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The Blue Lagoon at the Silfra Canyon where substrates are separated by a freshwater spring and where the Eurasian and American tectonic plates meet, Thingvellir National Park, Iceland June 2014  -  Michael Pitts/ npl
90675276
90675276 The Blue Lagoon at the Silfra Canyon where substrates are separated by a freshwater spring and where the Eurasian and American tectonic plates meet, Thingvellir National Park, Iceland June 2014© Michael Pitts / NPL
Silfra Canyon, deep fault filled with fresh water in the rift valley between the Eurasian and American tectonic plates, at Thingvellir National Park, Iceland June 2014  -  Michael Pitts/ npl
90675275
90675275 Silfra Canyon, deep fault filled with fresh water in the rift valley between the Eurasian and American tectonic plates, at Thingvellir National Park, Iceland June 2014© Michael Pitts / NPL
Diver exploring the Silfra Canyon, deep fault filled with fresh water in the rift valley between the Eurasian and American tectonic plates, at Thingvellir National Park, Iceland June 2014  -  Michael Pitts/ npl
90675274
90675274 Diver exploring the Silfra Canyon, deep fault filled with fresh water in the rift valley between the Eurasian and American tectonic plates, at Thingvellir National Park, Iceland June 2014© Michael Pitts / NPL
Lateral moraine deposit at edge of Findel Glacier. Glacier in retreat with braided stream below. Zermatt, Valais, Switzerland. September 2019.
90853385
90853385 Lateral moraine deposit at edge of Findel Glacier. Glacier in retreat with braided stream below. Zermatt, Valais, Switzerland. September 2019.©
Medial moraine between two glaciers, the slight difference in speed of the glaciers results in curved drag patterns in the ice, aerial view. Lower Theodul Glacier, Zermatt, Valais, Switzerland. Septem...
90853382
90853382 Medial moraine between two glaciers, the slight difference in speed of the glaciers results in curved drag patterns in the ice, aerial view. Lower Theodul Glacier, Zermatt, Valais, Switzerland. Septem...©
Lateral moraine deposited at edge of Findel glacier. Glacier in retreat with braided river in valley, Matterhorn in distance. Zermatt, Valais, Switzerland. September 2019.
90853379
90853379 Lateral moraine deposited at edge of Findel glacier. Glacier in retreat with braided river in valley, Matterhorn in distance. Zermatt, Valais, Switzerland. September 2019.©
Glacial striations on rock near snout of Findel Glacier, created by abrasion at base of glacier when rocks are dragged over the bedrock. Zermatt, Valais, Switzerland. September 2019.
90853373
90853373 Glacial striations on rock near snout of Findel Glacier, created by abrasion at base of glacier when rocks are dragged over the bedrock. Zermatt, Valais, Switzerland. September 2019.©
Cwm Pen Llafar, u-shaped valley with meandering Afon Llafar river. View from Carnedd Dafydd towards Bethesda, Snowdonia National Park, Wales, UK. June 2019.
90853366
90853366 Cwm Pen Llafar, u-shaped valley with meandering Afon Llafar river. View from Carnedd Dafydd towards Bethesda, Snowdonia National Park, Wales, UK. June 2019.©
The Green Bridge of Wales, a natural rock arch comprising Carboniferous limestone, Castlemartin, Pembrokeshire, Wales. September 2017.
90817157
90817157 The Green Bridge of Wales, a natural rock arch comprising Carboniferous limestone, Castlemartin, Pembrokeshire, Wales. September 2017.© Graham Eaton
The Green Bridge of Wales, a natural rock arch comprising Carboniferous limestone, Castlemartin, Pembrokeshire, Wales. September 2017.
90817156
90817156 The Green Bridge of Wales, a natural rock arch comprising Carboniferous limestone, Castlemartin, Pembrokeshire, Wales. September 2017.© Graham Eaton
A wave-cut platform in Jurassic age, Liassic limestones (Blue Lias). Jointing and erosion patterns can be seen that have contributed to the break-up of the scattered boulders. Southerndown, South Glam...
90817147
90817147 A wave-cut platform in Jurassic age, Liassic limestones (Blue Lias). Jointing and erosion patterns can be seen that have contributed to the break-up of the scattered boulders. Southerndown, South Glam...© Graham Eaton
Wave-cut platform in Jurassic age, Liassic limestones (Blue Lias). Jointing and erosion patterns can be seen that have contributed to the break-up of the scattered boulders. Southerndown, South Glamor...
90817146
90817146 Wave-cut platform in Jurassic age, Liassic limestones (Blue Lias). Jointing and erosion patterns can be seen that have contributed to the break-up of the scattered boulders. Southerndown, South Glamor...© Graham Eaton
Wave cut notch at the base of a sea cliff, Burton Bradstock, Dorset, UK. The notch is eroded at beach level in cliffst of Jurassic, Bridport Sandstone. The notch will grow to a depth where the overlyi...
90817145
90817145 Wave cut notch at the base of a sea cliff, Burton Bradstock, Dorset, UK. The notch is eroded at beach level in cliffst of Jurassic, Bridport Sandstone. The notch will grow to a depth where the overlyi...© Graham Eaton
A glacial erratic of Silurian age sandstone, perched upon younger Carboniferous age limestones. The limestone forms a limestone pavement with the hill , Whernside, Yorkshire, England, UK.
90817143
90817143 A glacial erratic of Silurian age sandstone, perched upon younger Carboniferous age limestones. The limestone forms a limestone pavement with the hill , Whernside, Yorkshire, England, UK.© Graham Eaton
Glacial erratic of Silurian age sandstone, perched upon youger Carboniferous age limestones. The limestones form a limestone pavement with the hill Ingleborough in the background. Whernside, Yorkshire...
90817142
90817142 Glacial erratic of Silurian age sandstone, perched upon youger Carboniferous age limestones. The limestones form a limestone pavement with the hill Ingleborough in the background. Whernside, Yorkshire...© Graham Eaton
Roche moutonnee or Sheep's back at the head, Nant Ffrancon Valley, Snowdonia, Wales, UK, November. The rock is carved by ice moving down the valley leaving a relatively smooth back edge and top, w...
90817137
90817137 Roche moutonnee or Sheep's back at the head, Nant Ffrancon Valley, Snowdonia, Wales, UK, November. The rock is carved by ice moving down the valley leaving a relatively smooth back edge and top, w...© 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
An anticline in deformed Carboniferous sandstones and shale (Culm Measures) near Bude, Cornwall, UK, March. These rocks were deformed during the Hercynian or Variscan Orogeny, a mountain building even...
90795867
90795867 An anticline in deformed Carboniferous sandstones and shale (Culm Measures) near Bude, Cornwall, UK, March. These rocks were deformed during the Hercynian or Variscan Orogeny, a mountain building even...© Graham Eaton
Karst landscape in Carboniferous (Dinantian) Limestone, with Clints and Grykes developed on a limestone pavement. Malham, Yorkshire, UK, May
90795866
90795866 Karst landscape in Carboniferous (Dinantian) Limestone, with Clints and Grykes developed on a limestone pavement. Malham, Yorkshire, UK, May© Graham Eaton
A box fold formed by intersecting kink folds in Carboniferous age Sandstones and Shales (Culm Measures) at Menanchrurch near Bude, Cornwall, March. The deformation of the rocks formed during the Varis...
90795825
90795825 A box fold formed by intersecting kink folds in Carboniferous age Sandstones and Shales (Culm Measures) at Menanchrurch near Bude, Cornwall, March. The deformation of the rocks formed during the Varis...© Graham Eaton
Chevron folded Carboniferous age sandstone and shale (Culm Measures), deformed by compression during the Variscan or Hercynian orogeny, a geologic mountain-building event caused by Late Paleozoic cont...
90795824
90795824 Chevron folded Carboniferous age sandstone and shale (Culm Measures), deformed by compression during the Variscan or Hercynian orogeny, a geologic mountain-building event caused by Late Paleozoic cont...© Graham Eaton
A Limestone Pavement with well developed Clints (blocks) and Grykes (gaps). This is Carboniferous age limestone, part of a large area of Karst above Austwick, Yorkshire, UK. Slightly acidic rainfall,...
90795823
90795823 A Limestone Pavement with well developed Clints (blocks) and Grykes (gaps). This is Carboniferous age limestone, part of a large area of Karst above Austwick, Yorkshire, UK. Slightly acidic rainfall,...© Graham Eaton
A Limestone Pavement with well developed Clints (blocks) and Grykes (gaps). This is Carboniferous age limestone, part of a large area of Karst above Austwick, Yorkshire, UK. Slightly acidic rainfall,...
90795822
90795822 A Limestone Pavement with well developed Clints (blocks) and Grykes (gaps). This is Carboniferous age limestone, part of a large area of Karst above Austwick, Yorkshire, UK. Slightly acidic rainfall,...© 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
Chevron recumbent foldeding in Carboniferous age sandstone and shale (Culm Measures), deformed by compression during the Variscan or Hercynian orogeny, a geologic mountain-building event caused by Lat...
90795810
90795810 Chevron recumbent foldeding in Carboniferous age sandstone and shale (Culm Measures), deformed by compression during the Variscan or Hercynian orogeny, a geologic mountain-building event caused by Lat...© Graham Eaton
Chevron recumbent foldeding in Carboniferous age sandstone and shale (Culm Measures), deformed by compression during the Variscan or Hercynian orogeny, a geologic mountain-building event caused by Lat...
90795809
90795809 Chevron recumbent foldeding in Carboniferous age sandstone and shale (Culm Measures), deformed by compression during the Variscan or Hercynian orogeny, a geologic mountain-building event caused by Lat...© 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
Small Waterfalls at Sandy Mouth beach, near Bude, Cornwall, UK, March. The rocks are steeply dipping Carboniferous age, sandstone and shale (Culm Measures).
90795805
90795805 Small Waterfalls at Sandy Mouth beach, near Bude, Cornwall, UK, March. The rocks are steeply dipping Carboniferous age, sandstone and shale (Culm Measures).© Graham Eaton
A small waterfall at Sandy Mouth beach, near Bude, Cornwall, UK, March. The rocks are steeply dipping Carboniferous age, sandstone and shale (Culm Measures).
90795804
90795804 A small waterfall at Sandy Mouth beach, near Bude, Cornwall, UK, March. The rocks are steeply dipping Carboniferous age, sandstone and shale (Culm Measures).© Graham Eaton
The granite outcrop of Great Staple Tor, Princetown, Dartmoor, Devon, UK, May
90795798
90795798 The granite outcrop of Great Staple Tor, Princetown, Dartmoor, Devon, UK, May© Graham Eaton
Quartz infilled tension cracks in a boulder on the beach. Millock Haven, Cornwall, UK, March
90795796
90795796 Quartz infilled tension cracks in a boulder on the beach. Millock Haven, Cornwall, UK, March© Graham Eaton
A thrust fault in Carboniferous age Sandstones and shales (Culm Measures) at Crackington Haven, near Bude, Cornwall, March. The rocks comprise the Crackington Formation of thinly bedded turbidite sand...
90795792
90795792 A thrust fault in Carboniferous age Sandstones and shales (Culm Measures) at Crackington Haven, near Bude, Cornwall, March. The rocks comprise the Crackington Formation of thinly bedded turbidite sand...© Graham Eaton
A thrust fault in Carboniferous age Sandstones and shales (Culm Measures) at Crackington Haven, near Bude, Cornwall, March. The rocks comprise the Crackington Formation of thinly bedded turbidite sand...
90795791
90795791 A thrust fault in Carboniferous age Sandstones and shales (Culm Measures) at Crackington Haven, near Bude, Cornwall, March. The rocks comprise the Crackington Formation of thinly bedded turbidite sand...© Graham Eaton
A small relay thrust fault in steeply dipping Carboniferous age Sandstones and shales (Culm Measures) near Bude, Cornwall, March.
90795790
90795790 A small relay thrust fault in steeply dipping Carboniferous age Sandstones and shales (Culm Measures) near Bude, Cornwall, March.© Graham Eaton
An anticlinal fold in Carboniferous age sandstone and shales. This angular anticline is a kink fold with a defined fracture along the fold axis. These rocks were folded and faulted during the Variscan...
90795786
90795786 An anticlinal fold in Carboniferous age sandstone and shales. This angular anticline is a kink fold with a defined fracture along the fold axis. These rocks were folded and faulted during the Variscan...© Graham Eaton
Vertically dipping Cretaceous Chalk exposed at Bat's Head, near Weymouth, Dorset UK. Isolated from the headland is a small sea stack that once formed part of main cliff. A natural arch at the base...
90795785
90795785 Vertically dipping Cretaceous Chalk exposed at Bat's Head, near Weymouth, Dorset UK. Isolated from the headland is a small sea stack that once formed part of main cliff. A natural arch at the base...© Graham Eaton
Steeply dipping beds of Carboniferous age sandstone and shales (Culm measures) on the flank of a large fold. This deformation was formed by compression during the Variscan or Hercynian orogeny, a geol...
90795784
90795784 Steeply dipping beds of Carboniferous age sandstone and shales (Culm measures) on the flank of a large fold. This deformation was formed by compression during the Variscan or Hercynian orogeny, a geol...© 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
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
Folded Carboniferous age sandstone and shale (Culm Measures) in plan view, deformed by compression during the Variscan or Hercynian orogeny, a geologic mountain-building event caused by Late Paleozoic...
90795775
90795775 Folded Carboniferous age sandstone and shale (Culm Measures) in plan view, deformed by compression during the Variscan or Hercynian orogeny, a geologic mountain-building event caused by Late Paleozoic...© Graham Eaton
A Glacial Erratic at Norber near Austwick, Yorkshire, UK. This is one of the Norber erratics, where blocks of older Silurian sandstone were left on top of younger Carboniferous limestone by a retreati...
90795774
90795774 A Glacial Erratic at Norber near Austwick, Yorkshire, UK. This is one of the Norber erratics, where blocks of older Silurian sandstone were left on top of younger Carboniferous limestone by a retreati...© Graham Eaton
A Glacial Erratic at Norber near Austwick, Yorkshire, UK. This is one of the Norber erratics, where blocks of older Silurian sandstone were left on top of younger Carboniferous limestone by a retreati...
90795773
90795773 A Glacial Erratic at Norber near Austwick, Yorkshire, UK. This is one of the Norber erratics, where blocks of older Silurian sandstone were left on top of younger Carboniferous limestone by a retreati...© 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
Folded Carboniferous age sandstone and shale (Culm Measures) in plan view, deformed by compression during the Variscan or Hercynian orogeny, a geologic mountain-building event caused by Late Paleozoic...
90795768
90795768 Folded Carboniferous age sandstone and shale (Culm Measures) in plan view, deformed by compression during the Variscan or Hercynian orogeny, a geologic mountain-building event caused by Late Paleozoic...© Graham Eaton
An anticlinal fold in Carboniferous age sandstone and shales. This fold and deformation was formed by compression during the Variscan or Hercynian orogeny, a geologic mountain-building event caused by...
90795767
90795767 An anticlinal fold in Carboniferous age sandstone and shales. This fold and deformation was formed by compression during the Variscan or Hercynian orogeny, a geologic mountain-building event caused by...© Graham Eaton
Folded Carboniferous age sandstones, Hartland Quay, Devon, UK, May
90795766
90795766 Folded Carboniferous age sandstones, Hartland Quay, Devon, UK, May© Graham Eaton
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