  • Alexis Christensen - University of Utah
  • Melissa Fore, Oberlin College
  • Emiliano Fioriti - Sintesis, Atessa, Italy
  • Anna Pia Apilongo
  • Chris Motz - Oberlin College, Ohio
  • Luke Aspland - Lund University
  • Miriam Rothenberg
  • Sam Carrier - Oberlin College, Ohio
  • Archer Martin - American Academy in Rome
  • Hilary Conley - Florida State University
  • Sedef Kinaci
  • Christopher Pyrah - Oxford University
  • Emma Sanford - Oberlin College
  • Lucy Smith - Oberlin College
  • Samantha Mater - Oberlin College
  • Giuseppe Masilli

Research Body

Funding Body

  • Oberlin College

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