(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.
Monoclines Although we will discuss folds and faults separately, in the real world folds are generally closely associated withfaults. Examples of this close association are broad, regional features called monoclines. Monoclines are large,step-like folds in otherwise horizontal sedimentary strata.trike-Slip Faults Faults in which the movement is horizontal and parallel to the trend, or strike, of the fault surface are calledstrike-slip faults, as shown in Figure 6D. Because of their large size and linear nature, many strike-slip faultsproduce a trace that is visible over a great distance.