Stanage Edge south end from Burbage Edge; x2 vertical exaggeration

The southern end of Stanage Edge viewed from Burbage Edge. All the rocks in the photo are formed from the Chatsworth Grit (Namurian). The foreground rocks at the northern end of the Burbage Valley are at a lower elevation because of a fault between there and Stanage Edge.

The x2 vertical exaggeration helps bring out the geological and geomorphological features.