1998
DOI: 10.9750/psas.127.577.594
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Excavation of Roman, medieval and later features at Carriden Roman fort annexe in 1994

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Cited by 2 publications
(2 citation statements)
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“…In the part of the region argued here to have been in economic decay, the putative pre-Antonine fields at Castledykes (Maxwell & Wilson 1987) are intriguing given the site-specific palynological evidence for cultivation as well as grazing (see above). argued that the system at Carriden (see also Bailey 1997) may have been contemporaneous with Roman occupation, perhaps associated with the civilian settlement, though this has not been established, but the best known system at Inveresk (Thomas 1988;Bishop 2002), though close to another vicus, is multi-period with some elements having developed in later prehistory and some added after Roman occupation (Cook 2004). The Roman system is extensive, however, and Cook (2004) argues that it gradually evolved, perhaps from a pre-Antonine core.…”
Section: Land Uses and Land Use Change: Synthesis And Discussionmentioning
confidence: 99%
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“…In the part of the region argued here to have been in economic decay, the putative pre-Antonine fields at Castledykes (Maxwell & Wilson 1987) are intriguing given the site-specific palynological evidence for cultivation as well as grazing (see above). argued that the system at Carriden (see also Bailey 1997) may have been contemporaneous with Roman occupation, perhaps associated with the civilian settlement, though this has not been established, but the best known system at Inveresk (Thomas 1988;Bishop 2002), though close to another vicus, is multi-period with some elements having developed in later prehistory and some added after Roman occupation (Cook 2004). The Roman system is extensive, however, and Cook (2004) argues that it gradually evolved, perhaps from a pre-Antonine core.…”
Section: Land Uses and Land Use Change: Synthesis And Discussionmentioning
confidence: 99%
“…On the Forth estuary, the Wall east of Inveravon has evidence that the coast has retreated since Roman occupation. The fort at Carriden stands on a high cliff but the only limited evidence for the seaward defensive ditches (Bailey 1997) suggests that this cliff has retreated by an unknown distance since the second century ad: some of the most seaward fields of the system east of the fort also have no northern edges, though this need not imply contemporaneity of field system and fort. West of Bo'ness, the cliff is fronted by mudflat sediments that formed before the Antonine occupation and a 'Roman coastline' can be defined with reason (Bailey 1995b;Bailey & Cannel 1996) (illus 2).…”
Section: The Seamentioning
confidence: 99%