Crackington Haven low tide
Pencannow Point cliff at Crackington Haven
Crackington Haven recumbent folds
Crackington Haven recumbent folds interpretation
Crackington Haven sole structures 1
Crackington Haven sole structures 2
Crackington Haven and Cambeak
Crackington Haven from Pencannow Cliff
Little Barton Strand
Little Barton Strand westwards
The end of the Cleave valley
The Cleave valley
Castle Point and Orchard Strand
Little Barton Strand sole structures
Purple on gold
Clearing mist over Burbage Edge
Fair weather cumulus over Morwenstow
Vertical bedding slab at Northcott Mouth, Cornwall…
Plunging chevron folds at Northcott Mouth
Maer Down cliff convergence 1
Maer Down cliff convergence 2
Smooth Rock convergence 1
Smooth Rock convergence 2
On the edge - Pentargon waterfall
Pentargon valley and waterfall
Pentargon 2
Pentargon blue
Buckator cliffs, north Cornwall
Evening sky at Crackington Haven
The Lone Photographer
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
Millook Haven cliff detail 6
Millook Haven cliff detail 5
Millook Haven cliff detail 4
Millook Haven cliff detail 3
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Pentargon panorama
A panorama composed from four portrait-style photos joined using Canon's PhotoStitch software.
Just north-east of Boscastle, the short, steep-sided Pentargon valley ends abruptly, its waterfall plunging 120 ft over the sheer lip into the Pentargon inlet below. There are a number of these truncated valleys on the north Cornwall coast. Few of them extend far inland and often end with a spectacular, if small, waterfall over a vertical drop to the beach below.
The rocks are shales with thin turbidite sandstones - part of the Crackington Formation (upper Carboniferous) - which are deformed into tight horizontal recumbent folds.
Just north-east of Boscastle, the short, steep-sided Pentargon valley ends abruptly, its waterfall plunging 120 ft over the sheer lip into the Pentargon inlet below. There are a number of these truncated valleys on the north Cornwall coast. Few of them extend far inland and often end with a spectacular, if small, waterfall over a vertical drop to the beach below.
The rocks are shales with thin turbidite sandstones - part of the Crackington Formation (upper Carboniferous) - which are deformed into tight horizontal recumbent folds.
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