Hopetoun Sandstone

Hopetoun Sandstone was sourced from quarries in Edinburgh, Lanarkshire and West Lothian. The stone consisted originally of sand that was deposited on river floodplains in a tropical environment during the early part of the Carboniferous Period (c. 333 million years ago), when Scotland was at roughly the same latitude as the Horn of Africa is today. Hopetoun Sandstone was used locally and regionally, mainly to form masonry. 'Binny Sandstone', which is brown due to tiny particles of hydrocarbon residue scattered within the stone, is a distinctive variant of Hopetoun Sandstone. Hopetoun Sandstone is not quarried for building stone today.

Building Stone ID 10,030

Geological description

Rock category  
Sedimentary rock
Stone type  
Sandstone
Source bedrock unit  
Hopetoun Member (West Lothian Oil-Shale Formation)
Colour  
Light brown and light grey
Grain sorting  
Well-sorted
Grain-size  
Fine sand (0.125 to 0.25 mm) to medium sand (0.25 to 0.5 mm)
Cohesion  
Strongly cohesive
Water absorption  
High to low
Fabric  
Uniform (some orientated grains) and occasional lamination
Distinctive features  
Evidence for hydrocarbons

Historic significance

Maximum historical geographic reach  
Regional (score = 2)
Extent of historic building stone quarrying  
Most extensive (score = 4)
Historic significance score  
Highly significant (score = 6)

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