Fig 11.22
11.5 How do geologic structures relate to stress, strain, and strength?
Deformation by tension results in a lengthening of the landscape such as in the Basin and Range.
Horsts - blocks of crust jostled upwards along normal faults
Grabens - blocks of crust jostled downward along normal faults
We find common shear features along the California coast and compression in the eastern regions.
