2010
DOI: 10.1002/gea.20319
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Occupation surfaces sealed by the Avellino eruption of Vesuvius at the Early Bronze Age village of Afragola in southern Italy: A micromorphological analysis

Abstract: This paper reconstructs the use of space and defines activity areas within a single hut (Hut 8) at the Early Bronze Age village of Afragola (southern Italy). The village, consisting of a number of huts and other structures, was covered by approximately 1 m of volcanic ash during the eruption of Vesuvius in 3550 Ϯ 20 BP. Thirteen samples were collected from inside the hut to analyze the spatial variability in sedimentary characteristics among three areas of Hut 8-the apsidal, central, and entrance areas. The … Show more

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Cited by 10 publications
(5 citation statements)
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“…To study the record at higher resolution, samples of intact sediment blocks were also taken from various parts of the sequence using Kubiena tins for the preparation of thin sections for micromorphological analysis (e.g. Kourampas et al, 2009;Matarazzo et al, 2010). Samples of tephra were collected from the section shown in Fig.…”
Section: Field and Laboratory Methodsmentioning
confidence: 99%
“…To study the record at higher resolution, samples of intact sediment blocks were also taken from various parts of the sequence using Kubiena tins for the preparation of thin sections for micromorphological analysis (e.g. Kourampas et al, 2009;Matarazzo et al, 2010). Samples of tephra were collected from the section shown in Fig.…”
Section: Field and Laboratory Methodsmentioning
confidence: 99%
“…V/17 (Di Matarazzo et al, 2010;Albore Livadie et al, 2011), are mapped in Fig. 8, which represents a provisional map of this "destruction horizon".…”
Section: The Exploitation Areas At the Pda "Destruction Horizon"mentioning
confidence: 99%
“…According to Gé et al (1993), floors can be divided into passive, active, and reactive zones. Microstratigraphic and geochemical methods can be used to identify these zones, an approach that has been successful in certain sites (e.g., Hutson and Terry 2006;Matthews et al 1997; but see Macphail 2006 andMatarazzo et al 2010); however, the typical zone thickness of millimeters to centimeters typically prevents implementation of excavation strategies that can isolate discrete archaeological assemblages. Figure 13 illustrates how microstratigraphic methods can be used to identify the reactive zones of floors at the Aceramic Fig.…”
Section: Contacts Interfaces and Post-depositional Processesmentioning
confidence: 99%