Stanage south end 3
Stanage south end 4
Stanage south end millstones
Stanage boulders
Cross bedding view
White Path Moss and wall
Stanage north west view 1
Stanage north west view 2
Stanage north west view 3
Packhorse track up
Packhorse track down
Stanage Plantation view west
High Neb
Stanage Edge from Stanage Plantation
Edge projection
Colourful Edge
Climbing on Stanage 1
Climbing on Stanage 2
Balancing boulder and Hargreave's Original Route
Stanage panorama
Stanage panorama - x2 vertical exaggeration
Frosty bracken
Frosty oak leaf
Stanage south end: channel erosion surface
Stanage south end 1
White Path Moss, Stanage Edge
Bracken and birches
Derwent gold
Moorland gold
Moorland sunset 1
Moorland sunset 2
Mother Cap sunset 1
Mother Cap sunset 1 (uncropped)
Mother Cap gold
Mother Cap sunset 3
Mother Cap sunset 4
Derwent dusk
Beam me up, Sir William
Creigiau Eglwyseg, near Llangollen, Wales
Folding at Monkstone Point, near Saundersfoot, Pem…
Swine Sty and Big Moor
Spherical Autumn Tree - November 2007
Resting place
Mother Cap north face
Mother Cap west face
1/200 • f/8.0 • 10.0 mm • ISO 400 •
Canon EOS 350D DIGITAL
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Stanage south end 2


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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