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.
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.
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.