fcambridgeshirearchaeology Late Saxon to Post-medieval Manorial ...
fcambridgeshirearchaeology Late Saxon to Post-medieval Manorial ...
fcambridgeshirearchaeology Late Saxon to Post-medieval Manorial ...
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1 Introduction<br />
This archaeological evaluation was undertaken on land <strong>to</strong> the south of<br />
Wash Road, Kir<strong>to</strong>n, Lincolnshire (TF 3090 3780; Fig. 1) in advance of<br />
proposed construction of a s<strong>to</strong>rage and distribution park. The<br />
archaeological work was carried out in accordance with a trial trench<br />
Brief issued by Jane Young, South Kesteven and Bos<strong>to</strong>n Borough<br />
Planning Archaeologist (Young 2006), supplemented by a<br />
Specification by Jacobs Babtie dated 18th May 2006 (Jacobs Babtie<br />
2006). Another phase of the evaluation will take place <strong>to</strong> the south of<br />
Princess Road in 2007.<br />
The work was designed <strong>to</strong> assist in defining the character and extent of<br />
any archaeological remains within the proposed redevelopment area,<br />
in accordance with the guidelines set out in Planning and Policy<br />
Guidance 16 - Archaeology and Planning (Department of the<br />
Environment 1990). The results will enable decisions <strong>to</strong> be made by<br />
the Bos<strong>to</strong>n Planning Archaeologist, on behalf of Bos<strong>to</strong>n Borough<br />
Council (the Local Planning Authority) with regard <strong>to</strong> the treatment of<br />
any archaeological remains found.<br />
The site archive is currently held by CCC AFU and will be deposited<br />
with Lincoln Museum (museum accession number 2006.135). The site<br />
code was WRKI 06.<br />
2 Geology and Topography<br />
The drift geology of the area comprises Terring<strong>to</strong>n Beds, which<br />
(generally) comprise younger Marine Deposits (Romano-British <strong>to</strong> the<br />
present day), salt marsh, tidal creek and river deposits (sandy silt,<br />
sand and clay). These overlie clays that were deposited during the<br />
Jurassic period (British Geological Survey 1995).<br />
The natural deposits on the site varied from silty clays in the extreme<br />
south-eastern part <strong>to</strong> sandy silts with a little clay over much of the area.<br />
A borehole survey was undertaken although the results are not yet<br />
available. The backfill from some of the boreholes implies that at least<br />
some of the underlying solid geology consists of sands and gravels.<br />
The land is fairly flat with an extremely gentle north <strong>to</strong> south slope<br />
across the site with the northern part at Wash Road lying at between<br />
3.34 and 3.08m OD falling <strong>to</strong> between 2.97m and 2.96m OD at the<br />
south side by Princess Road.<br />
1<br />
CCC AFU Report No. 895