Little Barton Strand
Fold axial planar cleavage
Recumbent fold 3 at The Strangles
The Strangles recumbent fold 2
The Strangles recumbent fold couplet
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
Crackington Haven recumbent folds
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
Little Barton Strand westwards
Castle Point and Orchard Strand
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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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