Derwent gold
Stanage south end 2
Stanage south end: channel erosion surface
Moorland gold
Mother Cap sunset 1
Bracken and birches
Moorland sunset 2
Mother Cap sunset 4
Derwent dusk
Mother Cap gold
Mother Cap sunset 1 (uncropped)
Mother Cap sunset 3
Moorland sunset 1
Stanage south end 1
Mother Cap north face
Mother Cap west face
The South Face of Mother Cap
Stanage south end 4
Stanage south end 3
Balancing boulder and Hargreave's Original Route
Mother Cap: Moor and Sky
Stanage Edge and Cattis Side Moor
Crow Chin gulley and Jarvis Clough
Bamford Moor and Win Hill
Stanage from High Neb
Hathersage and the Derwent valley
Bamford Moor from High Neb
Stanage End view to Moscar
Stanage End Slab
Colourful Edge
Cross bedding view
Stanage boulders
Climbing on Stanage 1
Edge projection
Packhorse track up
White Path Moss and wall
Stanage north west view 2
Stanage north west view 1
Stanage north west view 3
Stanage Edge from Stanage Plantation
Packhorse track down
High Neb
Climbing on Stanage 2
Stanage panorama - x2 vertical exaggeration
Stanage panorama
Stanage Edge vertical exaggeration x3
Tor on Higger Tor
Nearly sunset
A bit of Edge
Higger Tor evening sun
Carl Wark from Higger Tor
Jane Eyre country: Green's Farm from North Lees, n…
Burbage from Higger Tor
Another bit of Burbage Edge
A bit of Burbage Edge
Mackeral sky over Burbage Brook
Burbage Edge view northwards ...
Faulted gritstone scarp on Burbage Edge
View to Sir William Hill
1/125 • f/8.0 • 10.0 mm • ISO 400 •
Canon EOS 350D DIGITAL
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Stanage south end millstones
The southern end of Stanage Edge, the longest of the Eastern Edges, in the Peak District National Park, Derbyshire.
Stanage Edge is comprised of Rivelin Grit (aka Chatsworth Grit), Namurian age, Upper Carboniferous. The coarse-grained gritstone was deposited in a series of delta distributary channels. The gritstone is normally strongly cross-bedded, and intraformational erosion surfaces are common.
The Edge has been worked for millstones in several places and examples such as these can be found in many places, lying where they were abandoned when the demand for imported French stones rose in the latter part of the 19th century.
Stanage Edge is comprised of Rivelin Grit (aka Chatsworth Grit), Namurian age, Upper Carboniferous. The coarse-grained gritstone was deposited in a series of delta distributary channels. The gritstone is normally strongly cross-bedded, and intraformational erosion surfaces are common.
The Edge has been worked for millstones in several places and examples such as these can be found in many places, lying where they were abandoned when the demand for imported French stones rose in the latter part of the 19th century.
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