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Much of the image consists of blank locations now with little or no radar response. The "courtyard" wall is still showing highly, however, and there are continuing ideas of a difficult surface area in the SE corner. Time slice from 23 to 25ns. This last slice is now practically all blank, however a few of the walls are still revealing strongly.

How deep are these slices? The software application I have access to makes estimating the depth a little difficult. If, however, the leading 3 pieces represent the ploughsoil, which is most likely about 30cm think, I would guess that each slice is about 10cm and we are only coming down about 80cm in overall.



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Luckily for us, many of the websites we have an interest in lie just below the plough zone, so it'll do! How does this compare to the other approaches? Comparison of the Earth Resistance information (leading left), the magnetometry (bottom left), the 1517ns time piece (top right) and the 1921ns time piece (bottom left).

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Magnetometry, as talked about above, is a passive method determining local variations in magnetism against a localised no value. Magnetic susceptibility study is an active strategy: it is a procedure of how magnetic a sample of sediment might be in the existence of a magnetic field. Just how much soil is evaluated depends on the size of the test coil: it can be extremely small or it can be fairly large.

The sensor in this case is extremely little and samples a tiny sample of soil. The Bartington magnetic vulnerability meter with a large "field coil" in use at Verulamium throughout the course in 2013. Top soil will be magnetically boosted compared to subsoils merely due to natural oxidation and reduction.

By measuring magnetic susceptibility at a reasonably coarse scale, we can spot locations of human occupation and middens. We do not have access to a reliable mag sus meter, however Jarrod Burks (who helped teach at the course in 2013) has some excellent examples. Among which is the Wildcat site in Ohio.

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These towns are often set out around a central open area or plaza, such as this reconstructed example at Sunwatch, Dayton, Ohio. Sunwatch Village, Dayton, Ohio (photo: Jarrod Burks). At the Wildcat website, the magnetometer study had found a variety of features and houses. The magnetic susceptibility study helped, however, specify the primary location of occupation and midden which surrounded the more open location.

Jarrod Burks' magnetic vulnerability survey results from the Wildcat website, Ohio. Red is high, blue is low. The strategy is for that reason of great usage in defining areas of basic occupation rather than identifying particular features.

Geophysical surveying is a used branch of geophysics, which utilizes seismic, gravitational, magnetic, electrical and electromagnetic physical methods at the Earth's surface area to measure the physical homes of the subsurface - Geophysical Survey in Carine WA 2022. Geophysical surveying techniques typically determine these geophysical properties in addition to abnormalities in order to evaluate various subsurface conditions such as the presence of groundwater, bedrock, minerals, oil and gas, geothermal resources, voids and cavities, and much more.