Title: |
St Stephen's Beacon, St Stephen-in-Brannel, Cornwall |
Series: |
Historic England Research Reports
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Downloads: |
nmr1-517162_212912.pdf (25 MB)
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Download
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Licence Type: |
Creative Commons Attribution 4.0 International Licence
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DOI |
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Publication Type: |
Report (in Series)
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Abstract: |
The Earth Resistance survey was focused on the area in the immediate vicinity of the
upstanding remains at the summit of the Beacon.
Measurements were recorded over six 30m grids established with a Trimble R8s GNSS
using a Geoscan RM85 earth resistance meter, internal multiplexer, and a PA5
electrode frame in the Twin-Electrode configuration, to allow two separate surveys with
electrode separations of 0.5m and 1.0m to be collected simultaneously. The 0.5m
electrode separation coverage was designed to detect near-surface anomalies in the
upper 0.5m of the subsurface whilst the 1.0m separation survey allowed anomalies to a
depth of about 1-1.25m to be detected. For the 0.5m electrode separation survey readings
were taken at a sample density of 0.5m x 1.0m whilst for the 1.0m separation survey they
were taken at a density of 1.0m x 1.0m.
A 3d-Radar MkIV GeoScope Continuous Wave Step Frequency (CWSF) Ground
Penetrating Radar (GPR) system was used to conduct the survey collecting data with a
multi-element DXG1820 vehicle towed, ground coupled antenna array (Linford et al. 2010;
Eide et al. 2018). A roving Trimble R8s Global Navigation Satellite System (GNSS) receiver was mounted on the GPR antenna array, that together with a second R8s base
station was used to provide continuous positional control for the survey collected along the
instrument swaths.
The GNSS base station receiver was adjusted to
the National Grid Transformation OSTN15 using the Trimble VRS Now Network RTK
delivery service. This uses the Ordnance Survey’s GNSS correction network (OSNet) and
gives a stated accuracy of 0.01-0.015m per point with vertical accuracy being half as
precise.
Data were acquired at a 0.075m x 0.075m sample interval across a continuous wave step
frequency range from 40MHz to 2.99GHz in 4MHz increments using a dwell time of 2ms. A
single antenna element was monitored continuously to ensure data quality during
acquisition together with automated processing software to produce real time amplitude
time slice representations of the data as each successive instrument swath was recorded
in the field (Linford 2013).
A magnetometer survey was also attempted using two Bartington grad-601 fluxgate
magnetometers. However, this was unsuccessful due to equipment malfunction and no
usable results were obtained. The earth resistance survey has detected anomalies associated with the main beacon
cairn, together with responses to areas of visible clearance bonfires and possible historic
clay extraction. Additional anomalies of possible archaeological or geological origin are
also evident within the data. The Ground Penetrating Radar survey has responded to
near-surface compacted ground due to vehicle tracks, footpaths and animal runs with
deeper, mainly low amplitude anomalies associated with the underlying igneous geology.
The geophysical surveys have not detected any unequivocal evidence for additional
subsurface remains due to Bronze Age or later activity at the site. However, some
anomalies to the southwest of the cairn, may tentatively be suggested to
have an association with it. |
Author: |
Megan Clements
Andrew W Payne
Neil T Linford
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Publisher: |
Historic England
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Year of Publication: |
2023
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Locations: |
Parish: |
St. Stephen-in-Brannel |
District: |
Cornwall |
County: |
Cornwall |
Country: |
England |
Grid Reference: 195982, 54507 (Easting, Northing)
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Subjects / Periods: |
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Identifiers: |
OASIS Id: |
nmr1-517162 |
Report id: |
32/2023 |
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Source: |
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Relations: |
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Created Date: |
18 Jul 2023 |