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
Buckator cliffs, north Cornwall
The Strangles cliffs, near Crackington Haven, Nort…
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
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Painted Lady feeding
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Sucking the nectar
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Stanage Edge and Cattis Side Moor
Hathersage and the Derwent valley
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Stanage from High Neb
1/100 • f/7.1 • 10.0 mm • ISO 200 •
Canon EOS 350D DIGITAL
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Upside-down rocks at Millook Haven, Cornwall


The is an unusual detail view of the rocks at Millook Haven, north Cornwall.
The striped rocks are turbidites belonging to the Crackington Formation (upper Carboniferous). Way-up structures in the sandstone bands such as fining-up sequences, small-scale slump structures, ripple marks and grooves, etc, demonstrate that these northward dipping rocks (part of the famous chevron fold sequence) have been inverted and are upside-down.
The striped rocks are turbidites belonging to the Crackington Formation (upper Carboniferous). Way-up structures in the sandstone bands such as fining-up sequences, small-scale slump structures, ripple marks and grooves, etc, demonstrate that these northward dipping rocks (part of the famous chevron fold sequence) have been inverted and are upside-down.
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