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Sandstone Quarry Corncockle

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The late permian to triassic sediments of the solway basin consist of a layer-cake succession of mature, predominantly fine-grained red clastics laid down in semi-arid alluvial plain to arid sabkha and saline marginal marine or lacustrine environments.The cumbrian coastal group consists of basal clastics and eden shales.The basal clastics are thin regolith deposits resting unconformably on.


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