Detailed magnetic survey known as magnetometry is an effective and efficient geophysical survey technique used to define areas of past human activity by mapping spatial variations and contrast in the magnetic properties of soil, subsoil and bedrock. The technique can be carried out over areas of grass, crop and open soil. Archaeological Surveys use a multi-sensor cart based system combined with RTK GNSS for precise positioning. The cart is either pushed by the operator on foot or towed using an ATV.  As standard we collect data along 0.5m traverses at 0.15m centres; this provides significantly higher resolution than standard which results in higher quality reports.

Truckle Hill Roman villa and prehistoric siteThe image to the right represents magnetometer data collected at Truckle Hill Roman Villa in Wiltshire. The black lines represent magnetically enhanced soil and imply the presence of cut ditch-like features whilst the narrow white lines indicate material of low magnetic susceptibility; in this case the oolitic limestone footings of the villa complex (top right of image).

Recent excavation work confirmed the large ditch surrounding the villa, probably dating to the 3rd century. The ditch in the centre of the image appears as a possible 'cross-dyke' and is prehistoric although it is mirrored to the north by parallel Roman ditches. Late Iron Age ditches are visible at the bottom of the image.

Weakly magnetic iron minerals are always present in soil and magnetic enhancement is associated with localised zones of higher magnetic susceptibility and permanently magnetised thermoremnant material.

Magnetic susceptibility relates to the induced magnetism of a material when in the presence of a magnetic field. Within soils this can effectively be considered as a permanent magnetism due to the presence of the Earth's magnetic field. Thermoremnant magnetism is permanent and acquired by iron minerals that, after heating to a specific temperature known as the Curie Point, are effectively demagnetised followed by re-magnetisation by the Earth's magnetic field on cooling.

Silting and deliberate infilling of ditches and pits with magnetically enhanced soil creates a relative contrast against the much lower levels of magnetism within the subsoil into which the feature is cut. Systematic mapping of magnetic anomalies will produce linear and discrete areas of enhancement allowing assessment and characterisation of subsurface features. Material such as subsoil and non-magnetic bedrock used to create former earthworks and walls may be mapped as areas of lower enhancement compared to surrounding soils.

By plotting data collected in the field as a greyscale, a plan of magnetic anomalies can be created. Archaeological features are then characterised by their pattern and form.

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