Stanage south end 3
Cross bedding view
White Edge 1
Erosion surface
Froggatt Edge cross bedding
Hay Wood quarry cross bedding
Porth Selau sands
Porth Selau sands 2
Skipsea Withow Mere, Holderness coast, East Yorksh…
Peat section in the Skipsea Withow Mere, Holdernes…
Aberystwyth Grits
Burton Cliff golden light 1
Burton Cliff golden light 2
Gold and indigo convergence, Burton Cliff
Burton Cliff near sunset 1
Burton Cliff near sunset 2
Angular unconformity at Horton-in-Ribblesdale
Upside-down rocks at Millook Haven, Cornwall
Millook Haven cliff detail 6
Crackington Haven sole structures 1
Crackington Haven sole structures 2
Little Barton Strand sole structures
Vertical bedding slab at Northcott Mouth, Cornwall…
Stanage south end 1
Mother Cap sunset 1
Mother Cap sunset 1 (uncropped)
Mother Cap gold
Mother Cap sunset 3
Mother Cap sunset 4
Mother Cap north face
Mother Cap west face
The South Face of Mother Cap
Striped cliffs at Hunstanton, Norfolk.
Hope Gap karst
Hope Gap
Upper Burbage Bridge plant straps
Pleistocene river gravels of the proto-Thames
Cliff erosion 1
Gwna Mélange on the Lleyn Peninsula, NW Wales
A bit of Burbage Edge
Another bit of Burbage Edge
Ringing Roger
Orgreave S24's washout (3 of 3)
Orgreave S24's washout (2 of 3)
Orgreave S24's washout (1 of 3)
1/200 • f/5.6 • 10.0 mm • ISO 200 •
Canon EOS 350D DIGITAL
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Stanage south end: channel erosion surface
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 (as in this photo) are common.
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 (as in this photo) are common.
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