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Cannongate Wall

Glen Tilt Marble

  • Metamorphic
  • Marble
  • Ordovician

This stone is older than it looks. Send it to someone five minutes away.

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Just found Glen Tilt Marble in Cannongate Wall.

Ordovician marble, quarried at Glen Tilt, Blair Atholl, Tayside, Scotland. Nearest stop: Edinburgh Waverley.

This stone is older than it looks — worth five minutes if you're nearby.
https://www.londonpavementgeology.co.uk/location/2541-cannongate-wall/

Location Details

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Location of Geological Feature
Cannongate wall showcases Scottish stones, inscribed with quotes from poetry etc. Only a few are included here. More information can be found in the guide listed below.
Rock Type
Marble
Geological Age
Ordovician
Quarry Location
Glen Tilt, Blair Atholl, Tayside, Scotland
Category
Metamorphic
Nearest station
Edinburgh Waverley
Address
The Royal Mile, Edinburgh EH8 8BR
Find out more
http://www.edinburghgeolsoc.org/downloads/lbgcleaflet_canongatewalla4.pdf
Cannongate Wall — Glen Tilt Marble
Glen Tilt Marble at Cannongate Wall
Glen Tilt Marble at Cannongate Wall (detail 2)
    Entry submitted by Ruth Siddall

More stone at Cannongate Wall

  • Easdale Slate
  • Ledmore Marble
  • Torridonian Sandstone

Nearby

The closest other recorded buildings.

  • Canongate WallCaldercruix Dolerite10 m · about 1 min walk
  • Scottish ParliamentKemnay Granite60 m · about 1 min walk
  • Queen's GalleryStainton Stone90 m · about 1 min walk
  • Rockstar Games NorthCaithness Flagstone180 m · about 3 min walk
  • New StreetCaithness Stone450 m · about 7 min walk
  • Hutton Memorial Garden PlaqueClashach Sandstone510 m · about 8 min walk

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Funding, sponsorship and supporting institutions

  • Marelambis Ltd.
  • University College London
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  • Geologists' Association Curry Fund
  • Geoscience Wales
  • The Geological Society
  • London Geodiversity Partnership

With donations from individuals in the oil and gas industry who wish to remain anonymous.

Building stone data by Ruth Siddall, Dave Wallis and contributors. Project founded by Dave Wallis.

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