Kylesku and the Stack of Glencoul
Loch Glencoul panorama
Glencoul geological interpretation
Traeth Llyfn rock ridges, Pembrokeshire
Traeth Llyfn, Pembrokeshire
Lichen at Traeth Llyfn in the late afternoon sun
The Blasted Heath
Calum's Road with wheelbarrow, Raasay
Quinag: Bealach a' Chornaidh
Quinag: start of the walk in
Quinag: Spidean Còinich
Quinag: Sàil Gharbh
Quinag: Skyscape over the Assynt Culmination
Quinag: looking to the Glencoul thrust and beyond
Quinag: looking to Ben More Assynt
Quinag: Sàil Gharbh south-east face.
Quinag: Spidean Còinich and Lochan Bealach Cornadh
Quinag: Spidean Còinach panorama
Quinag: Through the bealach
Quinag: Torridonian Sandstone on Sàil Gharbh
Quinag: Torridonian Sandstone pavement and Sàil Gh…
Quinag: Sàil Gharbh summit shelter and trig point
Quinag: Spidean Còinich from Sàil Gharbh summit
The 'Multi-couloured Rock Stop' detail 1
The 'Multi-couloured Rock Stop' detail 2
The 'Multi-couloured Rock Stop' information board
Sheared Lewisian Gneiss (close-up view)
Sheared Lewisian Gneiss
Loch Duartmore, Sutherland
'Multi-coloured Rock Stop' panoramic view
The 'Multi-coloured Rock Stop', Loch na Fiacail, S…
Laxford Bay, Sutherland
Stronchrubie Crag and imbricate thrust zone, Inchn…
Achmelvich Bay north inlet, Sutherland
Stac Pollaidh summit ridge
Lewisian foreland from Stac Pollaidh
Cùl Mòr from Stac Pollaidh
Cloud over Cùl Mòr
Beinn Mhòr Coigich viewed from Stac Pollaidh
Suilven from Stac Pollaidh ridge
The spires of Stac Pollaidh
The South Face of Stac Pollaidh
Porth Maenmelyn, Pembrokeshire, Wales
Old path to beach, Porth Maenmelyn, Pembrokeshire
Pillow lavas at Porth Maenmelyn, Pembrokeshire
1/100 • f/7.1 • 30.0 mm • ISO 100 •
Canon EOS 350D DIGITAL
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Quinag and Loch a' Chàirn an Bhàin


The north faces of Sàil Ghorm (right) and Sàil Ghàrbh (left) , the two northern spurs of Quinag, with Loch a' Chàirn an Bhàin in the foreground, taken from near Kylestrome at grid ref. NC 21161 34782.
Quinag is comprised of Torridonian Sandstone resting unconformably on Lewisian Gneiss which forms the rough hummocky ground in the foreground and middle distance. The very summit of Sàil Ghàrbh is comprised of pale grey Cambrian Basal Quartzite, also resting unconformably on the Torridonian Sandstone. So there is a double unconformity in this photo.
Quinag is comprised of Torridonian Sandstone resting unconformably on Lewisian Gneiss which forms the rough hummocky ground in the foreground and middle distance. The very summit of Sàil Ghàrbh is comprised of pale grey Cambrian Basal Quartzite, also resting unconformably on the Torridonian Sandstone. So there is a double unconformity in this photo.
Colin Ashcroft has particularly liked this photo
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