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    • Structural Geology
  • (35)
Minor normal or extensional faults exposed in the cliffs and also on the shore wave-cut platform. Nash Point, South Glamorgan Heritage Coast, Llantwit Major, Wales, UK. September 2017. The cliffs com...
90817163
90817163 Minor normal or extensional faults exposed in the cliffs and also on the shore wave-cut platform. Nash Point, South Glamorgan Heritage Coast, Llantwit Major, Wales, UK. September 2017. The cliffs com...© Graham Eaton
Bedding planes and joint network in Jurassic age Blue Lias limestone and shale exposed at low tide at Nash Point, South Glamorgan Heritage Coast, Wales, September 2017.
90817161
90817161 Bedding planes and joint network in Jurassic age Blue Lias limestone and shale exposed at low tide at Nash Point, South Glamorgan Heritage Coast, Wales, September 2017.© Graham Eaton
Several faults cutting through Jurassic age, Liassic Limestones (Blue Lias) near Southerndown, South Glamorgan Heritage Coast, Wales, UK. September. The faults can be seen displacing the bedding plane...
90817154
90817154 Several faults cutting through Jurassic age, Liassic Limestones (Blue Lias) near Southerndown, South Glamorgan Heritage Coast, Wales, UK. September. The faults can be seen displacing the bedding plane...© Graham Eaton
Faulted Jurassic age Liassic limestones (Blue Lias) exposed in the cliffs and on the foreshore. Southerndown, South Glamorgan Heritage Coast, Wales, UK. September
90817140
90817140 Faulted Jurassic age Liassic limestones (Blue Lias) exposed in the cliffs and on the foreshore. Southerndown, South Glamorgan Heritage Coast, Wales, UK. September© Graham Eaton
Conjugate kink bands in Carboniferous turbidite shales, Bude, Cornwall, UK, May
90795868
90795868 Conjugate kink bands in Carboniferous turbidite shales, Bude, Cornwall, UK, May© Graham Eaton
Load casts on the underside of a sandstone bed of Carboniferous age, Culm Measures (Bude Formation), Bude, Cornwall, UK, May.
90795821
90795821 Load casts on the underside of a sandstone bed of Carboniferous age, Culm Measures (Bude Formation), Bude, Cornwall, UK, May.© Graham Eaton
Load casts on the underside of a sandstone bed of Carboniferous age, Culm Measures (Bude Formation), Bude, Cornwall, UK, May.
90795820
90795820 Load casts on the underside of a sandstone bed of Carboniferous age, Culm Measures (Bude Formation), Bude, Cornwall, UK, May.© Graham Eaton
A monocline fold with a minor thrust fault in Carboniferous age sandstones, Bude, Cornwall, UK, May.
90795816
90795816 A monocline fold with a minor thrust fault in Carboniferous age sandstones, Bude, Cornwall, UK, May.© Graham Eaton
Tightly folded Pre-Cambrian age, Quartz Mica Schist, a metamorphic rock. These are ductile folds generated under compression. Rhoscolyn Wales, UK, June
90795811
90795811 Tightly folded Pre-Cambrian age, Quartz Mica Schist, a metamorphic rock. These are ductile folds generated under compression. Rhoscolyn Wales, UK, June© Graham Eaton
Recumbent folds in Carboniferous age sandstones and Shale (Bude Formation), Bude, Cornwall, UK, May. The rocks were deformed during the Hercynian Orogeny or mountain building event.
90795808
90795808 Recumbent folds in Carboniferous age sandstones and Shale (Bude Formation), Bude, Cornwall, UK, May. The rocks were deformed during the Hercynian Orogeny or mountain building event.© Graham Eaton
Recumbent folds in Carboniferous age sandstones and Shale (Bude Formation), Bude, Cornwall, UK, May. The rocks were deformed during the Hercynian Orogeny or mountain building event.
90795807
90795807 Recumbent folds in Carboniferous age sandstones and Shale (Bude Formation), Bude, Cornwall, UK, May. The rocks were deformed during the Hercynian Orogeny or mountain building event.© Graham Eaton
Tilted beds of Carboniferous age, Culm Measures (Bude Formation) Sandy Mouth, near Bude, Cornwall, UK, May
90795803
90795803 Tilted beds of Carboniferous age, Culm Measures (Bude Formation) Sandy Mouth, near Bude, Cornwall, UK, May© Graham Eaton
Sole marks on the underside of a bed of Carboniferous age, turbidite sandstone. Bude, Cornwall, UK, may. Sole marks are formed by flowing water or currents and can indicate the flow direction when the...
90795802
90795802 Sole marks on the underside of a bed of Carboniferous age, turbidite sandstone. Bude, Cornwall, UK, may. Sole marks are formed by flowing water or currents and can indicate the flow direction when the...© Graham Eaton
En echelon tension (or parallel) cracks in Carboniferous age turbidite sandstones, Bude, Cornwall, UK, May. The tension cracks have formed in the more competent sandstones as the rocks were folded. T...
90795795
90795795 En echelon tension (or parallel) cracks in Carboniferous age turbidite sandstones, Bude, Cornwall, UK, May. The tension cracks have formed in the more competent sandstones as the rocks were folded. T...© Graham Eaton
Tilted beds of sandstone and thin shales of the Carboniferous, Culm Measures (Bude Formation) Sandy Mouth near Bude, Cornwall, UK, May. The bed represent cycles of deposition associated with climate c...
90795783
90795783 Tilted beds of sandstone and thin shales of the Carboniferous, Culm Measures (Bude Formation) Sandy Mouth near Bude, Cornwall, UK, May. The bed represent cycles of deposition associated with climate c...© Graham Eaton
Tilted beds of Carboniferous age, Culm Measures (Bude Formation) sandstone and shale, Bude, Cornwall, UK, May.
90795782
90795782 Tilted beds of Carboniferous age, Culm Measures (Bude Formation) sandstone and shale, Bude, Cornwall, UK, May.© Graham Eaton
A Chevron or Kink fold anticline in Carboniferous age turbidite sediments. Bude, Cornwall, UK, may.
90795781
90795781 A Chevron or Kink fold anticline in Carboniferous age turbidite sediments. Bude, Cornwall, UK, may.© Graham Eaton
Ductile folding in Pre-Cambrian age, metamorphic, Chlorite Schist. Llyn, Wales, UK, May
90795780
90795780 Ductile folding in Pre-Cambrian age, metamorphic, Chlorite Schist. Llyn, Wales, UK, May© Graham Eaton
Crenulation cleavage developed in Pre-Cambrian age, metamorphic, Chlorite Schist. Llyn, Wales, UK, May
90795778
90795778 Crenulation cleavage developed in Pre-Cambrian age, metamorphic, Chlorite Schist. Llyn, Wales, UK, May© Graham Eaton
Crenulation cleavage developed in Pre-Cambrian age chlorite schist, a metamorphic rock Llyn, Wales, UK, May
90795777
90795777 Crenulation cleavage developed in Pre-Cambrian age chlorite schist, a metamorphic rock Llyn, Wales, UK, May© Graham Eaton
Tilted beds of sandstone and thin shales of the Carboniferous, Culm Measures (Bude Formation) Sandy Mouth near Bude, Cornwall, UK, May. The bed represent cycles of deposition associated with climate c...
90795776
90795776 Tilted beds of sandstone and thin shales of the Carboniferous, Culm Measures (Bude Formation) Sandy Mouth near Bude, Cornwall, UK, May. The bed represent cycles of deposition associated with climate c...© Graham Eaton
Small extension (normal) faults within a layer of shale between two layers of more competent sandstone. Carboniferous, turbidites, Bude, Cornwall, UK, May.
90795771
90795771 Small extension (normal) faults within a layer of shale between two layers of more competent sandstone. Carboniferous, turbidites, Bude, Cornwall, UK, May.© Graham Eaton
A small fault offsetting Carboniferous limestone that forms the side of a collapse arch. Penmon, Anglesey, Wales, UK, June
90795769
90795769 A small fault offsetting Carboniferous limestone that forms the side of a collapse arch. Penmon, Anglesey, Wales, UK, June© Graham Eaton
Folded Carboniferous age sandstones, Hartland Quay, Devon, UK, May
90795766
90795766 Folded Carboniferous age sandstones, Hartland Quay, Devon, UK, May© Graham Eaton
Monocline fold that has been faulted during the Variscan orogeny, in Carboniferous sandstone and shale. Broad Haven, Pembrokeshire, Wales, UK, May
90773380
90773380 Monocline fold that has been faulted during the Variscan orogeny, in Carboniferous sandstone and shale. Broad Haven, Pembrokeshire, Wales, UK, May© Graham Eaton
Large anticlinal fold, caused by deformation during the Variscan orogeny, in Carboniferous, Coal Measures sandstones and shale. Braod Haven, Pembrokeshire, Wales
90773379
90773379 Large anticlinal fold, caused by deformation during the Variscan orogeny, in Carboniferous, Coal Measures sandstones and shale. Braod Haven, Pembrokeshire, Wales© Graham Eaton
Small anticlinal fold in Carboniferous, Coal Measures rocks. Broad Haven, Pembrokeshire, Wales, UK, May.
90773378
90773378 Small anticlinal fold in Carboniferous, Coal Measures rocks. Broad Haven, Pembrokeshire, Wales, UK, May.© Graham Eaton
Small anticlinal fold in carboniferous, Coal Measures rocks, Broad Haven, Pembrokeshire, Wales, UK, May.
90773377
90773377 Small anticlinal fold in carboniferous, Coal Measures rocks, Broad Haven, Pembrokeshire, Wales, UK, May.© Graham Eaton
Monocline fold that has been faulted during the Variscan orogeny, in Carboniferous sandstone and shale. Broad Haven, Pembrokeshire, Wales, UK, May
90773222
90773222 Monocline fold that has been faulted during the Variscan orogeny, in Carboniferous sandstone and shale. Broad Haven, Pembrokeshire, Wales, UK, May© Graham Eaton
A monocline fold that has been faulted during the Variscan orogeny, in Carboniferous sandstone and shale. Broad Haven, Pembrokeshire, Wales, UK, May
90773221
90773221 A monocline fold that has been faulted during the Variscan orogeny, in Carboniferous sandstone and shale. Broad Haven, Pembrokeshire, Wales, UK, May© Graham Eaton
The Ladies Cave anticline, an asymmetric chevron fold formed during the Variscan orogeny, in Carboniferous, Westphalian, Lower Coal Measures, sediments. Saundersfoot, Pembrokeshire, Wales. June 2017
90773214
90773214 The Ladies Cave anticline, an asymmetric chevron fold formed during the Variscan orogeny, in Carboniferous, Westphalian, Lower Coal Measures, sediments. Saundersfoot, Pembrokeshire, Wales. June 2017© Graham Eaton
The Ladies Cave anticline, an asymmetric chevron fold formed during the Variscan orogeny, in Carboniferous, Westphalian, Lower Coal Measures, sediments. Saundersfoot, Pembrokeshire, Wales. June 2017
90773213
90773213 The Ladies Cave anticline, an asymmetric chevron fold formed during the Variscan orogeny, in Carboniferous, Westphalian, Lower Coal Measures, sediments. Saundersfoot, Pembrokeshire, Wales. June 2017© Graham Eaton
The Ladies Cave anticline, an asymmetric chevron fold formed during the Variscan orogeny, in Carboniferous, Westphalian, Lower Coal Measures, sediments. Saundersfoot, Pembrokeshire, Wales. June 2017
90773212
90773212 The Ladies Cave anticline, an asymmetric chevron fold formed during the Variscan orogeny, in Carboniferous, Westphalian, Lower Coal Measures, sediments. Saundersfoot, Pembrokeshire, Wales. June 2017© Graham Eaton
Small thrust fault in Ordovician age sedimentary rocks - geological feature caused by horizontal compression of rock layers, resulting in a low angle reverse fault. Cilan Head, Abersoch, Wales, UK. De...
90773208
90773208 Small thrust fault in Ordovician age sedimentary rocks - geological feature caused by horizontal compression of rock layers, resulting in a low angle reverse fault. Cilan Head, Abersoch, Wales, UK. De...© Graham Eaton
Angular unconformity, between the underlying Cambrian age sedimentary rocks and the overlying Ordovician sedimentary rocks.  Trwyn Wylfa, Abersoch, Wales, August. An unconformity represents a time ga...
90773192
90773192 Angular unconformity, between the underlying Cambrian age sedimentary rocks and the overlying Ordovician sedimentary rocks. Trwyn Wylfa, Abersoch, Wales, August. An unconformity represents a time ga...© Graham Eaton
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