Vertical bedding slab at Northcott Mouth, Cornwall…
Maer Down cliff convergence 1
Maer Down cliff convergence 2
Smooth Rock convergence 1
Smooth Rock convergence 2
Plunging chevron folds at Northcott Mouth
Maer Cliff syncline 1
Maer Cliff syncline 2
Maer Cliff incompetent deformation
Maer Cliff incompetent deformation - detail
Northcott Mouth anticline 1
Northcott Mouth anticline - detail
Syncline, Wrangle Point, near Bude, Cornwall
Wrangle Point chevron folds
Syncline axis, Wrangle Point, near Bude, Cornwall.
Syncline axis (detail), Wrangle Point, near Bude,…
Plunging chevron folds (detail)
Plunging chevron folds at Wrangle Point, Crooklets…
Syncline at Wrangle Point, Crooklets, near Bude.
1/100 • f/8.0 • 17.0 mm • ISO 100 •
Canon EOS 350D DIGITAL
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Anticline, Crooklets, near Bude, Cornwall
An anticline in the Bude Formation (upper Carboniferous) at Crooklets, near Bude, Cornwall. The Bude Formation here consists of alternating thin beds of turbidite sandstones (pale grey/brown) and fine-grained shaly siltstones/mudstones (darker grey).
Minor crumpling on the south (right-hand) limb of the fold has resulted in near vertical or slightly overturned bedding. The sandstones display sedimentary structures which can be used to determine the 'way up' of the bedding. Here, the sedimentary structures are mostly rippled upper surfaces and small-scale slump or load structures on the basal surfaces. The latter can be seen in detail in the next two photos:
www.ipernity.com/doc/earthwatcher/39024212
www.ipernity.com/doc/earthwatcher/39024210
Minor crumpling on the south (right-hand) limb of the fold has resulted in near vertical or slightly overturned bedding. The sandstones display sedimentary structures which can be used to determine the 'way up' of the bedding. Here, the sedimentary structures are mostly rippled upper surfaces and small-scale slump or load structures on the basal surfaces. The latter can be seen in detail in the next two photos:
www.ipernity.com/doc/earthwatcher/39024212
www.ipernity.com/doc/earthwatcher/39024210
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