(From Tempur-Pedic's Website) Tempur-Pedic mattresses have been designed to be paired with a Tempur-Pedic foundation. However, we understand that some consumers wish to use their existing platform style bed with slats (as opposed to a flat surface) with our mattress.
The type of motion along a fault depends on the type of fault. The main types of faults are described below. 1  Normal dip-slip fault. 2  Normal faults happen in areas where the rocks are pulling apart (tensile forces) so that the rocky crust of an area is able to take up more space. 3  The rock on one side of the fault is moved down relative to the rock on the other side of the fault.
Figure 10l-12: Animation of a horst fault. The final major type of fault is the strike-slip or transform fault. These faults are vertical in nature and are produced where the stresses are exerted parallel to each other (Figure 10l-13). A well-known example of this type of fault is the San Andreas fault in California.