Frosty bracken
Frosty oak leaf
Frosty brambles
Frosty gorse 3
Frosty gorse 2
Frosty gorse 1
Upper Limb Brook cascade
Gold on the beeches
Big buggers
Winter hedgerow - sepia
Winter hedgerow
Layers over Bradway - sepia
Layers over Bradway
Beeches dawn rime
Beeches sunrise 1
Beeches sunrise 2
Beeches sunrise 3
Beeches sunrise 4
Frosty leaves
Frosty leaves and yellow light
Dawn hedgerow
Dawn flight to Venus
Dawn Gateway to Heaven
Stanage panorama
Balancing boulder and Hargreave's Original Route
Climbing on Stanage 2
Climbing on Stanage 1
Colourful Edge
Edge projection
Stanage Edge from Stanage Plantation
High Neb
Stanage Plantation view west
Packhorse track down
Packhorse track up
Stanage north west view 3
Stanage north west view 2
Stanage north west view 1
White Path Moss and wall
Cross bedding view
Stanage boulders
Stanage south end millstones
Stanage south end 4
Stanage south end 3
Stanage south end 2
Stanage south end: channel erosion surface
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Stanage panorama - x2 vertical exaggeration


A panoramic view northwards from Stanage Edge, with Dennis Knoll and Bamford Moor visible in the middle distance, the Hope Valley, Mam Tor and the Kinderscout plateau on the skyline. This photo is comprised of two images stitched together using Canon's PhotoStitch software, then a x2 vertical exaggeration applied in Photoshop, to emphasise the geological features. It also makes an interesting effect!
Stanage Edge is 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.
Stanage Edge is 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.
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