Little Haven - The Settlands; detail of incompeten…
Little Haven - The Settlands; detail of incompeten…
Little Haven - The Settlands; detail of overturned…
Little Settlands - incompetent deformation 2
Little Settlands - incompetent deformation 1
Little Settlands - inverted thin coals and disturb…
The Settlands sand trees 1
The Settlands sand trees 2
Conglomerates at Gravel Bay
Conglomerate at Gravel Bay: close-up view 1
Conglomerate at Gravel Bay: close-up view 2
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Druidston Haven: Cliff Section 6
Druidston Haven: Cliff Section 6 interpretation
Druidston Haven: Cliff Section 5
Druidston Haven: Cliff Section 5 interpretation
Druidston Haven: Cliff Section 4
Little Haven - The Settlands; recumbent fold, thru…
Little Haven - The Settlands; recumbent fold, thru…
Little Haven - The Settlands panorama - geological…
Fox Hole Anticline - northern limb jointing with c…
Little Haven - Fox Hole Anticline
Little Haven north side panorama
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Trefrane Cliff Colliery chimney 2
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Pentre Ifan
1/160 • f/7.1 • 20.0 mm • ISO 100 •
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EF-S15-85mm f/3.5-5.6 IS USM
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Little Haven - The Settlands; detail of southern anticline
Structural geology of Little Haven and The Settlands
The cliffs from Little Haven to Broad Haven (and northward) display a spectacular range of geological structures, folding, faulting and thrusting, mainly in the Lower Coal Measures. The relatively weak mudstone and shale-dominated sequences show much incompetent deformation: tight, thrusted and overturned folds, in contrast to the thicker, stronger, sandstones which have formed relatively open and concentric folds.
This is a closer view of the small anticline at the southern end of The Settlands. This open, concentric fold is comprised mostly of strong, competent sandstones in the core, overlain by dark shaly beds. The sandsones may possibly be correlated with the sandstones in the large and well-developed Fox Hole anticline situated immediately to the south (right), althought there is a significant fault between the two features and the correlation is by no means certain.
The cliffs from Little Haven to Broad Haven (and northward) display a spectacular range of geological structures, folding, faulting and thrusting, mainly in the Lower Coal Measures. The relatively weak mudstone and shale-dominated sequences show much incompetent deformation: tight, thrusted and overturned folds, in contrast to the thicker, stronger, sandstones which have formed relatively open and concentric folds.
This is a closer view of the small anticline at the southern end of The Settlands. This open, concentric fold is comprised mostly of strong, competent sandstones in the core, overlain by dark shaly beds. The sandsones may possibly be correlated with the sandstones in the large and well-developed Fox Hole anticline situated immediately to the south (right), althought there is a significant fault between the two features and the correlation is by no means certain.
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