In common with most people I feel as though many aspects of my life have been on hold for the past 12 months. My list of places to visit gets longer and longer. Now that lockdown is easing I seem to have a mental log-jam of what to do and what to see.
I have been planning on visiting the Cross Dyke of Horn Ridge for quite some time as it is one of the few local dykes that I haven’t visited, once again, it was a chance online conversation with a friend that spurred me into action.
The sun was shining, the forecast was giving out wintery showers, this was perfect for me, half decent weather and less chance of meeting anyone on the moor-top.
I drove down to Farndale and walked up the keepers track that runs up the side of Monket House Crags. The track is not too steep and takes you through an area covered in spoil heaps from the 19th century jet workings. When I started walking the sun was shining, within a few minutes a wintery squall blew in from the north leaving a dusting of snow on the hillside. The squall was intense but short lived, this became the pattern for the rest of the day.
I followed the track south, along the gentle rise of Horn Ridge. From the high point, the land begins to gently slope down to the south, the eye is drawn along the valley of the River Dove to the dale end with the moorland above Hutton Le Hole and the Vale of Pickering in the far distance.
As you walk down towards the very obvious earthwork you become very aware that you are on a narrowing promontory of moorland with the fertile dale on either side, hemmed in by the dark domineering presence of Rudland Rigg to the East and Blakey Ridge to the West. As you near the Dyke you can see through the central gap to a fairly level area with the barrow beyond, the effect is quite striking.
The Dyke itself runs the full width of the upland, terminating where the land drops off at either end. Its total length is approximately 300m.
Approaching it from the north it appears to be quite an impressive earthwork as a deep ditch has been dug along its whole length. When viewed from the south it appears less imposing.
A section of the Dyke was excavated by Raymond H. Hayes. He was unable to find any evidence that might give a date to the earthwork. He observed that with the ditch ‘its builders did not cut the rock as in Iron Age or Roman ditches.’
There are a couple of stone settings within the dyke on the south side but these look like a modern shelter or grouse butt and a trap built by keepers to catch small mammals. These moors are not a friendly place for any creature that threatens the grouse population. Last year 5 dead Buzzards were discovered hidden beneath a rock just 3km north of the Dyke.
Walking south towards the barrow, a squall blows in, the views are lost.
The barrow is a very sad sight. It is quite large, approx 10-15m diameter. It is hard to fully gauge its dimensions as it is in a terrible state of repair. The scheduling entry for the monument mentions ‘a central excavation hollow around 4m by 2m, with a second 1m diameter pit in its west side.’ The keepers have also recently built a trap into one of the holes in the mound.
I took a walk along the western edge of the ridge. There are reports of cairns and hut circles in this area. I was just starting to spot them when a heavy snow storm started. My mind turned to driving up the steep bank to Blakey Ridge. Under normal circumstances I wouldn’t mind being trapped in Farndale but with the current conditions i.e. the Feversham Arms being closed, I decided that the western edge of Horn Ridge was one for another day and turned for home.
‘Evidence for prehistoric salt production in Britain has been confined to the Bronze and Iron Ages. This article presents new evidence for Early Neolithic (3800–3700 BC) salt-working at Street House, Loftus, in north-east England.’
Thanks to Jon Purday for pointing me to the article. Jon’s comment, ‘Extending the locality’s chemical processing even further back to a Neolithic salt works at Loftus.’
A week or so ago I took a walk across the Bran Sands with my friend Graham Vasey. Graham was filming the area and I was trying to capture some field recordings. Unfortunately it was blowing a gale, the wind making it almost impossible to capture the sounds of the sands.
The other day the weather was beautiful and the winds were light so I returned to the Gare to try and make some recordings. The Gare was busy with people coming and going, constant traffic noise replaced wind noise, a conspiracy between the natural and human worlds.
The riding school is currently awaiting demolition to make way for a new housing development. The main building was originally built in 1914 as an infectious diseases hospital with separate male and female wards.
The Prehistoric Round Barrow on the margins of the woods at the top of Patterson’s Bank is currently being destroyed by cyclists. The Barrow is one of few that survive in this area. It is a Scheduled Monument and is legally protected. It is also a burial monument and contains the remains of our Prehistoric ancestors. Action is urgently required to prevent the destruction of this beautiful monument.
A recent online conversation with a friend re-sparked my curiosity about the Tank Road. It’s an area that I’ve visited many times over the years, I’ve always felt that it was an important place but I’ve never fully got to grips with it. So I decided to walk it and try to pull together a description of the area.
I’ve always known it as the Tank Road or Old Tank Road, presumably it got this name from when it was used as a Tank training ground during WWII. The road itself is only 3.5km long, it runs between the main north-south roads to Castleton and Danby. From east to west, the road starts on the main north-south road to Danby and then crosses Gerrick Moor, Tomgate Moor and Middle heads where it meets the Castleton Road at White Cross on Three Howes Ridge.
On walking the road it becomes apparent that it was a busy route in the past, there is evidence of a number of sunken trackways, following the line of the road and joining the road from other routes, this becomes more obvious when you look at the LIDAR images of the area.
Regarding the origins of the road itself. There have been two excellent books written on the trackways of the North York Moors, Old Roads and Pannierways in North East Yorkshire by Raymond H. Hayes and Trods of the North York Moors by Christopher P. Evans. Hayes regards the route as possibly part of the Pannierman’s Causeway from Castleton to Staithes. Evans thinks it is part of a trod from Liverton Moor to Commondale. I suspect this route may have its origins in Prehistory.
Walking from east to west.
The road starts at the bend of the road that runs from the A171 to Danby where there is a small parking area. I definitely would not recommend trying to drive along the road. The road crosses a number water courses, the boggy areas have been filled with building rubble, it’s not unusual to find parts of cars on the side of the road.
The most prominent monument at the start of the road is a large Barrow, one of a group known as Robin Hood’s Butts. Danby Beacon can be seen in the distance in the image above .
The next group of monuments lie just south of the road comprising of a barrow and an embanked circular feature known as an Enclosed Urnfield. The enclosure and barrow date to the Bronze Age. The enclosure was a place where the cremated remains of the dead were placed, often in small pottery vessels. This type of monument is quite rare, they are generally only found in Northern England and Southern Scotland. Only 50 examples are known, 3 of which are within a few minutes walk of the Tank Road.
Photographing many of these prehistoric monuments is quite difficult, most of them are fairly low-lying features, covered in heather on a heather moor. The vegetation is quite low at the moment so this is probably the best time of the year to visit and once you get you eye in they are not to difficult to spot. I’ve included a few Open Access LIDAR images as they give a better idea of the form of the monuments.
To the north of the road is a large standing stone. The stone is unusual as it is ‘L’ shaped and its surface has fossil ripple marks on its surface. There are no obvious outcrops of stone on this part of the moor, but there is an outcrop with similar ripple marks on the western flanks of Siss Cross Hill just under 2km away. Perhaps this was the source of the stone.
In the top image, behind the standing stone, you can see the large burial mound of Herd Howe in the middle distance and beyond that Freebrough Hill. Just below Herd Howe is an enclosure that dates to the Iron Age. I have previously written an account of the enclosure, Herd Howe and the nearby Cross Dyke.
On my last two walks along the road I have seen quite a number of geese. I presume they are overwintering here. On my last visit this pair flew towards me honking, circled me and then headed back to Dimmingdale.
Leaving the road I followed a track south to have a look at Siss Cross. The cross is a crude unworked upright stone, it may be a replacement for the original cross. Running down the hill from the cross are a number of sunken trackways, perhaps the cross was a route-marker. Back in the 19th Century local Antiquarian J.C Atkinson discovered what he described as a flint tool making site just south of Siss Cross. He collected enough flint tools and debitage to fill ‘half a fair sized fishing basket’. The flint tools are thought to have been made by Mesolithic hunter gatherers. The site would have been a good place for a hunting camp, it is well drained and has a large viewshed, even on a muggy day I was able to look along the Esk Valley and make out the distinctive profile of the RAF site on Fylingdales Moor over 21km away.
I headed back to the Tank Road via the Trig point on the top of Siss Cross Hill. There is another Enclosed Urnfield with associated Barrows here. Unlike the previous enclosure this one is oval in shape and quite large 38x20m. Interestingly, the enclosure and the two associated barrows are aligned on the western-most Barrow of the Robin Hood’s Butts group. This alignment is also roughly the direction of the Midsummer sunrise and Midwinter sunset. The enclosure is also intervisible with the third Enclosed Urnfield on Moorsholm Rigg.
I walked back onto the road from Siss Hill and followed it down into Ewe Crag Slack. The slack is a former glacial drainage channel and is generally quite boggy. The keepers and the farmer struggle to keep the road passable down here, the place is a jumble of boulders, concrete posts and deep muddy ruts.
Ewe Crag Slack is a significant location in the study of prehistory on the moors as it was one of a number of places where Paleoenvironmental pollen cores were taken from the peat and the sediments below it. The data from Ewe Crag helped provide evidence that the people who lived here during the Mesolithic period may have been actively managing the land. The pollen cores showed evidence of forest destruction and subsequent soil erosion, this combined with charcoal deposits suggests that people may have been creating forest clearings much earlier that was previously thought.
I noticed this boulder by the side of the road. The boulder has been broken but you can see that it’s original form was rounded. The rock type looks like a fine grained igneous rock, basalt or andesite. I presume it is a glacial erratic. It’s curious because less than a kilometre away, at Dimmingdale, is a barrow that was excavated in the 19th Century by J.C. Atkinson, the same antiquarian who found the Siss Cross Flints. Atkinson wrote that the barrow contained ‘blocks of basalt from the Cleveland Dyke’. It is possible that the stones came from the Cleveland Dyke, the nearest potential outcrop that I’m aware of is at Scale Cross 4.2km away, where it was quarried in the modern era. I wonder if the barrow stones may have originated closer to home as glacial erratics washed-down to Dimmingdale when the ice began to melt. One for further research.
Walking the final section of the road to White Cross my camera battery died. The final 2 images were taken when wandering the road in 2017, they are a Danby-Moorsholm guidestone & White Cross.
