Spurn Neck; looking out to sea
Spurn Neck view south
Spurn groyne 1
Spurn groyne 2
Spurn groyne 3
Spurn groyne and large vessel
Spurn Chalk Bank view north 1
Spurn Chalk Bank view north 2
Spurn Chalk Bank view WNW to Immingham
Spurn Warren view NE
Spurn Warren view SW to lighthouses
Spurn Warren view W to Grimsby
Spurn Warren view NE
Spurn High Lighthouse 1
Spurn High Lighthouse 2
Spurn High Lighthouse 3
Spurn Lower Lighthouse
Spurn lighthouses view NE
Spurn Warren view E to wind farm
Spurn east beach bank, swales and ripples 1
Spurn east beach bank, swales and ripples 2
Spurn north end view SW over the Spurn Neck
View south east over Dore and Totley from Lady Can…
Spurn Neck sand ripples 1
Spurn Neck close-up of peaty layer
Spurn Neck Basement Till and peaty layer
Rough Standhills early autumn pine avenue
Early autumn colours in Rough Standhills 4
Early autumn colours in Rough Standhills 3
Early autumn colours in Rough Standhills 2
Early autumn colours in Rough Standhills 1
Handfasting Ground devastation 2
Handfasting Ground devastation 1
Beech in the spotlight
Looking to Fulwood Hall
Wigley Farm fields view to Castle Dyke Lodge 3
Wigley Farm fields view to Castle Dyke Lodge 2
Wigley Farm fields view to Castle Dyke Lodge 1
Lonely sycamore and Wigley Farm fields
Lonely sycamore in September
Midnight clouds and stars
Comet Neowise from near Burbage Bridge
Altocumulus with fallstreaks
Cat's ear at ground level
Garden wilderness
1/200 • f/5.6 • 70.0 mm • ISO 100 •
Canon EOS 600D
EF-S15-85mm f/3.5-5.6 IS USM
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Spurn Neck sand ripples 2


A visit to Spurn Point 4
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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