Smooth Rock convergence 1
Smooth Rock convergence 2
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
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
Pentargon panorama
On the edge - Pentargon waterfall
1/100 • f/6.3 • 20.0 mm • ISO 100 •
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Maer Down cliff convergence 2


Nearly vertically bedded sandstones of the Bude Formation (upper Carboniferous) at Maer Down cliff between Northcott Mouth and Bude, north Cornwall.
The Bude Formation consists mainly of deltaic and some turbidite sandstones interbedded with shales. The sandstones are relatively thick, compared with those in the underlying Crackington Formation, and as a result, more competent.
The Bude Formation consists mainly of deltaic and some turbidite sandstones interbedded with shales. The sandstones are relatively thick, compared with those in the underlying Crackington Formation, and as a result, more competent.
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