A basalt plug which is the only remaining evidence of the volcano which existed on this site 330-340 million years ago.
A basalt plug which is the only remaining evidence of the volcano which existed on this site 330-340 million years ago.
A geological information board describing the geology and landscape evolution of the Campsie Fells.
Many different types of rock have been used in the construction of Glasgow's buildings. A booklet describing a geological trail around the buildings of Central Glasgow is available to download.
Geological information boards describing the geology and landscape evolution of the Campsie Fells.
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.
A walk around the building stones of Glasgow University. The guide contains colour photos and an easy to follow map of the campus.
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.
Sedimentary and volcanic rocks of Lower Carboniferous age and evidence for the Campsie Fault.