Load structures on turbidite sandstones, Crooklets…
Load structures on turbidite sandstones, Crooklets…
Shower over Tintagel
The Mouls
Sunlit Rumps from Pentire Point, north Cornwall
Showery Tor 1
Showery Tor 2
Showery Tor 3
Rough Tor from Little Rough Tor
Rough Tor from Little Rough Tor cairn
View NE from Rough Tor
Small tor on Rough Tor
View SW from Rough Tor
Memorial on Rough Tor
Brown Willy summit
View E from Brown Willy
View S by W from Brown Willy
View SE to Rough Tor
Charlotte Dymond Memorial 1
Charlotte Dymond Memorial 2
Charlotte Dymond Memorial 3
Bossiney Haven and Lye Rock, Tintagel, Cornwall
Spectacular cirrus clouds over Scourie Bay, Suther…
Syncline, Wrangle Point, near Bude, Cornwall
Syncline axis (detail), Wrangle Point, near Bude,…
Syncline axis, Wrangle Point, near Bude, Cornwall.
Wrangle Point chevron folds
Plunging chevron folds (detail)
Plunging chevron folds at Wrangle Point, Crooklets…
Byrhtnoth
River Blackwater at Maldon, Essex
Syncline at Wrangle Point, Crooklets, near Bude.
Sevensouls Rock, north Cornwall.
Rocky Valley 3, near Tintagel, Cornwall
Rocky Valley 2, near Tintagel, Cornwall
Rocky Valley, near Tintagel, Cornwall
Upper Lathkill Dale near Monyash, Derbyshire
Sink Hole at the base of Mam Tor, Derbyshire
Whitbarrow Scar from Witherslack Hall, Cumbria.
Brown Willy on Bodmin Moor, Cornwall
Heading into Beer
Hooken Cliff
River Otter skyscape
Beach pebbles, Budleigh Salterton
Budleigh convergence
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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