Nolton Haven channel sandstones
Nolton Haven channel sandstones 2
Nolton Haven channel sandstones 3
Nolton Haven channel lag deposit in beach boulder…
Nolton Haven channel lag deposit in beach boulder…
Nolton Haven seaward view
Little Haven - Fox Hole Anticline
Fox Hole Anticline - northern limb
The Settlands sand trees 1
The Settlands sand trees 2
The Settlands sand trees 3
Conglomerates at Gravel Bay
Conglomerate at Gravel Bay: close-up view 1
Conglomerate at Gravel Bay: close-up view 2
Gravel Bay - Moor Cliffs Formation 1
Gravel Bay - Moor Cliffs Formation 2
Gravel Bay - millipede-like burrows in Moor Cliffs…
Gravel Bay - Moor Cliffs Formation with calcretes…
Gravel Bay - Moor Cliffs Formation with calcretes…
Gravel Bay - calcrete horizon in Moor Cliffs Forma…
Syncline in Lower Coal Measures sandstones: Swallo…
Swallowtree Bay anticline-syncline couplet: detail…
Swallowtree Bay anticline-syncline couplet: detail…
Nolton Haven ironstone pebbles in channel lag depo…
Nolton Haven ironstone pebbles in channel lag depo…
Nolton Haven sandstone channel edge lag deposits 2
Nolton Haven sandstone channel edge lag deposits 1
Nolton Haven sandstone channel edge 2
Nolton Haven sandstone channel edge 1
Nolton Haven north west cliffs of Pennant Sandston…
Benacre cliffs: Norwich Crag cross-bedding detail
Benacre cliffs - Norwich Crag cross-bedded sands
Norwich Crag at Benacre cliffs
Benacre Cliffs - Norwich Crag bioturbated clay wit…
Benacre Cliffs cross-bedded gravels 2
Benacre Cliffs cross-bedded gravels 1
Collapsed pill box at Benacre Cliffs
Benacre Cliffs - Westleton Formation
Canisp from Creag Dharaich
Quinag: Cambrian Basal Quartzite - Torridonian unc…
Quinag: Cambrian Basal Quartzite - Torridonian unc…
Quinag: Spidean Còinich from Sàil Gharbh summit
Quinag: Spidean Còinich and Lochan Bealach Cornadh
Quinag: Spidean Còinich
Quinag: start of the walk in
1/80 • f/8.0 • 15.0 mm • ISO 400 •
Canon EOS 600D
EF-S15-85mm f/3.5-5.6 IS USM
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Nolton Haven sandstone channel scours
Nolton Haven to Newgale
The small Nolton-Newgale coalfield is separated by faulting from the main Pembrokeshire coalfield. It lies mostly within Pennant Sandstone Formation of the Upper Coal Measures rocks.
The cliffs of Nolton Haven expose predominantly deltaic channel sandstones, often with highly erosive bases with coarse, rip-up, channel-lag deposits. The general dip is around 20° to the south-west.
This photo shows laminated sandstones with two scoured channel bases cutting into the underlying channel-lag deposits. The walking stick is 90 cm long.
The small Nolton-Newgale coalfield is separated by faulting from the main Pembrokeshire coalfield. It lies mostly within Pennant Sandstone Formation of the Upper Coal Measures rocks.
The cliffs of Nolton Haven expose predominantly deltaic channel sandstones, often with highly erosive bases with coarse, rip-up, channel-lag deposits. The general dip is around 20° to the south-west.
This photo shows laminated sandstones with two scoured channel bases cutting into the underlying channel-lag deposits. The walking stick is 90 cm long.
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