Spurn Neck sand ripples 2
Spurn Neck view south
Spurn east beach bank, swales and ripples 1
Spurn east beach bank, swales and ripples 2
Swallowtree Bay anticline-syncline couplet: detail…
Swallowtree Bay anticline-syncline couplet: detail…
Syncline in Lower Coal Measures sandstones: Swallo…
Gravel Bay - calcrete horizon in Moor Cliffs Forma…
Gravel Bay - Moor Cliffs Formation with calcretes…
Gravel Bay - Moor Cliffs Formation with calcretes…
Gravel Bay - millipede-like burrows in Moor Cliffs…
Gravel Bay - Moor Cliffs Formation 2
Gravel Bay - Moor Cliffs Formation 1
Conglomerate at Gravel Bay: close-up view 2
Conglomerate at Gravel Bay: close-up view 1
Conglomerates at Gravel Bay
The Settlands sand trees 3
The Settlands sand trees 2
The Settlands sand trees 1
Fox Hole Anticline - northern limb
Little Haven - Fox Hole Anticline
Nolton Haven seaward view
Nolton Haven channel lag deposit in beach boulder…
Nolton Haven channel lag deposit in beach boulder…
Nolton Haven channel sandstones 3
Nolton Haven channel sandstones 2
1/200 • f/5.6 • 15.0 mm • ISO 100 •
Canon EOS 600D
EF-S15-85mm f/3.5-5.6 IS USM
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Spurn Neck sand ripples 1
A visit to Spurn Point 3
Spurn Neck eastern low tide zone.
Asymmetric ripples in beach sand, presumably formed by the previous flood tide(s). The steeper, lee, side of the ripples face west (left); the gentle, stoss, sides face east (right). This indicates that these ripples were formed by water flow moving from right to left, i.e. by the incoming tide. They have clearly survived the previous ebbing tide, suggesting that the incoming tide flows faster than the ebb.
Spurn Neck eastern low tide zone.
Asymmetric ripples in beach sand, presumably formed by the previous flood tide(s). The steeper, lee, side of the ripples face west (left); the gentle, stoss, sides face east (right). This indicates that these ripples were formed by water flow moving from right to left, i.e. by the incoming tide. They have clearly survived the previous ebbing tide, suggesting that the incoming tide flows faster than the ebb.
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