The famous Zig Zag folds in the cliffs at Millhook Haven.
Sandstone and shale beds of the Crackington Formation have been spectacularly deformed
into a vertical cascade of zigzag folds (anticlines and synclines), lying on their sides ,
as a result of the Variscan Orogeny (mountain-building) at the end of the Carboniferous Period.
Location - Millook Haven is to the South of Widemouth Bay in Gallery 7
Location: SS 1852.0020