Details

The monument includes two intersecting earthworks known as Woodhouse Moor Rein
and South Dyke, which form part of the Aberford Dyke system.
South Dyke comprises three sections of earthworks of differing character; the
western part, west of the intersection with Woodhouse Moor Rein, has a
substantial bank with a ditch at its south side. For most of this section the
bank and ditch are at the top of the scarp south of Cock Beck: the ditch is 1m
deep and 10m wide and the bank 12m wide and 2m high. At the extreme western
end, however, the bank turns north, with the ditch now on its west side, down
the scarp towards Cock Beck. Excavation and geophysical survey in advance of
construction works for the A1 Aberford By-pass, have shown that the monument
survived below ground further west, beyond where it is visible as a surface
feature, up to the edge of the culvert carrying Cock Beck under the Aberford
By-pass. Evidence for two major ditches was found, one aligned south east to
north west, probably continuing the line of the known north west aligned
section of the South Dyke, the other a probable palaeo-channel running roughly
parallel to the present course of the Cock Beck. Both these ditches were
destroyed by construction works for the Aberford By-pass and are not included
in the scheduling.
In the central part of South Dyke, east of Woodhouse Moor Rein, the earthwork
survives only as a cropmark, but significant archaeological deposits will
remain below ground.
At the eastern end of South Dyke the ditch has been filled in with material
from the bank, with the result that the ditch appears as a level area with a
slight scarp to its south. The bank appears as a stony break of slope on the
north side of the ditch. Under trees growing in the bank, the bank survives as
an upstanding feature.
Woodhouse Moor Rein is visible as a substantial earthwork with a ditch at its
south west side, running south east from Cock Beck to Lotherton Cottages. At
its northern end, approximately 25m south of Cock Beck, the bank is about 0.5m
high and the ditch 0.5m deep.
South of Stocking Lane the bank is very substantial, some 16m wide and 5m
high, with a ditch 9m wide and 2m deep. South of Collier Lane, the bank and
ditch are again substantial, the bank being 13m wide and 1.5m in height and
the ditch about 7m wide and 1.7m deep.
While those parts of the Aberford Dykes lying north of the Cock Beck are well
positioned to have repelled invasion from the south, South Dyke appears not to
have been as well located as it has a steep slope to the north down to the
Cock Beck and higher ground to the south. Despite this poor defensive
position, the earthwork does appear to face south. South Dyke appears to have
been superceded by the Woodhouse Moor Rein, which is in a stronger position.
All walls, fences, septic tanks and road surfaces are excluded from the
scheduling, although the ground beneath these features is included.

MAP EXTRACT
The site of the monument is shown on the attached map extract.
It includes a 2 metre boundary around the archaeological features,
considered to be essential for the monument's support and preservation.

Source: Historic England

Reasons for Scheduling

The Aberford Dykes are substantial linear earthworks situated in North and
West Yorkshire, east of Leeds. They lie north and south of Cock Beck with the
modern village of Aberford at their approximate centre.
They are visible as rock-cut ditches and banks. Most of the earthworks run
approximately east-west. The ditch is on the south side of the bank and some
parts of the earthworks have an additional counterscarp bank on the same side.
The earthworks north of Cock Beck (including sections known as The Ridge,
Becca Banks and the earthwork at Field Lane) mostly occupy commanding
positions at the top of the scarp and may once have formed a single boundary.
The earthworks south of Cock Beck include the South Dyke which occupies the
top of the scarp above the beck and, crossing it, Woodhouse Moor Rein,
running north east-south west along a low rounded ridge.
The Aberford Dykes have been identified as defences of the British kingdom of
Elmet against the Anglo-Saxons in the late sixth and early seventh centuries,
or as boundaries to defend the Anglo-Saxon kingdom of Deira against the
Mercians in the seventh century AD. They have also been interpreted as dykes
built to defend the territories of the Brigantes against the advance of the
Roman Empire in the first century AD. There is no documentary evidence for the
date of the Dykes, however, and firm archaeological dating evidence is sparse.
They may not all belong to one period but relate to a number of different
events. The style of construction has parallels in both the Roman and the
early post-Roman periods. Excavation at Field Lane retrieved Roman period
pottery from deposits associated with the silting up of the ditch. It is
therefore likely that, here at least, the ditch was open during the Roman
period.
The size and extent of the Aberford Dykes imply a considerable expenditure of
time and labour, suggesting a degree of social organisation at the time of
their construction and a strong concern for territorial control, whether
military, organisational or symbolic. All known lengths of the Aberford Dykes
where significant archaeological deposits are likely to survive are considered
to be nationally important.

The linear earthworks known as Woodhouse Moor Rein and South Dyke, part of the
Aberford Dyke system survive well, and will preserve significant
archaeological information about the Roman and post-Roman periods in this
region.

Source: Historic England

Sources

Books and journals
WYAS, , A1-M1 Link Road, (1997)

Source: Historic England