Minden Pictures

Results for
- Variscan
(26)

Angular unconformity, marking two very distinct geologic periods, where the rocks formed under very different conditions. This shows a Variscan unconformity between the highly-folded greywackes and sh...

90827235

90827235 Angular unconformity, marking two very distinct geologic periods, where the rocks formed under very different conditions. This shows a Variscan unconformity between the highly-folded greywackes and sh...© Luis Quinta

Angular unconformity on the coast. Marking two very distinct geologic periods, where the rocks formed under very different conditions. This shows a Variscan unconformity between the highly-folded grey...

90827233

90827233 Angular unconformity on the coast. Marking two very distinct geologic periods, where the rocks formed under very different conditions. This shows a Variscan unconformity between the highly-folded grey...© Luis Quinta

Angular unconformity on the coast. Marking two very distinct geologic periods, where the rocks formed under very different conditions, Ponta do Telheiro, Portugal. This shows a Variscan unconformity b...

90827232

90827232 Angular unconformity on the coast. Marking two very distinct geologic periods, where the rocks formed under very different conditions, Ponta do Telheiro, Portugal. This shows a Variscan unconformity b...© Luis Quinta

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

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

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

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

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

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

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

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

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

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 sandstone and shale (Culm Measures) deformed by compression during the Variscan or Hercynian orogeny, a geologic mountain-building event caused by Late Paleozoic continental c...

90795759

90795759 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 continental c...© 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

90773378

90773378 Small anticlinal fold in Carboniferous, Coal Measures rocks. Broad Haven, Pembrokeshire, Wales, UK, May.© Graham Eaton

90773377

90773377 Small anticlinal fold in carboniferous, Coal Measures rocks, Broad Haven, Pembrokeshire, Wales, UK, May.© Graham Eaton

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

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

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

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