Little Settlands - incompetent deformation 1
Little Settlands - incompetent deformation 2
Little Settlands - inverted thin coals and disturb…
The Settlands sand trees 1
The Settlands sand trees 2
The Settlands sand trees 3
Marros Sands
Marros Sands panorama
Marros Sands and Top Castle hill fort panorama
Marros west cliffs
Telpyn-Marros panorama
Marros west - Teague's Wood and drift-filled valle…
Marros west - cryogenic anticline and solifluction…
Marros west - cryogenic anticline and solifluction…
West of Telpyn Point - fault in Telpyn Point Sands…
Cliff section east of Amroth 1
Cliff section east of Amroth 2
Limb Valley Autumn beeches panorama
Limb Valley Autumn trees panorama
Limb Valley Autumn trees
View south from Dunstaffnage Castle near Oban, Sco…
Ben Cruachan from Dunstaffnage Castle
Dunstaffnage Castle gatehouse top floor
Little Haven - The Settlands; detail of incompeten…
Little Haven - The Settlands; detail of incompeten…
Little Haven - The Settlands; detail of southern a…
Little Haven - The Settlands; recumbent fold, thru…
Little Haven - The Settlands; recumbent fold, thru…
Little Haven - The Settlands panorama - geological…
Little Haven - The Settlands panorama
Fox Hole Anticline - northern limb with mine adit
Fox Hole Anticline - northern limb jointing with c…
Fox Hole Anticline - northern limb 3
Fox Hole Anticline - northern limb 2
Fox Hole Anticline - northern limb
Little Haven - Fox Hole Anticline
Little Haven north side geological interpretation
Little Haven north side panorama
Little Haven view north over Rooks Bay and The Set…
The Settlands at Little Haven from coastal path
Newgale Sands 3
Small Copper at Trefrane Cliff Colliery
Trefrane Cliff Colliery chimney 4
Trefrane Cliff Colliery chimney 3
Trefrane Cliff Colliery chimney 2
1/160 • f/7.1 • 15.0 mm • ISO 200 •
Canon EOS 600D
EF-S15-85mm f/3.5-5.6 IS USM
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Coasts of the sea: animals, vegetation and coastal geology
Coasts of the sea: animals, vegetation and coastal geology
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Little Haven - The Settlands; detail of overturned 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 close-up view of the prominent overturned, nearly recumbent, chevron-style anticline at the northern end of The Settlands. The relatively weak mudstone and shale sequence has deformed incompetently, with some thickening in the hinge zone.The dark shale bed just below the centre of the photo is at the horizon of the Amman Marine Band.
The overturned northern limb of the fold is separated from the nearly horizontal upper limb by a near-horizontal thrust. Below this thrust, disturbed, separate, repeated portions of the hinge zone are visible, one of which has developed axial planar cleavage in the grey seatearth with brown ironstone bands and nodules.
Above the anticline, another significant, higher, thrust has carried more sandy beds over the top.
See notes for individual descriptions of areas on the photo.
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 close-up view of the prominent overturned, nearly recumbent, chevron-style anticline at the northern end of The Settlands. The relatively weak mudstone and shale sequence has deformed incompetently, with some thickening in the hinge zone.The dark shale bed just below the centre of the photo is at the horizon of the Amman Marine Band.
The overturned northern limb of the fold is separated from the nearly horizontal upper limb by a near-horizontal thrust. Below this thrust, disturbed, separate, repeated portions of the hinge zone are visible, one of which has developed axial planar cleavage in the grey seatearth with brown ironstone bands and nodules.
Above the anticline, another significant, higher, thrust has carried more sandy beds over the top.
See notes for individual descriptions of areas on the photo.
Fred Fouarge has particularly liked this photo
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