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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)

  • In San Giovanni (Tornareccio) this season, three adjacent fields were investigated (SG T9000, SG T10000, and SG T11000). These areas were chosen in order to confirm whether certain observations made during field walking and geophysical survey corresponded with archaeological deposits. Excavation will continue in two of these areas (SG T10000 and SG T11000) in 2015.

    SG T9000, located in an olive grove that constrained its dimensions, was 16.65m in length but only 0.61m in width, with two extensions, a western one (1.74m in length) and an eastern one (2.65m in length). Under a heavy deposit of colluvial soil, a series of anthropogenic layers were uncovered, all consonant with domestic debris of Roman Imperial – late Roman date. These layers were densely packed with large amounts of roofing tile and other ceramic building materials, fragments of cocciopesto flooring, small amounts of intonaco wall plaster, pottery (both fine and cooking wares), and animal bone (particularly cow). Because of the constraints of the surrounding olive grove, the complete stratigraphic sequence could not be obtained.

    SG T10000 began as a 1.5m wide by 8.5m long slot – several extensions were added in response to the presence of a number of features including a lengthy wall segment with one spur wall, and a plaster platform, possibly associated with overlying material culture of Iron Age date. Further investigation of this area is planned for 2015.

    SG T11000, measuring1.7m wide and 7.2m in length, was opened in order to assess the geological (and potential archaeological) consequences of the bi-directional erosion at a significant change of slope. At 0.40m depth, the natural subsoil was encountered, but after cleaning an archaeological deposit of Iron Age materials was found similar to that in SG T10000. Further investigation of this area is planned for 2015.

  • Susan Kane - Oberlin College 

Director

Team

  • William Raynolds, New York University
  • Audra Mayhan, Salt Lake City, Utah
  • James Countryman - Oberlin College
  • Alexis Christensen - University of Utah
  • Emiliano Fioriti, Sintesis, Atessa, Italy
  • Luca Colantuono, Geo Logica s.n.c. Roma, Italy
  • Anna Pia Apilongo, Atessa, Italy
  • Luke Aspland - Lund University
  • Sam Carrier, Oberlin College
  • Melissa Fore, Oberlin College
  • Archer Martin - American Academy in Rome
  • Hilary Conley, Florida State University
  • Alexander Ekserdijan - Oxford University
  • Christopher Pyrah - Oxford University
  • Neville McFerrin, University of Michigan
  • Rachel Backshall - Oxford University
  • William Austin, Oberlin College
  • Giuseppe Masilli

Research Body

  • Oberlin College, Ohio
  • The British School at Rome
  • University of Oxford - University of Oxford

Funding Body

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