The Torridonian is a sedimentary sandstone which sits on top of the earliest rocks in Scotland. The map shows the sandstone as orange: it is on the western edge of the mainland, and on part of Skye. Geographically, this is part of the district of Wester Ross.
The sandstone is the earliest sedimentary rock in this part of the world. Under it lies much older gneiss known as the Lewisian complex. All the rock under the sandstone is igneous and metamorphosed igneous rock.
The sandstones are red beds laid down by rivers and lakes in a landscape of low rocky hills. A great thickness of red sandstone, brought in by rivers, buried the old hills. This took place in the Proterozoic, 1,200 to 544 million years ago (mya). There are older and younger sandstone groups, with a long period between them. The lower sandstone is a breccia, with broken fragments of earlier rocks.
References[change | change source]
- Park R.G; Stewart A.D. & Wright D.T. 2003. "3. The Hebridean terrane". In Trewin N.H.. The Geology of Scotland. London: Geological Society. pp. 45–61. . http://books.google.com/?id=ObdepEp9r7kC&pg=PA45&dq=%22hebridean+terrane%22+park+lewisian+torridon&cd=1#v=onepage&q=%22hebridean%20terrane%22%20park%20lewisian%20torridon&f=false. Retrieved 23 June 2010.
- Stewart A.D. 2002. The later Proterozoic Torridonian rocks of Scotland: their sedimentology, geochemistry and origin. Memoir. 24. London: Geological Society. . http://books.google.com/?id=4zICB4tt6joC&pg=PA3&lpg=PA3&dq=%22sleat+group%22+sedimentology#v=onepage&q=%22sleat%20group%22%20sedimentology&f=false.