Geotechnical and archaeological data from Bristol and Dover
Bristol
A comparison of
geotechnical and archaeological recording was made at Redcliffe
Street, Bristol. The area lies within the medieval suburb of
Redcliffe. Development since the 14th
Century has been concentrated in and around this area. The site was chosen for study because of the
completeness of the archaeological and geotechnical records, but also because
of its position. Redcliffe is situated
on the outside of a meander bend of the River Avon on deep alluvium. This provides a favourable environment for
the preservation of archaeological artefacts.
The study
highlighted a number of important points.
- A lack of detailed recording during geotechnical
investigations meant that important archaeological boundaries were
missed. For example, the boundary
between the modern cellar fill and medieval fill below the cellar
flagstones was missed.
- Drillers routinely logged additional important
information such as depth to ‘natural’ on site.
- Interfaces within made ground are often
distinguished through the types of inclusions present.
- Borehole heights were rarely accurately constrained
in three dimensional space.
Dover
Dover
was selected as an example are due to the familiarity
of one of the investigators, Dr. Martin Bates,
with both the field geoarchaeological program as well as the archaeological
investigations. Much of the
archaeological information was collected as part of a mitigation strategy
during the construction of the new A20 Road
and Sewer Scheme in Dover during
the early 1990’s.
The
archaeological investigation involved the use of historical archaeological
borehole and section data, geotechnical data, geoarchaeological borehole data
and excavation data carried out by Canterbury Archaeological Trust. The study highlighted a number of important
findings that build on those summarised above.
- Geotechnical
drill crews often log much more detail than is included in the interpretative
geotechnical report, which is written according to client
specifications. The study
highlighted that geotechnical drillers could record enough detail to
permit basic archaeological site interpretation.
- The depth
to ‘made ground’ was often over-estimated by the drillers. Many of the layers containing
archaeological artefacts or occupation surfaces were classed simply as
made ground. This is because no
criteria exist for recording made ground.
Simply classifying the ground as modern or old made ground would
have provided the archaeologist with more detail.
- Methods of
drilling can destroy complex stratigraphic sequences, such as where the
vertical distance between layers is small.
Where significant changes in archaeology occur, important information
may be destroyed by over-reliance on borehole logs.
- The general
geoarchaeological and geotechnical interpretations of the stratigraphy of
the site were similar, but that the geoarchaeological logs provided more
detailed local information. This illustrates
that geotechnical logs can be useful in directing future archaeological
investigations.
Summary
The Dover and Bristol studies showed that geotechnical drilling
crew could record enough detail to provide archaeologists with useful data for
assessing the archaeology of the site.
When briefed with a set of simple recording criteria for made ground,
geotechnical workers were quickly able to produce detailed borehole logs. Geotechnical drill crews routinely provide
relatively detailed borehole logs, suggesting that more detailed archaeological
recording is achievable.
However, the study has highlighted some
limitations of the geotechnical records:
- Interfaces
within the made ground were not recorded as a matter of routine. Recording the depths of stratigraphic
changes in the nature of made ground would be very useful
archaeologically.
- Although
inclusions were noted in many geotechnical logs, their depths were not
recorded. By recording the depth of
inclusions, useful data for archaeological site assessment may be
recorded.
- Complex
archaeological stratigraphies are better
recorded from geotechnical test pits than boreholes because drilling can
destroy fine stratigraphy.
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