Detailed magnetometry was carried out on 5 small areas targeting wind turbine locations of 1800m2 each. The results of the magnetometer survey show that levels of magnetic enhancement are low within the site. Positive area anomalies located within the majority of the survey areas do not have the characteristics of anthropogenically cut features but are likely to be responses to variable geology with the former depositional or erosional environment of the underlying alluvium. Negative linear anomalies have been located but the majority of these correspond to visible drainage channels within the survey areas.