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
Mehrauli Archaeological Park, Delhi, India
Mehrauli Archaeological Park
Mehrauli Archaeological Park
Mehrauli Archaeological Park
Not your average stone wall
The door to the fog
Mehrauli Archaeological Park
Through the arch
Elephants amid the corbels
Elephants in the opening
Monkeys on the roof
Entrance to the Taj Mahal
Intarsia in red
Taj Mahal Jawab
The red tower
Marble inlay
View from the Taj
Entering the Taj Mahal Complex
Interior of the Agra Fort
Agra Fort
Hanging on
Red Rock Wash - Willow Spring Gap
Red Rock Wash
09-keystone_thrust-1-80_adj
Head of a statue
Maer Down cliff convergence 1
Plunging chevron folds at Northcott Mouth
Vertical bedding slab at Northcott Mouth, Cornwall…
Fox Hole anticline, Little Haven, Pembrokeshire
Český ráj_5
Trees on a Rock
18-jack&maddy_ig_adj
14-red_rock_ig_adj
Rock Graffiti
Bonsai Fukien Tea Tree Clinging to Sandstone – Nat…
18-cyn_end_ig
16-j&john_on_trail_ig
crag_view
trail_view
john_on_trail3
PC210713
PC210709
First Creek, Red Rock Canyon, Nevada
PC210707
PC210706
PC210705
PC210704
PC210702
Concretions
First Creek
Tiské stěny_14
Tiské stěny_13
Tiské stěny_12
Tiské stěny_11
Tiské stěny_10
Tiské stěny_9
Tiské stěny_8
1/100 • f/6.3 • 20.0 mm • ISO 100 •
Location
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Maer Down cliff convergence 2
![Maer Down cliff convergence 2 Maer Down cliff convergence 2](https://cdn.ipernity.com/200/38/04/39023804.d3d93a6d.640.jpg?r2)
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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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