Swallowtree Bay anticline-syncline couplet: detail…
Swallowtree Bay anticline-syncline couplet: detail…
Swallowtree Bay anticline-syncline couplet: detail…
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Summit of Houndkirk Hill looking NNE
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Swallowtree Bay anticline-syncline couplet: detail…
Swallowtree Bay anticline-syncline couplet: detail…
Swallowtree Bay anticline-syncline couplet: detail…
Swallowtree Bay anticline-syncline couplet: detail…
Swallowtree Bay anticline-syncline couplet: detail…
Swallowtree Bay anticline-syncline couplet
Syncline in Lower Coal Measures sandstones: Swallo…
Asymmetric anticline, Swallowtree Bay north
Ladies Cave Anticline: interior hinge zone
Ladies Cave Anticline
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Extentional faults detail: Saundersfoot south
Extentional faults: Saundersfoot south
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Druidston Haven: Cliff Section 4
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Druidston Haven: Cliff Section 6
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Gravel Bay - Moor Cliffs Formation
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Conglomerates at Gravel Bay
Conglomerate at Gravel Bay: close-up view 1
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Swallowtree Bay anticline-syncline couplet: detail 6
Saundersfoot to Swallowtree Bay geological structures
Detail view no.6 of the asymmetric anticline-syncline couplet in Lower Coal Measures sandstones and siltstones, just south of Swallowtree Bay.
This photo mainly shows the vertical limb of the fold couplet pair. The axis of the anticline is on the left. In the centre, the vertical limb is composed mainly of sandstones with thin darker silty laminae. The sandstone beds show a strong fracture fan cleavage perpendicular to the bedding, especially marked on this vertical limb of the fold.
I took this photo for the shapes, textures and colours as well as the geological interest, hence I omitted a scale object. The section shown is about 2 metres in height.
The photo of the entire structure is here:
Detail view no.6 of the asymmetric anticline-syncline couplet in Lower Coal Measures sandstones and siltstones, just south of Swallowtree Bay.
This photo mainly shows the vertical limb of the fold couplet pair. The axis of the anticline is on the left. In the centre, the vertical limb is composed mainly of sandstones with thin darker silty laminae. The sandstone beds show a strong fracture fan cleavage perpendicular to the bedding, especially marked on this vertical limb of the fold.
I took this photo for the shapes, textures and colours as well as the geological interest, hence I omitted a scale object. The section shown is about 2 metres in height.
The photo of the entire structure is here:
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