Pentargon panorama
Little Barton Strand
Cambeak late afternoon glow
The Strangles beach
Fault zone detail at The Strangles
Fault zone at The Strangles
Fold axial planar cleavage
Recumbent fold 3 at The Strangles
The Strangles recumbent fold 2
The Strangles recumbent fold couplet
Samphire Rock and Northern Door
The Strangles cliff
Millook Haven cliff detail 6
Millook Haven cliff detail 5
Millook Haven cliff
Millook Haven cliff detail 4
Millook Haven cliff detail 3
Millook Haven cliff detail 2
Millook Haven cliff detail 1
Millook Haven cliff
Afternoon light on The Strangles beach
Folded and inverted turbidites at Millook Haven, C…
The Strangles cliffs, near Crackington Haven, Nort…
Upside-down rocks at Millook Haven, Cornwall
Buckator cliffs, north Cornwall
Pentargon blue
Pentargon 2
Pencannow Point cliff at Crackington Haven
Crackington Haven low tide
Pentargon valley and waterfall
On the edge - Pentargon waterfall
Crackington Haven recumbent folds interpretation
Crackington Haven sole structures 1
Crackington Haven sole structures 2
Little Barton Strand westwards
The end of the Cleave valley
Castle Point and Orchard Strand
Little Barton Strand sole structures
Aberystwyth Grits
Zig-Zag folds at Millook Haven
1/160 • f/6.3 • 85.0 mm • ISO 100 •
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Crackington Haven recumbent folds
A zoomed-in view of the base of the cliff on the north side of Crackington Haven, north Cornwall.
Grey shales and thin turbidite sandstones, (pale grey-brown) of the Crackington Formation (upper Carboniferous) have been strongly deformed into isoclinal recumbent folds by the Variscan earth movements at the end of the Carboniferous.
For an interpretation and further details, see this photo:
Grey shales and thin turbidite sandstones, (pale grey-brown) of the Crackington Formation (upper Carboniferous) have been strongly deformed into isoclinal recumbent folds by the Variscan earth movements at the end of the Carboniferous.
For an interpretation and further details, see this photo:
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