Near Moor is a moor on the western margins of the Cleveland Hills. The moor is at its highest in the north-east where it meets the wooded escarpment edge of the Cleveland hills, it then slopes gently southwards towards Crabdale. Near moor is bounded by Far Moor To the East, Pamperdale Moor to the South and the valley of Scarth Nick and Scarth Wood Moor to the west.
The moor is managed for grouse shooting. The vegetation of the moor is predominantly heather with patches of moorland grasses and sedges.
The rocks here are mainly Jurassic Sandstones, formed 170 million years ago in shallow estuaries and deltas. To the north, below the escarpment edge, there are many old jet workings. Blocks of ‘White Flint’ can be found on the moor-top.
Both Near Moor and the adjacent Scarth Wood Moor were used by the people of the Bronze Age, there are the remains of ancient walls, enclosures, trackways and cairns dotted across both moors.
There are a number of cup-marked rocks on the moor, all are very weathered and barely recognisable.
There are the remains of quarries on the margins of the moor, local stone masons also used the prehistoric walls as a source of stone.
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.
Early Man in North East Yorkshire. Frank Elgee. 1930
Old Roads & Pannierways in North East Yorkshire. Raymond H Hayes. 1988
We took a drive up to Northumberland to visit the most northerly English Stone Circle, Duddo aka The Singing Stones aka The Women.
Whilst in the area we dropped in at a couple of Prehistoric Rock Art sites. First stop was Roughting Linn where ate our lunch down besides the lovely waterfall. We then walked through the bluebell-clad ramparts of the ancient promontory fort to the large outcrop in the woods. The Fell Sandstone outcrop is covered in Prehistoric rock carvings and is the largest carved rock in Britain. The most of the carvings have been placed around the edges of the outcrop and have been compared to Irish Passage Grave Art.
This part of Northumberland is littered with Prehistoric Rock Art sites, most have wonderful views over the nearby fertile valleys. Many sites are intervisible with each other, quite a few also have nearby earthworks which have been interpreted as Iron Age in date. The carvings themselves are thought to be Neolithic/Early Bronze Age in date, the relationship between the carvings and the earthworks is not fully understood but it does indicate that these sites had a degree of continuity lasting for a considerable period of time.
We headed over to Weetwood Moor to check-out the carvings on the outcrops there before moving on to Chattonpark hill and the wonderful Ketley Crags, a Prehistoric Rock Shelter, its floor covered in deep cup and ring carvings.
On such a night the hills dissolved
And re-assembled in a shifting mist,
Numb with moonlight’s touch.
We learnt that silence was not hostile,
Took upon ourselves its deepest strength
Waiting for dawn’s layered sun.
A moon that placed
As crow’s shout cracked the sky
Fled from the triggered bird-song
Hesitant, then loud.
Before our eyes, a second birth,
A new-created universe,
Green and blue and gold.
Fluted stones whose shape had shifted
With emitted heat
From bearded barley heads,
Buried to the hips,
Reclaimed their circle and identity,
Guarding and inviting
As the sun’s diurnal course
Played a slow game
With shadow shapes
Time and time and time again.
Solstice: Duddo by Stan Beckensall from Northumberland Power of Place. 2001