Explore the remains of a Carboniferous volcano at the Duncryne Hill, Gartocharn.
Explore the remains of a Carboniferous volcano at the Duncryne Hill, Gartocharn.
Sedimentary rocks from the Carboniferous period and evidence of the Quaternary glaciation.
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 from the website.
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 from the website.
Geological information boards describing the geology and landscape evolution of the Campsie Fells.