Faults and fractures in upper Campanian aged Flamborough Chalk Formation
Well developed normal faults offset the chalk beds
Highly complex normal and reverse fault interaction resulting in variable bed dips and geometries
Normal fault with ca. 6 inches offset exposed as a 'scarp' in the bedding surface (foreground)
View of highly faulted chalk beds
Echinoid fossils are very common in the Chalk beds
Crinoids and sponges are also common