The face of long-covered parts of Hadrian’s Wall was revealed during excavation by the WallCAP project. CREDIT: WallCAP
Many
miles of Hadrian’s Wall survive beneath turf and rubble, unexplored and often
under threat from erosion, people, and animals. A recent excavation at Walltown
Crags in Northumberland, undertaken in advance of fixing some of this damage,
revealed sections of the Wall that had not been seen for centuries.
The dig took place in October as part of
the WallCAP project. Run by Newcastle University and funded by the National Lottery
Heritage Fund, the project aims to draw local volunteers into investigating and
protecting the many Heritage at Risk sites along the Wall.
Two small trenches were opened, running
both across and up to the Wall. The first trench ran across an Edwardian ditch
and bank, and also revealed one new course of wall, which was found to be
sitting directly on weathered bedrock. Below the early 20th-century spoil, large
stones from a previous wall collapse were discovered. These earlier excavators
had left no mementos of their work, and the trench may simply have been an attempt
driven by local curiosity to expose some of the wall-face and create a local
attraction.
A second trench was positioned just east of the Edwardian
trench, and ran from the south, over the buried curtain wall, and down the
north face. This section of the Wall had been hidden for some time, probably
for centuries. Excavation revealed up to seven surviving courses of wall, which
were almost completely unweathered and clearly constructed without bonding,
indicating that it probably remained unaltered from its original construction –
an unusual occurrence. The wall was again constructed directly onto bedrock,
but here it was pristine and sharp, reflecting the centuries it had remained unexposed
to the elements.
In addition to conserving the Wall, the WallCAP
project is conducting research, including on the source of the stones used to
construct it. During this excavation, it was noted that, while the majority of
facing stones were locally quarried sandstone, one south-facing stone glowed an
orangey pink, suggesting that it had been hewn from igneous rock, probably from
the Cheviot Hills to the north.