Contents of 11.5 How do geologic structures relate to stress, strain, and strength?

Fig 11.10

11.5 How do geologic structures relate to stress, strain, and strength?

cross section shows how sedimentary rocks will often slip along their bedding planes.

Fig 11.25

Folded sedimentary layers draped over a fault. Sedimentary rocks will often slip along their bedding planes before they fracture.