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EMAP_Progress_Reports_2009_2.pdf - The Heritage Council

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Waterford<br />

reinforced by the addition of a stone retaining wall in the early/mid-twelfth century (Hurley<br />

1997b, 10).<br />

<strong>The</strong> original church of the Holy Trinity (Christchurch) was built before A.D. 1185. It was<br />

probably built in the mid-eleventh century (Bradley & Halpin 1992) after the Stage 2 defences<br />

had fallen out of use. Excavations have established that St. Peter’s church was also built at<br />

this stage while other churches such as St. Mary’s and St. Olaf’s may date to the same<br />

period.<br />

Settlement rapidly expanded to the west (Phase 4) outside the line of the early/late-twelfth<br />

century stone wall constructed along the line of Arundel Square and Bakehouse Lane. <strong>The</strong>re<br />

is evidence that this was well underway by the mid-twelfth century when a number of houses<br />

were found to be built above the backfilled ditch. <strong>The</strong> line of another later twelfth century<br />

(possibly pre-Anglo-Norman) defensive bank and ditch was uncovered in excavations further<br />

west (Wren 1998, 2000, 2001 & 2002; Moran 1999). Subsequently, this defensive ditch and<br />

bank fell out of use and was replaced in the early-thirteenth century by a new defensive wall<br />

with gate-towers.<br />

Fig. 285: Topopgraphical development of Scandinavian Waterford (after Hurley et al. 1997,<br />

7).<br />

DEFENCES<br />

Ninth-century Dún Defences<br />

It has been suggested that the original nucleus of the Scandinavian town was in the area of<br />

Reginald’s Tower (Bradley & Halpin 1992, 108). Hurley’s model (1997, 8-11) has proposed a<br />

westward expansion with the Phase 1 tenth-century Dún (Dundory) comprising a small<br />

triangular space between the confluence of the two rivers. A subsequent developmental<br />

phase (2) - indicated by the layout of properties in early maps- may have involved the<br />

enclosure by ramparts of a further strip, west of the primary nucleus towards the end of the<br />

tenth century (Fig. 285).<br />

609

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