Sky, sea, beach and marshes
Cliffs of composed of Otter Sandstone, Budleigh Sa…
Budleigh Salterton Pebble Beds
Budleigh Salterton Pebble Beds - faulted
Load structures on turbidite sandstones, Crooklets…
Load structures on turbidite sandstones, Crooklets…
Quinag: Sàil Gharbh - south-west approach to the s…
The Buck Stone, Staunton, Forest of Dean, Gloucest…
The Buck Stone, Staunton, Forest of Dean, Gloucest…
'Pipe Rock' at Skiag Bridge, Loch Assynt, Sutherla…
'Pipe Rock' at Skiag Bridge, Loch Assynt, Sutherla…
'Pipe Rock' at Skiag Bridge, Loch Assynt, Sutherla…
Storm beach at Aberbach, Pembrokeshire, Wales.
Suilven from Stac Pollaidh ridge
Quinag and Loch a' Chàirn an Bhàin
Quinag: start of the walk in
Quinag: Spidean Còinich
Quinag: Spidean Còinich and Lochan Bealach Cornadh
Quinag: Spidean Còinich from Sàil Gharbh summit
Quinag: Cambrian Basal Quartzite - Torridonian unc…
Quinag: Cambrian Basal Quartzite - Torridonian unc…
Canisp from Creag Dharaich
Benacre Cliffs - Westleton Formation
Chavery Coal and roof measures, Duckmanton Railway…
Vertical bedding slab at Northcott Mouth, Cornwall…
Little Barton Strand sole structures
Crackington Haven sole structures 2
Crackington Haven sole structures 1
Millook Haven cliff detail 6
Upside-down rocks at Millook Haven, Cornwall
Angular unconformity at Horton-in-Ribblesdale
Burton Cliff near sunset 2
Burton Cliff near sunset 1
Gold and indigo convergence, Burton Cliff
Burton Cliff golden light 2
Burton Cliff golden light 1
Aberystwyth Grits
Peat section in the Skipsea Withow Mere, Holdernes…
Skipsea Withow Mere, Holderness coast, East Yorksh…
Porth Selau sands 2
Porth Selau sands
Hay Wood quarry cross bedding
Froggatt Edge cross bedding
Erosion surface
White Edge 1
1/13 • f/11.0 • 20.0 mm • ISO 800 •
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Chavery Coal and roof strata, Duckmanton Railway Cutting
This is the Duckmanton Railway Cutting Site of Special Scientific Interest, near Chesterfield, north-east Derbyshire. In the lower part of the section is the Chavery Coal, overlain by shaly mudstones containing non-marine bivalves and ostracods. This exposure of the Chavery coal was worked (illegally) by desperate miners during the 1984-85 miners' strike. (Chris Darmon, pers. comm.)
The railway cutting is a site of international geological importance, as it contains the stratotype section for the Anthracoceras vanderbeckei (Clay Cross) marine band which is the boundary between the Langsettian and Duckmantian Stages of the Carboniferous, informally the junction between the Lower and Middle Coal Measures.
The site is managed by the Derbyshire Wildlife Trust and is accessible by permit only.
www.derbyshirewildlifetrust.org.uk/reserves/duckmanton-railway-cutting
The railway cutting is a site of international geological importance, as it contains the stratotype section for the Anthracoceras vanderbeckei (Clay Cross) marine band which is the boundary between the Langsettian and Duckmantian Stages of the Carboniferous, informally the junction between the Lower and Middle Coal Measures.
The site is managed by the Derbyshire Wildlife Trust and is accessible by permit only.
www.derbyshirewildlifetrust.org.uk/reserves/duckmanton-railway-cutting
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