Plunging chevron folds at Northcott Mouth
Maer Down cliff convergence 1
Maer Down cliff convergence 2
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
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
Pentargon valley and waterfall
Pentargon 2
Pentargon blue
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Vertical bedding slab at Northcott Mouth, Cornwall.


This vertical slab of sandstone is at Northcott Mouth, near Bude, north Cornwall. See geotag for exact location.
This is part of the Bude Formation (upper Carboniferous) - 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.
This slab is the part of the vertical northern limb of an asymmetric anticline, and the view is of the underside of he bedding. There are sole structures - mostly trains of ripples/scours - on this surface, proving that it is the base of the bed.
I would guess that the local rock climbing fraternity have given this slab a name, so if anyone knows it please let me know. Thanks!
This is part of the Bude Formation (upper Carboniferous) - 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.
This slab is the part of the vertical northern limb of an asymmetric anticline, and the view is of the underside of he bedding. There are sole structures - mostly trains of ripples/scours - on this surface, proving that it is the base of the bed.
I would guess that the local rock climbing fraternity have given this slab a name, so if anyone knows it please let me know. Thanks!
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