Take a step back in time at Campsie Glen! Here you can stand on the site of an ancient lagoon, and climb your way up through a series of ancient lava flows – a remnant of the Campsie Hills volcanic past.
Take a step back in time at Campsie Glen! Here you can stand on the site of an ancient lagoon, and climb your way up through a series of ancient lava flows – a remnant of the Campsie Hills volcanic past.
An association of serpentenite, chert and pillow lavas that represents an ophiolite suite.
The relationships between the Dalradian block and the Midland Valley; details of the structure and stratigraphy of the Highland Border Complex; recumbent folding in Upper Dalradian rocks.
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.
Stratigraphy and sedimentation of the Lower and Upper Devonian; the angular unconformity which separates them.