2015
DOI: 10.1016/j.jasrep.2015.07.003
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A submerged monolith in the Sicilian Channel (central Mediterranean Sea): Evidence for Mesolithic human activity

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Cited by 14 publications
(15 citation statements)
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References 33 publications
(38 reference statements)
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“…The Pantelleria Vecchia Bank, made of sandstones, is located at 18 miles from Pantelleria Island. It is composed of two main shoals, varying from 16 to 24 meters depth; the surrounding areas are located at depths ranging from 46 to 60 meters [28]. The Graham Bank, along with Terrible Bank and Nerita Bank, is part of a large volcanic relief named Empedocle Seamount.…”
Section: Methodsmentioning
confidence: 99%
“…The Pantelleria Vecchia Bank, made of sandstones, is located at 18 miles from Pantelleria Island. It is composed of two main shoals, varying from 16 to 24 meters depth; the surrounding areas are located at depths ranging from 46 to 60 meters [28]. The Graham Bank, along with Terrible Bank and Nerita Bank, is part of a large volcanic relief named Empedocle Seamount.…”
Section: Methodsmentioning
confidence: 99%
“…Site abbreviations as in Table 1 present, respectively (Lambeck et al, 2011;Abelli et al, 2014). Therefore, Pantelleria was closer to the Sicilian coast than Lipari, given the presence of a large continental platform to the south-west of Sicily (Lodolo & Ben-Avraham, 2015). The distribution of Pantelleria obsidians in Sicily shows a singular bipartition: while the archaeological sites of the central-western sector have variable percentages of Pantellerian obsidians, though always lower than Lipari obsidians, the sites of the eastern sector of Sicily are completely devoid.…”
Section: Discussionmentioning
confidence: 95%
“…The Pantelleria Vecchia Bank is composed of two main shoals, which elevate from 46-60 m to 16-24 m depth, and a number of smaller isolated bathymetric highs (Lodolo & Ben-Avraham, 2015).…”
Section: Study Areamentioning
confidence: 99%