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3 Earthworks
The disposition of a series of major linear earthworks (shown on the map) within
the region, in particular the Aberford Dykes and Grim's Ditch are considered
to have possible associations with territorial conflicts of the period. The
Aberford Dykes, to the east of Barwick, considered to be some of the most
impressive monuments in Yorkshire comprise 'The Ridge/Becca Banks', 'South
Dyke' and 'The Rein', the overall complex totalling 4½ miles in length.
Grim's Ditch, a linear bank and ditch, extends for about 5½ miles in a
north-south alignment, from near the River Aire at Swillington, bypassing
Temple Newsam, Colton and Austhorpe, to cross Whinmoor and beyond. Both
series of earthworks are scheduled ancient monuments.
The main component of the Aberford Dykes is The Ridge/Becca Banks, an
extensive ditch and embankment which follows the north side of the Cock Beck
from the outskirts of Barwick across the (A1) Great North Road, to the east
of Aberford, a length of nearly three miles. This dyke is formed by a ditch,
rock-cut in places, with a stone revetted embankment rising some 25 feet
above the dyke bottom.
Becca Banks must have presented a formidable obstacle
in its original state, especially as additional heightening could have been
achieved by surmounting the bank with a timber pallisade. In fact, narrow
trenches have been revealed suggesting possible slot holes for the placement
of timber uprights, providing extra protection for defenders.
South Dyke extends for about 1000 yards along the southern edge of the Cock
Beck, being intersected by the Rein which is aligned in a south-easterly
direction and is a mile in length. Becca Banks and the Rein both face south
and the South Dyke faces north. Much of Grim's Ditch is now badly degraded
by weathering and ploughing, the best preserved sections having a bank some
eight feet high with a ditch varying from 30 to 40 feet wide.
The northern
length of the dyke has been obliterated by housing and other development.
The name 'Grim' is associated with many prominent earthworks. It was an
alias or by-name for the principal Norse god Woden, from whom the royal
house of Mercia claimed descent.
The origin and dating of these earthworks
is the subject of some speculation. The Rein, for instance is thought to be
not contemporary with the other elements of the Aberford Dykes, but an Iron
Age boundary dyke, with no military function. Grim's Ditch, which faces
east, and the South Dyke, which faces north, are considered by some learned
bodies, to have comprised defence works for the kingdom of Elmet against the
Anglo-Saxons in the early seventh century.
Grim's Ditch may have formed part
of the overall system of earthworks, or because of its more westerly
location, a late boundary defence line. If the main earthworks are Dark Age
in date, the centre to which they appear to strategically relate is Leeds,
lying directly behind Grim's Ditch. It is hoped that further research will
eventually reveal the history of these impressive ancient monuments.
4 Village Place Names
There appears to be no consensus of the origin of the regional name 'Elmet';
although considered to be British, its derivation remains obscure. The affix
has been identified with the Welsh 'Elfed', the name of a cantred, or county
division in Carmarthen, and possibly based on an old Welsh tribal name. A
popular alternative of uncertain concept is the meaning 'elm-wood'. In
addition to Barwick, and Sherburn, the 'in-Elmet' affix applied, at one
time, to the West Yorkshire townships of Burton Salmon, Clifford, High
Melton, Kirkby Wharfe, Micklefield, Saxton, South Kirkby and Sutton (see
Map).
It is significant that practically all save one of these 'in-Elmet' place
names are located on, or in the vicinity of a narrow north to south aligned
band of Magnesian Limestone outcrop of the Permian Series, centred some
twelve miles east of Leeds. This strip of low-lying limestone, extending
southwards from the Ripon area, comprises terrains of well-drained loamy
soil and abundant springs and water courses, providing desirable conditions
for sustaining early settlements. The western margin of the slightly raised
escarpment would also be adaptable for defensive purposes.
At its most powerful, Elmet is thought to have extended some distance
eastwards but the above place name evidence suggests that, for quite some
time the strip of Magnesian Limestone formed the eastern division between
the Britons of Elmet and the Anglo-Saxons, who were able to establish their
settlements up to but not beyond this boundary.
Place names with the element 'inga/ingas', 'ingaham' or 'ham', generally
taken as an indication of early seventh century Anglo-Saxon settlement, e.g.
Collingham, Bramham, Ledsham, are found to roughly coincide with the
geographic distribution of the 'in-Elmet' place names.
5 Archaeology
Whilst there is evidence that Elmet was a realm of some importance at
the height of its powers, practically no archaeological material originating
from the region, other than the earthworks, has been discovered.
However a link with the former kingdom has been traced as far away as the
Llyn peninsula in north-west Wales. A two-line Latin inscription on a rough
stone now preserved in Llanaelhaearn church (about six miles north of
Pwllheli) reads: "ALIORTUS ELMETIACO HIC IACET" - recording that
Aliortus, the Elmetian or man of Elmet, lies here. Hugh Hawkins, a member of
the Historical Society, visited the church in 1991 and photographed the
unique inscription.
This early Christian memorial stone, ascribed to the late fifth or sixth
century, was unearthed from a field near the church, known as the Gardd-y-Saint
(the Garden of the Saints) and set into the west wall of the church.
A particular aspect of the inscription is the correct grammatical spelling
of 'IACET', thus not only are the newcomer's remains authentically
commemorated but due recognition is given to his distant Celtic homeland of
Elmet.
6 Christianity in Elmet
Elmet is believed to have been of Christian faith at the time of the
English occupation, with established religious centres, which continued to
be used as church sites. Bede apparently knew there were (or had been)
British Christians to the west of Northumbria, and that Elmet contained 'loca
sacra' or holy places, "...if only as despised village churches of
wood".
A guide to potential early church sites are those containing the element 'eccles'
(from the British 'egles' - a church) - and used in Anglo-Saxon place names
referring to religious sites or establishments. All the seven 'eccles' place
names in the historic county of Yorkshire fall within the region of Elmet.
They are; Eccleshill, 'Ecclesdo' in Kirkheaton, Exley in Southowram, Exley
Head in Keighley, Eccles in Haworth township, Ecclesgrass Head in Horsforth
and Great Eccles in Allerton.
[Other 'eccles' in South Yorkshire are: Ecclesfield north of Sheffield
and Eccleshall, west of Sheffield. There is an Iccles Near Templeborough
Roman Fort at Rotherham - RW.]
The early British frequently adopted an oval shape for the churchyard, and
All Saints Parish Church at Bramham is the classic example of this form. The
height of the graves above the adjoining road suggests burials over a long
period, with the site being successor to earlier religious establishments.
An indication of Elmet's Christianity is gleaned from the story of the
dedication of Ripon Minster in AD 670/671 (some 50 years after the conquest
of Elmet). Rev. Colman quotes from Bishop Browne's 'Lessons from Early
English Church History' that "Wilfrith then read out a list of places
which had formerly been occupied by the British clergy, and of the lands
which had been given to the Church in days even then long gone by. If
therefore, here in our Elmet in the seventh century, men could point out
ancient possessions of the Church, we can realize how long and firmly
Christianity had been established in this region".
7 Elmetian Sub Kingdoms
There are several small 'sub kingdoms' in the southern part of Elmet
that can be recognised by the close grouping of place names. They are:
'Balne' with Balne, Balne Moor, Thorpe in Balne, and possibly
Barnsdale. All are on the edge of a marshy area north of Doncaster. The area
probably takes it name from the ancient spa at nearby Askern. Latin balneum
meaning bath'.
'Meisen' with Misson, Misterton, and the now dry lake of Meisen
near Wroot in the marsh area south of Hatfield Chase.
'Morthen' to the south of Conisborough with Morthen, Brampton en
le Morthen and Loughton en le Morthen.
Close by to the south of Tickhill there is 'Lindrick' with
Carlton in Lindrick. To the north of Castleford there is the district of 'Led'
with, Ledsham, Ledstone, and possibly Leeds.
There are a group Anglo-Saxon villages near the river Aire north of
Pontefract taking their name from the people of Friesia,
they are 'Fryston', Water Fryston. Ferry Fryston, and Monk Fryston.
This area is on two sides of the river so there must have been a ferry,
hence the name Ferry Fryston - RW.]
References
West Yorkshire; An Archaeological Survey to AD 1500 M L Faull
& S A
Moorhouse (1981)
Roman and Anglian Settlement Patterns in Yorkshire M L
Faull (1974)
Early Territorial Organization in Gwynedd and Elmet G R J Jones (1975)
Anglo-Saxon England F M Stenton (1971)
Place Names of The West Riding of Yorkshire A H Smith (1928)
Aberford Dykes; the first defence of the Brigantes? Leslie Alcock (1954)
Yorkshire Abbeys and the Wool Trade Herbert E Wroot
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