
Excavations at Biggin Street, Dover
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A Forgotten Kentish Rebellion, September-October 1470
Faversham's Role in the Armada and Counter-Armada
Excavations at Biggin Street, Dover
David Wilkinson and Duncan Wood
EXCAVATIONS AT BIGGIN STREET, DOVER
DA YID WILKINSON AND DUNCAN WOOD
with contributions by
K. Atherton, K. Brown, P. Blinkhorn, P. Booth, B. Charles,
C. Ingrem and H. Lamdin-Whymark
In January 1999 the Oxford Archaeological Unit (now Oxford Archaeology)
undertook an excavation in advance of the construction of a
new retail store on the site of a former Post Office at Biggin Street,
Dover (NGR TR 3172 4162: Fig. 1). A desk-based assessment had
been produced and the site had already been evaluated. The excavation
identified archaeological deposits from various phases of occupation.
These include the location of Roman boundary ditches/gullies, a
possible Saxon cultivation soil, several late medieval/post-medieval
wells, a post-medieval cultivation soil and post-medieval structural
features (wall remnants). Artefacts recovered from the site ranged in
date through all of these periods, and some residual flint artefacts
were also found. Excavations were limited to the locations of the
foundation piles, allowing a proportion of the archaeological deposits
to be preserved in situ. The excavation strategy was designed
by Paul Chadwick of CgMs Consulting, acting as Archaeological
Consultant to the developers, Chartwell Land Development Limited,
who funded the archaeological fieldwork and publication.
The site lies on the corner of Biggin Street and Priory Street in the
town centre of Dover (Fig. 2). The site geology consists of brickearth
overlying a buff chalky clay with shattered flint known as Coombe
Rock. The base geology is Middle and Lower Chalk. The site lies on
the approximate edge of an inner basin on the west side of Dover and
at the mouth of a west-east dry valley (Fig. 1 ). Both of these topographical
features have dictated the nature of the site drift geology
which formed during the Devensian and mid Holocene. Jn situ
alluvial deposits relating to the inner basin were identified during an
archaeological evaluation (OAU, June 1994) approximately 20m to
the north of the present Biggio Street frontage.
153
Fig. I Site Location in Dover.
Prloty Groun