Crook Hill summits and wall
Heather and rock
The Strangles cliffs, near Crackington Haven, Nort…
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Afternoon light on The Strangles beach
Millook Haven cliff
Millook Haven cliff detail 1
Millook Haven cliff detail 2
Millook Haven cliff detail 3
Millook Haven cliff detail 4
Millook Haven cliff detail 5
Millook Haven cliff detail 6
Millook Haven cliff
The Strangles cliff
Samphire Rock and Northern Door
The Strangles recumbent fold couplet
The Strangles recumbent fold 2
Recumbent fold 3 at The Strangles
Fold axial planar cleavage
Fault zone at The Strangles
Fault zone detail at The Strangles
The Strangles beach
Crook Hill SE top from NW top
Crook Hill view NW
Ladybower from Crook Hill
Ladybower and Ashop valley from Crook Hill
Far Deep Clough from Crook Hill
Crook Hill view NW from SE top
Crook Hill
Profile of a Painted Lady
Painted Lady from the front
Painted Lady feeding
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It looks like a bee....
Sucking the nectar
Buzz buzz buzz
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Hathersage and the Derwent valley
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Bamford Moor from High Neb
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Stanage End view to Moscar
Stanage End boundary stone
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Crook Hill NW top


A view of the NW summit (382 m) of Crook Hill, near Ladybower in the Peak District, looking to the SE. Although not of great elevation compared with the heights all around, Crook Hill's airy rocky summits offer a lovely viewpoint of the surrounding moors and gritstone edges.
The summits are residual tors composed of Kinderscout Grit (Namurian) with a solifluction mantle of gritstone blocks all around.
The SW faces of both tors display the steepest slopes probably because material removed from the summit by freeze-thaw conditions has been steadily removed by successive phases of gelifluction and/or solifluction into the deep Ashop valley below. In contrast, on the NE slopes with an aspect facing away from most of the sun's warmth, the material has not been transported so far from its source and remains mostly piled up around the summit tors.
The summits are residual tors composed of Kinderscout Grit (Namurian) with a solifluction mantle of gritstone blocks all around.
The SW faces of both tors display the steepest slopes probably because material removed from the summit by freeze-thaw conditions has been steadily removed by successive phases of gelifluction and/or solifluction into the deep Ashop valley below. In contrast, on the NE slopes with an aspect facing away from most of the sun's warmth, the material has not been transported so far from its source and remains mostly piled up around the summit tors.
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