Gravel Bay - Moor Cliffs Formation with calcretes…
Gravel Bay - calcrete horizon in Moor Cliffs Forma…
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Spurn Neck sand ripples 2
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Spurn east beach bank, swales and ripples 2
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
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The Settlands sand trees 2
The Settlands sand trees 1
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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
Nolton Haven channel sandstones
Nolton Haven sandstone channel scours
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
1/80 • f/6.3 • 15.0 mm • ISO 100 •
Canon EOS 600D
EF-S15-85mm f/3.5-5.6 IS USM
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Gravel Bay - Moor Cliffs Formation with calcretes 1
Freshwater West, Gravel Bay and East Pickard Bay
Moor Cliffs Formation in Gravel Bay.
This photo shows the mainly reddened mudstone beds in the Moor Cliffs Formation at the western end of Gravel Bay. The white mottling in the mudstones shows extensive calcrete soil horizons. The sequence is dipping to the north (right) at approx. 65°.
The walking stick is about 0.9 m long.
Background:
The Moor Cliffs Formation overlies the Freshwater East conglomerates, seen in previous photos, and spans the boundary between the Silurian and Devonian periods. It consists of red mudstones and siltstones with occasional thin sandstone beds. These were deposited on a low-reflief floodplain at the edge of an arid continental margin, the sandstones being deposited by seasonal braided streams, the muds and silts deposited in ephemeral marginal lakes. When not inundated, the muds and silts developed carbonate-rich calcrete (caliche) soil horizons along dessication cracks, burrows and early plant root systems.
Moor Cliffs Formation in Gravel Bay.
This photo shows the mainly reddened mudstone beds in the Moor Cliffs Formation at the western end of Gravel Bay. The white mottling in the mudstones shows extensive calcrete soil horizons. The sequence is dipping to the north (right) at approx. 65°.
The walking stick is about 0.9 m long.
Background:
The Moor Cliffs Formation overlies the Freshwater East conglomerates, seen in previous photos, and spans the boundary between the Silurian and Devonian periods. It consists of red mudstones and siltstones with occasional thin sandstone beds. These were deposited on a low-reflief floodplain at the edge of an arid continental margin, the sandstones being deposited by seasonal braided streams, the muds and silts deposited in ephemeral marginal lakes. When not inundated, the muds and silts developed carbonate-rich calcrete (caliche) soil horizons along dessication cracks, burrows and early plant root systems.
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