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N R GOULTY

Biographic Data

ID5217358
NAMEN R GOULTY
GIVEN NAMESN R
FAMILY NAMEGOULTY
SIGNATUREGOULTY N R
AFFILIATIONSDurham University
VERIFIEDNo
TOTAL WORKS4
TOTAL CITATIONS0
WORKS AS AUTHOR4
WORKS AS EDITOR0
FIRST PUBLICATION YEAR1990
LATEST PUBLICATION YEAR2003
H-INDEX0
  • Comparison of geophysical techniques for investigating an infilled ditch at Bury Walls hill fort, Shropshire

    Open Access•Ruth Murdie, R E Murdie et al.•ARTICLE•Archaeological Prospection•2003•References: 1

    Five geophysical survey techniques were used to investigate the infilled section of the outer ditch at the Iron Age hill fort of Bury Walls, Shropshire. The techniques were resistance mapping and four profiling methods: resistivity sounding, ground‐penetrating radar (GPR), P‐wave seismic refraction and S‐wave seismic refraction. The ditch was clearly visible on the resistance map and on GPR profiles, but no depth estimate was obtainable from thes…

  • Completion of the Seismic Refraction Survey to Locate the Vallum at Vindobala, Hadrian's Wall

    Open Access•N R GOULTY, Alison Hudson et al.•ARTICLE•Archaeometry•1994•References: 4

    The vallum is a major earthwork along the south side of Hadrian's Wall. All surface traces of it have been obliterated over a 500‐m‐long stretch past the fort of Vindobala at Rudchester, Northumberland. To the west of the fort, the vallum's course had previously been delineated by running shear‐wave seismic refraction lines to obtain depth profiles of rockhead. We have now run more seismic refraction lines, using both shear waves and compressiona…

  • Mapping the Pre-Holocene Surface of an Infilled Valley in the East Kent Fens, UK, with a Shear-Wave Seismic Refraction Survey

    Open Access•Antony J Long, Christopher Gunn et al.•ARTICLE•The Holocene•1992

    In a study of the Holocene sediments in the Hacklinge-Deal area of the East Kent Fens, Southeastern England, hand-coring data has shown that the pre-Holocene surface in this area is incised by one or more valley features, now infilled with unconsolidated Holocene sediments. A shear-wave seismic refraction survey was carried out along profiles where hand-coring had failed to penetrate to bedrock in an attempt to define the detailed form of the pre…

  • Delineation of the Vallum at Vindobala, Hadrian's Wall, by a Shear‐wave Seismic Refraction Survey

    Open Access•N R GOULTY, John P Gibson et al.•ARTICLE•Archaeometry•1990

No prominent works on this page.

  • Delineation of the Vallum at Vindobala, Hadrian's Wall, by a Shear‐wave Seismic Refraction Survey

    Open Access•N R GOULTY, John P Gibson et al.•ARTICLE•Archaeometry•1990

  • Mapping the Pre-Holocene Surface of an Infilled Valley in the East Kent Fens, UK, with a Shear-Wave Seismic Refraction Survey

    Open Access•Antony J Long, Christopher Gunn et al.•ARTICLE•The Holocene•1992

    In a study of the Holocene sediments in the Hacklinge-Deal area of the East Kent Fens, Southeastern England, hand-coring data has shown that the pre-Holocene surface in this area is incised by one or more valley features, now infilled with unconsolidated Holocene sediments. A shear-wave seismic refraction survey was carried out along profiles where hand-coring had failed to penetrate to bedrock in an attempt to define the detailed form of the pre…

  • Completion of the Seismic Refraction Survey to Locate the Vallum at Vindobala, Hadrian's Wall

    Open Access•N R GOULTY, Alison Hudson et al.•ARTICLE•Archaeometry•1994•References: 4

    The vallum is a major earthwork along the south side of Hadrian's Wall. All surface traces of it have been obliterated over a 500‐m‐long stretch past the fort of Vindobala at Rudchester, Northumberland. To the west of the fort, the vallum's course had previously been delineated by running shear‐wave seismic refraction lines to obtain depth profiles of rockhead. We have now run more seismic refraction lines, using both shear waves and compressiona…

  • Comparison of geophysical techniques for investigating an infilled ditch at Bury Walls hill fort, Shropshire

    Open Access•Ruth Murdie, R E Murdie et al.•ARTICLE•Archaeological Prospection•2003•References: 1

    Five geophysical survey techniques were used to investigate the infilled section of the outer ditch at the Iron Age hill fort of Bury Walls, Shropshire. The techniques were resistance mapping and four profiling methods: resistivity sounding, ground‐penetrating radar (GPR), P‐wave seismic refraction and S‐wave seismic refraction. The ditch was clearly visible on the resistance map and on GPR profiles, but no depth estimate was obtainable from thes…

Geology (4 works) · Seismic refraction (4 works) · Seismology (4 works) · Bedrock (3 works) · Geomorphology (3 works) · Seismic Waves and Analysis (3 works) · Ditch (2 works) · Geology (2 works) · Geology and Paleoclimatology Research (2 works) · Geophysics (2 works)

Ethnos_APP • Open Source Project • MIT License • Frontend v2.0.0 • Privacy and Cookies • API Documentation: api.ethnos.app/docs • API Source Code: GitHub • DOI: 10.5281/zenodo.17049435 • Frontend Source Code: GitHub • DOI: 10.5281/zenodo.17050053 • cruz.rio.br • Expectantes Misericordiae