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grahamcheckley | profile | all galleries >> Scottish Wildlife - Arthur's Seat (Holyrood Park) >> Arthur's Seat - Geology tree view | thumbnails | slideshow

Arthur's Seat - Geology

350 million years ago the place that is now Edinburgh lay near the equator, and was a landscape of rivers with, perhaps, an adjoining tropical sea. While life was present on land there were no flowering plants and the highest forms of vertebrate life on land were early lizards, the latter now identified in the fossil record as Westlothiana lizziae. See http://www.answers.com/topic/westlothiana.

The eruption of Edinburgh’s volcano changed that peaceful scene, and this gallery will be an attempt to tell part of that story in pictures.
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Camstayne Sandstone
Camstayne Sandstone
Mud crack Cast
Mud crack Cast
Arthur's Seat
Arthur's Seat
Arthurs Seat and Whinny Hill
Arthurs Seat and Whinny Hill
Whinny Hill (Volcanic Cone)
Whinny Hill (Volcanic Cone)
Whinny Hill and Lang Rig
Whinny Hill and Lang Rig
Lava Blocks from Lang Rig
Lava Blocks from Lang Rig
Tuff (compacted volcanic ash)
Tuff (compacted volcanic ash)
Fossilised Roots
Fossilised Roots
Crater traces
Crater traces
Crater Traces
Crater Traces
Dasses intrusion
Dasses intrusion
Dases intrusion Feldspar crystals
Dases intrusion Feldspar crystals
Dasses intrusion
Dasses intrusion
Arthur's Seat intrusion
Arthur's Seat intrusion
Salisbury Crags and the Radical Road
Salisbury Crags and the Radical Road
Margin in Long Quarry
Margin in Long Quarry
Sediments in Long Quarry
Sediments in Long Quarry
Sandstones plus Intrusion
Sandstones plus Intrusion
Sedimentary Raft (Xenolith)
Sedimentary Raft (Xenolith)
Breccia at Cat Nick
Breccia at Cat Nick
Bedded Ash
Bedded Ash
Onion weathering
Onion weathering
Samsons Ribs
Samsons Ribs
Pulpit Rock
Pulpit Rock
Camstayne sedimentary rock
Camstayne sedimentary rock
Hutton's Section
Hutton's Section
Hutton's Section
Hutton's Section
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