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Vertical aerial view.

SC 380358

Description Vertical aerial view.

Collection Scottish Development Department: Commissioned Aerial Imagery

Catalogue Number SC 380358

Category On-line Digital Images

Scope and Content Geology, Holyrood Park, City of Edinburgh The origins of Holyrood Park lie in a massive volcano that erupted through a group of low-lying islands about 350 million years ago, a time when Edinburgh lay near to the Tropics. Remains of the original sandstones lie on the backslope of Salisbury Crags. The volcano stretched up well above the present summit of Arthur's Seat. Subsequent erosion has removed much of the rock, but remains of the original cone may be seen on Whinny Hill. Later volcanic action led to the formation of Salisbury Crags. Since then the whole mass has been tilted to the east by earth movements, and more recently ice action has played its part. The movement of the glaciers eroded out the steep west-facing crags and laid down sediments to the east. Source: RCAHMS contribution to SCRAN.

External Reference Clyde 8218, 1.498

Permalink http://canmore.org.uk/collection/380358

File Format (TIF) Tagged Image File Format bitmap

Collection Hierarchy - Item Level

People and Organisations

Events

Attribution & Licence Summary

Attribution: © RCAHMS

You may: copy, display, store and make derivative works [eg documents] solely for licensed personal use at home or solely for licensed educational institution use by staff and students on a secure intranet.

Under these conditions: Display Attribution, No Commercial Use or Sale, No Public Distribution [eg by hand, email, web]

Full Terms & Conditions and Licence details

MyCanmore Text Contributions