Axial planar cleavage in sandstone. Note the syncline (left) and anticline (right) exposed
in the cliff in the background. Note also how the cleavage, exposed in the foreground, is parallel
to the axial surfaces of the folds. Devonian Old Red Sandstone, SW Wales, UK.
Return to Ductile Features
Return to Structural Geology
Return to Images
Return to Home Page