Roseberry Common

Downs, Moorland in Yorkshire

England

Roseberry Common

Roseberry Topping The crowded summit of Roseberry Topping  seen from the quieter and 4 metres higher trig point on Guisborough Moor.
Roseberry Topping Credit: T Eyre

Roseberry Common is a picturesque area located in North Yorkshire, England. Situated on the edge of the North York Moors National Park, it encompasses both downs and moorland landscapes, offering diverse natural beauty and recreational opportunities.

The common is primarily known for its iconic landmark, the Roseberry Topping. This distinct hill, standing at 1,049 feet, is often referred to as the "Yorkshire Matterhorn" due to its resemblance to the famous Swiss mountain. It attracts hikers and climbers from far and wide, providing stunning panoramic views from its summit.

Aside from the Roseberry Topping, the common boasts an array of rolling hills, heather-clad moorlands, and lush grasslands. These landscapes are home to a variety of wildlife, including birds, rabbits, and deer, making it a popular destination for nature enthusiasts and photographers.

For outdoor enthusiasts, Roseberry Common offers an extensive network of walking trails and bridleways, allowing visitors to explore the area at their own pace. These trails cater to all abilities, from gentle strolls to challenging hikes, providing something for everyone.

The common is also steeped in history, with remnants of Iron Age settlements and ancient burial mounds scattered throughout the landscape. These archaeological sites add an intriguing dimension to the area, offering a glimpse into its rich past.

Roseberry Common is easily accessible, with nearby parking facilities and public transport links. It has become a beloved destination for locals and tourists alike, offering a tranquil escape from the hustle and bustle of everyday life and a chance to immerse oneself in the natural beauty of Yorkshire's downs and moorland.

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Roseberry Common Images

Images are sourced within 2km of 54.507422/-1.1025116 or Grid Reference NZ5812. Thanks to Geograph Open Source API. All images are credited.

Roseberry Topping The crowded summit of Roseberry Topping  seen from the quieter and 4 metres higher trig point on Guisborough Moor.
Roseberry Topping
The crowded summit of Roseberry Topping seen from the quieter and 4 metres higher trig point on Guisborough Moor.
Dikes A view taken from the top of Cliff Rigg, the farm on the right is Rye Hill, which was on the south-eastern boundary of the ancient open field system known as ‘Wood Field’. Beyond was the common land, formerly ‘Dikes’. Just a hawthorn hedge, probably dating from the time of enclosure in 1658, separates the two.
Dikes
A view taken from the top of Cliff Rigg, the farm on the right is Rye Hill, which was on the south-eastern boundary of the ancient open field system known as ‘Wood Field’. Beyond was the common land, formerly ‘Dikes’. Just a hawthorn hedge, probably dating from the time of enclosure in 1658, separates the two.
Newton Moor A collection of photographs taken around midday by Geographers from all over Britain and Ireland. 
See all the images on the map: <a title="https://www.geograph.org.uk/stuff/xmas.php?year=2021" href="https://www.geograph.org.uk/stuff/xmas.php?year=2021">Link</a>
Newton Moor
A collection of photographs taken around midday by Geographers from all over Britain and Ireland. See all the images on the map: Link
Path descending Ayton Bank This is footpath number 10.57/001, which I suspected might have been on the line of an old tramway, but I was wrong. There were old tramways serving mines in this area, but this wasn't one of them. Plenty of new tree saplings in evidence, with the area to the left pockmarked by old mine drifts and spoil heaps.
Path descending Ayton Bank
This is footpath number 10.57/001, which I suspected might have been on the line of an old tramway, but I was wrong. There were old tramways serving mines in this area, but this wasn't one of them. Plenty of new tree saplings in evidence, with the area to the left pockmarked by old mine drifts and spoil heaps.
Old spoil tips on Ayton Bank Something of a guessing game here. Are these from old alum mines, jet workings or iron mines?  Mick Garratt is the local expert and a similar photo by him describes the tips as from the old Ayton Banks iron ore mine.  I'm not so sure, as old 6" OS maps from between the 1850's and 1920's show various mining activities on this hillside. Those highest up are from Alum mines, which produce a lot of shale, but they were higher than this and probably long abandoned. The old maps show several small tips running in a line along the hillside at this level from old jet workings, and I suspect these tips are from those workings. The iron mine was a little further south in the adjoining square, so I don't think these tips are to do with the iron mining industry.
Old spoil tips on Ayton Bank
Something of a guessing game here. Are these from old alum mines, jet workings or iron mines? Mick Garratt is the local expert and a similar photo by him describes the tips as from the old Ayton Banks iron ore mine. I'm not so sure, as old 6" OS maps from between the 1850's and 1920's show various mining activities on this hillside. Those highest up are from Alum mines, which produce a lot of shale, but they were higher than this and probably long abandoned. The old maps show several small tips running in a line along the hillside at this level from old jet workings, and I suspect these tips are from those workings. The iron mine was a little further south in the adjoining square, so I don't think these tips are to do with the iron mining industry.
Gribdale Terrace The initial thought is that these must have been erected for miners in the local iron ore mine or even for the jet mining, but the dates don't seem to match. The terrace first appears on the 1913 OS map, and it seems that they were for quarrymen working in the Whinstone quarry further down the hill. The whinstone follows the long thin line of the Cleveland Dyke which runs across much of the North York Moors from Great Ayton towards Robin Hood's Bay with the best deposits at this western end. Quarrying for whinstone, largely used in road construction, carried on in this area until the 1960's.
Gribdale Terrace
The initial thought is that these must have been erected for miners in the local iron ore mine or even for the jet mining, but the dates don't seem to match. The terrace first appears on the 1913 OS map, and it seems that they were for quarrymen working in the Whinstone quarry further down the hill. The whinstone follows the long thin line of the Cleveland Dyke which runs across much of the North York Moors from Great Ayton towards Robin Hood's Bay with the best deposits at this western end. Quarrying for whinstone, largely used in road construction, carried on in this area until the 1960's.
Pinchinthorpe The Domesday Book records two manors in Pinchinthorpe.  The eastern half, centred on the modern Pinchinthorpe House (but not as far as the Pinchinthorpe Visitor Centre) and the western half comprising Pinchinthorpe Hall.

The photo shows almost the full extent of the western half. Bottom left, partially hidden by trees is Pinchinthorpe Hall. The farm on the right is High Farm. The two farms in the right distance are Spite Hall Farm and Low Farm, also part of the manor. It’s a long narrow manor, I am actually standing on the south-eastern tip.

The fields north of the A173 between the hall and High Farm contain lots of humps and bumps, the site of the medieval hamlet. The name itself, Pinchinthorpe, comes from the Norman family of ‘Pinchum’, the 12th-century holders of the manor.

The most interesting building through is Pinchinthorpe Hall, a 17th-century house which stands in moated grounds. The moated site and post medieval gardens are currently on Historic England’s Heritage at Risk register as “generally unsatisfactory with major localised problems”. The risk seems to be from gardening. The hall itself has recently been reopened as a hospitality venue.

For over 400 years the manor was in the hands of the Catholic Lee family. The family seems to have avoided holding positions of public office and this may have been because of their recusancy.

Main source: Dixon, Grace. “Two Ancient Townships – Studies of Pinchinthorpe and Hutton Lowcross”. 1991. ISBN 0 9507827 2 6.

For sources and references see my blog <span class="nowrap"><a title="http://www.fhithich.uk/?p=27311" rel="nofollow ugc noopener" href="http://www.fhithich.uk/?p=27311">Link</a><img style="margin-left:2px;" alt="External link" title="External link - shift click to open in new window" src="https://s1.geograph.org.uk/img/external.png" width="10" height="10"/></span>
Pinchinthorpe
The Domesday Book records two manors in Pinchinthorpe. The eastern half, centred on the modern Pinchinthorpe House (but not as far as the Pinchinthorpe Visitor Centre) and the western half comprising Pinchinthorpe Hall. The photo shows almost the full extent of the western half. Bottom left, partially hidden by trees is Pinchinthorpe Hall. The farm on the right is High Farm. The two farms in the right distance are Spite Hall Farm and Low Farm, also part of the manor. It’s a long narrow manor, I am actually standing on the south-eastern tip. The fields north of the A173 between the hall and High Farm contain lots of humps and bumps, the site of the medieval hamlet. The name itself, Pinchinthorpe, comes from the Norman family of ‘Pinchum’, the 12th-century holders of the manor. The most interesting building through is Pinchinthorpe Hall, a 17th-century house which stands in moated grounds. The moated site and post medieval gardens are currently on Historic England’s Heritage at Risk register as “generally unsatisfactory with major localised problems”. The risk seems to be from gardening. The hall itself has recently been reopened as a hospitality venue. For over 400 years the manor was in the hands of the Catholic Lee family. The family seems to have avoided holding positions of public office and this may have been because of their recusancy. Main source: Dixon, Grace. “Two Ancient Townships – Studies of Pinchinthorpe and Hutton Lowcross”. 1991. ISBN 0 9507827 2 6. For sources and references see my blog LinkExternal link
Cockle Scar When we look at a landscape photo it is very easy to be overwhelmed by the big picture and to miss the little features.

In centuries past, these features meant something, far more than now, and they had names.

It is these features that reveal interesting aspects of the landscape.

The distinctive change in steepness of the north-western face of Roseberry is clearly visible from the Cleveland Plain. This is a shot along the slope. Newton-under-Roseberry is the village extreme right.

And the edge on left is Cockle Scar, a name which I think most people climbing Roseberry will not be familiar with, anxious to achieve the summit.

Climb the wooden steps then the diagonal path through Newton Wood and when you get to the gate you will have crested Cockle Scar. It’s about at the 200m contour level.

The scar is formed from a seam of rock called the Staithes Sandstone Formation, which is more resistant to erosion than Redcar Mudstone Formation below it.

When the last ice age ice sheets swept along the Cleveland Plain from the north-west, the softer mudstone was more readily eroded leaving the edge.

Staithes sandstone is thinly bedded therefore not used much for building, and so not quarried.

Unlike the ‘cap’ of Roseberry which is a different sandstone, the Saltwick Sandstone Formation.

Cockle Scar is not named on the modern Tourist O.S. Maps. I haven’t come across many modern references.

The 2006 book “Roseberry Topping” is one, issued by the Great Ayton Community Archaeology Project.

Early last century, SirAlfred Pease (1857-1939) mentioned the feature in his memoires.

Is there a danger of it being lost?

For sources and references see my blog <span class="nowrap"><a title="http://www.fhithich.uk/?p=27429" rel="nofollow ugc noopener" href="http://www.fhithich.uk/?p=27429">Link</a><img style="margin-left:2px;" alt="External link" title="External link - shift click to open in new window" src="https://s1.geograph.org.uk/img/external.png" width="10" height="10"/></span>
Cockle Scar
When we look at a landscape photo it is very easy to be overwhelmed by the big picture and to miss the little features. In centuries past, these features meant something, far more than now, and they had names. It is these features that reveal interesting aspects of the landscape. The distinctive change in steepness of the north-western face of Roseberry is clearly visible from the Cleveland Plain. This is a shot along the slope. Newton-under-Roseberry is the village extreme right. And the edge on left is Cockle Scar, a name which I think most people climbing Roseberry will not be familiar with, anxious to achieve the summit. Climb the wooden steps then the diagonal path through Newton Wood and when you get to the gate you will have crested Cockle Scar. It’s about at the 200m contour level. The scar is formed from a seam of rock called the Staithes Sandstone Formation, which is more resistant to erosion than Redcar Mudstone Formation below it. When the last ice age ice sheets swept along the Cleveland Plain from the north-west, the softer mudstone was more readily eroded leaving the edge. Staithes sandstone is thinly bedded therefore not used much for building, and so not quarried. Unlike the ‘cap’ of Roseberry which is a different sandstone, the Saltwick Sandstone Formation. Cockle Scar is not named on the modern Tourist O.S. Maps. I haven’t come across many modern references. The 2006 book “Roseberry Topping” is one, issued by the Great Ayton Community Archaeology Project. Early last century, SirAlfred Pease (1857-1939) mentioned the feature in his memoires. Is there a danger of it being lost? For sources and references see my blog LinkExternal link
Ayton Banks Ironstone Mine I thought I would have a look around the Ayton Banks Ironstone Mine before the summer vegetation growth takes hold, only to find when I got home that I have already posted a photo of the old drift entrance. But that was an eternity ago, in January 2015.

Ayton Banks Ironstone Mine was the smallest of the three mines around Great Ayton, containing about 1½ million tons of rather poor quality ironstone.

It was completely surrounded by the workings of the Pease & Partners’ Ayton Mine — that’s its official name which must have led to some confusion and probably one of the reasons why locally that was called ‘Monument Mine’.

To give some comparison, in 1917, Ayton Banks Mine was producing 1,500 tons per week whereas Monument Mine was 2,100 per week.

Ayton Banks was operated by the Tees Furnace Company, which at the time also ran the Roseberry Mine.

The mine is pretty unique in that due to its constricted surface works, there was no room below the mine entrance to dump spoil below the drift entrance and so had to be transported up the slope.

Another difficulty, which Ayton Banks shared with Monument Mine, is that the whinstone dyke had to be penetrated in order to access the ore to the north of it.

Initially a branch line provided a connection to the whinstone quarry’s narrow gauge railway and thence onto the mainline sidings, but soon an aerial ropeway was constructed connecting with sidings near the foot of Cliff Rigg. The bases for these ropeway towers can be seen today in Cliff Rigg Wood.

The featured image shows a concrete bunker and behind a chute where the ironstone was tipped into the ropeway tubs. In the cutting I counted at least three bases, possibly for the ropeway or engine or boiler foundations.

One photo shows a group of boy miners with their ponies at Ayton Banks mine. Left to Right: Harold Robinson; Henry Hogben; George Williamson; George Haswell; Robert Bennison; George Bailey; Marvin Porritt.

In the photo, George Williamson seems happy, the others stare tentatively into the Edwardian camera unsure whether to smile. The ponies look quite comical under their skull caps.

The 1911 census records that Williamson was born in 1900, Hogben 1902 and Haswell 1899. So I guess the photo was taken about the mid-1910s.

In 1913, another pony boy, John Garbutt, aged just 14 so would have been born in the same year as Haswell, was killed in Ayton Banks Mine, crushed by a wagon. At the inquiry it was found that Garbutt was killed as “the result of his own improper conduct” presumably absolving the company of all responsibility.

Perhaps the lads were thinking of their lost friend.

The mine had a short operational life. From 1909, at the height of the boom years to the post-war depression in 1921.

For links, references and supplementary photo, see my blog <span class="nowrap"><a title="http://www.fhithich.uk/?p=27475" rel="nofollow ugc noopener" href="http://www.fhithich.uk/?p=27475">Link</a><img style="margin-left:2px;" alt="External link" title="External link - shift click to open in new window" src="https://s1.geograph.org.uk/img/external.png" width="10" height="10"/></span>
Ayton Banks Ironstone Mine
I thought I would have a look around the Ayton Banks Ironstone Mine before the summer vegetation growth takes hold, only to find when I got home that I have already posted a photo of the old drift entrance. But that was an eternity ago, in January 2015. Ayton Banks Ironstone Mine was the smallest of the three mines around Great Ayton, containing about 1½ million tons of rather poor quality ironstone. It was completely surrounded by the workings of the Pease & Partners’ Ayton Mine — that’s its official name which must have led to some confusion and probably one of the reasons why locally that was called ‘Monument Mine’. To give some comparison, in 1917, Ayton Banks Mine was producing 1,500 tons per week whereas Monument Mine was 2,100 per week. Ayton Banks was operated by the Tees Furnace Company, which at the time also ran the Roseberry Mine. The mine is pretty unique in that due to its constricted surface works, there was no room below the mine entrance to dump spoil below the drift entrance and so had to be transported up the slope. Another difficulty, which Ayton Banks shared with Monument Mine, is that the whinstone dyke had to be penetrated in order to access the ore to the north of it. Initially a branch line provided a connection to the whinstone quarry’s narrow gauge railway and thence onto the mainline sidings, but soon an aerial ropeway was constructed connecting with sidings near the foot of Cliff Rigg. The bases for these ropeway towers can be seen today in Cliff Rigg Wood. The featured image shows a concrete bunker and behind a chute where the ironstone was tipped into the ropeway tubs. In the cutting I counted at least three bases, possibly for the ropeway or engine or boiler foundations. One photo shows a group of boy miners with their ponies at Ayton Banks mine. Left to Right: Harold Robinson; Henry Hogben; George Williamson; George Haswell; Robert Bennison; George Bailey; Marvin Porritt. In the photo, George Williamson seems happy, the others stare tentatively into the Edwardian camera unsure whether to smile. The ponies look quite comical under their skull caps. The 1911 census records that Williamson was born in 1900, Hogben 1902 and Haswell 1899. So I guess the photo was taken about the mid-1910s. In 1913, another pony boy, John Garbutt, aged just 14 so would have been born in the same year as Haswell, was killed in Ayton Banks Mine, crushed by a wagon. At the inquiry it was found that Garbutt was killed as “the result of his own improper conduct” presumably absolving the company of all responsibility. Perhaps the lads were thinking of their lost friend. The mine had a short operational life. From 1909, at the height of the boom years to the post-war depression in 1921. For links, references and supplementary photo, see my blog LinkExternal link
View to Roseberry Topping from the A171
View to Roseberry Topping from the A171
Roseberry Topping Distinctive cone shaped summit of just over 1,000 feet above sea level, set slightly adrift of the Cleveland Hills proper.
Seen here from the village of Newton, at the western foot of the hill.
A spur from the Cleveland Way gives the National Trail walkers access to the top from the east.
Roseberry Topping
Distinctive cone shaped summit of just over 1,000 feet above sea level, set slightly adrift of the Cleveland Hills proper. Seen here from the village of Newton, at the western foot of the hill. A spur from the Cleveland Way gives the National Trail walkers access to the top from the east.
St. Oswald's Church, Newton under Roseberry Dedicated to the Northumbrian King Oswald.
Parts of the church are of Norman origin, but extensively re-constructed in Victorian times.
Grade II Listed Building
St. Oswald's Church, Newton under Roseberry
Dedicated to the Northumbrian King Oswald. Parts of the church are of Norman origin, but extensively re-constructed in Victorian times. Grade II Listed Building
The King's Head, Newton-under-Roseberry Hostelry on the main A173, near Great Ayton
The King's Head, Newton-under-Roseberry
Hostelry on the main A173, near Great Ayton
Dikes Lane Heading east into the Cleveland Hills
Dikes Lane
Heading east into the Cleveland Hills
Anglo-Saxon carved stone — “a dragon attacking a quadruped” Built into the fabric of St. Oswald’s Church suggesting the existence of a much earlier church.
Anglo-Saxon carved stone — “a dragon attacking a quadruped”
Built into the fabric of St. Oswald’s Church suggesting the existence of a much earlier church.
Rainbow over Great Ayton Moor Taken across the autumn bracken.
Rainbow over Great Ayton Moor
Taken across the autumn bracken.
Old Boundary Marker on the A173 between Pinchinthorpe Hall and Newton under Roseberry Parish Boundary Marker in the hedge on the east side of the A173 between Pinchinthorpe Hall and Newton under Roseberry. On the former boundary of Pinchinthorpe and Newton parishes but entirely in Guisborough parish since 1974. No inscription visible. Grade II Listed details <span class="nowrap"><a title="https://historicengland.org.uk/listing/the-list/list-entry/1329558" rel="nofollow ugc noopener" href="https://historicengland.org.uk/listing/the-list/list-entry/1329558">Link</a><img style="margin-left:2px;" alt="External link" title="External link - shift click to open in new window" src="https://s1.geograph.org.uk/img/external.png" width="10" height="10"/></span>.

Milestone Society National ID: YN_PINNEW01pb
Old Boundary Marker on the A173 between Pinchinthorpe Hall and Newton under Roseberry
Parish Boundary Marker in the hedge on the east side of the A173 between Pinchinthorpe Hall and Newton under Roseberry. On the former boundary of Pinchinthorpe and Newton parishes but entirely in Guisborough parish since 1974. No inscription visible. Grade II Listed details LinkExternal link. Milestone Society National ID: YN_PINNEW01pb
Hutton Moor Looking east towards Highcliff Nab.
Hutton Moor
Looking east towards Highcliff Nab.
Show me another place!

Roseberry Common is located at Grid Ref: NZ5812 (Lat: 54.507422, Lng: -1.1025116)

Division: North Riding

Unitary Authority: Redcar and Cleveland

Police Authority: Cleveland

What 3 Words

///overt.detonated.iteration. Near Great Ayton, North Yorkshire

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Nearby Amenities

Located within 500m of 54.507422,-1.1025116
Roseberry Topping
Ele: 322
Man Made: survey_point
Natural: peak
Survey Point: pillar
Wikidata: Q8519110
Wikipedia: en:Roseberry Topping
Lat/Long: 54.5053975/-1.1072207
Barrier: kissing_gate
Lat/Long: 54.5047435/-1.1063152
Little Roseberry
Natural: peak
Lat/Long: 54.5071829/-1.0957766
Colour: RED
Information: route_marker
Ref: Roseberry Common - RED MTB
Tourism: information
Lat/Long: 54.5057765/-1.1070715
Cockle Scar
Place: locality
Lat/Long: 54.5080564/-1.108547
Roseberry Common
Place: locality
Lat/Long: 54.5090674/-1.1032576
Roseberry Mine
Abandoned: yes
Historic: mine
Man Made: mine
Mineral: iron_ore
Wikidata: Q105563571
Wikipedia: en:Roseberry Mine
Lat/Long: 54.5033894/-1.1008366
Roseberry Topping
Ele: 322
Natural: peak
Wikidata: Q8519110
Wikipedia: en:Roseberry Topping
Lat/Long: 54.5054442/-1.1072285
Abandoned: yes
Historic: mine_shaft
Man Made: mineshaft
Lat/Long: 54.5070261/-1.1014652
The data included in this document is from www.openstreetmap.org. The data is made available under ODbL.

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