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
Wide open
Solstice 2009
Snowy handfasting ground
Snowy Limb Brook 1
Snowy branches
Snowy Limb Brook 2
Snowy gateway to heaven
Snowy cold and gold
Snow field at the edge
Descent into the snowy beeches
Looking up at the snowy beeches
In among the snowy beeches
Snowy blue and gold
Snowy beeches - extraordinary light
Duckmanton Railway Cutting SSSI
Duckmanton Railway Cutting SSSI (2)
Chavery Coal and roof measures, Duckmanton Railway…
Smooth Rock convergence 1
Maer Down cliff convergence 2
Maer Down cliff convergence 1
Plunging chevron folds at Northcott Mouth
Vertical bedding slab at Northcott Mouth, Cornwall…
Fair weather cumulus over Morwenstow
Clearing mist over Burbage Edge
Purple on gold
Little Barton Strand sole structures
Castle Point and Orchard Strand
The Cleave valley
The end of the Cleave valley
Little Barton Strand westwards
Little Barton Strand
Crackington Haven from Pencannow Cliff
Crackington Haven and Cambeak
Crackington Haven sole structures 2
Crackington Haven sole structures 1
Crackington Haven recumbent folds interpretation
Crackington Haven recumbent folds
Pencannow Point cliff at Crackington Haven
Crackington Haven low tide
1/100 • f/6.3 • 10.0 mm • ISO 200 •
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Smooth Rock convergence 2
Chevron fold syncline in sandstones of the Bude Formation (upper Carboniferous) at Maer Cliff between Northcott Mouth and Bude, north Cornwall. 'Smooth Rock' is the name given to the steeply dipping slab on the right - a favourite with rock climbers.
The Bude Formation consists mainly of deltaic and some turbidite sandstones interbedded with shales. The sandstones are relatively thick, compared with the underlying Crackington Formation, and as a result, more competent. The response to the Variscan earth movements at the end of the Carboniferous was to form more open, mostly upright or slightly asymmetric angular folds, compared with the cascades of tight recumbent folds which characterise the Crackington Formation a few kilometres to the south.
The Bude Formation consists mainly of deltaic and some turbidite sandstones interbedded with shales. The sandstones are relatively thick, compared with the underlying Crackington Formation, and as a result, more competent. The response to the Variscan earth movements at the end of the Carboniferous was to form more open, mostly upright or slightly asymmetric angular folds, compared with the cascades of tight recumbent folds which characterise the Crackington Formation a few kilometres to the south.
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