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.
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.