The gradiometer survey has produce mixed results. In the main survey area data were severely affected by a pre-existing buried metal pipe, running alongside the plastic water pipe. However, several broad ditch type anomalies were noted though no particular pattern could be established. Resistance survey identified anomalies suggestive of possible structural remains, but excavation revealed these to be naturally occurring chalk outcrops. A small survey to the northwest of the main area of investigation produced a very weak, sub-circular, magnetic anomaly that proved on excavation to be prehistoric in date.