Resistivity survey measures the electrical resistance of the earth’s soil moisture content. A twin probe configuration is normally carried out, which involves the pairing of electrodes (one current and one potential), with one pair remaining in a fixed position (remote probes), whilst the mobile probes measure variations in electrical resistance across the survey grids. Resistance is measured in ohms, and this method generally detects to a depth of 1m.

Features such as wall foundations are usually identified as high resistance anomalies, as well as rubble spreads, made surfaces (i.e. yards and paths) and metalled roads and trackways.

 In contrast, low resistance values are normally associated with water-retentive features such as large pits, ditches, drains and gullies. This technique is usually recommended for prospection of known or suspected structural remains.

Medieval Monastic Grange
and Bronze Age Barrows

Frequently Asked Questions
About Resistivity Surveys

Find out more about resistivity surveys from our frequently asked questions. If you require any further information, feel free to get in contact on 01522 704900. 

A resistivity survey maps differences in the electrical resistance of the ground. These differences can indicate buried features whose materials or moisture content contrast with the surrounding soil.

It can help locate wall foundations, rubble spreads, yards, paths and metalled roads. Moisture-retaining features such as pits, ditches, drains and gullies can also produce detectable contrasts.

Our usual twin-probe arrangement uses one fixed pair of electrodes and one mobile pair. The surveyor moves the mobile probes across a grid to record changes in resistance and build a picture of the site.

The twin-probe method described on this page generally investigates to around one metre. This is an approximate working depth, not a guarantee: the ground conditions, probe spacing and nature of the feature affect detection.

Stone foundations and rubble can retain less moisture than the soil around them, making it harder for electrical current to pass. They may therefore appear as high-resistance anomalies, although the local conditions influence the response.

The fills of ditches and pits may hold more water than the surrounding ground. Where that moisture contrast exists, they can conduct current more readily and appear as low-resistance anomalies.

No excavation is normally needed to collect the readings. Small probes are inserted into the ground to make electrical contact, allowing the area to be investigated with minimal surface disturbance.

Yes. The technique relies partly on moisture contrasts, so very dry ground, saturation and seasonal changes can influence the readings. Site conditions should be considered when choosing the survey timing and interpreting the results.

Yes. The methods measure different physical properties, so they can provide complementary evidence. Resistivity is particularly useful when structural remains are suspected, while gradiometry can help investigate magnetic contrasts across the site.

Please provide a site location, a plan of the survey area, the approximate size and details of any suspected remains or previous investigations. Information about access, vegetation and ground conditions will also help us discuss the scope with you.