Decoding Capua’s roof terracotta
A multi-analytical study of the Fondo Patturelli sanctuary and Alveo Marotta furnace (6th century BCE – 1st century BCE)
Datos Bibliográficos
| ID | 13097254 |
|---|---|
| Autores | Maria Verde (0000-0002-1661-2613, University of Naples Federico II, autor de correspondencia), Alberto De Bonis (0000-0002-8088-9481, University of Naples Federico II, autor de correspondencia), Natalie Wagner (0009-0008-1233-9323, Deutsches Archäologisches Institut, Abteilung Rom), Francesca d’Aniello (University of Naples Federico II), Vincenzo Morra (0000-0002-3310-8603, University of Naples Federico II) |
| Año | 2024 |
| Volumen | 58 |
| Páginas | 104708-104708 |
| Fecha de publicación | 2024-07-29 |
| Peer Reviewed | Sí |
| Open Access | Sí |
| Tipo | ARTICLE |
| Revista | Journal of Archaeological Science Reports (JOURNAL) |
| Identificadores de la revista | ISSN: 2352-409X • E-ISSN: 2352-4103 |
| Editorial | Elsevier BV (PUBLISHER) |
| DOI | 10.1016/j.jasrep.2024.104708 |
| OpenAlex | W4401064878 |
| Idioma | EN |
| Citas recibidas | 1 |
| Referencias citadas | 26 |
The main focus of this study was to examine 25 samples of archaeological ceramic materials currently preserved in the Archaeological Museum of the Ancient Capua and Mitreo investigated in the framework of an international project. These samples primarily consist of architectural terracotta from the Fondo Patturelli extra-urban sanctuary, as well as architectural terracotta, pottery and waste material from the nearby Alveo Marotta furnace. To investigate these artifacts, a multi-analytical mineralogical-petrographic approach was performed. Thin section observations revealed that almost all samples exhibit a coarse-grained paste. The fragments were categorized into three petrographic groups based on the type and quantity of temper, which is mostly composed of volcanic grains. They include lithics and juvenile fragments (obsidians and pumices) ascribed to the products of the major Campanian eruptions as detected via FESEM-EDS. Bulk chemical analyses (WD-XRF) show that almost all samples form a homogeneous group made with Ca-rich clayey raw materials, also including three wastes of tiles from the Alveo Marotta. By contrast, other two wastes from Alveo Marotta were produced with Ca-poor clay suggesting the use of a different raw material. From a technological point of view the samples are characterized by a thermal range that varies from 750 to 900 °C, notably different between the earlier and later production periods, with the former fired at lower temperatures
Archaeology · Art · Breccia · Geochemistry · Geography · Mineralogy · Petrography · Pottery · Temple · Terracotta · Archaeological Research and Protection · Building materials and conservation · Cultural Heritage Materials Analysis · Geology · Paleontology
Ceramic Petrography
Hematite nucleation and growth in the firing of carbonate-rich clay for pottery production
Summary of "Concerning some additional aids in studying sedimentary formations," by M. S. Shvetsov
Carbonate and silicate phase reactions during ceramic firing
Tectono-stratigraphic setting of the Campania region (southern Italy)
Differently Calenian
Raw Materials for Archaeological Pottery from the Campania Region of Italy
Distinctive Volcanic Material for the Production of Campana A Ware
Multianalytical investigation of wasters from the Tower 8/Porta di Nola refuse middens in Pompeii
Technological examination of Neolithic-Bronze Age pottery from central and southeast Europe and from the Near East
Minero‐petrographic characterization of fine ware from Cales (South Italy)
Unglazed pottery from the masjed-i jom'e of Isfahan (Iran)
The ancient pozzolanic mortars of the Thermal complex of Baia (Campi Flegrei, Italy)
| Obras citantes distintas | 1 |
|---|---|
| Citas por año | 1 |
| Intervalo de citas | 2025 - 2025 (1) |
| Velocidad de citación | recent |
| Altamente citado | No |
| Tipos de cita | Neutras: 1 |