Lilla Howe

My friend Graham Vasey and I took a walk up to Lilla Howe, Graham was wanting to have a look at Lilla Cross and make some images as part of his ongoing Dainn series, exploring landscape and folklore.

Lilla Howe is classified as a Bowl Barrow, a large burial mound built of turf and stone. It dates from the Bronze Age and is part of a chain of barrows that run from the southern edge of the Esk valley to the Tabular Hills. This and other lines of Barrows on the moors may once have been used as boundary markers, defining the territories or estates of different groups, the mounds of the ancestors, perhaps indicating legitimacy and continuity of ownership. This use continues today as many of the more prominent moorland barrows continue to define modern boundaries.

Lilla Howe is a very ancient and important landmark, it marks the junction of four ancient parishes, Allerston, Fylingdales Moor, Goathland and Lockton. This boundary was first recorded in AD 1078 but may be much older.

The stone cross has a ‘G’ carved into its north face, this signifies Goathland, there is a ‘C’ on the southern face which is thought to represent Cholmley. The Cholmley family took ownership of the land in the sixteenth century following the Dissolution of the Monasteries, the estate had previously been owned by Whitby Abbey.

It was also a junction of two significant trackways running south from the coast to the Vale of Pickering, The Old Salt or Fish Road and the Pannier Man’s Way. These tracks are now lost beneath RAF Fylingdales. Lilla Howe continues to be used as a boundary marker, it is a junction for a modern parliamentary constituency boundary.

This section of the moors is also significant as it is the point where the moorland becks and streams run to the south. The northern moors are drained by two major rivers, The Esk and the Leven. The becks and rivers of the southern moors drain into the River Derwent. Derwent Head, the source of the River Derwent is less than a mile south of Lilla Howe.

Lilla Cross sits on top of Lilla Howe, it is one of a few surviving, intact moorland crosses. The tradition is that the cross was erected as a memorial to Lilla, a lord at the court of King Edwin.

The prehistoric burial mound was re-used during the early Medieval period, two Gold discs and four silver strap-ends were found in the mound, these items were used to re-enforce the tradition that this was the burial site of Lilla, therefore dating the cross to the seventh century. Unfortunately the objects found in the mound are Scandinavian in design and date to the tenth century.

Bede’s account of Lilla

…there came to the kingdom an assassin whose name was Eomer, who had been sent by Cwichelm, King of the West Saxons, hoping to deprive King Edwin of his Kingdom and his life. He came on Easter Day to the King’s hall which then stood by the River Derwent. He entered the hall on the pretence of delivering a message from his lord, and while the cunning rascal was expounding his pretended mission, he suddenly leapt up, drew the sword from beneath his cloak, and made a rush at the King. Lilla, a most devoted thegn, saw this, but not having a shield in his hand to protect the King from death, he quickly interposed his own body to receive the blow. His foe thrust the weapon with such force that he killed the thegn and wounded the King as well through his dead body.

Etymolgy – Rivers

Derwent – Derived from British derva ‘oak’ Welsh derw &c. The name means ‘river where oaks were common’.

Esk – A British-river name identical with Axe, Exe and with Usk in Wales and Isch and others on the continent. British Isca became Esca, whence OE Esce and Aesce, which gave Esk and with metathesis Exe and Axe…and probably comes from pid-ska or pit-ska the root being pi- in Greek piduo ‘to gush forth’.

Leven – A British river-name identical with Libnios c150 Ptolemy (in Ireland) and Llyfni, Llynfi in Wales. The name may be derived from the adjective for ‘smooth’ found in Welsh llyfn.

Sources

Early Man in North East Yorkshire. Frank Elgee. 1930

Old Roads & Pannierways in North East Yorkshire. Raymond H Hayes. 1988

Lilla Cross on Lilla Howe, Fylingdales Moor. Historic England

Map reproduced with the permission of the National Library of Scotland

Bede. The Ecclesiastic History of the English Nation. 1949

The Concise Oxford Dictionary of English Place-Names. Eilert Ekwall. 1974

Blackpark Standing Stone & Cross Dyke

Boundaries, Pits & Zeppelins

I’ve been interested in the notion of boundaries recently so decided to combine this with a wander over Easington High Moor following the route of an eighteenth century perambulation that I found posted online a few years ago.

Manorial perambulations are an ancient practice, the boundaries of the district are walked to confirm ownership and ensure that no territorial infringements have taken place. What is interesting about this route is that it continues to be used as a formal boundary to define at least 13 different regional, county, unitary authority, parliamentary, and parish territories.

The route starts on the little-walked western section of the moor beside the Danby Road at a stone called Harlow Bush, the perambulation states that it is also called Harlot-Busk,  Harlot-Thorn, otherwise Harlow-Thorn, otherwise High- Thorn.

The early OS map shows Harlow Bush and High Thorn as two separate stones. I was unable to find the latter stone but there has been much road widening since the map was drawn so the stone has either been removed or is lost in a mass of gorse and brambles at the junction between the Danby and Moors road. it doesn’t take the moor long to swallow-up the fallen.

A number of the stones have dates carved into them, mainly from the early 1800s and post-date the enclosure of the moor in 1817. The names of the perambulation sites imply that prominent stones and trees were used as boundary markers, this was formalised during the 19th century by the erection of many of the boundary stones that we see across the northern moors today. Some of them, especially the earth-fast stones, probably pre-date this period.

Others stand beside older stones and bear their names.

I cross a marshy section and come across a long section of cast iron pipe. The 40″ diameter pipe is a remnant from an attempt to build a railway across the moor. The railway, known locally as Paddy Waddell’s Railway, was supposed to be built to carry iron ore from the mines at Skelton and Brotton to the ironworks of Grosmont. The project was halted due to lack of funds and a recession in the iron trade

The Great Dinnod stone has fallen, beside it is a concrete post marked GT on one face and DT on the other. Further along the low ridge is the Little Dinnod, still standing.

Beneath the Great Dinnod ridge is a beautiful low grassy valley, it’s a marked contrast to the heather moorland that surrounds it. The valley terminates at the Mellowdale Slack. As I walk along the slack, dozens of tiny birds fly out around me and land in the trees. It’s a magical place. I stop and sit in the shade of a beautiful Rowan listening to the chirruping birds and watch dragonflies busying themselves along the valley.

Refreshed, I climb up onto Middle Rigg to have a look at a form of Prehistoric boundary marker, a Segmented Pit Alignment or SEPA. Double pit alignments have been found in other parts of our islands but this particular class of monument is unique to the North York Moors. This definition is taken from the excellent official blog for the North York Moors National Park

A SEPA earthwork however is made up of two or three pairs of pits inside two parallel enclosing banks largely made from the spoil from the pits, these are generally in what appear to be conjoined segments. The segmentation suggests development over time rather than a linear structure created in one go as a land boundary.

In each case the SEPAs appear to be aligned with nearby Bronze Age barrows (burial mounds), which suggest the SEPA are Bronze Age too and could have had a related ritual purpose. The alignment of all the SEPAs is north-west to south-east. This alignment seems to have taken precedence to any alignment with the barrows. The parallel banks were oddly low, which means the earthworks were not prominent in the landscape when they were constructed, unlike the barrows.

Most of the pits are filled with grasses and sedges, the low enclosing banks are visible where the heather has been burned-off.

One of the pits has an excavation trench running across the pit and bank. This may have been left from Canon Atkinson’s 1848 excavation where he interpreted the pits as the remains of an ancient British pit village.

There is another line of pits close to the SEPA, this has a much more recent history and has nothing to do with boundaries. The LIDAR image above shows the pit alignments and barrows of Middle Rigg. It also shows a curving line of four pits, these are bomb craters caused by the dropping of bombs during a Zeppelin raid on the North Eastern coast in May 1916. A full account of the raid can be read here

I walk over the rigg to the Long Stone. This beautiful monolith with it’s strange disc is probably one of the tallest stones of the Northern Moors and is one of my favourites. Is it prehistoric? I don’t know but would like to think so. It is also a fitting end point for my wander across this section of this lovely moor.

Sources

Maps and Lidar image reproduced with the permission of the National Library of Scotland

The Official Blog of the North York Moors National Park

Zeppelin Raids Gothas and ‘Giants’, Britain’s first blitz by Ian Castle

The Sheep Fold by Bryan Hoggarth

Rey Cross ii

OE stan ‘stone, stones’ is a very common pl. el. It is used alone as a pl. n. in STAINES, STEANE, STONE, where a Roman milestone or some prominant stone of another kindmay be referred to.

The Concise Oxford Dictionary of English Place Names. Eilert Ekwall. 1959

I recently took a trip over the Pennines to Cumbria. On the way home I stopped on Stainmore to have a look at Rey’s Cross. The Cross is located in a lay-by beside the A66. The A66 crosses the Pennines through the Stainmore Gap, a Pennine pass that was created by the flow of ice sheets during past glacial periods.

Historically, This part of Stainmore has always been important. The moor is rich in late Prehistoric remains. It was also the site of a large Roman marching camp, within the ruins of the camp is a wrecked prehistoric stone circle. Legend has it that the stone cross was raised as a memorial to Eric Bloodaxe, the last king of York, who was slain on the moor in 954.

The cross, situated near the highest point of Stainmore, is close to an ancient county boundary, is a weathered shaft set into a substantial stone base and is thought to date to the early anglo saxon period. The name`Rey’ is thought to have been derived from the Old Norse element `hreyrr’ which can be taken to mean a heap of stones forming a boundary.

One of the earliest references to the stone is from The Chronicle of Lanercost where it is call ” Rer Cros in Staynmor ” The chronicler states that it was set up as a boundary marker. The boundary was between the Westmoringas and the Northumbrians, the Glasgow diocesan border, before that it marked the border between the Cumbrians and the Northumbrians.

The antiquarian William Camden tells us ” This stone was set up as a boundary between England and Scotland, when William (the Conqueror) first gave Cumberland to the Scots.”  Camden was incorrect, at the time of the Norman conquest much of Cumberland was already under Scot’s rule. The historic county of Cumberland was not established until 1177, however the stone could still have marked the boundary of the territory.

The A99 was widened in the early 1990’s so in 1990 the stone was moved from the south side of the road to its present site on the north side. An archaeological survey and excavation was undertaken as part of a wider archaeological project, sadly no burial was found beneath or around the stone.

What fascinates me about this stone is that it marks a place that has been significant to the people of our islands for thousands of years. The people of the Neolithic period used this as route way between the east and west coasts. Later, the people bronze age erected a stone circle close to the site. Later still, the Romans heavily fortified road to guard the legions marching between Catterick and Penrith and it has remained the primary northern trans-pennine link ever since.  A hundred or so metres west of the stone is the modern east/west boundary between Cumbria and Durham and the route was also once the medieval border between Scotland and England. East meets west, north meets south all within sight of the weather-beaten old stone.