Roseberry Topping
United Kingdom /
England /
Great Ayton /
A173
World
/ United Kingdom
/ England
/ Great Ayton
World / United Kingdom / England
hill, Site of Special Scientific Interest - SSSI (UK)
Roseberry Topping is a distinctive hill on the border between North Yorkshire and the borough of Redcar and Cleveland, England, of which it has long been a symbol. Its summit has a distinctive half-cone shape with a jagged cliff, which has led to many comparisons with the much higher Matterhorn in Switzerland.
At 1049 ft (320 m), Roseberry Topping was traditionally thought to be the highest hill on the North York Moors; however, the nearby Urra Moor is higher, at 1490 ft (454 m).
Geology
The hill is an outlier of the North York Moors uplands. It is formed from sandstone laid down in the Middle and Lower Jurassic periods, between 208 and 165 million years ago, which constitutes the youngest sandstone to be found in any of the National Parks in England and Wales. Its distinctive conical shape is the result of the hill's hard sandstone cap protecting the underlying shales and clays from erosion by the effects of ice, wind and rain.
Until 1914, the summit resembled a sugarloaf until a geological fault and possibly nearby alum and ironstone mining caused its collapse.[1] The area immediately below the summit is still extensively pitted and scarred from the former mineworks. The summit has magnificent views across the Cleveland plain as far as the Pennines on a clear day, some 60 to 80 km (40 to 50 miles) away.
History
The Roseberry area has been inhabited for thousands of years and the hill has long attracted attention for its distinctive shape. A Bronze Age hoard was discovered on the slopes of the hill and is now in the Sheffield City Museum. It was occupied during the Iron Age; walled enclosures and the remains of huts dating from the period are still visible in the hill's vicinity.
The hill was held in special regard by the Vikings who settled in Cleveland in large numbers during the early medieval period and gave the area many of its place names. They gave Roseberry Topping its present name, which is one of only a handful of known pagan names in England. "Roseberry" is a corruption of Odins-Beorge ("Odin's Hill"), in reference to the Norse god Odin. The name mutated in successive years to Othensberg, Ohenseberg, Ounsberry and Ouesberry before finally settling on Roseberry. "Topping" is a corruption of toppen, an Old Norse word for a hill.
Roseberry Topping can be seen from many miles away and was long used by sailors and farmers as an indicator of impending bad weather. An old rhyme commemorates this usage:
When Roseberry Topping wears a cap, Let Cleveland then beware of a clap!
The hill was private property for many years, formerly being part of a game estate. An old shooting box can still be seen on its southern flank. Roseberry Topping is now managed by the National Trust and is open to the public. It is not part of the North York Moors National Park but is managed, in effect, as an adjunct of the park.
A spur of the Cleveland Way National Trail runs up to the summit. The path has been a popular sight-seeing excursion for centuries due to the spectacular views of the Cleveland area from the summit; as early as 1700, travellers were recommended to visit the peak to see "the most delightful prospect upon the valleys below to the hills above."
The site was notified as a geological Site of Special Scientific Interest in 1954, with a boundary extension in 1986 bringing the designated area to 10.86 hectares. The site is listed as being of national importance in the Geological Conservation Review.
Photos:
1) Unknown
2) www.geograph.org.uk/photo/5288879
3) www.geograph.org.uk/photo/3993466
At 1049 ft (320 m), Roseberry Topping was traditionally thought to be the highest hill on the North York Moors; however, the nearby Urra Moor is higher, at 1490 ft (454 m).
Geology
The hill is an outlier of the North York Moors uplands. It is formed from sandstone laid down in the Middle and Lower Jurassic periods, between 208 and 165 million years ago, which constitutes the youngest sandstone to be found in any of the National Parks in England and Wales. Its distinctive conical shape is the result of the hill's hard sandstone cap protecting the underlying shales and clays from erosion by the effects of ice, wind and rain.
Until 1914, the summit resembled a sugarloaf until a geological fault and possibly nearby alum and ironstone mining caused its collapse.[1] The area immediately below the summit is still extensively pitted and scarred from the former mineworks. The summit has magnificent views across the Cleveland plain as far as the Pennines on a clear day, some 60 to 80 km (40 to 50 miles) away.
History
The Roseberry area has been inhabited for thousands of years and the hill has long attracted attention for its distinctive shape. A Bronze Age hoard was discovered on the slopes of the hill and is now in the Sheffield City Museum. It was occupied during the Iron Age; walled enclosures and the remains of huts dating from the period are still visible in the hill's vicinity.
The hill was held in special regard by the Vikings who settled in Cleveland in large numbers during the early medieval period and gave the area many of its place names. They gave Roseberry Topping its present name, which is one of only a handful of known pagan names in England. "Roseberry" is a corruption of Odins-Beorge ("Odin's Hill"), in reference to the Norse god Odin. The name mutated in successive years to Othensberg, Ohenseberg, Ounsberry and Ouesberry before finally settling on Roseberry. "Topping" is a corruption of toppen, an Old Norse word for a hill.
Roseberry Topping can be seen from many miles away and was long used by sailors and farmers as an indicator of impending bad weather. An old rhyme commemorates this usage:
When Roseberry Topping wears a cap, Let Cleveland then beware of a clap!
The hill was private property for many years, formerly being part of a game estate. An old shooting box can still be seen on its southern flank. Roseberry Topping is now managed by the National Trust and is open to the public. It is not part of the North York Moors National Park but is managed, in effect, as an adjunct of the park.
A spur of the Cleveland Way National Trail runs up to the summit. The path has been a popular sight-seeing excursion for centuries due to the spectacular views of the Cleveland area from the summit; as early as 1700, travellers were recommended to visit the peak to see "the most delightful prospect upon the valleys below to the hills above."
The site was notified as a geological Site of Special Scientific Interest in 1954, with a boundary extension in 1986 bringing the designated area to 10.86 hectares. The site is listed as being of national importance in the Geological Conservation Review.
Photos:
1) Unknown
2) www.geograph.org.uk/photo/5288879
3) www.geograph.org.uk/photo/3993466
Wikipedia article: http://en.wikipedia.org/wiki/Roseberry_Topping
Nearby cities:
Coordinates: 54°30'19"N 1°6'25"W
- Hatfield Moor Nature Reserve (Humberhead Peatlands) 105 km
- Fenn's, Whixall and Bettisfield Mosses National Nature Reserve 206 km
- Dersingham Bog National Nature Reserve 212 km
- Wenlock Edge 240 km
- Loch Leven 240 km
- Colne Estuary National Nature Reserve 325 km
- Cefn Bryn (Ridge Hill) 384 km
- Arne SSSI and RSPB reserve 428 km
- South Dorset Coast SSSI 439 km
- Bermuda Triangle 6002 km
- Blue Lake Wood 2 km
- Hutton Wood 2.7 km
- Ayton Banks Wood 2.7 km
- Lonsdale 3.6 km
- Guisborough 4.2 km
- Park Wood 4.5 km
- Guisborough Wood 5.1 km
- East Middlesbrough and Eston & Southbank 6.4 km
- Stewart Park 7.4 km
- Middlesbrough Municipal Golf Club 8.9 km