Photographs of the spectacular limestone pavements of the Stennerskeugh and Fell End Clouds on Ravenstonedale Common in the Yorkshire Dales National Park of Cumbria.
Cold Keld, a delightful 17th century cottage at Fell End near Ravenstonedale, Cumbria, UK.
Limekiln and Lakeland Fell ponies at Fell End near Ravenstonedale, Cumbria.
Lime kiln and Lakeland fell ponies at Fell End near Ravenstonedale in Cumbria.
Fell ponies at Fell End on Ravenstonedale Common, with a distant view of Cautley Crags, Cumbria.
Cairn, Fell End Clouds on Ravenstonedale Common with a backdrop of Harter Fell in the Yorkshire Dales of Cumbria.
Cairn and limestone pavement at Fell End Clouds, Ravenstonedale Common on the western slopes of Wild Boar Fell in the Yorkshire Dales of Cumbria.
The limestone amphitheatre of the Fell End Clouds, Ravenstonedale Common on the lower slopes of Wild Boar Fell in the Yorkshire Dales National Park, Cumbria.
The name, 'Clouds' is thought to originate from the Anglo-Saxon word 'clod' which meant rocky ground.
The limestone amphitheatre of the Fell End Clouds, Ravenstonedale Common on the lower slopes of Wild Boar Fell in the Yorkshire Dales National Park, Cumbria.
The name, Clouds is thought to originate from the Anglo-Saxon word 'clod' which meant rocky ground.
Looking towards the Stennerskeugh Clouds from the limestone terraces of Fell End Clouds on the western slopes of Wild Boar Fell in the Yorkshire Dales of Cumbria.
The name, Clouds is thought to originate from the Anglo-Saxon word 'clod' which meant rocky ground.
The limestone pavements of the Stennerskeugh Clouds, Ravenstonedale Common on the western slopes of Wild Boar Fell in the Yorkshire Dales National Park, Cumbria..
The name, Clouds is thought to originate from the Anglo-Saxon word 'clod' which meant rocky ground.
Looking towards the Stennerskeugh Clouds from the limestone terraces of Fell End Clouds, Ravenstonedale Common on the western slopes of Wild Boar Fell in the Yorkshire Dales National Park, Cumbria.
The name, Clouds is thought to originate from the Anglo-Saxon word 'clod' which meant rocky ground.
Harry Hope's Land and a ruined walled enclosure at Dale Slack, Ravenstonedale Common on the lower slopes of Wild Boar Fell in the Yorkshire Dales, Cumbria.
The last occupant of this ruined farmhouse was Harry Hope who farmed this land until 1820. Cautley Crags and Harter Fell lie on the other side of the valley.
The farmhouse of Harry Hope at Dale Slack, Ravenstonedale Common on the lower slopes of Wild Boar Fell in the Yorkshire Dales, Cumbria.
The last occupant of this ruined farmhouse was Harry Hope who farmed this land until 1820.
Room with a view in the farmhouse of Harry Hope at Dale Slack, Ravenstonedale Common on the lower slopes of Wild Boar Fell in the Yorkshire Dales, Cumbria.
Old mineral workings at Fell End Clouds, Ravenstonedale Common on the slopes of Wild Boar Fell in Cumbria.
One of a row of several trench-like surface mines. The lead ore, galena would have been the main product of the workings, but baryte and malachite may also have been found. The small white lead tolerant flower, spring sandwort, grows around the workings.
Old mineral workings at Fell End Clouds, Ravenstonedale Common on the slopes of Wild Boar Fell in Cumbria.
One of a row of several trench-like surface mines. The lead ore, galena would have been the main product of the workings, but baryte and malachite may also have been found. The small white lead tolerant flower, spring sandwort, grows around the workings.
Old mineral workings at Fell End Clouds, Ravenstonedale Common on the slopes of Wild Boar Fell in Cumbria.
One of a row of several trench-like surface mines. The lead ore, galena would have been the main product of the workings, but baryte and malachite may also have been found. The small white lead tolerant flower, spring sandwort, grows around the workings.
The Dent Fault near Ravenstonedale in the Yorkshire Dales of Cumbria.
To the west of the A683 are the smooth, rounded shapes of the Howgills made up of old Silurian rocks of the Lake District. To the east are the newer Carboniferous limestones of The Dales. During the upheaval of the Dent Fault the older Silurian rocks rose up 2400m against the horizontal limestone strata, forcing the limestones into a vertical position.
The Dent Fault near Ravenstonedale in the Yorkshire Dales of Cumbria.
To the west of the A683 are the smooth, rounded shapes of the Howgills made up of old Silurian rocks of the Lake District. To the east are the newer Carboniferous limestones of The Dales. During the upheaval of the Dent Fault the older Silurian rocks rose up 2400m against the horizontal limestone strata, forcing the limestones into a vertical position.
Rainbow over The Street at the foot of Wild Boar Fell near Ravenstonedale in Cumbria.
The limestone pavement of the Stennerskeugh Clouds, on the lower slopes of Wild Boar Fell near Ravenstonedale in the Yorkshire Dales National Park, Cumbria. The name, Clouds is thought to originate from the Anglo-Saxon word 'clod' which meant rocky ground.
The limestone pavement of the Stennerskeugh Clouds, on the lower slopes of Wild Boar Fell near Ravenstonedale in the Yorkshire Dales National Park, Cumbria.
The name, Clouds is thought to originate from the Anglo-Saxon word 'clod' which meant rocky ground.