Dundee Flagstone

Dundee Flagstone was sourced from numerous quarries in Angus, Dundee, Kincardineshire and Perthshire. The stone consisted originally of fine sand and mud that was deposited by rivers during the early part of the Devonian Period (c. 405 million years ago), when Scotland was south of the Equator at roughly the same latitude as southern Angola is today. The stone typically breaks preferentially along parallel bedding planes, forming tabular blocks ('flags') of hard, durable stone. This building stone includes the well-known 'Carmyllie Flagstone'. Dundee Flagstone was used locally and regionally for paving, roofing, masonry and millstones, and it was used nationally and internationally for paving. Today, Dundee Flagstone is extracted for building stone at one quarry.

Building Stone ID 10,081

Geological description

Rock category  
Sedimentary rock
Stone type  
Sandstone,Siltstone
Source bedrock unit  
Dundee Flagstone Formation
Colour  
Medium grey to purplish brown
Grain sorting  
Well-sorted to moderately well-sorted
Grain-size  
Fine sand (0.125 to 0.25 mm) to very fine sand (0.032 to 0.125 mm)
Cohesion  
Strongly cohesive
Water absorption  
Low to very low
Fabric  
Parallel lamination to occasional lamination
Distinctive features  
None

Historic significance

Maximum historical geographic reach  
International (score = 4)
Extent of historic building stone quarrying  
Most extensive (score = 4)
Historic significance score  
Most significant (score = 8)

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