Upside-down rocks at Millook Haven, Cornwall
Folded and inverted turbidites at Millook Haven, C…
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
Cambeak late afternoon glow
The Lone Photographer
Evening sky at Crackington Haven
Heather and rock
Crook Hill summits and wall
Crook Hill NW top
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
Look at that pollen sac!
It looks like a bee....
Sucking the nectar
Buzz buzz buzz
Stanage Edge and Cattis Side Moor
Hathersage and the Derwent valley
Bamford Moor and Win Hill
Stanage from High Neb
Bamford Moor from High Neb
1/80 • f/5.0 • 20.0 mm • ISO 100 •
Canon EOS 350D DIGITAL
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The Strangles cliffs, near Crackington Haven, North Cornwall


Originally uploaded for the Guesswhere UK group.
This is a view of the upper cliff overlooking The Strangles, near Crackington Haven, north Cornwall. The cliff is comprised of the Crackington Formation: upper Carboniferous turbidites and shales, which have been subjected to intense folding and a near-horizontal axial-planar, slaty cleavage is well developed in the shaly parts of the sequence, as in this location. The cliff has been extensively quarried in the past for slates.
This is a view of the upper cliff overlooking The Strangles, near Crackington Haven, north Cornwall. The cliff is comprised of the Crackington Formation: upper Carboniferous turbidites and shales, which have been subjected to intense folding and a near-horizontal axial-planar, slaty cleavage is well developed in the shaly parts of the sequence, as in this location. The cliff has been extensively quarried in the past for slates.
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