Loch Duartmore, Sutherland
Sheared Lewisian Gneiss
Sheared Lewisian Gneiss (close-up view)
The 'Multi-couloured Rock Stop' information board
The 'Multi-couloured Rock Stop' detail 2
The 'Multi-couloured Rock Stop' detail 1
Quinag and Loch a' Chàirn an Bhàin
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.
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
Loch Cùl Fraioch and the Torridonian mountains
Stoer cloudscape
Sunny Culkein
Suilven from Sìdhean Mòr
Landscape with clouds
Stoer Head lighthouse
Old Man of Stoer
Location
Lat, Lng:
You can copy the above to your favourite mapping app.
Address: unknown
You can copy the above to your favourite mapping app.
Address: unknown
See also...
Keywords
Authorizations, license
-
Visible by: Everyone -
All rights reserved
-
1 375 visits
'Multi-coloured Rock Stop' panoramic view


A panoramic view of the 'Multicoloured Rock Stop' taken from the lay-by on the A838 near Laxford Bridge, Sutherland. Made from 4 photos stitched together.
The rock cutting offers superb exposures of the cross-cutting relationships and deformational history of the Lewisian gneiss, 'Scourie' dykes and later Laxfordian granite pegmatite sheet-like intrusions.
There is an information board in the lay-by with diagrams and a concise explanation here...

... but more details are given in Goodenough and Krabbendam (2011), below.
"Grey quartzo-feldspathic gneisses show a well-developed gneissosity, dipping gently south. Dark-green to black amphibolite-bearing basic sheets also dip gently south and are approximately parallel to the gneissosity. However, detailed examination... shows that the basic sheets have cross-cutting relationships with the gneiss. The basic sheets are probably Scourie Dykes ... but have been deformed into sub-parallelism to the gneissosity by later deformation. Both the gneisses and the basic sheets are cut by a swarm of pegmatitic granite sheets, some of which show boudinage. One of the granite sheets has been dated at c. 1855 Ma."
(Goodenough, K. M. & Krabbendam, M. (eds.), 2011. A geological excursion guide to the north-west Highlands of Scotland, British Geological Survey, Edinburgh. p.205)
The rock cutting offers superb exposures of the cross-cutting relationships and deformational history of the Lewisian gneiss, 'Scourie' dykes and later Laxfordian granite pegmatite sheet-like intrusions.
There is an information board in the lay-by with diagrams and a concise explanation here...

... but more details are given in Goodenough and Krabbendam (2011), below.
"Grey quartzo-feldspathic gneisses show a well-developed gneissosity, dipping gently south. Dark-green to black amphibolite-bearing basic sheets also dip gently south and are approximately parallel to the gneissosity. However, detailed examination... shows that the basic sheets have cross-cutting relationships with the gneiss. The basic sheets are probably Scourie Dykes ... but have been deformed into sub-parallelism to the gneissosity by later deformation. Both the gneisses and the basic sheets are cut by a swarm of pegmatitic granite sheets, some of which show boudinage. One of the granite sheets has been dated at c. 1855 Ma."
(Goodenough, K. M. & Krabbendam, M. (eds.), 2011. A geological excursion guide to the north-west Highlands of Scotland, British Geological Survey, Edinburgh. p.205)
(deleted account) has particularly liked this photo
- Keyboard shortcuts:
Jump to top
RSS feed- Latest comments - Subscribe to the comment feeds of this photo
- ipernity © 2007-2025
- Help & Contact
|
Club news
|
About ipernity
|
History |
ipernity Club & Prices |
Guide of good conduct
Donate | Group guidelines | Privacy policy | Terms of use | Statutes | In memoria -
Facebook
Twitter
Sign-in to write a comment.