1999
DOI: 10.1002/(sici)1099-0763(199906)6:2<107::aid-arp121>3.3.co;2-s
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Ground penetrating radar investigations at North Ballachulish Moss, Highland, Scotland

Abstract: Ground-penetrating radar was used to map the underlying topography of North BallachulishMoss. Ground-truthing, in the form of sediment coring and test-pitting, provided corroborative evidence for the peat depths as defined by the radar survey. Trial trenching revealed that a suite of radar anomalies identified during the course of the survey related to a buried prehistoric surface with an associated abundance of wooden stakes and twigs.

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Cited by 5 publications
(7 citation statements)
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“…The linear high amplitude reflections in the GPR timeslices starting at 0.44 m (see Figure (C)) deep were interpreted as being caused by the timbers encountered in the excavation, or their direct impact on the peat horizon they sit upon. There are other instances of GPR detection of waterlogged timbers (Clarke, Utsi, & Utsi, ; Utsi, , , ) so this is not a surprising outcome. The resistivity anomaly is co‐located with the timbers, but the bog oak was not detected with this technique, reaffirming our suspicion that some other factor is involved.…”
Section: Validation and Discussionmentioning
confidence: 86%
See 1 more Smart Citation
“…The linear high amplitude reflections in the GPR timeslices starting at 0.44 m (see Figure (C)) deep were interpreted as being caused by the timbers encountered in the excavation, or their direct impact on the peat horizon they sit upon. There are other instances of GPR detection of waterlogged timbers (Clarke, Utsi, & Utsi, ; Utsi, , , ) so this is not a surprising outcome. The resistivity anomaly is co‐located with the timbers, but the bog oak was not detected with this technique, reaffirming our suspicion that some other factor is involved.…”
Section: Validation and Discussionmentioning
confidence: 86%
“…This is a function of both the original chemistry of the soil, and the processes it has been subjected to, including the addition of material such as ash, waste products, pottery and food waste, as well as in situ heating or burning, and oxidizing and reducing cycles not related to heat. This is further affected by the compaction of the soil; how many of those magnetized or magnetizable particles are packed into a given spatial unit of the soil that is being surveyed (Clarke, ; Dalan & Banerjee, ; Dearing, ; Gaffney & Gater, ; Marmet et al, ; Thompson & Oldfield, ). Given that these soils were saturated, and not considered to be from a settlement, or otherwise anthropogenically influenced, the usual expectations of higher soil magnetism (as measured by magnetic susceptibility) in the topsoil and in the fills of features like pits and ditches did not apply.…”
Section: Validation and Discussionmentioning
confidence: 99%
“…There remain challenges in identifying waterlogged archaeology within peatlands by geophysics due to a lack of physical contrasts (e.g. Clarke et al, 1999) and a variety of different techniques have been applied to address this (e.g. Schleifer et al, 2002).…”
Section: Proposed Methodologymentioning
confidence: 99%
“…The surface was bumpy and uneven, which resulted in unstable contact between the antenna and the ground surface and uneven rotation of the odometer wheel. Disrupted continuous contact causes problems in data acquisition by introducing a degree of interference, reducing reliance on positional information, and lessening the penetration depth (Clarke et al 1999). Such conditions, though, are typical for various forms of wetland environments in Finland.…”
Section: Geophysical Anomalies and The Ground Truthing Datamentioning
confidence: 99%