St Bees Sandstone
St Bees Sandstone was sourced from at least eighteen quarries near the towns of Annan and Kirkpatrick Fleming, in Dumfriesshire. The stone consisted originally of sand that was deposited by rivers during the early part of the Triassic Period (c. 250 million years ago), when Scotland was at roughly the same latitude as the centre of today's Sahara desert. A tiny proportion of iron, which is in an oxidised (‘rusted’) state, gives the stone a rich orange colour. St Bees Sandstone has been used locally, regionally, nationally and internationally, mainly to form masonry. Today, St Bees Sandstone is extracted for building stone at two quarries in Scotland and two quarries in England.
Geological description
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Source bedrock unit
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St Bees Sandstone Member (Chester Formation)
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Colour
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Brownish orange to orange
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Grain-size
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Fine sand (0.125 to 0.25 mm) to medium sand (0.25 to 0.5 mm)
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Cohesion
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Strongly cohesive
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Grain sorting
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Moderately well-sorted to well-sorted
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Water absorption
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Low to moderate
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Fabric
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Parallel lamination and uniform
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Distinctive features
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None
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