Marros west - cryogenic anticline and solifluction…
Marros west - cryogenic anticline and solifluction…
St Brides Haven solifluction deposit
Spurn Neck Basement Till and peaty layer
Spurn Neck close-up of peaty layer
Stac Pollaidh west end
Gathering Hill from the Snake Pass summit, Derbysh…
Canisp from Creag Dharaich
Suilven from Creag Dharaich
Evening over the Lewisian Foreland
Quinag: Torridonian Sandstone pavement and Sàil Gh…
Quinag: Spidean Còinich and Lochan Bealach Cornadh
Quinag: start of the walk in
Quinag: Bealach a' Chornaidh
Lewisian foreland from Stac Pollaidh
Suilven from Stac Pollaidh ridge
The spires of Stac Pollaidh
Quinag: Sàil Gharbh - south-west approach to the s…
View SE to Rough Tor
View E from Brown Willy
View SW from Rough Tor
Small tor on Rough Tor
Rough Tor from Little Rough Tor cairn
Rough Tor from Little Rough Tor
Showery Tor 3
Showery Tor 2
Showery Tor 1
1/80 • f/8.0 • 15.0 mm • ISO 100 •
Canon EOS 600D
EF-S15-85mm f/3.5-5.6 IS USM
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Marros west - Teague's Wood and drift-filled valley
Marros Sands to Amroth
Just east of Amroth, we cross the county boundary into Carmarthenshire. The fine beach of Marros Sands, some 4 km east of Amroth is relatively isolated between Telpyn Point and Ragwen Point. There is no road access; the only way to get here is along the coastal paths, along the beach at lowest tide, or by boat.
At the western end of Marros Sands the Teague's Wood valley cuts down to the beach. The valley centre is filled with solifluction deposits ('Head') formed by freeze-thaw cycles of permafrost melting and refreezing at the end of the last glacial period (Devensian).
Just east of Amroth, we cross the county boundary into Carmarthenshire. The fine beach of Marros Sands, some 4 km east of Amroth is relatively isolated between Telpyn Point and Ragwen Point. There is no road access; the only way to get here is along the coastal paths, along the beach at lowest tide, or by boat.
At the western end of Marros Sands the Teague's Wood valley cuts down to the beach. The valley centre is filled with solifluction deposits ('Head') formed by freeze-thaw cycles of permafrost melting and refreezing at the end of the last glacial period (Devensian).
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