News & Projects
The last few weeks has seen several successful surveys using the Geoscan MSP25 resistivity cart with additional gradiometer for the collection of simultaneous magnetic data. High resolution datasets have provided detail over two Roman sites with data captured through brambles in woodland where GNSS linked cart data and handheld surveying would have been impossible.
Magnetic debris is located by virtually all magnetometry surveys and often dismissed as modern topsoil junk. However, we shouldn't be too hasty in considering this material insignificant, it represents something and perhaps could be the only archaeological evidence of a past event, activity, settlement, etc. This article considers sources of magnetic debris and what sort of archaeological information may be derived from it.
My day of work with Archaeological Surveys LTD carrying out a ground penetrating RADAR survey.
Magnetometry undertaken at Tysoe, Warwickshire in 2017 and 2018 has revealed further evidence for extensive Romano-British and prehistoric settlement. Several sites previously identified by fieldwalking in the 1990s, and geophysics in 2010/2011, were chosen for additional wide area magnetometry survey. The results indicate numerous enclosures, field systems and track ways surrounding core settlement areas. The complexity of many of the sites infers long periods of settlement, possibly from the Bronze Age to the end of the Roman period.
Magnetometry with Sensys FGM650 gradiometers. Archaeological Surveys director David Sabin considers the benefits of using fixed tension band gradiometers, particularly for cart-based surveys.
The Stonehenge Chubb Centenary Day, at Shrewton near Stonehenge, included several cricket matches between teams of archaeologists and Shrewton village. Cecil Chubb, born at Shrewton and a cricketer for the village, bought Stonehenge at auction in 1915 and gifted the monument to the nation in 1918. The cricket matches were played in good spirit with some of the archaeologists dressing for the period.