The Devonian Period

 

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The Carboniferous Period

 

  • During the Devonian Period the Arran land mass was at a latitude of 0oN and the predominant environments  were fluviatile and lacustrine, i.e. rivers and lakes. The Devonian rocks of Arran belong to a sub-division of the Devonian called the Old Red Sandstone which itself can be sub-divided into the Lower Old Red sandstone and the Upper Old Red Sandstone.  Numerous geologists and sedimentologists have studied the ORS rocks  of Arran and the Midland Valley of Scotland and for more detail on further sub-divisions and contention in the classification of the sediments readers are referred to McKerrow & Atkins (1989) and references therein.

 

  • The Lower Old Red Sandstone of Arran outcrops in many places and is represented by conglomerates with rounded clasts of quartzite and vein quartz, red pebble rich grits and thin bedded sandstones and siltstones.  During the interval between the deposition of the Lower  Old Red Sandstone and the Upper Old Red Sandstone. The Lower Old Red Sandstone sediments were folded and underwent faulting due to major crustal movements, they were also denuded and eroded by the elements and in some locations completely removed. In Image 1 we can see an example of the Gavrock member of the Lower Old Red Sandstone, it is exposed in Glen Rosa, here it is green coloured as it has been altered. The iron in the coatings on the quartz grains has been reduced and has turned from red to green.

Image 1. Lower Old Red Sandston-Gavrock member, Glen Rosa

  • The Upper Old Red Sandstone is represented on Arran as red-cross bedded sandstones (Image 2) and siltstones and conglomerates hosting angular vein quartz and meta-sediment fragments, with some rounded quartzite fragments (Image 3). In some of the Upper Old Red Sandstone Units reduction spots can be seen (Image 4) and in-filled mud cracks can be also be noted.

Image 2. Cross-bedded ORS on Corrie Shore.

Image 3. An Upper Old Red Sandstone Conglomerate exposed on Corrie Shore.

Image 4. A mud cast in the centre of a reduction spot on the surface of an Upper  Old Red Sandstone Unit

exposed at Corrie Shore.

 

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This site was last updated Thursday, 12 October 2006