A large deeply-eroded volcanic vent of Lower Carboniferous age.
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Founded 1858
A large deeply-eroded volcanic vent of Lower Carboniferous age.
Succession of Carboniferous rock types and junctions of the Carboniferous with the Devonian and the Permian.
Dalradian schists, Hutton's classic unconformity and Permian sandstones and breccias.
Sedimentary and volcanic rocks of Lower Carboniferous age and evidence for the Campsie Fault.
Beautifully preserved fossil tree stumps and roots from the Carboniferous period in Glasgow’s Victoria park.