Around the towns of Kilsyth and Cumbernauld lies an area rich in geology interest, natural and industrial heritage.
Around the towns of Kilsyth and Cumbernauld lies an area rich in geology interest, natural and industrial heritage.
Prominent basalt rock feature that can be visited via Strathkelvin Railway Path/John Muir Way.
History, nature and geology can be enjoyed at this site.
Explore the remains of a Carboniferous volcano at the Duncryne Hill, Gartocharn.
Sedimentary rocks from the Carboniferous period and evidence of the Quaternary glaciation.
A basalt plug which is the only remaining evidence of the volcano which existed on this site 330-340 million years ago.